Three-dimensional electron diffraction on clinkers: the belite α′H incommensurate modulated structure

Plana-Ruiz, S.; Götz, E.; Neumann, T.; Schwesig, P.; Kolb, U.

doi:10.1107/S205252062400146X

research papers

STRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS

ISSN: 2052-5206

Volume 80| Part 2| April 2024| Pages 105-116

https://doi.org/10.1107/S205252062400146X

Open

access

Three-dimensional electron diffraction on clinkers: the belite α′_H incommensurate modulated structure

Sergi Plana-Ruiz,^a,^b ^* Emilia Götz,^b Thomas Neumann,^c Peter Schwesig ^d and Ute Kolb ^b,^e ^*

^aServei de Recursos Científics i Tècnics, Universitat Rovira i Virgili, Avinguda Països Catalans 26, Tarragona, Catalonia 43007, Spain, ^bInstitut für Angewandte Geowissenschaften, Technische Universität Darmstadt, Petersenstrasse 23, Darmstadt, Hessen 64287, Germany, ^cSchwenk Zement GmbH & Co. Kg, Laudenbacher Weg 5, Karlstadt, Bavaria 97753, Germany, ^dMaster Builders Solutions Deutschland GmbH, Dr.-Albert-Frank-Strasse 32, Trostberg, Bavaria 83308, Germany, and ^eInstitut für Anorganische Chemie und Analytische Chemie, Johannes Gutenberg University of Mainz, Duesbergweg 10-14, Mainz, Rheinland-Pfalz 55128, Germany
^*Correspondence e-mail: sergi.plana@urv.cat, kolb@uni-mainz.de

Edited by J. Hadermann, University of Antwerp, Belgium (Received 8 January 2024; accepted 13 February 2024; online 6 March 2024)

Traditional X-ray methods are extensively applied to commercial cement samples in order to determine their physical and chemical properties. Powder patterns are routinely used to quantify the composition of these phase mixtures, but structure determination becomes difficult because of reflection overlapping caused by the high number of different crystal structures. The fast-growing 3D electron diffraction technique and its related automated acquisition protocols arise as a potentially very interesting tool for the cement industry, since they enable the fast and systematic acquisition of diffraction data from individual particles. In this context, electron diffraction has been used in the investigation of the different crystalline phases present in various commercial clinkers for cement. Automated data collection procedures and subsequent data processing have enabled the structural characterization of the different crystal structures from which the α′_H polymorph of Ca₂SiO₄ (belite) exhibited satellite reflections. Its average crystal structure has been known since 1971 and satellite reflections have been reported previously, yet the modulation was never fully described by means of the superspace formalism. Here, the incommensurately modulated structure is solved and refined using harmonic and crenel functions in the superspace group Pnma(α00)0ss, showing the potential of 3D electron diffraction for systematic crystallographic characterizations of cement. A full description of the different belite polymorphs is provided considering this modulated structure.

Keywords: three-dimensional electron diffraction; 3D ED; electron microscopy; modulated structures; cement.

B-IncStrDB reference: 7bhGderGvHs

CCDC references: 2332749; 2338192; 2338193; 2338194

1. Introduction

Cement is a key material in our society as it is a strong building material that can withstand long periods of time. This results in cement being the largest manufactured product by mass on Earth. Combined with water and mineral aggregates it forms concrete, the second most used substance in the world due to its simple production from widely available materials, its easiness to place it and adjust it to complex geometries, and its high strength and density (Scrivener et al., 2018 ). Nevertheless, one of the major concerns is the emission of CO₂, which is mainly driven by decarbonatization (around 40% of produced CO₂ comes from de-calcination of limestone). Its production dependence on the burning of fossil fuels contributes up to 8% of global anthropogenic carbon dioxide emissions, thus its proper characterization to foresee alternative components is needed to reduce its impact (Mahasenan et al., 2003 ; Olivier et al., 2016 ).

The main component of cement is clinker, an aggregate of different crystallographic phases. Alite (Ca₃SiO₅; 50–70%), belite (Ca₂SiO₄; 15–30%), aluminate (Ca₃Al₂O₆; 5–10%) and ferrite (Ca₂AlFeO₅; 5–15%) are its main constituents and the different phase ratios determine the strength development of the resulting cement. Several other chemical components like alkali sulfates or calcium oxides are also present in much lower amounts (Taylor, 1997 ). Fig. 1 shows scanning electron microscopy (SEM) images and chemical maps of a typical clinker sample. Its microstructure can be described as large alite and small belite grains crystallized in different polymorphs inside a matrix of ferrites and aluminates, which in turn crystallize in the brownmillerite phase with varying Al/Fe ratios (Kim et al., 1992 ; Richardson et al., 1993 ; Redhammer et al., 2004 ; Dunstetter et al., 2006 ).

Figure 1
SEM images and chemical mapping of a typical clinker sample. Silicon and calcium energy-dispersive X-ray spectroscopy maps allow the identification of alite (Ca₃SiO₅) as the large grains and belite (Ca₂SiO₄) as the small ones, since the Si and Ca signals are lower and higher, respectively, for alite.

Alite and belite constituents can crystallize in different phases with closely related cell parameters and space groups. Almost all these crystal structures were determined from X-ray diffraction methods, but single-crystal studies had to be done with crystalline domains grown under laboratory conditions since powder investigations on commercial clinkers or cement samples resulted in diffractograms with severe overlapping of reflections. Although this procedure provides an accurate way of properly characterizing these structures, it may hinder other crystallographic effects produced in the manufacturing process. On the other hand, powder X-ray diffraction (PXRD) gives very precise phase quantifications of the different crystal phases inside the mixture, but it requires the input of all the structures that are thought to be inside to run the Rietveld method (De la Torre & Aranda, 2003 ). In this context, transmission electron microscopy (TEM) appears as an alternative and complementary characterization tool that can give very useful insights.

TEM has been used to visualize morphology, twinning and crystalline structures since the initial studies on cement (Remy et al., 1995 ). Electron diffraction was frequently used to identify superstructure reflections and suggest different hypothetical structures that were subsequently fitted in PXRD or single-crystal X-ray diffraction (SCXRD) patterns (Jelenić & Bezjak, 1982 ; Thompson et al., 1987 ; Fukuda & Maki, 1989 ). However, electron diffraction analyses were restricted to pure geometric descriptions and its potential for further crystallographic investigations was untapped due to the lack of necessary tools.

In this work, the use of three-dimensional electron diffraction (3D ED) (Kolb et al., 2007 , 2008 ; Gemmi et al., 2019 ) with an automated data acquisition approach is presented as a new and reliable way of studying the different crystalline phases of clinkers. Such a methodology allows the accurate identification of crystallographic features from individual crystals inside phase mixtures that may be difficult to observe and properly analyse in PXRD, thus increasing the reliability of the available models used later in the quantification of powder patterns. In particular, this work has focused on the investigation of the belite polymorphs present in different commercial clinkers.

2. Materials and methods

2.1. The different polymorphs of belite

Belite is one of the major constituents of clinker, thus the structural characterization of its different polymorphs is key to foresee and understand the performance of the resulting cement. Fig. 2 shows a scheme of the different crystal structures that belite (C₂S) transitions to according to the temperature.

Figure 2
A schematic presentation of the belite (C₂S) phase transitions between the different polymorphs with respect to temperature (Kim et al., 1992

; Taylor, 1997

The only phase that is thermodynamically stable at room temperature is the orthorhombic γ-C₂S (Fukuda & Maki, 1989). All other polymorphs require the addition of dopants that partially substitute the silicon by phosphorus and/or the calcium by potassium or strontium, as well as the precipitation of minor oxides that induce strain in the crystal structure (Morsli et al., 2007 ). In the case of the clinker manufacturing process, belite grains contain these different crystal phases and the interest is in preserving the high-temperature polymorphs because of their higher reactivity at room temperature. Table 1 summarizes the crystallographic information on C₂S polymorphs according to the literature.

Table 1
Crystal structure information for the different polymorphs of C₂S obtained by SCXRD or PXRD

The adjusted setting is provided for further clarity of the crystal structure description of the polymorph phase transitions (Section 3.2.4).

		Standard setting		Adjusted setting
Polymorph	Crystal system	Lattice parameters	Space group	Lattice parameters	Space group
γ	Orthorhombic	a = 11.214 Å	Pnma^(a)	a = 5.081 Å	Pcmn^{(b), (c)}
		b = 6.758 Å		b = 6.778 Å
		c = 5.076 Å^(a)		c = 11.244 Å^(b)
β	Monoclinic	a = 5.502 Å	P12₁/n1^(d)	a = 5.502 Å	P12₁/n1^{(d), (e)}
		b = 6.745 Å		b = 6.745 Å
		c = 9.297 Å		c = 9.297 Å
		β = 94.59°^(d)		β = 94.59°^(d)
$[\alpha_L^{\prime}]$ (2a, b, 2c)†	Orthorhombic	a = 11.184 Å	Pbcn^(f)	a = 11.184 Å	Pcnb^(f)Pmnb or Pmnn^(g)
		b = 18.952 Å		b = 6.837 Å
		c = 6.837 Å^(f)		c = 18.952 Å^(f)
$[\alpha_L^{\prime}]$ (a, 3b, c)†	Orthorhombic	a = 9.500 Å	Pna2₁^(h)	a = 5.601 Å	P2₁nb^(h)Pmnb⁽ⁱ⁾
		b = 5.601 Å		b = 20.863 Å
		c = 20.863 Å^(h)		c = 9.500 Å^(h)
$[\alpha_H^{\prime}]$	Orthorhombic	a = 6.767 Å	Pnma^(a)	a = 5.519 Å	Pmnb^{(a), (f), (i)}
		b = 5.519 Å		b = 6.767 Å
		c = 9.303 Å^(a)		c = 9.303 Å^(a)
α	Hexagonal / triclinic	a = 5.579 Å	P6₃/mmc^(b)	a = 5.579 Å	P6₃/mmc^(b) $[P {\overline 3} m1]$ ^(j)
α	Hexagonal / triclinic	c = 7.150 Å^(b)	P6₃/mmc^(b)	c = 7.150 Å^(b)	P6₃/mmc^(b) $[P {\overline 3} m1]$ ^(j)
References: (a) Mumme et al. (1995), (b) Udagawa et al. (1980), (c) Smith et al. (1965 ), (d) Jost et al. (1977), (e) Midgley (1952 ), (f) Regourd et al. (1968), (g) Sarkar (1980 ), (h) Il'inets & Bikbau (1990), (i) Saalfeld (1975) and (j) Bredig (1950 ).

†The notation in parentheses refers to the extension of the respective unit cell with respect to the unit-cell parameters of $[\alpha_H^{\prime}]$ (of the adjusted setting) required to obtain the superstructure.

The γ polymorph is an orthorhombic crystal that resembles the olivine-type structure and contains two independent calcium cations surrounded by six oxygen environments (Udagawa et al., 1980 ). When the temperature is increased, different superstructures are obtained that are generally referred to as $[\alpha_L^{\prime}]$ (Regourd et al., 1968 ; Il'inets & Bikbau, 1990 ). These can be understood as intermediate phases between γ and $[\alpha_H^{\prime}]$ since their superstructure can be derived from the basic unit cell of $[\alpha_H^{\prime}]$ , where oxygen and calcium have split positions and the calcium cations are surrounded by eight or ten oxygen environments (Mumme et al., 1995 ). The α polymorph crystallizes in the hexagonal or trigonal crystal system and, in this case, six and seven oxygen-coordinated environments for the calcium cations are observed (Udagawa et al., 1980). When the temperature is decreased from 700°C or higher to around 600°C, the monoclinic phase is formed with calcium coordinated by six or eight oxygen anions. If the temperature is then decreased further down to room temperature, the γ form is retrieved once again. If enough dopants are added or the belite crystals are sufficiently small, the β polymorph is stabilized and it is prevented from reducing to γ. Since the γ crystal phase is less dense, the clinker production process tries to minimize this transformation because it would produce a more voluminous powder on cooling that results in less strength, an effect called dusting (Taylor, 1997).

The α, $[\alpha_L^{\prime}]$ , $[\alpha_H^{\prime}]$ and β phases are classified as glaserite-type structures and they can be subsequently described by the movement of calcium cations and changes in the silicon tetrahedra orientations. The lower the temperature, the lower the symmetry of the related crystalline phase. The nature of the transition between $[\alpha_L^{\prime}]$ and $[\alpha_H^{\prime}]$ also leads to the observation of modulated features in the form of extra reflections in zone-axis electron diffraction patterns (Saalfeld, 1975 ; Jelenić & Bezjak, 1982; Fukuda & Maki, 1989). Although these features have been explained using supercells and chemically and crystallographically meaningful descriptions for more than half a century, crystal structure refinements including incommensurate modulations are yet to be explored to comprehend fully the solid-state nature of the compound.

2.2. Sample preparation

Three different clinker samples were obtained from the Schwenk Zement KG plant in Bernburg, Germany. They were differentiated by the amount of sewage that was ejected from the burner pipe inside the rotary kiln, namely 0, 2.5 or 5 tonnes per hour, referred in this work as clinker_0, clinker_2.5 and clinker_5, respectively. In all cases, the final amount of sewage used during their production was the same, since the amount that was not shot from the pipe was introduced in the input mixture of the kiln. The ground clinkers were then chemically treated by BASF Construction Solutions GmbH to dissolve the aluminates and ferrites (hydroxide/sugar extraction) in order to easily identify the calcium silicate phases. The resulting powders were dispersed in ethanol and sprayed on TEM carbon-coated copper grids with a UIS250v Hielscher sonifier. The Cu grids were cleaned with argon plasma for one minute before and after the powder was sprayed onto them to eliminate remaining organic compounds and minimize carbon contamination during the TEM measurements.

2.3. Data acquisition

The prepared copper grid samples were loaded on an FEI single-tilt holder or a Fischione tomography holder and inserted in an FEI Tecnai F30 field-emission gun operated at 300 kV. The microscope was aligned in scanning transmission electron microscope (STEM) mode with Microprobe illumination. The same data acquisition procedure was carried out for all samples: initial energy-dispersive X-ray spectroscopy (EDS) measurements to identify particles with calcium and silicon, followed by a 3D ED acquisition by means of the Fast-ADT routine, an acquisition method developed for the systematic and routine collection of 3D ED data (Plana-Ruiz et al., 2020 ). Spot size 6, gun lens 1 and a 50 µm condenser aperture were used to acquire the EDS spectra with an EDAX EDAM III detector. Spot size 6, gun lens 8 and a 10 µm condenser aperture were selected to set a quasi-parallel beam between 150 and 200 nm in diameter to check the particle crystallinity and acquire the diffraction data. STEM images were acquired with a Fischione high-angle annular dark-field (HAADF) detector mounted on the side port of the TEM column and diffraction patterns were collected with a Gatan US4000 with binning 2 and different exposure times. Five crystals were investigated in clinker_0, six in clinker_2.5 and three in clinker_5, from which 3D ED data sets with and without 1° of precession angle were acquired for each particle. Electron beam precession was applied with the DigiStar unit provided by NanoMegas SPRL. Its alignment in STEM mode is described elsewhere (Barnard et al., 2017 ; Plana-Ruiz et al., 2018 ).

2.4. Data processing

EDS data were processed with the ES Vision software (Emispec Systems Inc.) to calculate the atom percentage weight of the different crystals. The 3D ED data were reconstructed with the eADT program to explore the observable diffraction space, and to determine the unit cells and initial extraction of reflection intensities (Kolb et al., 2019 ). Ab initio structure determinations were carried out with SIR2014 from the hkl files generated by eADT (Cascarano et al., 2010 ; Burla et al., 2015 ). PETS2 was used to extract the intensity of reflections from precessed electron diffraction data sets by means of the fitting of a double-peaked curve function (Palatinus et al., 2019 ) for further refinements. Kinematical and dynamical refinements were performed with JANA2006 with these hkl files (Petříček et al., 2014 ; Palatinus, Petříček & Corrêa, 2015 ; Palatinus, Corrêa et al., 2015 ). Ab initio structure solutions for the modulated structure were obtained from the SUPERFLIP program integrated in JANA2006 (Palatinus & Chapuis, 2007 ). Visualizations of the crystal structure models were created using VESTA 3 (Momma & Izumi, 2011 ).

3. Results and discussion

3.1. Identification of belite polymorphs

EDS spectra allowed a direct identification of the calcium silicate phases, and the quantification of the Ca/Si ratio was accurate enough to distinguish between alite and belite crystal phases (Ca/Si ≃ 3 for alite and Ca/Si ≃ 2 for belite). In this way, 3D ED data sets from suspected belite crystals were analysed for polymorph identification. Table S1 in the supporting information provides the acquisition and output parameters of successful ab initio structure solutions by direct methods. Three, one and two β-C₂S single crystals were identified in clinker_0, clinker_2.5 and clinker_5, respectively, and one $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ single crystal was found in each sample. The unit cells of these nine crystals were determined from the data sets collected without precession (Table 2). Unit-cell parameters in 3D ED tend to be inaccurate and a scale correction to their absolute values has been applied. The scale factor was obtained by calculating the average ratio between the unit-cell parameters of the best quality β-C₂S data set and the values reported by Jost et al. (1977 ). The β polymorph was used for this scaling as its crystal structure is better understood than the $[\alpha_H^{\prime}]$ phase. One scale factor was retrieved and applied for each clinker sample.

Table 2
Determined unit-cell parameters from all measured belite crystals in the different clinker samples and the already reported values

No. (polymorph)	a (Å)	b (Å)	c (Å)	α (°)	β (°)	γ (°)
clinker_0
1 (β)	5.537	6.717	9.278	90.4	94.3	90.3
2 (β)	5.525	6.750	9.274	89.6	94.1	90.3
3 (β)†	5.497	6.780	9.246	90.3	94.3	90.0
4 ( $[\alpha_H^{\prime}]$ )	5.496	6.776	9.252	89.9	89.9	89.5
clinker_2.5
1 (β)†	5.544	6.690	9.306	90.0	94.2	89.5
2 ( $[\alpha_H^{\prime}]$ )	5.514	6.765	9.250	90.5	89.5	89.8
clinker_5
1 (β)†	5.538	6.783	9.279	89.9	94.6	90.8
2 (β)	5.478	6.751	9.334	89.6	94.2	90.2
3 ( $[\alpha_H^{\prime}]$ )	5.444	6.775	9.348	90.4	90.3	89.8
Literature
β (Jost et al., 1977)	5.502	6.745	9.297	90.0	94.59	90.0
$[\alpha_H^{\prime}]$ (Mumme et al., 1995)	5.519	6.767	9.303	90.0	90.0	90.0

†Twinned crystal from which one of the unit cells is provided.

The reconstruction of the observable diffraction space on the β-C₂S data sets revealed that all measured specimens contained at least one crystal with a typical non-merohedral twin along the [100] direction of the monoclinic cell. Fig. 3 shows a STEM-HAADF image of one of the measured twinned crystals and the projection along the b* axis of one reconstruction. The diffraction contrast in the STEM image enables the direct visualization of the twin boundaries, and two monoclinic unit cells with the same unit-cell parameters but differently oriented are needed to index all reflections.

Figure 3
(a) A STEM-HAADF image of a twinned β-C₂S crystal. The red circle marks the region illuminated by the electron beam for the acquisition of the diffraction data set. (b) A projection of the reconstructed space along the b* axis acquired from the twinned β-C₂S crystal. The red and blue overlapping rhomboids represent the projected monoclinic unit cells for the two differently oriented cells, and the dashed lines are displayed for clarity to show which reflections belong to the different twins.

Reflection intensity integration and extraction of the β-C₂S data sets was carried out with eADT. In the case of twinned crystals, two separate hkl files were obtained for each unit cell. The observation of the reflection condition h + l = 2n in the h0l reconstructed section pointed to the already reported P12₁/n1 space group. Structure solution via direct methods and a kinematical refinement performed with SIR2014 provided in all cases the crystal structure in the literature (Jost et al., 1977). Interestingly, since the twinned crystal data sets have low reflection overlap, which is mainly seen at low diffraction data resolutions, both hkl files in the three cases result in successful structure determination without significant structural differences between them.

In the case of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ data sets, the reconstructions revealed extra reflections that do not fit the reported $[\alpha_L^{\prime}]$ superstructure or $[\alpha_H^{\prime}]$ structure. These extra reflections are located along the b* axis of the Pmnb setting at ±0.3725, ±0.3795 and ±0.3563 of $[{\bf b}^*]$ for clinker_0, clinker_2.5 and clinker_5, respectively. The values tend to approach an irrational number, thus large supercells would be required in order to have lattices that fit all observed reflections well, yet the number of structural parameters would be too large and the description would not be accurate. Such features were initially reported by Jelenić & Bezjak (1982), who identified extra reflections at ∼3/8 and ∼5/8 from the main ones. However, no further structural investigations were undertaken. If these reflections are momentarily ignored, the systematic absences in the h0l and hk0 reconstructed sections confirm the Pmnb space group, and the retrieved structure solutions via direct methods correspond to the crystal structure reported by Mumme et al. (1995). Nevertheless, the satellite reflections are not weak, as is shown in Fig. 4, and they cannot be ignored for a proper crystal structure determination. For this reason, the procedure to determine the crystalline phase must include the significant incommensurate characteristic of the acquired diffraction patterns.

Figure 4
(a) A precessed diffraction pattern along [ $[10 {\overline 2}]$ ] from one of the $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ crystals that shows strong extra reflections, and (b) an intensity histogram of ( $[{\overline 2} h {\overline 1}]$ ) that corresponds to the blue region marked in panel (a).

3.2. Crystal structure of belite $[\alpha_H^{\prime}]$

Satellite reflections were identified in the diffraction data sets of the $[\alpha_H^{\prime}]$ polymorph for each clinker sample. However, the clinker_5 data exhibit textured reflections as well as strong background intensity, decreasing the quality of the reflection intensities. For this reason, this data set has been excluded from the following crystallographic analysis.

The Pmnb setting was used in previous sections to enable easy visualization of the phase transitions between the glaserite-type structures of belite. Here the orientation matrix of the standard Pnma setting is chosen, and the modulation wavevectors become 0.3725a* and 0.3795a* for the clinker_0 and clinker_2.5 data sets, respectively.

3.2.1. Average structure model

First, the structure analysis of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ is carried out by ignoring the satellite reflections. The 0kl, h0l and hk0 sections displayed in Fig. 5 show the reflection conditions related to the extinction symbol Pn-a, i.e. the n-glide plane perpendicular to the a axis that produces the k + l = 2n condition in the 0kl section, and the a-glide plane perpendicular to the c axis related to the h = 2n condition in the hk0 section. The resulting extinction symbol points toward the Pn2₁a and Pnma space groups as possible candidates.

Figure 5
0kl, h0l and hk0 sections of the reconstructed space from clinker_0 (upper figures) and clinker_2.5 (lower figures). The red rectangles correspond to the projected unit cells along the different directions of the sections. The blue circles and dashed lines mark the positions of the systematic extinctions according to the Pn-a extinction symbol.

The reported crystal structures of $[\alpha_H^{\prime}]$ are always in the Pnma space group (Regourd et al., 1968; Saalfeld, 1975; Mumme et al., 1995). These models place the calcium and two oxygen positions on the mirror plane or slightly shifted from it and half occupied to compensate for the creation of the symmetrically related atom on the other side of the plane. For this reason, a structure solution with the Pn2₁a space group is a reasonable assumption because it allows these atoms to sit at any specific position along the b axis without the limitation of the mirror symmetry. In this way, structure solutions were obtained from direct methods and the retrieved models were refined by three cycles of the least-squares refinement routine in SIR2014.

The resulting models from direct methods provided less distorted silicon tetrahedra for the Pnma solutions than the Pn2₁a ones. While the silicon to oxygen distances are ranged between 1.54 and 1.61 Å in the Pnma structure, the range is increased up to 1.42–1.87 Å for the Pn2₁a case. Kinematical refinements were carried out in JANA2006 to check whether the distortions observed in the Pn2₁a model are minimized by the least-squares procedure, but the geometrical distortions in the tetrahedra were greatly increased so these structure models were disregarded from further crystal refinement. On the other hand, the structure models with the Pnma space group provided good tetrahedral geometry and the Si—O distances ranged between 1.57 and 1.69 Å. The difference Fourier maps in the first refinement executions showed extra potentials around the oxygen positions placed on the mirror plane (4c Wyckoff position), so they were moved out of the symmetry-limited position and the occupancy factor was set to 0.5. Extra spherical potential was also observed close to the oxygen atom on the 8d Wyckoff site in both data sets that indicated their splitting. In this case, an extra oxygen atom was added and the occupancy factors were set to 0.5 for each atom of the pair. During the refinement, the atomic displacement parameters (ADPs) were restricted to be the same for both oxygen atoms and their total occupancy was restricted to 1. The occupancy and ADP of a single atom was then refined. Table 3 shows the figures of merit for these kinematical refinements in which the ADPs turned out positive and low, and the least-squares procedure converged.

Table 3
Resulting figures of merit from the structure refinements of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ in space group Pnma from JANA2006

The number of reflections, goodness of fit (GoF), R and R_w parameters are calculated and reported from observed and all (obs/all) reflections. The criterion for observed reflections was I(g) > 3σ(g). The `Refl./Param.' measure refers to the number of observed reflections over the number of refined parameters. R₁ and R_w are based on the square root of reflection intensities. Dynamical refinements were carried out with N_or of 128, g_max of 1.6 Å⁻¹, $[S_{g}^{\max}({\rm matrix})]$ of 0.01 Å⁻¹, $[S_{g}^{\max}({\rm refine})]$ of 0.1 Å⁻¹ and RS_g of 0.4

	clinker_0		clinker_2.5
	Kinematical	Dynamical	Kinematical	Dynamical
Completeness (%)	72.9		85.3
R_int	0.135		0.116
No. of reflections at 0.7 Å	415/436	1710/2440	451/498	1489/1996
Refl./Param.	16.0	12.5	17.3	10.4
GoF	15.1/14.7	2.03/1.77	13.6/12.9	2.37/2.09
R	0.205/0.208	0.0557/0.0787	0.191/0.200	0.0550/0.0708
R_w	0.251/0.251	0.0562/0.0585	0.226/0.226	0.0607/0.0623

The structure models obtained from the kinematical refinements were then used for dynamical refinements to refine the anisotropic ADPs and obtain a more accurate description of the crystal. The obtained R₁(obs) values of 0.0557 and 0.0550 for the clinker_0 and clinker_2.5 data sets, respectively, demonstrate the reliability of the retrieved structure model.

The refinement of the $[\alpha_H^{\prime}]$ model from the clinker_0 sample results in positive principal components of the anisotropic ADP tensors and the equivalent isotropic ADPs (B_iso) range between 1.2 and 2.4 Å², indicating a reliable positioning of the atoms. The visualization of atom volumes scaled according to the anisotropic ADPs in Fig. 6 shows that split oxygen atoms near the mirror planes (placed at y = 0.25 and y = 0.75) have a displacement along the b axis, and the remaining pair of split oxygen atoms tend to move to each other while the oxygen to silicon distance is maintained. Calcium atoms also display a movement parallel to the b axis, although less severe, and silicon atoms do not exhibit such significant anisotropic displacement. Interestingly, atom O1 has a higher occupation factor than its split pair, O1_2, which points towards a preferred positioning across the cells.

Figure 6
Averaged structure models of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ after dynamical refinements from (a) the clinker_0 and (b) the clinker_2.5 data sets. Purple atoms correspond to calcium, orange ones to silicon and red ones to oxygen. Atom volumes are scaled according to the principal components of the anisotropic ADPs.

The dynamical refined model taken from clinker_2.5 also results in positive principal ADP components, but atom O3 exhibits a significantly higher component along the b axis (Fig. 6). The small distance between these split oxygen atoms in comparison to the crystal structure of clinker_0 indicates that the ADPs and the pair distance along the y component are correlated, yet the least-squares procedure estimates these values to minimize the R₁ value. Furthermore, the data set does not cover either the b or c axes (Fig. 5) and, consequently, the resulting electrostatic potential is spread along these directions. Therefore, the high ADP could be explained as an effect of the symmetry-constrained position, missing diffraction space information and the use of an average structure to describe the modulation. In the case of atom O2, the pair distance is higher and the resulting ADP through the b-axis direction is not that strong. The left oxygen pair and the calcium positions show the same behaviour as the model from clinker_0, but silicon has a slightly higher displacement along the b axis. The higher occupation factor for atom O1 than for O1_2 also suggests the preferred positioning of this oxygen atom seen in the structure from clinker_0.

The very similar refined crystal structures determined from these two different diffraction data sets illustrate that the structure model is reliable, and it can be used to analyse clinker mixtures manufactured under different conditions. Nonetheless, the significant anisotropic behaviour of the found ADPs indicates that a strong structural modulation is present in the crystalline material, which at the same time is observed in the strong satellite reflections. Therefore, the shown models can only be considered as the average structure and the incommensurate characteristic of the diffraction data needs to be taken into account for a proper crystal structure description.

3.2.2. Characterization and refinement of the modulated structure

The hk0 sections in Figs. 5(c) and 5(f), as well as the projections of the reconstructed observable diffraction space in Fig. S1, show that the satellite reflections cannot be ignored because of their strong intensity, thus the superspace formalism needs to be used for a correct crystal structure characterization.

The indexing of all reflections in the reconstructed space requires the expansion of the 3D space to a (3+d)D superspace. In the presented case, a (3+1)D superspace is required since there is only one modulation wavevector along the a* axis, $[{\bf q}]$ = 0.3725a* for clinker_0 and $[{\bf q}]$ = 0.3795a* for clinker_2.5 ( $[{\bf g}]$ = h a* + k b* + l c* + m q). First-order satellites are clearly seen in both data sets, but second-order ones do not appear, hence m is restricted to 1, leading to an almost 100% indexing of all observed reflections.

The Pnma space group identified in the average structure is a good starting point because the main reflections correctly follow its reflection conditions. The International Tables for Crystallography Vol. C (Prince, 2004 ) show two possible superspace groups for the space group number 62: 62.1, Pnma(00γ)000, and 62.2, Pnma(00γ)0s0. In the first one, the superspace symmetry operations do not have any glide components along the additional dimension, while the second one applies a 1/2 translation along the fourth superspace coordinate for the mirror plane perpendicular to $[{\bf b}]$ . Although not listed, Pnma(00γ)s00 and Pnma(00 γ)ss0 are also possible and they have to be considered. If these superspace groups are taken into account with the modulation vector along the a* axis, the subsequent reflection conditions according to the different superspace groups are identified and listed in Table 4. Such conditions can now be evaluated in the reconstructed sections shown in Fig. 5 but using the four indices, hklm.

Table 4
Superspace groups compatible with the Pnma space group and one modulation wavevector along the a* axis

Superspace group	Reflection conditions
Pnma(α00)000	hk0m: h = 2n, 0kl0: k + l = 2n
Pnma(α00)000	h00m: h = 2n, 0k00: k = 2n, 00l0: l = 2n
Pnma(α00)0s0	hk0m: h = 2n, h0lm: m = 2n, 0kl0: k + l = 2n
Pnma(α00)0s0	h00m: h + m = 2n, 0k00: k = 2n, 00 l0: l = 2n
Pnma(α00)00s	hk0m: h + m = 2n, 0kl0: k + l = 2n
Pnma(α00)00s	h00m: h + m = 2n, 0k00: k = 2n, 00l0: l = 2n
Pnma(α00)0ss	hk0m: h + m = 2n, h0lm: m = 2n, 0kl0: k + l = 2n
Pnma(α00)0ss	h00m: h + m = 2n, 0k00: k = 2n, 00l0: l = 2n

The h0lm sections of Figs. 5(b) and 5(d) clearly show that no satellite reflections are visible, therefore the h0lm:m = 2n condition is fulfilled because the fourth index m is limited to ±1 and should be visible in this plane. The hk0m sections displayed in Fig. 7 show that the h = 2n condition for the main reflections of the sub-plane hk0 is fulfilled, i.e. there are no significant strong reflections along the blue dashed lines. This indicates the presence of the a-glide plane perpendicular to the c axis. However, satellite reflections are observed here and almost all of them appear around the reflections in the hk00 rows with h = 2n + 1 (marked by red dashed arrows in Fig. 8). Some weak reflections violate these conditions, but this is most probably a result of dynamical effects. When considering these two reflection conditions, the h + m = 2n condition is obtained for the hk0m plane. From the symmetry point of view, a 1/2 translation along the fourth superspace coordinate for the a-glide plane perpendicular to $[{\bf c}]$ has to be added to the 1/2 translation for the mirror plane perpendicular to $[{\bf b}]$ identified in the h0lm plane. Therefore, the superspace group for the incommensurately modulated structure of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ should be Pnma(00)0ss.

Figure 7
hk0m sections from the reconstructions of the observable diffraction space that correspond to (a) the clinker_0 and (b) the clinker_2.5 diffraction data sets. Red and blue dashed lines correspond to hk00 rows with even and odd h indices, respectively. Red dashed arrows point to the visible satellite reflections from their closest main reflection.

Figure 8
(x_s,2, x_s,4) de Wolff sections of O2 and O3 domains from (a)–(b) clinker_0 and (c)–(d) clinker_2.5. The vertical axis corresponds to x_s,4 (t = [0, 2]) and the horizontal axis to x_s,2. Red lines correspond to the dynamical refined crenel functions assigned to the atomic domains.

At this point, main and satellite reflection intensities were integrated and extracted from PETS2, and the obtained hklm reflection files were imported to JANA2006. First, the charge-flipping algorithm implemented in SUPERFLIP was used to obtain structure models that directly contained a first-order harmonic function for each atomic domain, as this algorithm is able to retrieve electrostatic potentials in an n-dimensional space (Palatinus & Chapuis, 2007; Palatinus, 2013 ). One of the oxygen atoms on the 4c position was missing in both diffraction data sets but they were found by a Fourier synthesis. It is worth noting that the Fourier synthesis also considers the 4D space, thus the suggested domains and their related averaged positions include modulation parameters as well. Both initial structure models were retrieved with two of the oxygen atoms placed on 4c positions. After all atomic positions were found, a first kinematical refinement was done with unconstrained modulation parameters but fixed isotropic ADPs. Inspection of the (x_s,1, x_s,4), (x_s,2, x_s,4) and (x_s,3, x_s,4) de Wolff sections (de Wolff, 1974 ) for all atoms revealed that a harmonic function fits well for calcium, silicon and the oxygen atom on the 8d site, yet the oxygen atoms on the mirror plane exhibit discontinuous trends in the (x_s,2, x_s,4) de Wolff section. This suggests that the displacive modulation of O2 and O3 atomic domains could be better described by crenel functions. In this way, the x_s,2 and x_s,4 coordinates of the maximum peaks in the (x_s,2, x_s,4) de Wolff sections for O2 and O3 were used to place these atomic domains out of the mirror plane (shift along the b axis and occupancy set to 1) and assign crenel functions with x⁰_s,4 parameters initially set to the found x_s,4 coordinates for subsequent refinements and Δ = 0.5. The symmetry of the superspace group ensures that there is no discontinuity along the direction of x_s,4 for these atomic domains while they follow discontinuous functions. Fig. 8 shows the (x_s,2, x_s,4) de Wolff sections of O2 and O3 for both diffraction data sets and Fig. S2 shows all other de Wolff plots.

Once the modulation functions were clear, further least-squares refinements were performed. First, the modulated model was refined with free modulation parameters (except Δ) and fixed isotropic ADPs. After convergence, the modulation parameters were fixed and the isotropic ADPs were refined, which led to convergence and small and positive ADPs. Finally, all structural parameters were refined and the least-squares procedure converged with well fitted functions to the de Wolff sections and physically meaningful isotropic ADPs. These kinematical refined models were then used as input to dynamical refinements (Palatinus, 2017 ). The same refinement workflow as the kinematical case was followed, but the optimization of the orientation angles from all patterns according to the calculated dynamical reflection intensities was carried out prior to the last refinement execution with all structural parameters free. Table 5 shows the resulting figures of merit from the dynamical refinements of the two data sets, and Tables S2 and S3 show the structural parameters for both refined incommensurately modulated structures. Low isotropic ADPs, well fitted modulation functions and good R₁ values considering main, satellite or all reflections demonstrate the reliability of the determined crystal structure.

Table 5
Resulting figures of merit (obs/all) from the dynamical refinements of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ in JANA2006

The criterion for observed (obs) reflections was I(g) > 3σ(g). The `Refl./Param.' measure refers to the number of observed reflections over the number of refined parameters in the least-squares procedure. R and R_w are based on the square root of reflection intensities. N_or of 128, g_max of 1.6 Å⁻¹, $[S_{g}^{\max}({\rm matrix})]$ of 0.01 Å⁻¹, $[S_{g}^{\max}({\rm refine})]$ of 0.1 Å⁻¹ were selected in both data sets, but RS_g was set to 0.4 for clinker_0 and 0.5 for clinker_2.5.

	clinker_0	clinker_2.5
Main reflections
No. of reflections at 0.7 Å	1726/2500	1848/2466
R	0.0710/0.0954	0.0763/0.0928
R_w	0.0730/0.0757	0.0825/0.0841
Satellite reflections
No. of reflections at 0.7 Å	2007/4796	1228/4531
R	0.199/0.279	0.159/0.312
R_w (%)	0.195/0.208	0.178/0.199
All reflections
No. of reflections at 0.7 Å	3733/7296	3076/6997
Refl./Param.	29.6	23.8
R	0.123/0.182	0.0964/0.169
R_w	0.112/0.120	0.0985/0.105

3.2.3. Crystal structure description

The reference crystal structure of $[\alpha_H^{\prime}]$ from Mumme et al. (1995) shows that all atoms except silicon are split into half-occupied positions. However, no satellite reflections were reported in that publication, most likely because of the high population of reflections in the PXRD. The electron diffraction structure analysis carried out here demonstrates that the atomic position splitting observed in powder diffraction comes from the intrinsic incommensurate modulation of the crystal structure. In fact, the average structure retrieved using only the main reflections coincides with the X-ray model without the splitting of the calcium positions. It is worth noting as well that the obtained unit-cell parameters are very similar between the two data sets of electron diffraction, but also to the X-ray structure, which indicates that this crystal structure can be reliably used for phase quantifications in powder patterns of different cement samples [data from Mumme et al. (1995): a = 6.7673 Å, b = 5.5191 Å and c = 9.3031 Å; this work, clinker_0: a = 6.776 Å, b = 5.496 Å and c = 9.252 Å; this work, clinker_2.5: a = 6.765 Å, b = 5.514 Å and c = 9.250 Å].

Nevertheless, the strong intensities of the satellite reflections observed in both diffraction data sets, as well as the high anisotropy of the ADPs for the average structure, imply that the modulation cannot be ignored for a proper crystal structure determination. Inspection of the reconstructed observable diffraction space pointed to the superspace group Pnma(α00)0ss as the symmetry group that fits to the reflection conditions. The subsequent structure solutions and least-squares refinements in JANA2006 showed that such a superspace group allows us to solve and refine the crystal structure using harmonic and crenel functions to describe the incommensurate modulation. The high ADPs obtained in the averaged models were not retrieved in the refined modulated structures.

The visualization and description of aperiodic crystals is not trivial because such crystals are represented in a (3+d)D space, yet they need to be illustrated back to the physical 3D space (Wagner & Schönleber, 2009 ). One way is to build a superstructure with the unit cell of the aperiodic crystal as the subcell of the supercell. Fig. 9 shows such a superstructure along $[{\bf b}]$ and $[{\bf c}]$ for the clinker_0 refined model (9 × $[{\bf a}]$ , 2 × $[{\bf b}]$ , 2 × $[{\bf c}]$ ). Since the modulation wavevector is along the a* axis, the crystal structure preserves the translational symmetry in the xy plane, which means that the orientation and geometry of the Si–O tetrahedra as well as the calcium positions can change while going through the x component of the unit-cell framework, but the atomic positions translated through the y and z components are preserved. This can be seen in Fig. 9, as the tetrahedron positions and geometries in the subcell limited by the dotted lines are the same when shifted to the subcells along $[{\bf b}]$ or $[{\bf c}]$ , yet they change along $[{\bf a}]$ . Another interesting characteristic of the approximated superstructure is that the best supercell to fit all reflections can be identified by checking which subcell most closely resembles the initial one. This coincides with the cell that corresponds to an integer period of the modulation wavevector. In the case of $[\alpha_H^{\prime}]$ , this is fulfilled after eight subcells and it is shown in Fig. 9, where the ninth subcell (labelled 8) is the most comparable to the first one (labelled 0).

Figure 9
The approximated superstructure with 9 × $[{\bf a}]$ , 2 × $[{\bf b}]$ and 2 × $[{\bf c}]$ with respect to the unit cell of the incommensurately modulated structure of clinker_0. The upper figure is the projection along the b axis, and the lower one is along $[{\bf c}]$ . Calcium atoms have been omitted for clarity of the modulated distortion and orientation of Si–O tetrahedra. Dotted lines are displayed to show the positions of the subcells.

The projections of the superstructure in Fig. 9 graphically show that the geometry of the silicon–oxygen tetrahedra and their orientations change through the a axis as a consequence of the modulation of their atoms. A better way of quantifying these modulation characteristics is to plot the interatomic distances with respect to the phase t of the modulation wavevector. Fig. 10 shows the silicon to oxygen distance plots for the models from clinker_0 and clinker_2.5. Atom O3 presents the longer distance to Si, up to 1.721 (6) Å and 1.663 (3) Å for clinker_0 and clinker_2.5, respectively. The harmonic modulation of silicon and the discontinuous positioning of atoms O2 and O3 result in a decrease in the Si—O3 distance and an increase in the Si—O2 distance for every half period of the modulation function, which tend to average distances of 1.661 (4) Å (clinker_0) and 1.627 (3) Å (clinker_2.5) until the oxygen atoms jump to the mirror-related positions. Atom O1 and its symmetry-related oxygen atom O1s7 that completes the tetrahedron have silicon–oxygen curves that are almost in phase between them. This indicates that the harmonic modulation of silicon is in phase to one of these oxygen atoms, while the other is out of phase due to the symmetry relation. Such a particular displacement points towards a silicon to oxygen distance that changes due to the higher displacement value of the oxygen with respect to the silicon atom, but the direction of the silicon–oxygen movement is almost the same for one of the oxygen atoms and the other way around for the symmetry-related one.

Figure 10
Distances between silicon and the four tetrahedral oxygen atoms with respect to the modulation phase t. Panel (a) corresponds to clinker_0 and panel (b) to clinker_2.5.

The calcium coordination is complicated to illustrate through superstructure projections and interatomic distance plots because of the high number of related oxygen atoms. Nevertheless, careful inspection of both refined structures shows that calcium has octahedral and dodecahedral coordination when Ca—O distances between 2.2 and 3.2 Å are considered. The geometry of these coordination environments changes through the a axis and that is why the Ca—O distance for some oxygen atoms is increased to ∼3.2 Å, compared with the ∼2.8 Å distance of the averaged structure.

The use of crenel functions for atoms O2 and O3 confirms that the split and half-occupied atoms in the average structure are a good approximation of the real nature of the crystal structure. However, the rest of the atoms require harmonic functions to describe its intrinsic modulation. Table 6 reports the distances between split positions for the structure reported by Mumme et al. (1995), the average structures and the total modulated displacements for the modulated structures. These values show that in general the total movement of the atoms in the modulated crystal structure is larger than the reported one on the average structures, especially for atom O1. Silicon also has a displacive modulation that is not directly detected in the average approximations, although much weaker, but which provides a better description of the crystal structure. Finally, it is worth noting that the values of the model from clinker_0 are higher than clinker_2.5, which demonstrates that the modulation is stronger in the first data set, as visible also in the stronger intensities of satellite reflections.

Table 6
Distances (Å) between split positions for the average structures and the total modulated displacements (Å) for the modulated structures of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$

		Average structure		Modulated structure
Atom	Mumme et al. (1995)	clinker_0	clinker_2.5	clinker_0	clinker_2.5
Ca1	0.34770			0.404 (1)	0.320 (1)
Ca2	0.24394			0.396 (1)	0.324 (1)
Si1				0.272 (1)	0.278 (1)
O1	0.58797†	0.696 (12)†	0.670 (11)†	0.938 (1)	0.81 (1)
O2	0.63470	0.684 (6)	0.22 (5)	0.665 (1)	0.617 (1)
O3	0.76495	0.790 (5)	0.754 (10)	0.797 (1)	0.723 (1)

†These values correspond to the O1—O1_2 distance.

3.2.4. Phase transitions of the belite polymorphs

The structures of the different belite polymorphs can be derived from the hexagonal closest packing of atoms (Bragg & Claringbull, 1965 ). The γ phase has an olivine-type structure, the α and β polymorphs are β-K₂SO₄-type structures, and $[\alpha_L^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ is a superstructure of such a β-K₂SO₄-type structure (Udagawa et al., 1980). When the temperature is increased, CaO_n polyhedra in the β-K₂SO₄-type structures increase in size, while the size of the SiO₄ tetrahedra does not change (Smyth & Hazen, 1973 ). This large size difference leads to tilting, shifting and distortion of the SiO₄ tetrahedra (Toraya & Yamazaki, 2002 ). On the other hand, this size difference is not present in the olivine-type structure of the γ polymorph, which explains why calcium is octahedrally coordinated in γ but has more adjacent oxygen atoms in the other polymorphs, ranging up to a tenfold coordination. A comparable behaviour of metastable phases containing different Ca coordination numbers is vaterite, which was also solved by 3D ED (Mugnaioli et al., 2012 ).

In order to study and illustrate the phase transitions of the different belite phases, three characteristic viewing directions were selected that correspond to the main directions in most belite polymorphs: the ∼5, ∼7 and ∼9 Å axes. Starting with the high-temperature α-C₂S, the hexagonal axis can be seen along the c axis (∼7 Å axis) in Fig. 11(a). In this case, the hexagon is constructed from two mutually displaced triangles of SiO₄ tetrahedra that are in two different planes along c. Along the b axis [∼5 Å axis; Fig. 11(b)], the SiO₄ tetrahedra are arranged in slightly shifted rows through the c direction. Along the ( $[{\overline 2} {\overline 1} 0]$ ) direction [∼9 Å axis; Fig. 11(c)], they are arranged in rows running along b. Because of the P6₃/mmc space group, the oxygen atoms of the SiO₄ tetrahedra and some Ca positions are split in the direction of the c axis.

Figure 11
(a)–(c) The α-C₂S structure along (a) the c axis, (b) the b axis and (c) the ( $[{\overline 2} {\overline 1} 0]$ ) direction. (d)–(f) The average structure of $[\alpha_H^{\prime}]$ belite along (d) the a axis, (e) the b axis and (f) the c axis. (g)–(i) The β-C₂S structure along (g) the b axis, (h) the a axis and (i) the c axis. (j)–(l) The structure of γ-C₂S along (j) the a axis, (k) the c axis and (l) the b axis. Panels (a), (d) and (g) correspond to the ∼7 Å direction, (b), (e) and (h) to the ∼5 Å direction, and (c), (f) and (i) to the ∼9 Å direction. The viewing directions of γ-C₂S are selected accordingly for proper comparison. The projections in (b), (e), (h) and (k) display the original cell of α-C₂S as dashed black lines to illustrate the formation of tetrahedron pairs in $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ . The structures are displayed as 2 × 2 × 2 of the respective unit cells. Ca is displayed in purple, Si in orange and O in red.

Upon cooling, the statistically ordered α-C₂S transitions to the $[\alpha_H^{\prime}]$ polymorph at 1425°C. Here, the orientation of the cell changes with the transformation matrix [0 0 1; 0 1 0; −2 −1 0] and an origin shift of (0, ¼, ¼). Along the ∼7 Å direction, which originally indicated sixfold symmetry, a slight tilting and twisting of the split SiO₄ tetrahedra is visible [Fig. 11(d)]. The two triangles that form the hexagon are also slightly tilted with respect to each other. Along the c direction (∼9 Å axis), rows of split SiO₄ tetrahedra can be seen, but every other tetrahedron is rotated with respect to the b axis [Fig. 11(f)]. This change in the structure is achieved by a combination of a rotation around $[{\bf c}]$ and a slight rotation around $[{\bf a}]$ , and an additional ¼ shift in $[{\bf a}]$ and $[{\bf c}]$ . Along the b axis (∼5 Å axis), the splitting of the tetrahedra cannot be seen. The rotation of the tetrahedra results in the formation of tetrahedron pairs in this direction [black dashed rectangle in Fig. 11(e)].

Upon further cooling, a transformation to $[\alpha_L^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ occurs at about 1160–1177°C. In this case, the b and c axes are interchanged, while the orientation of the a axis remains the same. The ordering leads to a change in space group to Pna2₁. The biggest difference with respect to the $[\alpha_H^{\prime}]$ structure can be seen in the ∼9 Å direction. In the incommensurate modulated structure of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ , the Si tetrahedra are tilted irregularly along the a axis [Fig. 12(a)]. In the $[\alpha_L^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ structure the tetrahedra are now ordered along the a axis in an up–up–down pattern [Fig. 12(b)], causing a threefold superstructure and explaining the tripling of the 7 Å axis (a* direction), which coincides with the direction of the modulation vector of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ .

Figure 12
Rows of Si tetrahedra projected along the ∼9 Å viewing direction of (a) the incommensurate modulated structure of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ , (b) $[\alpha_L^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ and (c) β-C₂S. The tilt of each tetrahedron is illustrated by the black arrow below it. Ca positions have been omitted for clarity. Si is displayed in orange and O in red.

Upon further cooling, the structure is transformed to β-C₂S. In this process, the orthorhombic crystal system is converted into a monoclinic one and the orientations of the axes change according to the transformation matrix [0 1 0; 0 0 1; 1 0 0]. The biggest distortion is seen in the ∼7 Å viewing direction where the original sixfold symmetry is strongly distorted and the distances between the triangles change [Fig. 11(g)]. In the ∼5 Å direction, the tetrahedron pairs remain, but are slightly distorted with respect to each other [Fig. 11(h)]. The rows of tetrahedra observed in the ∼9 Å direction break up [Fig. 11(i)]. In comparison to the $[\alpha_L^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ structure, the tilting of the Si tetrahedra changes from an up–up–down to an alternating down–up pattern [Fig. 12(c)].

Transformation to the γ phase, which is stable at room temperature, changes the crystal system back to orthorhombic. In this case, however, the structure resembles the olivine-type structure instead of the β-K₂SO₄-type structure. These significant changes are caused by large rotational movements around all three axes. Accordingly, the axis lengths also change and no longer correspond to the ones defined above. Instead, the ∼7 Å axis now shows the tetrahedron pairs together [Fig. 11(k)]. Additionally, the tetrahedral hexagon along the ∼5 Å direction is no longer recognizable [Fig. 11(j)]. The greatest change can be seen along the ∼11 Å axis, where the rows of tetrahedra are no longer present [Fig. 11(l)].

4. Conclusions

For more than half a century the crystalline characterization of cement samples has been hampered by the difficulties of acquiring diffraction data sets from individual crystals of actual cement powders. The development of the 3D ED technique and systematic acquisition methods in a transmission electron microscope, like the Fast-ADT routine, have proved in this work to be suitable for the identification and crystallographic analysis of individual particles in clinker powders.

The processing of the acquired diffraction data sets has shown that most acquisitions belong to β-C₂S, some of which contain the typical non-merohedral [100] twinning of monoclinic crystals. The reconstruction of the observable diffraction space from the $[\alpha_H^{\prime}]$ polymorph data sets exhibits an incommensurately modulated component along the a axis that was previously reported but never properly characterized. The inspection of the reconstructed space indicates that the structure could be described in the Pnma(α00)0ss superspace group and hklm files were extracted for structure determinations based on the superspace formalism. The subsequent use of harmonic and crenel functions to describe the modulation of all atoms in dynamical refinements results in good figures of merit as well as good fitting of the functions in the de Wolff sections, which confirms the proper crystal structure determination of the novel incommensurately modulated structure.

The fact that two different diffraction data sets from two different manufactured samples result in such close refined structure models indicates that the crystalline description of $[\alpha_H^{\prime} {\hbox{-}} {\rm C}_2 {\rm S}]$ in this work is generally valid for different processed cements. The structure published by Mumme et al. (1995) and the refined average structures reported here show that these models do not deviate strongly from the real crystalline nature of the material, and they can be used as good approximations. Nevertheless, the incommensurately modulated structure provides a better model for this crystalline phase, which can be used in the phase quantifications frequently carried out in PXRD patterns to enhance the reliability of fitting by the Rietveld method.

Supporting information

B-IncStrDB reference: 7bhGderGvHs

CCDC references: 2332749; 2338192; 2338193; 2338194

Crystal structure: contains datablocks global, 0k_average_dyn, 0k_modulated_dyn, 2p5K_average_dyn, 2p5K_modulated_dyn. DOI: https://doi.org/10.1107/S205252062400146X/je5054sup1.cif

Structure factors: contains datablock 0K_modulated_dyn. DOI: https://doi.org/10.1107/S205252062400146X/je50540k_modulated_dynsup2.hkl

Structure factors: contains datablock 2p5K_modulated_dyn. DOI: https://doi.org/10.1107/S205252062400146X/je50542p5K_modulated_dynsup3.hkl

Additional tables and figures. DOI: https://doi.org/10.1107/S205252062400146X/je5054sup4.pdf

Computing details top

(0k_average_dyn) top

Crystal data top

Ca₈O₁₆Si₄	Z = 1
M_r = 689	F(000) = 344
Orthorhombic, Pnma	D_x = 3.320 Mg m⁻³
Hall symbol: -P -2xabc;-2yb;-2zac	Electron radiation, λ = 0.0197 Å
a = 6.776 Å	µ = 0 mm⁻¹
b = 5.496 Å	T = 293 K
c = 9.252 Å	Nanocrystals of up to 500 nm in size
V = 344.55 Å³

Data collection top

TEM diffractometer	h = −9→9
10028 measured reflections	k = −7→7
2439 independent reflections	l = −10→10
1709 reflections with I > 3σ(I)

Refinement top

Refinement on F	137 parameters
R[F² > 2σ(F²)] = 0.056	0 restraints
wR(F²) = 0.059	0 constraints
S = 2.03	Weighting scheme based on measured s.u.'s w = 1/(σ²(F) + 0.0001F²)
2439 reflections	(Δ/σ)_max = 0.033

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å²) top

	x	y	z	U_iso*/U_eq	Occ. (<1)
Ca1	0.66658 (12)	0.75	0.5706 (2)	0.0251 (6)
Ca2	0.49080 (11)	0.25	0.79563 (19)	0.0161 (5)
Si1	0.78069 (16)	0.25	0.4128 (3)	0.0158 (7)
O1	0.7521 (6)	0.5203 (6)	0.8014 (7)	0.0258 (18)	0.621 (4)
O2	0.6574 (3)	0.3219 (4)	0.5622 (7)	0.030 (2)	0.5
O3	1.0073 (3)	0.3122 (5)	0.4500 (7)	0.024 (2)	0.5
O1_2	0.8219 (9)	0.5103 (11)	0.8563 (14)	0.0258 (18)	0.379 (2)

Atomic displacement parameters (Å²) top

	U¹¹	U²²	U³³	U¹²	U¹³	U²³
Ca1	0.0123 (4)	0.0387 (6)	0.0244 (17)	0	−0.0005 (6)	0
Ca2	0.0090 (4)	0.0275 (5)	0.0118 (14)	0	−0.0004 (5)	0
Si1	0.0114 (5)	0.0201 (7)	0.016 (2)	0	0.0002 (7)	0
O1	0.026 (2)	0.0194 (9)	0.032 (5)	−0.0089 (13)	0.0070 (18)	−0.0099 (17)
O2	0.0141 (11)	0.037 (2)	0.039 (6)	−0.0012 (8)	0.0088 (17)	0.0096 (17)
O3	0.0159 (11)	0.042 (3)	0.014 (5)	−0.0063 (8)	0.0023 (15)	−0.0050 (14)
O1_2	0.026 (2)	0.0194 (9)	0.032 (5)	−0.0089 (13)	0.0070 (18)	−0.0099 (17)

Geometric parameters (Å, º) top

Ca1—Ca1ⁱ	3.7887 (11)	Ca2—Si1^xii	3.050 (3)
Ca1—Ca1ⁱⁱ	3.7887 (11)	Ca2—O1	2.312 (4)
Ca1—Ca2	3.6476 (15)	Ca2—O1^xii	2.373 (4)
Ca1—Ca2ⁱⁱⁱ	3.6476 (15)	Ca2—O1^xiii	2.373 (4)
Ca1—Ca2^iv	3.444 (2)	Ca2—O1^xiv	2.312 (4)
Ca1—Ca2ⁱⁱ	3.552 (2)	Ca2—O3^xii	2.381 (7)
Ca1—Ca2^v	3.7296 (11)	Ca2—O3^xiii	2.381 (7)
Ca1—Ca2^vi	3.7296 (11)	Ca2—O1_2^xii	2.309 (9)
Ca1—Si1	3.2064 (16)	Ca2—O1_2^xiii	2.309 (9)
Ca1—Si1ⁱⁱⁱ	3.2064 (16)	Si1—O1^iv	1.645 (5)
Ca1—Si1^vii	3.186 (3)	Si1—O1^xv	1.645 (5)
Ca1—Si1ⁱⁱ	3.0346 (14)	Si1—O2	1.663 (6)
Ca1—O2	2.355 (2)	Si1—O2^xiv	1.663 (6)
Ca1—O2^viii	2.355 (2)	Si1—O3	1.610 (3)
Ca1—O3^ix	2.244 (2)	Si1—O3^xiv	1.610 (3)
Ca1—O3^x	2.244 (2)	Si1—O1_2^iv	1.579 (7)
Ca1—O1_2^iv	2.446 (11)	Si1—O1_2^xv	1.579 (7)
Ca1—O1_2^xi	2.446 (11)	O1—O1_2	0.696 (12)
Ca2—Ca2^xii	3.4916 (12)	O2—O2^xiv	0.790 (3)
Ca2—Ca2^v	3.4916 (12)	O3—O3^xiv	0.684 (4)

Ca1ⁱ—Ca1—Ca1ⁱⁱ	92.99 (3)	Ca1^vii—Ca2—O3^xii	40.37 (6)
Ca1ⁱ—Ca1—Ca2	57.03 (3)	Ca1^vii—Ca2—O3^xiii	40.37 (6)
Ca1ⁱ—Ca1—Ca2ⁱⁱⁱ	123.28 (3)	Ca1^vii—Ca2—O1_2^xii	141.60 (19)
Ca1ⁱ—Ca1—Ca2^iv	98.45 (5)	Ca1^vii—Ca2—O1_2^xiii	141.60 (19)
Ca1ⁱ—Ca1—Ca2ⁱⁱ	59.48 (3)	Ca1ⁱ—Ca2—Ca1^xii	98.03 (4)
Ca1ⁱ—Ca1—Ca2^v	86.043 (18)	Ca1ⁱ—Ca2—Ca1^xvii	98.03 (4)
Ca1ⁱ—Ca1—Ca2^vi	178.93 (5)	Ca1ⁱ—Ca2—Ca2^xii	58.54 (4)
Ca1ⁱ—Ca1—Si1	50.58 (3)	Ca1ⁱ—Ca2—Ca2^v	93.48 (5)
Ca1ⁱ—Ca1—Si1ⁱⁱⁱ	127.47 (7)	Ca1ⁱ—Ca2—Si1^xii	134.71 (4)
Ca1ⁱ—Ca1—Si1^vii	114.17 (4)	Ca1ⁱ—Ca2—O1	104.59 (17)
Ca1ⁱ—Ca1—Si1ⁱⁱ	54.72 (3)	Ca1ⁱ—Ca2—O1^xii	55.56 (15)
Ca1ⁱ—Ca1—O2	41.26 (9)	Ca1ⁱ—Ca2—O1^xiii	55.56 (15)
Ca1ⁱ—Ca1—O2^viii	134.23 (10)	Ca1ⁱ—Ca2—O1^xiv	104.59 (17)
Ca1ⁱ—Ca1—O3^ix	131.91 (11)	Ca1ⁱ—Ca2—O3^xii	163.14 (6)
Ca1ⁱ—Ca1—O3^x	116.55 (10)	Ca1ⁱ—Ca2—O3^xiii	163.14 (6)
Ca1ⁱ—Ca1—O1_2^iv	46.79 (16)	Ca1ⁱ—Ca2—O1_2^xii	43.2 (3)
Ca1ⁱ—Ca1—O1_2^xi	99.4 (2)	Ca1ⁱ—Ca2—O1_2^xiii	43.2 (3)
Ca1ⁱⁱ—Ca1—Ca2	123.28 (3)	Ca1^xii—Ca2—Ca1^xvii	94.92 (3)
Ca1ⁱⁱ—Ca1—Ca2ⁱⁱⁱ	57.03 (3)	Ca1^xii—Ca2—Ca2^xii	60.57 (2)
Ca1ⁱⁱ—Ca1—Ca2^iv	98.45 (5)	Ca1^xii—Ca2—Ca2^v	130.679 (16)
Ca1ⁱⁱ—Ca1—Ca2ⁱⁱ	59.48 (3)	Ca1^xii—Ca2—Si1^xii	55.36 (3)
Ca1ⁱⁱ—Ca1—Ca2^v	178.93 (5)	Ca1^xii—Ca2—O1	156.48 (16)
Ca1ⁱⁱ—Ca1—Ca2^vi	86.043 (18)	Ca1^xii—Ca2—O1^xii	42.49 (15)
Ca1ⁱⁱ—Ca1—Si1	127.47 (7)	Ca1^xii—Ca2—O1^xiii	100.68 (10)
Ca1ⁱⁱ—Ca1—Si1ⁱⁱⁱ	50.58 (3)	Ca1^xii—Ca2—O1^xiv	88.28 (10)
Ca1ⁱⁱ—Ca1—Si1^vii	114.17 (4)	Ca1^xii—Ca2—O3^xii	66.04 (7)
Ca1ⁱⁱ—Ca1—Si1ⁱⁱ	54.72 (3)	Ca1^xii—Ca2—O3^xiii	78.78 (8)
Ca1ⁱⁱ—Ca1—O2	134.23 (10)	Ca1^xii—Ca2—O1_2^xii	56.9 (3)
Ca1ⁱⁱ—Ca1—O2^viii	41.26 (9)	Ca1^xii—Ca2—O1_2^xiii	111.50 (16)
Ca1ⁱⁱ—Ca1—O3^ix	116.55 (10)	Ca1^xvii—Ca2—Ca2^xii	60.57 (2)
Ca1ⁱⁱ—Ca1—O3^x	131.91 (11)	Ca1^xvii—Ca2—Ca2^v	130.679 (16)
Ca1ⁱⁱ—Ca1—O1_2^iv	99.4 (2)	Ca1^xvii—Ca2—Si1^xii	55.36 (3)
Ca1ⁱⁱ—Ca1—O1_2^xi	46.79 (16)	Ca1^xvii—Ca2—O1	88.28 (10)
Ca2—Ca1—Ca2ⁱⁱⁱ	97.77 (5)	Ca1^xvii—Ca2—O1^xii	100.68 (10)
Ca2—Ca1—Ca2^iv	129.92 (2)	Ca1^xvii—Ca2—O1^xiii	42.49 (15)
Ca2—Ca1—Ca2ⁱⁱ	116.51 (3)	Ca1^xvii—Ca2—O1^xiv	156.48 (16)
Ca2—Ca1—Ca2^v	56.48 (2)	Ca1^xvii—Ca2—O3^xii	78.78 (8)
Ca2—Ca1—Ca2^vi	123.92 (6)	Ca1^xvii—Ca2—O3^xiii	66.04 (7)
Ca2—Ca1—Si1	72.12 (4)	Ca1^xvii—Ca2—O1_2^xii	111.50 (16)
Ca2—Ca1—Si1ⁱⁱⁱ	169.84 (6)	Ca1^xvii—Ca2—O1_2^xiii	56.9 (3)
Ca2—Ca1—Si1^vii	57.96 (4)	Ca2^xii—Ca2—Ca2^v	152.01 (7)
Ca2—Ca1—Si1ⁱⁱ	69.21 (4)	Ca2^xii—Ca2—Si1^xii	76.17 (5)
Ca2—Ca1—O2	42.06 (14)	Ca2^xii—Ca2—O1	138.48 (10)
Ca2—Ca1—O2^viii	139.72 (15)	Ca2^xii—Ca2—O1^xii	41.15 (9)
Ca2—Ca1—O3^ix	119.00 (12)	Ca2^xii—Ca2—O1^xiii	41.15 (9)
Ca2—Ca1—O3^x	104.79 (11)	Ca2^xii—Ca2—O1^xiv	138.48 (10)
Ca2—Ca1—O1_2^iv	91.9 (2)	Ca2^xii—Ca2—O3^xii	106.54 (7)
Ca2—Ca1—O1_2^xi	156.02 (19)	Ca2^xii—Ca2—O3^xiii	106.54 (7)
Ca2ⁱⁱⁱ—Ca1—Ca2^iv	129.92 (2)	Ca2^xii—Ca2—O1_2^xii	51.09 (16)
Ca2ⁱⁱⁱ—Ca1—Ca2ⁱⁱ	116.51 (3)	Ca2^xii—Ca2—O1_2^xiii	51.09 (16)
Ca2ⁱⁱⁱ—Ca1—Ca2^v	123.92 (6)	Ca2^v—Ca2—Si1^xii	131.82 (6)
Ca2ⁱⁱⁱ—Ca1—Ca2^vi	56.48 (2)	Ca2^v—Ca2—O1	42.48 (10)
Ca2ⁱⁱⁱ—Ca1—Si1	169.84 (6)	Ca2^v—Ca2—O1^xii	124.75 (13)
Ca2ⁱⁱⁱ—Ca1—Si1ⁱⁱⁱ	72.12 (4)	Ca2^v—Ca2—O1^xiii	124.75 (13)
Ca2ⁱⁱⁱ—Ca1—Si1^vii	57.96 (4)	Ca2^v—Ca2—O1^xiv	42.48 (10)
Ca2ⁱⁱⁱ—Ca1—Si1ⁱⁱ	69.21 (4)	Ca2^v—Ca2—O3^xii	101.16 (7)
Ca2ⁱⁱⁱ—Ca1—O2	139.72 (15)	Ca2^v—Ca2—O3^xiii	101.16 (7)
Ca2ⁱⁱⁱ—Ca1—O2^viii	42.06 (14)	Ca2^v—Ca2—O1_2^xii	109.5 (2)
Ca2ⁱⁱⁱ—Ca1—O3^ix	104.79 (11)	Ca2^v—Ca2—O1_2^xiii	109.5 (2)
Ca2ⁱⁱⁱ—Ca1—O3^x	119.00 (12)	Si1^xii—Ca2—O1	109.70 (17)
Ca2ⁱⁱⁱ—Ca1—O1_2^iv	156.02 (19)	Si1^xii—Ca2—O1^xii	90.94 (15)
Ca2ⁱⁱⁱ—Ca1—O1_2^xi	91.9 (2)	Si1^xii—Ca2—O1^xiii	90.94 (15)
Ca2^iv—Ca1—Ca2ⁱⁱ	59.85 (4)	Si1^xii—Ca2—O1^xiv	109.70 (17)
Ca2^iv—Ca1—Ca2^v	81.26 (3)	Si1^xii—Ca2—O3^xii	31.54 (6)
Ca2^iv—Ca1—Ca2^vi	81.26 (3)	Si1^xii—Ca2—O3^xiii	31.54 (6)
Ca2^iv—Ca1—Si1	60.07 (4)	Si1^xii—Ca2—O1_2^xii	107.9 (3)
Ca2^iv—Ca1—Si1ⁱⁱⁱ	60.07 (4)	Si1^xii—Ca2—O1_2^xiii	107.9 (3)
Ca2^iv—Ca1—Si1^vii	131.18 (4)	O1—Ca2—O1^xii	158.9 (2)
Ca2^iv—Ca1—Si1ⁱⁱ	135.28 (8)	O1—Ca2—O1^xiii	97.38 (14)
Ca2^iv—Ca1—O2	89.62 (13)	O1—Ca2—O1^xiv	79.97 (13)
Ca2^iv—Ca1—O2^viii	89.62 (13)	O1—Ca2—O3^xii	91.92 (18)
Ca2^iv—Ca1—O3^ix	43.41 (17)	O1—Ca2—O3^xiii	81.31 (18)
Ca2^iv—Ca1—O3^x	43.41 (17)	O1—Ca2—O1_2^xii	142.3 (3)
Ca2^iv—Ca1—O1_2^iv	51.67 (17)	O1—Ca2—O1_2^xiii	89.7 (2)
Ca2^iv—Ca1—O1_2^xi	51.67 (17)	O1^xii—Ca2—O1^xiii	77.53 (14)
Ca2ⁱⁱ—Ca1—Ca2^v	119.56 (4)	O1^xii—Ca2—O1^xiv	97.38 (14)
Ca2ⁱⁱ—Ca1—Ca2^vi	119.56 (4)	O1^xii—Ca2—O3^xii	108.43 (16)
Ca2ⁱⁱ—Ca1—Si1	68.78 (5)	O1^xii—Ca2—O3^xiii	119.73 (17)
Ca2ⁱⁱ—Ca1—Si1ⁱⁱⁱ	68.78 (5)	O1^xii—Ca2—O1_2^xii	17.0 (3)
Ca2ⁱⁱ—Ca1—Si1^vii	168.97 (4)	O1^xii—Ca2—O1_2^xiii	79.6 (2)
Ca2ⁱⁱ—Ca1—Si1ⁱⁱ	75.43 (6)	O1^xiii—Ca2—O1^xiv	158.9 (2)
Ca2ⁱⁱ—Ca1—O2	87.74 (16)	O1^xiii—Ca2—O3^xii	119.73 (17)
Ca2ⁱⁱ—Ca1—O2^viii	87.74 (16)	O1^xiii—Ca2—O3^xiii	108.43 (16)
Ca2ⁱⁱ—Ca1—O3^ix	102.39 (17)	O1^xiii—Ca2—O1_2^xii	79.6 (2)
Ca2ⁱⁱ—Ca1—O3^x	102.39 (17)	O1^xiii—Ca2—O1_2^xiii	17.0 (3)
Ca2ⁱⁱ—Ca1—O1_2^iv	40.2 (2)	O1^xiv—Ca2—O3^xii	81.31 (18)
Ca2ⁱⁱ—Ca1—O1_2^xi	40.2 (2)	O1^xiv—Ca2—O3^xiii	91.92 (18)
Ca2^v—Ca1—Ca2^vi	94.92 (3)	O1^xiv—Ca2—O1_2^xii	89.7 (2)
Ca2^v—Ca1—Si1	51.51 (5)	O1^xiv—Ca2—O1_2^xiii	142.3 (3)
Ca2^v—Ca1—Si1ⁱⁱⁱ	129.83 (3)	O3^xii—Ca2—O3^xiii	16.51 (10)
Ca2^v—Ca1—Si1^vii	66.68 (4)	O3^xii—Ca2—O1_2^xii	122.4 (3)
Ca2^v—Ca1—Si1ⁱⁱ	124.86 (4)	O3^xii—Ca2—O1_2^xiii	135.6 (3)
Ca2^v—Ca1—O2	44.79 (9)	O3^xiii—Ca2—O1_2^xii	135.6 (3)
Ca2^v—Ca1—O2^viii	139.70 (10)	O3^xiii—Ca2—O1_2^xiii	122.4 (3)
Ca2^v—Ca1—O3^ix	63.92 (10)	O1_2^xii—Ca2—O1_2^xiii	76.6 (3)
Ca2^v—Ca1—O3^x	48.39 (11)	Ca1^xvi—Si1—Ca1	117.97 (8)
Ca2^v—Ca1—O1_2^iv	79.59 (19)	Ca1^xvi—Si1—Ca1^iv	118.65 (5)
Ca2^v—Ca1—O1_2^xi	132.93 (17)	Ca1^xvi—Si1—Ca1ⁱ	74.70 (3)
Ca2^vi—Ca1—Si1	129.83 (3)	Ca1^xvi—Si1—Ca2^v	73.13 (6)
Ca2^vi—Ca1—Si1ⁱⁱⁱ	51.51 (5)	Ca1^xvi—Si1—O1^iv	155.58 (16)
Ca2^vi—Ca1—Si1^vii	66.68 (4)	Ca1^xvi—Si1—O1^xv	66.1 (2)
Ca2^vi—Ca1—Si1ⁱⁱ	124.86 (4)	Ca1^xvi—Si1—O2	72.78 (11)
Ca2^vi—Ca1—O2	139.70 (10)	Ca1^xvi—Si1—O2^xiv	45.30 (9)
Ca2^vi—Ca1—O2^viii	44.79 (9)	Ca1^xvi—Si1—O3	108.33 (17)
Ca2^vi—Ca1—O3^ix	48.39 (11)	Ca1^xvi—Si1—O3^xiv	87.17 (14)
Ca2^vi—Ca1—O3^x	63.92 (10)	Ca1^xvi—Si1—O1_2^iv	139.4 (3)
Ca2^vi—Ca1—O1_2^iv	132.93 (17)	Ca1^xvi—Si1—O1_2^xv	47.9 (4)
Ca2^vi—Ca1—O1_2^xi	79.59 (19)	Ca1—Si1—Ca1^iv	118.65 (5)
Si1—Ca1—Si1ⁱⁱⁱ	117.97 (7)	Ca1—Si1—Ca1ⁱ	74.70 (3)
Si1—Ca1—Si1^vii	115.18 (5)	Ca1—Si1—Ca2^v	73.13 (6)
Si1—Ca1—Si1ⁱⁱ	105.30 (4)	Ca1—Si1—O1^iv	66.1 (2)
Si1—Ca1—O2	30.12 (14)	Ca1—Si1—O1^xv	155.58 (16)
Si1—Ca1—O2^viii	147.95 (17)	Ca1—Si1—O2	45.30 (9)
Si1—Ca1—O3^ix	81.63 (10)	Ca1—Si1—O2^xiv	72.78 (11)
Si1—Ca1—O3^x	66.00 (10)	Ca1—Si1—O3	87.17 (14)
Si1—Ca1—O1_2^iv	28.6 (2)	Ca1—Si1—O3^xiv	108.33 (17)
Si1—Ca1—O1_2^xi	97.2 (2)	Ca1—Si1—O1_2^iv	47.9 (4)
Si1ⁱⁱⁱ—Ca1—Si1^vii	115.18 (5)	Ca1—Si1—O1_2^xv	139.4 (3)
Si1ⁱⁱⁱ—Ca1—Si1ⁱⁱ	105.30 (4)	Ca1^iv—Si1—Ca1ⁱ	99.34 (7)
Si1ⁱⁱⁱ—Ca1—O2	147.95 (17)	Ca1^iv—Si1—Ca2^v	145.74 (5)
Si1ⁱⁱⁱ—Ca1—O2^viii	30.12 (14)	Ca1^iv—Si1—O1^iv	52.6 (2)
Si1ⁱⁱⁱ—Ca1—O3^ix	66.00 (10)	Ca1^iv—Si1—O1^xv	52.6 (2)
Si1ⁱⁱⁱ—Ca1—O3^x	81.63 (10)	Ca1^iv—Si1—O2	151.93 (16)
Si1ⁱⁱⁱ—Ca1—O1_2^iv	97.2 (2)	Ca1^iv—Si1—O2^xiv	151.93 (16)
Si1ⁱⁱⁱ—Ca1—O1_2^xi	28.6 (2)	Ca1^iv—Si1—O3	96.1 (2)
Si1^vii—Ca1—Si1ⁱⁱ	93.54 (7)	Ca1^iv—Si1—O3^xiv	96.1 (2)
Si1^vii—Ca1—O2	92.05 (16)	Ca1^iv—Si1—O1_2^iv	73.8 (5)
Si1^vii—Ca1—O2^viii	92.05 (16)	Ca1^iv—Si1—O1_2^xv	73.8 (5)
Si1^vii—Ca1—O3^ix	88.51 (17)	Ca1ⁱ—Si1—Ca2^v	114.92 (9)
Si1^vii—Ca1—O3^x	88.51 (17)	Ca1ⁱ—Si1—O1^iv	84.08 (15)
Si1^vii—Ca1—O1_2^iv	143.3 (2)	Ca1ⁱ—Si1—O1^xv	84.08 (15)
Si1^vii—Ca1—O1_2^xi	143.3 (2)	Ca1ⁱ—Si1—O2	57.05 (13)
Si1ⁱⁱ—Ca1—O2	88.58 (5)	Ca1ⁱ—Si1—O2^xiv	57.05 (13)
Si1ⁱⁱ—Ca1—O2^viii	88.58 (5)	Ca1ⁱ—Si1—O3	160.3 (2)
Si1ⁱⁱ—Ca1—O3^ix	171.01 (8)	Ca1ⁱ—Si1—O3^xiv	160.3 (2)
Si1ⁱⁱ—Ca1—O3^x	171.01 (8)	Ca1ⁱ—Si1—O1_2^iv	65.0 (2)
Si1ⁱⁱ—Ca1—O1_2^iv	94.18 (15)	Ca1ⁱ—Si1—O1_2^xv	65.0 (2)
Si1ⁱⁱ—Ca1—O1_2^xi	94.18 (15)	Ca2^v—Si1—O1^iv	128.11 (18)
O2—Ca1—O2^viii	175.15 (19)	Ca2^v—Si1—O1^xv	128.11 (18)
O2—Ca1—O3^ix	100.10 (9)	Ca2^v—Si1—O2	59.95 (16)
O2—Ca1—O3^x	82.59 (9)	Ca2^v—Si1—O2^xiv	59.95 (16)
O2—Ca1—O1_2^iv	52.4 (3)	Ca2^v—Si1—O3	50.6 (2)
O2—Ca1—O1_2^xi	123.9 (3)	Ca2^v—Si1—O3^xiv	50.6 (2)
O2^viii—Ca1—O3^ix	82.59 (9)	Ca2^v—Si1—O1_2^iv	119.9 (4)
O2^viii—Ca1—O3^x	100.10 (9)	Ca2^v—Si1—O1_2^xv	119.9 (4)
O2^viii—Ca1—O1_2^iv	123.9 (3)	O1^iv—Si1—O1^xv	100.3 (3)
O2^viii—Ca1—O1_2^xi	52.4 (3)	O1^iv—Si1—O2	105.7 (2)
O3^ix—Ca1—O3^x	17.52 (10)	O1^iv—Si1—O2^xiv	129.5 (2)
O3^ix—Ca1—O1_2^iv	89.4 (2)	O1^iv—Si1—O3	95.7 (2)
O3^ix—Ca1—O1_2^xi	79.1 (2)	O1^iv—Si1—O3^xiv	115.2 (2)
O3^x—Ca1—O1_2^iv	79.1 (2)	O1^iv—Si1—O1_2^iv	24.8 (4)
O3^x—Ca1—O1_2^xi	89.4 (2)	O1^iv—Si1—O1_2^xv	111.9 (5)
O1_2^iv—Ca1—O1_2^xi	71.6 (3)	O1^xv—Si1—O2	129.5 (2)
Ca1^xvi—Ca2—Ca1	97.77 (5)	O1^xv—Si1—O2^xiv	105.7 (2)
Ca1^xvi—Ca2—Ca1^vii	101.62 (3)	O1^xv—Si1—O3	115.2 (2)
Ca1^xvi—Ca2—Ca1ⁱ	63.49 (4)	O1^xv—Si1—O3^xiv	95.7 (2)
Ca1^xvi—Ca2—Ca1^xii	80.02 (2)	O1^xv—Si1—O1_2^iv	111.9 (5)
Ca1^xvi—Ca2—Ca1^xvii	159.53 (5)	O1^xv—Si1—O1_2^xv	24.8 (4)
Ca1^xvi—Ca2—Ca2^xii	100.30 (4)	O2—Si1—O2^xiv	27.50 (13)
Ca1^xvi—Ca2—Ca2^v	62.94 (3)	O2—Si1—O3	104.5 (3)
Ca1^xvi—Ca2—Si1^xii	131.09 (3)	O2—Si1—O3^xiv	110.6 (3)
Ca1^xvi—Ca2—O1	104.31 (12)	O2—Si1—O1_2^iv	81.7 (5)
Ca1^xvi—Ca2—O1^xii	62.28 (11)	O2—Si1—O1_2^xv	104.6 (4)
Ca1^xvi—Ca2—O1^xiii	118.58 (15)	O2^xiv—Si1—O3	110.6 (3)
Ca1^xvi—Ca2—O1^xiv	43.86 (15)	O2^xiv—Si1—O3^xiv	104.5 (3)
Ca1^xvi—Ca2—O3^xii	116.15 (7)	O2^xiv—Si1—O1_2^iv	104.6 (4)
Ca1^xvi—Ca2—O3^xiii	131.08 (7)	O2^xiv—Si1—O1_2^xv	81.7 (5)
Ca1^xvi—Ca2—O1_2^xii	49.28 (17)	O3—Si1—O3^xiv	24.51 (14)
Ca1^xvi—Ca2—O1_2^xiii	106.3 (3)	O3—Si1—O1_2^iv	108.3 (3)
Ca1—Ca2—Ca1^vii	101.62 (3)	O3—Si1—O1_2^xv	131.9 (3)
Ca1—Ca2—Ca1ⁱ	63.49 (4)	O3^xiv—Si1—O1_2^iv	131.9 (3)
Ca1—Ca2—Ca1^xii	159.53 (5)	O3^xiv—Si1—O1_2^xv	108.3 (3)
Ca1—Ca2—Ca1^xvii	80.02 (2)	O1_2^iv—Si1—O1_2^xv	113.1 (4)
Ca1—Ca2—Ca2^xii	100.30 (4)	Ca2—O1—Ca2^v	96.37 (14)
Ca1—Ca2—Ca2^v	62.94 (3)	Ca2—O1—Si1^vii	113.8 (2)
Ca1—Ca2—Si1^xii	131.09 (3)	Ca2—O1—O1_2	119.1 (8)
Ca1—Ca2—O1	43.86 (15)	Ca2^v—O1—Si1^vii	144.1 (3)
Ca1—Ca2—O1^xii	118.58 (15)	Ca2^v—O1—O1_2	76.3 (8)
Ca1—Ca2—O1^xiii	62.28 (11)	Si1^vii—O1—O1_2	72.3 (8)
Ca1—Ca2—O1^xiv	104.31 (12)	Ca1—O2—Si1	104.6 (2)
Ca1—Ca2—O3^xii	131.08 (7)	Ca1—O2—O2^xiv	177.6 (6)
Ca1—Ca2—O3^xiii	116.15 (7)	Si1—O2—O2^xiv	76.3 (6)
Ca1—Ca2—O1_2^xii	106.3 (3)	Ca1^xviii—O3—Ca2^v	96.22 (18)
Ca1—Ca2—O1_2^xiii	49.28 (17)	Ca1^xviii—O3—Si1	152.7 (3)
Ca1^vii—Ca2—Ca1ⁱ	155.09 (4)	Ca1^xviii—O3—O3^xiv	81.2 (3)
Ca1^vii—Ca2—Ca1^xii	98.74 (4)	Ca2^v—O3—Si1	97.8 (2)
Ca1^vii—Ca2—Ca1^xvii	98.74 (4)	Ca2^v—O3—O3^xiv	81.7 (8)
Ca1^vii—Ca2—Ca2^xii	146.38 (6)	Si1—O3—O3^xiv	77.7 (3)
Ca1^vii—Ca2—Ca2^v	61.61 (4)	Ca1^vii—O1_2—Ca2^v	96.6 (2)
Ca1^vii—Ca2—Si1^xii	70.21 (5)	Ca1^vii—O1_2—Si1^vii	103.5 (6)
Ca1^vii—Ca2—O1	57.77 (15)	Ca1^vii—O1_2—O1	131.2 (8)
Ca1^vii—Ca2—O1^xii	137.65 (13)	Ca2^v—O1_2—Si1^vii	159.5 (7)
Ca1^vii—Ca2—O1^xiii	137.65 (13)	Ca2^v—O1_2—O1	86.6 (10)
Ca1^vii—Ca2—O1^xiv	57.77 (15)	Si1^vii—O1_2—O1	82.9 (6)

Symmetry codes: (i) −x+1, y−1/2, −z+1; (ii) −x+1, y+1/2, −z+1; (iii) x, y+1, z; (iv) −x+3/2, −y+1, z−1/2; (v) x+1/2, −y+1/2, −z+3/2; (vi) x+1/2, −y+3/2, −z+3/2; (vii) −x+3/2, −y+1, z+1/2; (viii) x, −y+3/2, z; (ix) −x+2, y+1/2, −z+1; (x) −x+2, −y+1, −z+1; (xi) −x+3/2, y+1/2, z−1/2; (xii) x−1/2, −y+1/2, −z+3/2; (xiii) x−1/2, y, −z+3/2; (xiv) x, −y+1/2, z; (xv) −x+3/2, y−1/2, z−1/2; (xvi) x, y−1, z; (xvii) x−1/2, −y+3/2, −z+3/2; (xviii) −x+2, y−1/2, −z+1.

(0k_modulated_dyn) top

Crystal data top

Ca₈O₁₆Si₄	Z = 1
M_r = 689	F(000) = 344
Orthorhombic, Pnma(α00)0ss†	D_x = 3.320 Mg m⁻³
q = 0.372500a*	Electron radiation, λ = 0.0197 Å
a = 6.776 Å	µ = 0 mm⁻¹
b = 5.496 Å	T = 293 K
c = 9.252 Å	Nanocrystals of up to 500 nm in size
V = 344.55 Å³

† Symmetry operations: (1) x₁, x₂, x₃, x₄; (2) −x₁+1/2, −x₂, x₃+1/2, −x₄+1/2; (3) −x₁, x₂+1/2, −x₃, −x₄+1/2; (4) x₁+1/2, −x₂+1/2, −x₃+1/2, x₄; (5) −x₁, −x₂, −x₃, −x₄; (6) x₁+1/2, x₂, −x₃+1/2, x₄+1/2; (7) x₁, −x₂+1/2, x₃, x₄+1/2; (8) −x₁+1/2, x₂+1/2, x₃+1/2, −x₄.

Data collection top

TEM diffractometer	θ_max = 0.8°, θ_min = 0.1°
29908 measured reflections	h = −9→9
7296 independent reflections	k = −7→7
3733 reflections with I > 3σ(I)	l = −10→10

Refinement top

Refinement on F	0 restraints
R[F² > 2σ(F²)] = 0.123	0 constraints
wR(F²) = 0.120	Weighting scheme based on measured s.u.'s w = 1/(σ²(F) + 0.0001F²)
S = 2.38	(Δ/σ)_max = 0.040
7296 reflections	Δρ_max = 21.89 e Å⁻³
126 parameters	Δρ_min = −5.27 e Å⁻³

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å²) top

	x	y	z	U_iso*/U_eq	Occ. (<1)
Ca1	1.16654 (15)	0.75	0.5714 (2)	0.0130 (3)*
Ca2	1.00881 (13)	0.75	0.2045 (2)	0.0069 (3)*
Si1	0.7195 (2)	0.75	0.5881 (4)	0.0100 (4)*
O1	0.7772 (3)	0.9827 (3)	0.6781 (5)	0.0150 (5)*
O2	0.8422 (4)	0.6772 (5)	0.4352 (7)	0.0215 (7)*	0.5
O3	0.4913 (4)	0.8101 (4)	0.5485 (6)	0.0194 (7)*	0.5

Geometric parameters (Å, º) top

	Average	Minimum	Maximum
Ca1—Ca1ⁱ	3.793 (2)	3.660 (2)	3.931 (2)
Ca1—Ca1ⁱⁱ	3.795 (2)	3.660 (2)	3.931 (2)
Ca1—Ca2	3.561 (3)	3.559 (3)	3.563 (3)
Ca1—Ca2ⁱⁱⁱ	3.731 (2)	3.493 (2)	3.980 (2)
Ca1—Ca2^iv	3.734 (2)	3.493 (2)	3.980 (2)
Ca1—Ca2ⁱ	3.642 (3)	3.638 (3)	3.646 (3)
Ca1—Ca2ⁱⁱ	3.642 (3)	3.638 (3)	3.646 (3)
Ca1—Ca2^v	3.451 (2)	3.449 (2)	3.454 (2)
Ca1—Si1	3.0343 (17)	3.0332 (17)	3.0354 (17)
Ca1—Si1ⁱ	3.213 (3)	3.136 (3)	3.291 (3)
Ca1—Si1ⁱⁱ	3.214 (3)	3.136 (3)	3.291 (3)
Ca1—Si1^vi	3.175 (4)	3.171 (4)	3.179 (4)
Ca1—O1ⁱ	2.765 (7)	2.340 (7)	3.206 (7)
Ca1—O1^vi	2.751 (7)	2.258 (8)	3.259 (8)
Ca1—O1^vii	2.773 (7)	2.340 (7)	3.206 (7)
Ca1—O1^viii	2.761 (7)	2.258 (8)	3.259 (8)
Ca1—O2ⁱⁱ	2.450 (3)	2.225 (3)	2.551 (3)
Ca1—O2^ix	2.448 (3)	2.225 (3)	2.551 (3)
Ca1—O3^x	2.246 (3)	2.215 (3)	2.274 (3)
Ca1—O3^xi	2.246 (3)	2.215 (3)	2.274 (3)
Ca2—Ca2^xii	3.4988 (14)	3.4911 (14)	3.5066 (14)
Ca2—Ca2^v	3.4987 (14)	3.4910 (14)	3.5066 (14)
Ca2—Si1^xiii	3.332 (3)	3.153 (3)	3.516 (3)
Ca2—Si1^xiv	3.335 (3)	3.153 (3)	3.516 (3)
Ca2—Si1^v	3.068 (4)	3.061 (4)	3.076 (4)
Ca2—O1^xiv	2.473 (4)	2.370 (4)	2.615 (4)
Ca2—O1ⁱ	2.357 (5)	2.325 (6)	2.410 (6)
Ca2—O1^vii	2.357 (5)	2.325 (6)	2.410 (6)
Ca2—O1^xv	2.473 (4)	2.370 (4)	2.615 (4)
Ca2—O2	2.437 (6)	2.423 (6)	2.472 (6)
Ca2—O2^xvi	2.437 (6)	2.423 (6)	2.472 (6)
Ca2—O3^v	2.388 (6)	2.361 (6)	2.403 (6)
Ca2—O3^xvii	2.388 (6)	2.361 (6)	2.403 (6)
Si1—O1	1.611 (6)	1.564 (6)	1.669 (6)
Si1—O1^xvi	1.611 (6)	1.564 (6)	1.669 (6)
Si1—O2	1.682 (6)	1.662 (6)	1.721 (6)
Si1—O2^xvi	1.683 (6)	1.662 (6)	1.721 (6)
Si1—O3	1.618 (3)	1.601 (3)	1.651 (3)
Si1—O3^xvi	1.617 (3)	1.601 (3)	1.651 (3)

Ca1ⁱ—Ca1—Ca1ⁱⁱ	92.77 (5)	92.70 (5)	92.84 (5)
Ca1ⁱ—Ca1—Ca2	59.26 (5)	57.97 (5)	60.46 (5)
Ca1ⁱ—Ca1—Ca2ⁱⁱⁱ	86.29 (5)	82.51 (4)	90.06 (5)
Ca1ⁱ—Ca1—Ca2^iv	177.32 (6)	175.27 (6)	179.28 (7)
Ca1ⁱ—Ca1—Ca2ⁱ	57.18 (5)	55.95 (5)	58.45 (5)
Ca1ⁱ—Ca1—Ca2ⁱⁱ	123.38 (4)	122.19 (4)	124.53 (4)
Ca1ⁱ—Ca1—Ca2^v	98.22 (6)	95.97 (6)	100.46 (6)
Ca1ⁱ—Ca1—Si1	54.78 (6)	53.96 (6)	55.62 (6)
Ca1ⁱ—Ca1—Si1ⁱ	50.52 (4)	48.75 (4)	52.31 (4)
Ca1ⁱ—Ca1—Si1ⁱⁱ	127.01 (9)	125.84 (8)	128.11 (9)
Ca1ⁱ—Ca1—Si1^vi	114.44 (7)	111.22 (7)	117.53 (7)
Ca1ⁱ—Ca1—O1ⁱ	53.17 (9)	48.02 (11)	57.64 (8)
Ca1ⁱ—Ca1—O1^vi	96.74 (10)	96.31 (12)	97.17 (9)
Ca1ⁱ—Ca1—O1^vii	100.01 (13)	98.38 (14)	101.28 (12)
Ca1ⁱ—Ca1—O1^viii	142.08 (13)	137.17 (14)	146.11 (12)
Ca1ⁱ—Ca1—O2ⁱⁱ	133.32 (11)	132.48 (11)	135.21 (11)
Ca1ⁱ—Ca1—O2^ix	40.55 (9)	39.78 (9)	42.39 (9)
Ca1ⁱ—Ca1—O3^x	132.89 (12)	126.94 (12)	136.12 (12)
Ca1ⁱ—Ca1—O3^xi	114.69 (11)	111.09 (10)	121.01 (11)
Ca1ⁱⁱ—Ca1—Ca2	59.24 (5)	57.97 (5)	60.46 (5)
Ca1ⁱⁱ—Ca1—Ca2ⁱⁱⁱ	177.34 (6)	175.27 (6)	179.28 (7)
Ca1ⁱⁱ—Ca1—Ca2^iv	86.22 (5)	82.51 (4)	90.06 (5)
Ca1ⁱⁱ—Ca1—Ca2ⁱ	123.40 (4)	122.19 (4)	124.53 (4)
Ca1ⁱⁱ—Ca1—Ca2ⁱⁱ	57.16 (5)	55.95 (5)	58.45 (5)
Ca1ⁱⁱ—Ca1—Ca2^v	98.20 (6)	95.97 (6)	100.46 (6)
Ca1ⁱⁱ—Ca1—Si1	54.76 (6)	53.96 (6)	55.62 (6)
Ca1ⁱⁱ—Ca1—Si1ⁱ	127.02 (9)	125.84 (8)	128.11 (9)
Ca1ⁱⁱ—Ca1—Si1ⁱⁱ	50.49 (4)	48.75 (4)	52.31 (4)
Ca1ⁱⁱ—Ca1—Si1^vi	114.39 (7)	111.22 (7)	117.53 (7)
Ca1ⁱⁱ—Ca1—O1ⁱ	99.99 (13)	98.38 (14)	101.28 (12)
Ca1ⁱⁱ—Ca1—O1^vi	142.02 (13)	137.17 (14)	146.11 (12)
Ca1ⁱⁱ—Ca1—O1^vii	53.22 (9)	48.02 (11)	57.64 (8)
Ca1ⁱⁱ—Ca1—O1^viii	96.75 (10)	96.31 (12)	97.17 (9)
Ca1ⁱⁱ—Ca1—O2ⁱⁱ	40.55 (9)	39.78 (9)	42.39 (9)
Ca1ⁱⁱ—Ca1—O2^ix	133.32 (11)	132.48 (11)	135.21 (11)
Ca1ⁱⁱ—Ca1—O3^x	114.62 (11)	111.09 (10)	121.01 (11)
Ca1ⁱⁱ—Ca1—O3^xi	132.83 (12)	126.94 (12)	136.12 (12)
Ca2—Ca1—Ca2ⁱⁱⁱ	119.56 (6)	116.38 (6)	122.58 (7)
Ca2—Ca1—Ca2^iv	119.50 (6)	116.38 (6)	122.58 (7)
Ca2—Ca1—Ca2ⁱ	116.44 (6)	113.93 (6)	118.91 (6)
Ca2—Ca1—Ca2ⁱⁱ	116.41 (6)	113.93 (6)	118.91 (6)
Ca2—Ca1—Ca2^v	59.84 (5)	59.72 (5)	59.96 (5)
Ca2—Ca1—Si1	75.41 (8)	75.37 (8)	75.46 (8)
Ca2—Ca1—Si1ⁱ	68.55 (7)	66.30 (7)	70.75 (8)
Ca2—Ca1—Si1ⁱⁱ	68.52 (7)	66.30 (7)	70.75 (8)
Ca2—Ca1—Si1^vi	168.56 (5)	168.11 (5)	169.03 (5)
Ca2—Ca1—O1ⁱ	40.96 (11)	40.55 (13)	41.44 (10)
Ca2—Ca1—O1^vi	152.26 (12)	149.78 (11)	154.56 (13)
Ca2—Ca1—O1^vii	40.96 (11)	40.55 (13)	41.44 (10)
Ca2—Ca1—O1^viii	152.21 (12)	149.78 (11)	154.56 (13)
Ca2—Ca1—O2ⁱⁱ	86.48 (15)	85.29 (15)	89.25 (15)
Ca2—Ca1—O2^ix	86.49 (15)	85.29 (15)	89.25 (15)
Ca2—Ca1—O3^x	101.45 (16)	101.10 (16)	101.99 (16)
Ca2—Ca1—O3^xi	101.46 (16)	101.10 (16)	101.99 (16)
Ca2ⁱⁱⁱ—Ca1—Ca2^iv	94.70 (4)	94.48 (4)	94.93 (4)
Ca2ⁱⁱⁱ—Ca1—Ca2ⁱ	56.63 (4)	54.56 (4)	58.85 (4)
Ca2ⁱⁱⁱ—Ca1—Ca2ⁱⁱ	123.98 (7)	121.80 (8)	126.00 (7)
Ca2ⁱⁱⁱ—Ca1—Ca2^v	81.18 (5)	79.20 (5)	83.05 (5)
Ca2ⁱⁱⁱ—Ca1—Si1	125.00 (7)	121.28 (7)	128.67 (8)
Ca2ⁱⁱⁱ—Ca1—Si1ⁱ	51.79 (6)	49.06 (6)	54.64 (7)
Ca2ⁱⁱⁱ—Ca1—Si1ⁱⁱ	129.67 (5)	127.16 (5)	132.01 (4)
Ca2ⁱⁱⁱ—Ca1—Si1^vi	66.66 (6)	64.97 (6)	68.14 (6)
Ca2ⁱⁱⁱ—Ca1—O1ⁱ	78.90 (12)	75.93 (11)	82.16 (13)
Ca2ⁱⁱⁱ—Ca1—O1^vi	39.08 (12)	35.85 (11)	43.08 (13)
Ca2ⁱⁱⁱ—Ca1—O1^vii	126.15 (10)	121.71 (9)	131.55 (12)
Ca2ⁱⁱⁱ—Ca1—O1^viii	84.36 (10)	81.07 (9)	87.67 (12)
Ca2ⁱⁱⁱ—Ca1—O2ⁱⁱ	138.60 (10)	135.64 (10)	142.63 (11)
Ca2ⁱⁱⁱ—Ca1—O2^ix	43.94 (9)	41.17 (9)	48.11 (10)
Ca2ⁱⁱⁱ—Ca1—O3^x	65.11 (9)	61.85 (9)	66.59 (9)
Ca2ⁱⁱⁱ—Ca1—O3^xi	47.52 (10)	46.03 (10)	50.61 (10)
Ca2^iv—Ca1—Ca2ⁱ	124.00 (7)	121.80 (8)	126.00 (7)
Ca2^iv—Ca1—Ca2ⁱⁱ	56.60 (4)	54.56 (4)	58.85 (4)
Ca2^iv—Ca1—Ca2^v	81.17 (5)	79.20 (5)	83.05 (5)
Ca2^iv—Ca1—Si1	124.93 (7)	121.28 (7)	128.67 (8)
Ca2^iv—Ca1—Si1ⁱ	129.69 (5)	127.16 (5)	132.01 (4)
Ca2^iv—Ca1—Si1ⁱⁱ	51.75 (6)	49.06 (6)	54.64 (7)
Ca2^iv—Ca1—Si1^vi	66.64 (6)	64.97 (6)	68.14 (6)
Ca2^iv—Ca1—O1ⁱ	126.21 (10)	121.71 (9)	131.55 (12)
Ca2^iv—Ca1—O1^vi	84.42 (10)	81.07 (9)	87.67 (12)
Ca2^iv—Ca1—O1^vii	78.84 (12)	75.93 (11)	82.16 (13)
Ca2^iv—Ca1—O1^viii	39.03 (12)	35.85 (11)	43.08 (13)
Ca2^iv—Ca1—O2ⁱⁱ	43.91 (9)	41.17 (9)	48.11 (10)
Ca2^iv—Ca1—O2^ix	138.64 (10)	135.64 (10)	142.63 (11)
Ca2^iv—Ca1—O3^x	47.49 (10)	46.03 (10)	50.61 (10)
Ca2^iv—Ca1—O3^xi	65.08 (9)	61.85 (9)	66.59 (9)
Ca2ⁱ—Ca1—Ca2ⁱⁱ	97.97 (6)	97.97 (6)	97.97 (6)
Ca2ⁱ—Ca1—Ca2^v	129.86 (6)	126.65 (6)	133.05 (6)
Ca2ⁱ—Ca1—Si1	69.23 (6)	67.46 (6)	70.97 (6)
Ca2ⁱ—Ca1—Si1ⁱ	72.24 (7)	71.34 (7)	73.13 (7)
Ca2ⁱ—Ca1—Si1ⁱⁱ	170.12 (8)	169.25 (8)	171.03 (8)
Ca2ⁱ—Ca1—Si1^vi	58.10 (6)	54.55 (6)	61.63 (6)
Ca2ⁱ—Ca1—O1ⁱ	96.68 (12)	93.98 (13)	99.05 (10)
Ca2ⁱ—Ca1—O1^vi	42.01 (9)	39.54 (10)	44.09 (7)
Ca2ⁱ—Ca1—O1^vii	156.81 (13)	154.03 (13)	158.76 (12)
Ca2ⁱ—Ca1—O1^viii	87.47 (13)	83.34 (14)	91.04 (12)
Ca2ⁱ—Ca1—O2ⁱⁱ	139.46 (15)	139.43 (14)	139.55 (16)
Ca2ⁱ—Ca1—O2^ix	41.57 (13)	41.52 (13)	41.67 (15)
Ca2ⁱ—Ca1—O3^x	119.91 (12)	115.21 (12)	123.06 (12)
Ca2ⁱ—Ca1—O3^xi	104.46 (11)	101.05 (11)	109.34 (12)
Ca2ⁱⁱ—Ca1—Ca2^v	129.84 (6)	126.65 (6)	133.05 (6)
Ca2ⁱⁱ—Ca1—Si1	69.20 (6)	67.46 (6)	70.97 (6)
Ca2ⁱⁱ—Ca1—Si1ⁱ	170.14 (8)	169.25 (8)	171.03 (8)
Ca2ⁱⁱ—Ca1—Si1ⁱⁱ	72.22 (7)	71.34 (7)	73.13 (7)
Ca2ⁱⁱ—Ca1—Si1^vi	58.06 (6)	54.55 (6)	61.63 (6)
Ca2ⁱⁱ—Ca1—O1ⁱ	156.78 (13)	154.03 (13)	158.76 (12)
Ca2ⁱⁱ—Ca1—O1^vi	87.43 (13)	83.34 (14)	91.04 (12)
Ca2ⁱⁱ—Ca1—O1^vii	96.70 (12)	93.98 (13)	99.05 (10)
Ca2ⁱⁱ—Ca1—O1^viii	42.05 (9)	39.54 (10)	44.09 (7)
Ca2ⁱⁱ—Ca1—O2ⁱⁱ	41.57 (13)	41.52 (13)	41.67 (15)
Ca2ⁱⁱ—Ca1—O2^ix	139.47 (15)	139.43 (14)	139.55 (16)
Ca2ⁱⁱ—Ca1—O3^x	104.40 (11)	101.05 (11)	109.34 (12)
Ca2ⁱⁱ—Ca1—O3^xi	119.85 (12)	115.21 (12)	123.06 (12)
Ca2^v—Ca1—Si1	135.14 (10)	135.05 (10)	135.22 (10)
Ca2^v—Ca1—Si1ⁱ	59.89 (6)	56.55 (6)	63.26 (6)
Ca2^v—Ca1—Si1ⁱⁱ	59.89 (6)	56.55 (6)	63.26 (6)
Ca2^v—Ca1—Si1^vi	131.00 (5)	130.76 (5)	131.25 (5)
Ca2^v—Ca1—O1ⁱ	45.12 (9)	41.63 (8)	49.26 (11)
Ca2^v—Ca1—O1^vi	116.48 (11)	110.64 (11)	122.83 (12)
Ca2^v—Ca1—O1^vii	45.06 (9)	41.63 (8)	49.26 (11)
Ca2^v—Ca1—O1^viii	116.40 (11)	110.64 (11)	122.83 (12)
Ca2^v—Ca1—O2ⁱⁱ	90.19 (13)	86.68 (12)	93.12 (14)
Ca2^v—Ca1—O2^ix	90.21 (13)	86.68 (12)	93.12 (14)
Ca2^v—Ca1—O3^x	43.45 (15)	42.67 (15)	43.89 (15)
Ca2^v—Ca1—O3^xi	43.45 (15)	42.67 (15)	43.89 (15)
Si1—Ca1—Si1ⁱ	105.29 (7)	102.94 (7)	107.60 (7)
Si1—Ca1—Si1ⁱⁱ	105.25 (7)	102.94 (7)	107.60 (7)
Si1—Ca1—Si1^vi	93.54 (9)	93.47 (9)	93.62 (9)
Si1—Ca1—O1ⁱ	99.99 (11)	95.10 (12)	104.30 (11)
Si1—Ca1—O1^vi	102.86 (12)	98.93 (13)	106.23 (11)
Si1—Ca1—O1^vii	100.03 (11)	95.10 (12)	104.30 (11)
Si1—Ca1—O1^viii	102.91 (12)	98.93 (13)	106.23 (11)
Si1—Ca1—O2ⁱⁱ	87.28 (9)	86.52 (8)	88.65 (9)
Si1—Ca1—O2^ix	87.29 (9)	86.52 (8)	88.65 (9)
Si1—Ca1—O3^x	168.89 (12)	164.42 (11)	176.42 (15)
Si1—Ca1—O3^xi	168.98 (12)	164.42 (11)	176.42 (15)
Si1ⁱ—Ca1—Si1ⁱⁱ	117.54 (10)	117.52 (10)	117.56 (10)
Si1ⁱ—Ca1—Si1^vi	115.44 (9)	111.35 (9)	119.45 (9)
Si1ⁱ—Ca1—O1ⁱ	29.67 (12)	29.32 (12)	30.16 (14)
Si1ⁱ—Ca1—O1^vi	85.90 (13)	82.46 (12)	89.87 (14)
Si1ⁱ—Ca1—O1^vii	92.27 (13)	89.65 (12)	95.23 (15)
Si1ⁱ—Ca1—O1^viii	135.95 (11)	134.83 (10)	137.46 (13)
Si1ⁱ—Ca1—O2ⁱⁱ	147.56 (16)	147.27 (16)	148.11 (18)
Si1ⁱ—Ca1—O2^ix	30.13 (14)	29.84 (13)	30.67 (15)
Si1ⁱ—Ca1—O3^x	81.84 (10)	77.04 (10)	85.29 (10)
Si1ⁱ—Ca1—O3^xi	65.35 (10)	61.87 (10)	70.09 (10)
Si1ⁱⁱ—Ca1—Si1^vi	115.38 (9)	111.35 (9)	119.45 (9)
Si1ⁱⁱ—Ca1—O1ⁱ	92.30 (13)	89.65 (12)	95.23 (15)
Si1ⁱⁱ—Ca1—O1^vi	135.97 (11)	134.83 (10)	137.46 (13)
Si1ⁱⁱ—Ca1—O1^vii	29.67 (12)	29.32 (12)	30.16 (14)
Si1ⁱⁱ—Ca1—O1^viii	85.86 (13)	82.46 (12)	89.87 (14)
Si1ⁱⁱ—Ca1—O2ⁱⁱ	30.12 (14)	29.84 (13)	30.67 (15)
Si1ⁱⁱ—Ca1—O2^ix	147.56 (16)	147.27 (16)	148.11 (18)
Si1ⁱⁱ—Ca1—O3^x	65.29 (10)	61.87 (10)	70.09 (10)
Si1ⁱⁱ—Ca1—O3^xi	81.78 (10)	77.04 (10)	85.29 (10)
Si1^vi—Ca1—O1ⁱ	144.45 (13)	140.61 (13)	148.52 (14)
Si1^vi—Ca1—O1^vi	29.74 (12)	29.15 (11)	30.42 (13)
Si1^vi—Ca1—O1^vii	144.38 (13)	140.61 (13)	148.52 (14)
Si1^vi—Ca1—O1^viii	29.73 (12)	29.15 (11)	30.42 (13)
Si1^vi—Ca1—O2ⁱⁱ	90.97 (16)	87.55 (15)	95.59 (17)
Si1^vi—Ca1—O2^ix	91.00 (16)	87.55 (15)	95.59 (17)
Si1^vi—Ca1—O3^x	88.98 (16)	88.16 (16)	89.39 (16)
Si1^vi—Ca1—O3^xi	88.99 (16)	88.16 (16)	89.39 (16)
O1ⁱ—Ca1—O1^vi	115.04 (16)	111.56 (15)	119.18 (18)
O1ⁱ—Ca1—O1^vii	64.81 (16)	64.19 (16)	65.43 (16)
O1ⁱ—Ca1—O1^viii	156.45 (13)	150.10 (12)	161.81 (14)
O1ⁱ—Ca1—O2ⁱⁱ	121.3 (2)	119.93 (19)	122.1 (2)
O1ⁱ—Ca1—O2^ix	57.30 (17)	55.58 (18)	58.15 (17)
O1ⁱ—Ca1—O3^x	86.65 (16)	79.61 (16)	89.97 (17)
O1ⁱ—Ca1—O3^xi	69.39 (16)	67.02 (15)	75.36 (16)
O1^vi—Ca1—O1^vii	156.45 (13)	150.10 (12)	161.81 (14)
O1^vi—Ca1—O1^viii	55.52 (14)	55.30 (14)	55.72 (14)
O1^vi—Ca1—O2ⁱⁱ	119.67 (19)	116.76 (19)	121.81 (19)
O1^vi—Ca1—O2^ix	64.61 (17)	62.18 (16)	66.82 (19)
O1^vi—Ca1—O3^x	84.14 (16)	77.43 (16)	89.89 (17)
O1^vi—Ca1—O3^xi	75.15 (17)	69.29 (16)	82.29 (18)
O1^vii—Ca1—O1^viii	114.98 (16)	111.56 (15)	119.18 (18)
O1^vii—Ca1—O2ⁱⁱ	57.30 (17)	55.58 (18)	58.15 (17)
O1^vii—Ca1—O2^ix	121.3 (2)	119.93 (19)	122.1 (2)
O1^vii—Ca1—O3^x	69.36 (16)	67.02 (15)	75.36 (16)
O1^vii—Ca1—O3^xi	86.62 (16)	79.61 (16)	89.97 (17)
O1^viii—Ca1—O2ⁱⁱ	64.60 (16)	62.18 (16)	66.82 (19)
O1^viii—Ca1—O2^ix	119.68 (19)	116.76 (19)	121.81 (19)
O1^viii—Ca1—O3^x	75.05 (17)	69.29 (16)	82.29 (18)
O1^viii—Ca1—O3^xi	84.03 (16)	77.43 (16)	89.89 (17)
O2ⁱⁱ—Ca1—O3^x	80.60 (10)	77.66 (10)	86.06 (11)
O2ⁱⁱ—Ca1—O3^xi	95.47 (10)	94.81 (10)	96.28 (10)
O2^ix—Ca1—O3^x	95.47 (10)	94.81 (10)	96.28 (10)
O2^ix—Ca1—O3^xi	80.66 (10)	77.66 (10)	86.06 (11)
Ca1—Ca2—Ca1^xviii	97.87 (5)	95.20 (5)	100.46 (6)
Ca1—Ca2—Ca1^xix	97.90 (5)	95.20 (5)	100.46 (6)
Ca1—Ca2—Ca1ⁱ	63.56 (5)	61.09 (5)	66.07 (5)
Ca1—Ca2—Ca1ⁱⁱ	63.59 (5)	61.09 (5)	66.07 (5)
Ca1—Ca2—Ca1^xii	155.15 (5)	155.06 (5)	155.25 (5)
Ca1—Ca2—Ca2^xii	93.53 (6)	93.39 (6)	93.67 (6)
Ca1—Ca2—Ca2^v	58.53 (5)	58.45 (5)	58.61 (5)
Ca1—Ca2—Si1^xiii	116.63 (8)	113.76 (8)	119.42 (8)
Ca1—Ca2—Si1^xiv	116.64 (8)	113.76 (8)	119.42 (8)
Ca1—Ca2—Si1^v	134.40 (5)	134.06 (5)	134.74 (5)
Ca1—Ca2—O1^xiv	109.1 (2)	98.2 (2)	119.20 (19)
Ca1—Ca2—O1ⁱ	50.84 (18)	40.44 (16)	61.40 (19)
Ca1—Ca2—O1^vii	51.03 (18)	40.44 (16)	61.40 (19)
Ca1—Ca2—O1^xv	109.1 (2)	98.2 (2)	119.20 (19)
Ca1—Ca2—O2	46.21 (10)	45.54 (10)	47.00 (10)
Ca1—Ca2—O2^xvi	46.22 (10)	45.54 (10)	47.00 (10)
Ca1—Ca2—O3^v	161.45 (8)	159.49 (8)	164.91 (7)
Ca1—Ca2—O3^xvii	161.49 (8)	159.49 (8)	164.91 (7)
Ca1^xviii—Ca2—Ca1^xix	94.71 (5)	94.48 (5)	94.93 (4)
Ca1^xviii—Ca2—Ca1ⁱ	79.99 (5)	76.92 (5)	83.29 (5)
Ca1^xviii—Ca2—Ca1ⁱⁱ	159.32 (6)	158.20 (6)	160.13 (6)
Ca1^xviii—Ca2—Ca1^xii	98.79 (6)	96.30 (6)	101.17 (6)
Ca1^xviii—Ca2—Ca2^xii	130.82 (5)	123.67 (5)	137.88 (5)
Ca1^xviii—Ca2—Ca2^v	60.36 (4)	57.83 (4)	62.69 (4)
Ca1^xviii—Ca2—Si1^xiii	64.01 (5)	60.39 (4)	67.69 (5)
Ca1^xviii—Ca2—Si1^xiv	140.63 (9)	138.61 (9)	142.55 (9)
Ca1^xviii—Ca2—Si1^v	55.34 (6)	52.55 (6)	58.00 (6)
Ca1^xviii—Ca2—O1^xiv	151.15 (19)	139.67 (16)	161.9 (2)
Ca1^xviii—Ca2—O1ⁱ	47.53 (18)	38.90 (19)	56.17 (17)
Ca1^xviii—Ca2—O1^vii	104.53 (10)	98.95 (10)	110.45 (10)
Ca1^xviii—Ca2—O1^xv	89.41 (11)	80.36 (11)	97.92 (11)
Ca1^xviii—Ca2—O2	119.83 (9)	113.06 (9)	122.80 (9)
Ca1^xviii—Ca2—O2^xvi	129.60 (10)	126.76 (10)	135.69 (11)
Ca1^xviii—Ca2—O3^v	64.56 (8)	63.48 (8)	66.55 (8)
Ca1^xviii—Ca2—O3^xvii	80.35 (9)	78.63 (9)	81.30 (9)
Ca1^xix—Ca2—Ca1ⁱ	159.32 (6)	158.20 (6)	160.13 (6)
Ca1^xix—Ca2—Ca1ⁱⁱ	80.01 (5)	76.92 (5)	83.29 (5)
Ca1^xix—Ca2—Ca1^xii	98.75 (6)	96.30 (6)	101.17 (6)
Ca1^xix—Ca2—Ca2^xii	130.75 (5)	123.67 (5)	137.88 (5)
Ca1^xix—Ca2—Ca2^v	60.37 (4)	57.83 (4)	62.69 (4)
Ca1^xix—Ca2—Si1^xiii	140.61 (9)	138.61 (9)	142.55 (9)
Ca1^xix—Ca2—Si1^xiv	63.99 (5)	60.39 (4)	67.69 (5)
Ca1^xix—Ca2—Si1^v	55.32 (6)	52.55 (6)	58.00 (6)
Ca1^xix—Ca2—O1^xiv	89.33 (11)	80.36 (11)	97.92 (11)
Ca1^xix—Ca2—O1ⁱ	104.60 (10)	98.95 (10)	110.45 (10)
Ca1^xix—Ca2—O1^vii	47.37 (18)	38.90 (19)	56.17 (17)
Ca1^xix—Ca2—O1^xv	151.08 (19)	139.67 (16)	161.9 (2)
Ca1^xix—Ca2—O2	129.52 (10)	126.76 (10)	135.69 (11)
Ca1^xix—Ca2—O2^xvi	119.75 (9)	113.06 (9)	122.80 (9)
Ca1^xix—Ca2—O3^v	80.35 (9)	78.63 (9)	81.30 (9)
Ca1^xix—Ca2—O3^xvii	64.56 (8)	63.48 (8)	66.55 (8)
Ca1ⁱ—Ca2—Ca1ⁱⁱ	97.97 (6)	97.97 (6)	97.97 (6)
Ca1ⁱ—Ca2—Ca1^xii	101.67 (5)	99.13 (5)	104.16 (5)
Ca1ⁱ—Ca2—Ca2^xii	63.06 (4)	58.47 (4)	67.61 (4)
Ca1ⁱ—Ca2—Ca2^v	100.31 (6)	96.19 (5)	104.43 (6)
Ca1ⁱ—Ca2—Si1^xiii	53.92 (7)	52.70 (7)	55.20 (7)
Ca1ⁱ—Ca2—Si1^xiv	130.87 (5)	129.73 (5)	131.91 (5)
Ca1ⁱ—Ca2—Si1^v	130.98 (7)	125.32 (7)	136.65 (8)
Ca1ⁱ—Ca2—O1^xiv	104.53 (14)	100.15 (13)	108.90 (14)
Ca1ⁱ—Ca2—O1ⁱ	57.50 (12)	48.44 (11)	66.68 (13)
Ca1ⁱ—Ca2—O1^vii	114.28 (19)	106.23 (18)	121.95 (19)
Ca1ⁱ—Ca2—O1^xv	48.91 (17)	37.17 (18)	60.09 (15)
Ca1ⁱ—Ca2—O2	41.81 (8)	36.65 (8)	44.27 (7)
Ca1ⁱ—Ca2—O2^xvi	56.29 (8)	53.76 (8)	61.38 (8)
Ca1ⁱ—Ca2—O3^v	113.56 (9)	111.93 (9)	117.14 (9)
Ca1ⁱ—Ca2—O3^xvii	133.19 (9)	129.79 (9)	134.75 (9)
Ca1ⁱⁱ—Ca2—Ca1^xii	101.63 (5)	99.13 (5)	104.16 (5)
Ca1ⁱⁱ—Ca2—Ca2^xii	62.99 (4)	58.47 (4)	67.61 (4)
Ca1ⁱⁱ—Ca2—Ca2^v	100.33 (6)	96.19 (5)	104.43 (6)
Ca1ⁱⁱ—Ca2—Si1^xiii	130.85 (5)	129.73 (5)	131.91 (5)
Ca1ⁱⁱ—Ca2—Si1^xiv	53.90 (7)	52.70 (7)	55.20 (7)
Ca1ⁱⁱ—Ca2—Si1^v	130.98 (7)	125.32 (7)	136.65 (8)
Ca1ⁱⁱ—Ca2—O1^xiv	48.83 (17)	37.17 (18)	60.09 (15)
Ca1ⁱⁱ—Ca2—O1ⁱ	114.13 (19)	106.23 (18)	121.95 (19)
Ca1ⁱⁱ—Ca2—O1^vii	57.62 (12)	48.44 (11)	66.68 (13)
Ca1ⁱⁱ—Ca2—O1^xv	104.46 (14)	100.15 (13)	108.90 (14)
Ca1ⁱⁱ—Ca2—O2	56.22 (8)	53.76 (8)	61.38 (8)
Ca1ⁱⁱ—Ca2—O2^xvi	41.74 (8)	36.65 (8)	44.27 (7)
Ca1ⁱⁱ—Ca2—O3^v	133.21 (9)	129.79 (9)	134.75 (9)
Ca1ⁱⁱ—Ca2—O3^xvii	113.58 (9)	111.93 (9)	117.14 (9)
Ca1^xii—Ca2—Ca2^xii	61.63 (5)	61.54 (5)	61.73 (5)
Ca1^xii—Ca2—Ca2^v	145.99 (8)	145.71 (7)	146.26 (8)
Ca1^xii—Ca2—Si1^xiii	56.50 (6)	54.91 (6)	58.10 (6)
Ca1^xii—Ca2—Si1^xiv	56.47 (6)	54.91 (6)	58.10 (6)
Ca1^xii—Ca2—Si1^v	70.10 (6)	69.94 (6)	70.27 (6)
Ca1^xii—Ca2—O1^xiv	52.89 (17)	42.70 (16)	63.69 (18)
Ca1^xii—Ca2—O1ⁱ	139.23 (15)	132.27 (17)	146.53 (14)
Ca1^xii—Ca2—O1^vii	139.09 (15)	132.27 (17)	146.53 (14)
Ca1^xii—Ca2—O1^xv	52.87 (17)	42.70 (16)	63.69 (18)
Ca1^xii—Ca2—O2	109.51 (10)	108.63 (10)	110.07 (10)
Ca1^xii—Ca2—O2^xvi	109.50 (10)	108.63 (10)	110.07 (10)
Ca1^xii—Ca2—O3^v	40.28 (7)	39.47 (7)	41.01 (7)
Ca1^xii—Ca2—O3^xvii	40.27 (7)	39.47 (7)	41.01 (7)
Ca2^xii—Ca2—Ca2^v	151.42 (8)	150.70 (8)	152.13 (8)
Ca2^xii—Ca2—Si1^xiii	68.09 (5)	64.47 (5)	71.54 (5)
Ca2^xii—Ca2—Si1^xiv	68.04 (5)	64.47 (5)	71.54 (5)
Ca2^xii—Ca2—Si1^v	131.30 (8)	130.80 (8)	131.80 (8)
Ca2^xii—Ca2—O1^xiv	42.26 (12)	41.52 (12)	43.38 (11)
Ca2^xii—Ca2—O1ⁱ	119.05 (15)	108.70 (14)	129.90 (16)
Ca2^xii—Ca2—O1^vii	119.13 (15)	108.70 (14)	129.90 (16)
Ca2^xii—Ca2—O1^xv	42.25 (12)	41.52 (12)	43.38 (11)
Ca2^xii—Ca2—O2	48.67 (9)	48.07 (9)	49.43 (9)
Ca2^xii—Ca2—O2^xvi	48.66 (9)	48.07 (9)	49.43 (9)
Ca2^xii—Ca2—O3^v	100.18 (8)	99.60 (8)	101.16 (8)
Ca2^xii—Ca2—O3^xvii	100.18 (8)	99.60 (8)	101.16 (8)
Ca2^v—Ca2—Si1^xiii	121.95 (6)	115.76 (6)	128.07 (6)
Ca2^v—Ca2—Si1^xiv	121.94 (6)	115.76 (6)	128.07 (6)
Ca2^v—Ca2—Si1^v	75.95 (6)	75.74 (6)	76.16 (6)
Ca2^v—Ca2—O1^xiv	142.11 (11)	126.30 (12)	157.27 (10)
Ca2^v—Ca2—O1ⁱ	44.96 (10)	42.57 (9)	48.34 (11)
Ca2^v—Ca2—O1^vii	44.91 (10)	42.57 (9)	48.34 (11)
Ca2^v—Ca2—O1^xv	142.20 (11)	126.30 (12)	157.27 (10)
Ca2^v—Ca2—O2	104.15 (11)	103.43 (11)	104.38 (11)
Ca2^v—Ca2—O2^xvi	104.14 (11)	103.43 (11)	104.38 (11)
Ca2^v—Ca2—O3^v	105.98 (8)	105.21 (8)	107.18 (8)
Ca2^v—Ca2—O3^xvii	105.99 (8)	105.21 (8)	107.18 (8)
Si1^xiii—Ca2—Si1^xiv	110.99 (7)	110.88 (7)	111.11 (7)
Si1^xiii—Ca2—Si1^v	85.99 (8)	81.36 (8)	90.58 (9)
Si1^xiii—Ca2—O1^xiv	95.72 (11)	86.13 (10)	105.80 (12)
Si1^xiii—Ca2—O1ⁱ	85.51 (12)	80.44 (12)	90.52 (12)
Si1^xiii—Ca2—O1^vii	161.78 (14)	157.99 (17)	168.62 (14)
Si1^xiii—Ca2—O1^xv	27.14 (13)	23.25 (15)	30.65 (10)
Si1^xiii—Ca2—O2	87.96 (10)	83.27 (10)	90.24 (10)
Si1^xiii—Ca2—O2^xvi	99.92 (9)	97.80 (9)	104.04 (9)
Si1^xiii—Ca2—O3^v	60.81 (9)	59.41 (9)	64.09 (9)
Si1^xiii—Ca2—O3^xvii	78.56 (10)	75.36 (10)	80.01 (10)
Si1^xiv—Ca2—Si1^v	85.99 (8)	81.36 (8)	90.58 (9)
Si1^xiv—Ca2—O1^xiv	27.08 (13)	23.25 (15)	30.65 (10)
Si1^xiv—Ca2—O1ⁱ	161.72 (14)	157.99 (17)	168.62 (14)
Si1^xiv—Ca2—O1^vii	85.45 (12)	80.44 (12)	90.52 (12)
Si1^xiv—Ca2—O1^xv	95.64 (11)	86.13 (10)	105.80 (12)
Si1^xiv—Ca2—O2	99.86 (9)	97.80 (9)	104.04 (9)
Si1^xiv—Ca2—O2^xvi	87.89 (10)	83.27 (10)	90.24 (10)
Si1^xiv—Ca2—O3^v	78.59 (10)	75.36 (10)	80.01 (10)
Si1^xiv—Ca2—O3^xvii	60.84 (9)	59.41 (9)	64.09 (9)
Si1^v—Ca2—O1^xiv	105.9 (2)	104.06 (19)	107.7 (2)
Si1^v—Ca2—O1ⁱ	97.02 (18)	87.72 (19)	106.50 (17)
Si1^v—Ca2—O1^vii	96.84 (18)	87.72 (19)	106.50 (17)
Si1^v—Ca2—O1^xv	105.9 (2)	104.06 (19)	107.7 (2)
Si1^v—Ca2—O2	175.81 (10)	165.45 (10)	180
Si1^v—Ca2—O2^xvi	175.68 (10)	165.45 (10)	180
Si1^v—Ca2—O3^v	31.45 (7)	30.98 (7)	32.22 (8)
Si1^v—Ca2—O3^xvii	31.46 (7)	30.98 (7)	32.22 (8)
O1^xiv—Ca2—O1ⁱ	154.2 (2)	147.8 (3)	164.8 (3)
O1^xiv—Ca2—O1^vii	98.56 (15)	82.16 (16)	114.72 (14)
O1^xiv—Ca2—O1^xv	74.93 (12)	73.89 (12)	75.96 (12)
O1^xiv—Ca2—O2	75.42 (19)	72.54 (18)	81.52 (19)
O1^xiv—Ca2—O2^xvi	72.4 (2)	63.4 (2)	76.23 (18)
O1^xiv—Ca2—O3^v	83.32 (19)	80.71 (17)	89.5 (2)
O1^xiv—Ca2—O3^xvii	79.3 (2)	74.6 (2)	81.6 (2)
O1ⁱ—Ca2—O1^vii	79.44 (16)	78.10 (16)	80.75 (16)
O1ⁱ—Ca2—O1^xv	98.62 (15)	82.16 (16)	114.72 (14)
O1ⁱ—Ca2—O2	84.69 (19)	74.17 (18)	89.44 (19)
O1ⁱ—Ca2—O2^xvi	81.60 (19)	76.87 (18)	92.3 (2)
O1ⁱ—Ca2—O3^v	110.84 (19)	104.57 (19)	121.67 (18)
O1ⁱ—Ca2—O3^xvii	127.48 (19)	115.98 (19)	135.56 (18)
O1^vii—Ca2—O1^xv	154.4 (2)	147.8 (3)	164.8 (3)
O1^vii—Ca2—O2	81.61 (19)	76.87 (18)	92.3 (2)
O1^vii—Ca2—O2^xvi	84.70 (19)	74.17 (18)	89.44 (19)
O1^vii—Ca2—O3^v	127.33 (19)	115.98 (19)	135.56 (18)
O1^vii—Ca2—O3^xvii	110.72 (19)	104.57 (19)	121.67 (18)
O1^xv—Ca2—O2	72.5 (2)	63.4 (2)	76.23 (18)
O1^xv—Ca2—O2^xvi	75.50 (19)	72.54 (18)	81.52 (19)
O1^xv—Ca2—O3^v	79.4 (2)	74.6 (2)	81.6 (2)
O1^xv—Ca2—O3^xvii	83.37 (19)	80.71 (17)	89.5 (2)
O2—Ca2—O3^v	143.60 (12)	141.47 (12)	145.71 (12)
O2—Ca2—O3^xvii	148.97 (11)	148.61 (11)	149.57 (11)
O2^xvi—Ca2—O3^v	148.97 (11)	148.61 (11)	149.57 (11)
O2^xvi—Ca2—O3^xvii	143.57 (12)	141.47 (12)	145.71 (12)
Ca1—Si1—Ca1ⁱ	74.71 (6)	72.52 (6)	76.94 (6)
Ca1—Si1—Ca1ⁱⁱ	74.74 (6)	72.52 (6)	76.94 (6)
Ca1—Si1—Ca1^xx	99.49 (9)	99.42 (9)	99.55 (9)
Ca1—Si1—Ca2^xxi	118.74 (8)	118.20 (8)	119.26 (8)
Ca1—Si1—Ca2^xxii	118.75 (8)	118.20 (8)	119.26 (8)
Ca1—Si1—Ca2^xii	114.88 (11)	114.80 (11)	114.96 (11)
Ca1—Si1—O1	77.31 (16)	63.27 (16)	90.93 (16)
Ca1—Si1—O1^xvi	77.10 (16)	63.27 (16)	90.93 (16)
Ca1—Si1—O2	57.87 (14)	56.88 (14)	58.93 (13)
Ca1—Si1—O2^xvi	57.89 (14)	56.88 (14)	58.93 (13)
Ca1—Si1—O3	159.8 (2)	157.1 (2)	162.3 (3)
Ca1—Si1—O3^xvi	159.9 (2)	157.1 (2)	162.3 (3)
Ca1ⁱ—Si1—Ca1ⁱⁱ	117.54 (11)	117.52 (11)	117.56 (11)
Ca1ⁱ—Si1—Ca1^xx	118.96 (10)	114.60 (9)	123.23 (10)
Ca1ⁱ—Si1—Ca2^xxi	63.65 (6)	61.14 (6)	66.20 (6)
Ca1ⁱ—Si1—Ca2^xxii	164.73 (8)	163.75 (7)	165.50 (9)
Ca1ⁱ—Si1—Ca2^xii	72.95 (8)	67.73 (7)	78.11 (8)
Ca1ⁱ—Si1—O1	149.91 (18)	139.90 (18)	158.2 (2)
Ca1ⁱ—Si1—O1^xvi	59.3 (3)	46.5 (3)	72.4 (2)
Ca1ⁱ—Si1—O2	46.97 (12)	41.18 (12)	50.19 (12)
Ca1ⁱ—Si1—O2^xvi	70.75 (14)	67.44 (13)	76.47 (14)
Ca1ⁱ—Si1—O3	106.20 (18)	103.44 (18)	110.78 (18)
Ca1ⁱ—Si1—O3^xvi	88.53 (16)	83.99 (15)	91.18 (16)
Ca1ⁱⁱ—Si1—Ca1^xx	118.88 (10)	114.60 (9)	123.23 (10)
Ca1ⁱⁱ—Si1—Ca2^xxi	164.71 (8)	163.75 (7)	165.50 (9)
Ca1ⁱⁱ—Si1—Ca2^xxii	63.60 (6)	61.14 (6)	66.20 (6)
Ca1ⁱⁱ—Si1—Ca2^xii	72.86 (8)	67.73 (7)	78.11 (8)
Ca1ⁱⁱ—Si1—O1	59.5 (3)	46.5 (3)	72.4 (2)
Ca1ⁱⁱ—Si1—O1^xvi	149.76 (18)	139.90 (18)	158.2 (2)
Ca1ⁱⁱ—Si1—O2	70.66 (14)	67.44 (13)	76.47 (14)
Ca1ⁱⁱ—Si1—O2^xvi	46.88 (12)	41.18 (12)	50.19 (12)
Ca1ⁱⁱ—Si1—O3	88.50 (16)	83.99 (15)	91.18 (16)
Ca1ⁱⁱ—Si1—O3^xvi	106.18 (18)	103.44 (18)	110.78 (18)
Ca1^xx—Si1—Ca2^xxi	68.03 (7)	65.67 (7)	70.24 (8)
Ca1^xx—Si1—Ca2^xxii	67.99 (7)	65.67 (7)	70.24 (8)
Ca1^xx—Si1—Ca2^xii	145.10 (6)	144.51 (6)	145.71 (6)
Ca1^xx—Si1—O1	60.3 (3)	42.8 (2)	78.3 (3)
Ca1^xx—Si1—O1^xvi	60.5 (3)	42.8 (2)	78.3 (3)
Ca1^xx—Si1—O2	152.10 (17)	148.51 (17)	155.35 (17)
Ca1^xx—Si1—O2^xvi	152.04 (17)	148.51 (17)	155.35 (17)
Ca1^xx—Si1—O3	97.2 (2)	96.6 (2)	97.4 (2)
Ca1^xx—Si1—O3^xvi	97.2 (2)	96.6 (2)	97.4 (2)
Ca2^xxi—Si1—Ca2^xxii	110.99 (7)	110.88 (7)	111.11 (7)
Ca2^xxi—Si1—Ca2^xii	93.97 (7)	88.97 (7)	98.78 (7)
Ca2^xxi—Si1—O1	127.6 (3)	110.9 (2)	144.4 (3)
Ca2^xxi—Si1—O1^xvi	44.96 (16)	36.35 (17)	55.06 (16)
Ca2^xxi—Si1—O2	108.30 (14)	102.40 (13)	113.29 (15)
Ca2^xxi—Si1—O2^xvi	133.52 (17)	128.65 (16)	139.10 (18)
Ca2^xxi—Si1—O3	77.98 (13)	74.54 (14)	82.05 (13)
Ca2^xxi—Si1—O3^xvi	58.03 (15)	54.02 (15)	61.25 (15)
Ca2^xxii—Si1—Ca2^xii	93.88 (7)	88.97 (7)	98.78 (7)
Ca2^xxii—Si1—O1	44.80 (16)	36.35 (17)	55.06 (16)
Ca2^xxii—Si1—O1^xvi	127.8 (3)	110.9 (2)	144.4 (3)
Ca2^xxii—Si1—O2	133.42 (17)	128.65 (16)	139.10 (18)
Ca2^xxii—Si1—O2^xvi	108.20 (14)	102.40 (13)	113.29 (15)
Ca2^xxii—Si1—O3	58.01 (15)	54.02 (15)	61.25 (15)
Ca2^xxii—Si1—O3^xvi	77.96 (13)	74.54 (14)	82.05 (13)
Ca2^xii—Si1—O1	124.8 (3)	115.4 (3)	135.2 (2)
Ca2^xii—Si1—O1^xvi	124.9 (3)	115.4 (3)	135.2 (2)
Ca2^xii—Si1—O2	58.95 (16)	58.03 (16)	60.02 (17)
Ca2^xii—Si1—O2^xvi	58.93 (16)	58.03 (16)	60.02 (17)
Ca2^xii—Si1—O3	50.4 (2)	49.7 (2)	50.7 (2)
Ca2^xii—Si1—O3^xvi	50.4 (2)	49.7 (2)	50.7 (2)
O1—Si1—O1^xvi	110.1 (4)	108.6 (4)	111.6 (4)
O1—Si1—O2	109.2 (3)	102.7 (3)	121.0 (3)
O1—Si1—O2^xvi	108.6 (3)	97.8 (3)	115.1 (2)
O1—Si1—O3	106.6 (2)	99.7 (2)	110.4 (2)
O1—Si1—O3^xvi	113.6 (2)	109.8 (2)	121.4 (2)
O1^xvi—Si1—O2	108.7 (3)	97.8 (3)	115.1 (2)
O1^xvi—Si1—O2^xvi	109.2 (3)	102.7 (3)	121.0 (3)
O1^xvi—Si1—O3	113.7 (2)	109.8 (2)	121.4 (2)
O1^xvi—Si1—O3^xvi	106.7 (2)	99.7 (2)	110.4 (2)
O2—Si1—O3	109.0 (3)	108.5 (3)	109.2 (3)
O2—Si1—O3^xvi	105.5 (3)	105.4 (3)	105.6 (3)
O2^xvi—Si1—O3	105.5 (3)	105.4 (3)	105.6 (3)
O2^xvi—Si1—O3^xvi	109.0 (3)	108.5 (3)	109.2 (3)
Ca1ⁱⁱ—O1—Ca1^xx	170.04 (18)	162.29 (16)	176.22 (19)
Ca1ⁱⁱ—O1—Ca2^xxii	81.99 (16)	74.64 (15)	88.17 (15)
Ca1ⁱⁱ—O1—Ca2ⁱⁱ	88.05 (14)	77.34 (14)	99.00 (14)
Ca1ⁱⁱ—O1—Si1	90.9 (3)	77.8 (3)	103.4 (4)
Ca1^xx—O1—Ca2^xxii	89.2 (2)	75.84 (15)	103.2 (2)
Ca1^xx—O1—Ca2ⁱⁱ	93.5 (3)	86.5 (2)	100.8 (3)
Ca1^xx—O1—Si1	90.0 (2)	72.6 (2)	107.0 (2)
Ca2^xxii—O1—Ca2ⁱⁱ	92.82 (16)	89.57 (17)	94.95 (15)
Ca2^xxii—O1—Si1	108.1 (2)	94.31 (18)	120.2 (3)
Ca2ⁱⁱ—O1—Si1	150.4 (3)	133.1 (3)	166.8 (3)
Ca1ⁱ—O2—Ca2	96.62 (17)	94.20 (16)	101.68 (19)
Ca1ⁱ—O2—Si1	102.9 (2)	99.7 (2)	108.1 (2)
Ca2—O2—Si1	160.20 (18)	149.97 (17)	165.67 (18)
Ca1^xxiii—O3—Ca2^xii	96.28 (17)	95.29 (17)	97.89 (18)
Ca1^xxiii—O3—Si1	152.9 (3)	152.0 (3)	153.3 (3)
Ca2^xii—O3—Si1	98.2 (2)	97.6 (2)	99.0 (2)

Symmetry codes: (i) −x₁+2, x₂−1/2, −x₃+1, −x₄+1/2; (ii) −x₁+2, x₂+1/2, −x₃+1, −x₄+1/2; (iii) −x₁+5/2, −x₂+1, x₃+1/2, −x₄+1/2; (iv) −x₁+5/2, −x₂+2, x₃+1/2, −x₄+1/2; (v) x₁+1/2, −x₂+3/2, −x₃+1/2, x₄; (vi) x₁+1/2, −x₂+3/2, −x₃+3/2, x₄; (vii) −x₁+2, −x₂+2, −x₃+1, −x₄; (viii) x₁+1/2, x₂, −x₃+3/2, x₄+1/2; (ix) −x₁+2, −x₂+1, −x₃+1, −x₄; (x) x₁+1, x₂, x₃, x₄; (xi) x₁+1, −x₂+3/2, x₃, x₄+1/2; (xii) x₁−1/2, −x₂+3/2, −x₃+1/2, x₄; (xiii) −x₁+3/2, −x₂+1, x₃−1/2, −x₄+1/2; (xiv) −x₁+3/2, −x₂+2, x₃−1/2, −x₄+1/2; (xv) −x₁+3/2, x₂−1/2, x₃−1/2, −x₄; (xvi) x₁, −x₂+3/2, x₃, x₄+1/2; (xvii) x₁+1/2, x₂, −x₃+1/2, x₄+1/2; (xviii) −x₁+5/2, −x₂+1, x₃−1/2, −x₄+1/2; (xix) −x₁+5/2, −x₂+2, x₃−1/2, −x₄+1/2; (xx) x₁−1/2, −x₂+3/2, −x₃+3/2, x₄; (xxi) −x₁+3/2, −x₂+1, x₃+1/2, −x₄+1/2; (xxii) −x₁+3/2, −x₂+2, x₃+1/2, −x₄+1/2; (xxiii) x₁−1, x₂, x₃, x₄.

(2p5K_average_dyn) top

Crystal data top

Ca₈O₁₆Si₄	Z = 1
M_r = 689	F(000) = 344
Orthorhombic, Pnma	D_x = 3.316 Mg m⁻³
Hall symbol: -P -2xabc;-2yb;-2zac	Electron radiation, λ = 0.0197 Å
a = 6.765 Å	µ = 0 mm⁻¹
b = 5.514 Å	T = 293 K
c = 9.25 Å	Nanocrystals of up to 500 nm in size
V = 345.05 Å³

Data collection top

TEM diffractometer	h = −8→8
10062 measured reflections	k = −7→7
1995 independent reflections	l = −11→12
1488 reflections with I > 3σ(I)

Refinement top

Refinement on F	143 parameters
R[F² > 2σ(F²)] = 0.055	0 restraints
wR(F²) = 0.062	0 constraints
S = 2.37	Weighting scheme based on measured s.u.'s w = 1/(σ²(F) + 0.0001F²)
1995 reflections	(Δ/σ)_max = 0.042

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å²) top

	x	y	z	U_iso*/U_eq	Occ. (<1)
Ca1	0.16773 (15)	0.75	0.42906 (13)	0.0256 (5)
Ca2	0.50905 (13)	0.75	0.70488 (13)	0.0172 (4)
Si1	0.28113 (18)	0.25	0.58717 (17)	0.0170 (6)
O1	0.7470 (7)	0.4794 (8)	0.8050 (5)	0.0313 (14)	0.647 (5)
O2	0.4946 (5)	0.770 (4)	0.4509 (4)	0.095 (3)	0.5
O3	0.1579 (4)	0.3184 (9)	0.4389 (4)	0.032 (2)	0.5
O1_2	0.6761 (12)	0.4871 (16)	0.8553 (12)	0.0313 (14)	0.353 (2)

Atomic displacement parameters (Å²) top

	U¹¹	U²²	U³³	U¹²	U¹³	U²³
Ca1	0.0156 (5)	0.0412 (11)	0.0200 (8)	0	0.0016 (5)	0
Ca2	0.0114 (5)	0.0286 (8)	0.0117 (6)	0	−0.0009 (4)	0
Si1	0.0146 (7)	0.0258 (13)	0.0106 (10)	0	−0.0008 (6)	0
O1	0.030 (2)	0.0249 (19)	0.039 (3)	−0.0082 (18)	−0.0135 (17)	0.0129 (19)
O2	0.0247 (17)	0.239 (10)	0.020 (2)	0.067 (6)	0.0038 (14)	0.007 (7)
O3	0.0181 (13)	0.060 (6)	0.018 (2)	0.0032 (17)	−0.0090 (12)	−0.0079 (17)
O1_2	0.030 (2)	0.0249 (19)	0.039 (3)	−0.0082 (18)	−0.0135 (17)	0.0129 (19)

Geometric parameters (Å, º) top

Ca1—Ca1ⁱ	3.8044 (10)	Ca2—O1	2.382 (5)
Ca1—Ca1ⁱⁱ	3.8044 (10)	Ca2—O1^vii	2.319 (5)
Ca1—Ca2	3.4411 (15)	Ca2—O1^xi	2.319 (5)
Ca1—Ca2ⁱⁱⁱ	3.6512 (11)	Ca2—O1^ix	2.382 (5)
Ca1—Ca2^iv	3.6512 (11)	Ca2—O2	2.354 (4)
Ca1—Ca2^v	3.7306 (10)	Ca2—O2^ix	2.354 (4)
Ca1—Ca2^vi	3.7306 (10)	Ca2—O1_2	2.305 (10)
Ca1—Ca2^vii	3.5521 (17)	Ca2—O1_2^ix	2.305 (10)
Ca1—Si1	3.2138 (10)	Si1—O1^xii	1.627 (5)
Ca1—Si1^viii	3.2138 (10)	Si1—O1^xi	1.627 (5)
Ca1—Si1ⁱⁱⁱ	3.181 (2)	Si1—O2^v	1.561 (4)
Ca1—Si1ⁱⁱ	3.0402 (16)	Si1—O2^xiii	1.561 (4)
Ca1—O2	2.223 (4)	Si1—O3	1.649 (4)
Ca1—O2^ix	2.223 (4)	Si1—O3^xiv	1.649 (4)
Ca1—O3	2.383 (5)	Si1—O1_2^xii	1.580 (9)
Ca1—O3^ix	2.383 (5)	Si1—O1_2^xi	1.580 (9)
Ca2—Ca2^vii	3.4840 (13)	O1—O1_2	0.670 (11)
Ca2—Ca2^x	3.4840 (13)	O2—O2^ix	0.22 (3)
Ca2—Si1^vi	3.0517 (19)	O3—O3^xiv	0.754 (7)

Ca1ⁱ—Ca1—Ca1ⁱⁱ	92.89 (3)	Ca1^v—Ca2—O1_2	56.5 (3)
Ca1ⁱ—Ca1—Ca2	98.31 (3)	Ca1^v—Ca2—O1_2^ix	112.2 (2)
Ca1ⁱ—Ca1—Ca2ⁱⁱⁱ	56.86 (2)	Ca1^vi—Ca2—Ca1^x	98.02 (3)
Ca1ⁱ—Ca1—Ca2^iv	123.21 (3)	Ca1^vi—Ca2—Ca2^vii	130.438 (18)
Ca1ⁱ—Ca1—Ca2^v	85.908 (16)	Ca1^vi—Ca2—Ca2^x	60.69 (2)
Ca1ⁱ—Ca1—Ca2^vi	178.75 (3)	Ca1^vi—Ca2—Si1^vi	55.49 (2)
Ca1ⁱ—Ca1—Ca2^vii	59.40 (2)	Ca1^vi—Ca2—O1	101.30 (11)
Ca1ⁱ—Ca1—Si1	50.49 (3)	Ca1^vi—Ca2—O1^vii	87.68 (11)
Ca1ⁱ—Ca1—Si1^viii	127.38 (5)	Ca1^vi—Ca2—O1^xi	155.58 (12)
Ca1ⁱ—Ca1—Si1ⁱⁱⁱ	114.07 (3)	Ca1^vi—Ca2—O1^ix	43.13 (11)
Ca1ⁱ—Ca1—Si1ⁱⁱ	54.64 (2)	Ca1^vi—Ca2—O2	70.0 (4)
Ca1ⁱ—Ca1—O2	126.7 (5)	Ca1^vi—Ca2—O2^ix	74.2 (4)
Ca1ⁱ—Ca1—O2^ix	121.7 (5)	Ca1^vi—Ca2—O1_2	112.2 (2)
Ca1ⁱ—Ca1—O3	41.09 (7)	Ca1^vi—Ca2—O1_2^ix	56.5 (3)
Ca1ⁱ—Ca1—O3^ix	133.95 (8)	Ca1^x—Ca2—Ca2^vii	93.73 (4)
Ca1ⁱⁱ—Ca1—Ca2	98.31 (3)	Ca1^x—Ca2—Ca2^x	58.55 (3)
Ca1ⁱⁱ—Ca1—Ca2ⁱⁱⁱ	123.21 (3)	Ca1^x—Ca2—Si1^vi	134.69 (4)
Ca1ⁱⁱ—Ca1—Ca2^iv	56.86 (2)	Ca1^x—Ca2—O1	54.92 (11)
Ca1ⁱⁱ—Ca1—Ca2^v	178.75 (3)	Ca1^x—Ca2—O1^vii	105.58 (12)
Ca1ⁱⁱ—Ca1—Ca2^vi	85.908 (16)	Ca1^x—Ca2—O1^xi	105.58 (12)
Ca1ⁱⁱ—Ca1—Ca2^vii	59.40 (2)	Ca1^x—Ca2—O1^ix	54.92 (11)
Ca1ⁱⁱ—Ca1—Si1	127.38 (5)	Ca1^x—Ca2—O2	164.56 (13)
Ca1ⁱⁱ—Ca1—Si1^viii	50.49 (3)	Ca1^x—Ca2—O2^ix	164.56 (13)
Ca1ⁱⁱ—Ca1—Si1ⁱⁱⁱ	114.07 (3)	Ca1^x—Ca2—O1_2	43.7 (3)
Ca1ⁱⁱ—Ca1—Si1ⁱⁱ	54.64 (2)	Ca1^x—Ca2—O1_2^ix	43.7 (3)
Ca1ⁱⁱ—Ca1—O2	121.7 (5)	Ca2^vii—Ca2—Ca2^x	152.28 (5)
Ca1ⁱⁱ—Ca1—O2^ix	126.7 (5)	Ca2^vii—Ca2—Si1^vi	131.58 (5)
Ca1ⁱⁱ—Ca1—O3	133.95 (8)	Ca2^vii—Ca2—O1	124.26 (12)
Ca1ⁱⁱ—Ca1—O3^ix	41.09 (7)	Ca2^vii—Ca2—O1^vii	42.88 (11)
Ca2—Ca1—Ca2ⁱⁱⁱ	129.857 (19)	Ca2^vii—Ca2—O1^xi	42.88 (11)
Ca2—Ca1—Ca2^iv	129.857 (19)	Ca2^vii—Ca2—O1^ix	124.26 (12)
Ca2—Ca1—Ca2^v	81.54 (3)	Ca2^vii—Ca2—O2	101.47 (9)
Ca2—Ca1—Ca2^vi	81.54 (3)	Ca2^vii—Ca2—O2^ix	101.47 (9)
Ca2—Ca1—Ca2^vii	59.74 (3)	Ca2^vii—Ca2—O1_2	109.3 (2)
Ca2—Ca1—Si1	60.16 (3)	Ca2^vii—Ca2—O1_2^ix	109.3 (2)
Ca2—Ca1—Si1^viii	60.16 (3)	Ca2^x—Ca2—Si1^vi	76.14 (4)
Ca2—Ca1—Si1ⁱⁱⁱ	131.61 (4)	Ca2^x—Ca2—O1	41.48 (11)
Ca2—Ca1—Si1ⁱⁱ	134.98 (5)	Ca2^x—Ca2—O1^vii	138.73 (11)
Ca2—Ca1—O2	42.71 (10)	Ca2^x—Ca2—O1^xi	138.73 (11)
Ca2—Ca1—O2^ix	42.71 (10)	Ca2^x—Ca2—O1^ix	41.48 (11)
Ca2—Ca1—O3	89.45 (8)	Ca2^x—Ca2—O2	106.23 (9)
Ca2—Ca1—O3^ix	89.45 (8)	Ca2^x—Ca2—O2^ix	106.23 (9)
Ca2ⁱⁱⁱ—Ca1—Ca2^iv	98.07 (3)	Ca2^x—Ca2—O1_2	51.6 (2)
Ca2ⁱⁱⁱ—Ca1—Ca2^v	56.31 (2)	Ca2^x—Ca2—O1_2^ix	51.6 (2)
Ca2ⁱⁱⁱ—Ca1—Ca2^vi	124.15 (4)	Si1^vi—Ca2—O1	91.71 (12)
Ca2ⁱⁱⁱ—Ca1—Ca2^vii	116.26 (3)	Si1^vi—Ca2—O1^vii	108.71 (12)
Ca2ⁱⁱⁱ—Ca1—Si1	71.87 (3)	Si1^vi—Ca2—O1^xi	108.71 (12)
Ca2ⁱⁱⁱ—Ca1—Si1^viii	169.87 (4)	Si1^vi—Ca2—O1^ix	91.71 (12)
Ca2ⁱⁱⁱ—Ca1—Si1ⁱⁱⁱ	58.07 (3)	Si1^vi—Ca2—O2	30.21 (10)
Ca2ⁱⁱⁱ—Ca1—Si1ⁱⁱ	69.20 (3)	Si1^vi—Ca2—O2^ix	30.21 (10)
Ca2ⁱⁱⁱ—Ca1—O2	114.5 (5)	Si1^vi—Ca2—O1_2	107.8 (2)
Ca2ⁱⁱⁱ—Ca1—O2^ix	109.9 (5)	Si1^vi—Ca2—O1_2^ix	107.8 (2)
Ca2ⁱⁱⁱ—Ca1—O3	42.12 (9)	O1—Ca2—O1^vii	159.21 (17)
Ca2ⁱⁱⁱ—Ca1—O3^ix	140.07 (9)	O1—Ca2—O1^xi	97.41 (16)
Ca2^iv—Ca1—Ca2^v	124.15 (4)	O1—Ca2—O1^ix	77.56 (16)
Ca2^iv—Ca1—Ca2^vi	56.31 (2)	O1—Ca2—O2	116.4 (4)
Ca2^iv—Ca1—Ca2^vii	116.26 (3)	O1—Ca2—O2^ix	112.7 (4)
Ca2^iv—Ca1—Si1	169.87 (4)	O1—Ca2—O1_2	16.3 (3)
Ca2^iv—Ca1—Si1^viii	71.87 (3)	O1—Ca2—O1_2^ix	80.1 (2)
Ca2^iv—Ca1—Si1ⁱⁱⁱ	58.07 (3)	O1^vii—Ca2—O1^xi	80.10 (16)
Ca2^iv—Ca1—Si1ⁱⁱ	69.20 (3)	O1^vii—Ca2—O1^ix	97.41 (16)
Ca2^iv—Ca1—O2	109.9 (5)	O1^vii—Ca2—O2	84.2 (4)
Ca2^iv—Ca1—O2^ix	114.5 (5)	O1^vii—Ca2—O2^ix	87.7 (4)
Ca2^iv—Ca1—O3	140.07 (9)	O1^vii—Ca2—O1_2	143.4 (3)
Ca2^iv—Ca1—O3^ix	42.12 (9)	O1^vii—Ca2—O1_2^ix	89.7 (2)
Ca2^v—Ca1—Ca2^vi	95.30 (3)	O1^xi—Ca2—O1^ix	159.21 (17)
Ca2^v—Ca1—Ca2^vii	119.58 (3)	O1^xi—Ca2—O2	87.7 (4)
Ca2^v—Ca1—Si1	51.48 (3)	O1^xi—Ca2—O2^ix	84.2 (4)
Ca2^v—Ca1—Si1^viii	130.18 (4)	O1^xi—Ca2—O1_2	89.7 (2)
Ca2^v—Ca1—Si1ⁱⁱⁱ	66.80 (3)	O1^xi—Ca2—O1_2^ix	143.4 (3)
Ca2^v—Ca1—Si1ⁱⁱ	124.68 (3)	O1^ix—Ca2—O2	112.7 (4)
Ca2^v—Ca1—O2	58.9 (5)	O1^ix—Ca2—O2^ix	116.4 (4)
Ca2^v—Ca1—O2^ix	53.9 (5)	O1^ix—Ca2—O1_2	80.1 (2)
Ca2^v—Ca1—O3	44.83 (7)	O1^ix—Ca2—O1_2^ix	16.3 (3)
Ca2^v—Ca1—O3^ix	140.11 (8)	O2—Ca2—O2^ix	5.4 (8)
Ca2^vi—Ca1—Ca2^vii	119.58 (3)	O2—Ca2—O1_2	130.7 (5)
Ca2^vi—Ca1—Si1	130.18 (4)	O2—Ca2—O1_2^ix	126.4 (5)
Ca2^vi—Ca1—Si1^viii	51.48 (3)	O2^ix—Ca2—O1_2	126.4 (5)
Ca2^vi—Ca1—Si1ⁱⁱⁱ	66.80 (3)	O2^ix—Ca2—O1_2^ix	130.7 (5)
Ca2^vi—Ca1—Si1ⁱⁱ	124.68 (3)	O1_2—Ca2—O1_2^ix	77.9 (3)
Ca2^vi—Ca1—O2	53.9 (5)	Ca1^xvii—Si1—Ca1	118.15 (5)
Ca2^vi—Ca1—O2^ix	58.9 (5)	Ca1^xvii—Si1—Ca1^xv	118.58 (3)
Ca2^vi—Ca1—O3	140.11 (8)	Ca1^xvii—Si1—Ca1ⁱ	74.88 (3)
Ca2^vi—Ca1—O3^ix	44.83 (7)	Ca1^xvii—Si1—Ca2^v	73.03 (4)
Ca2^vii—Ca1—Si1	68.80 (3)	Ca1^xvii—Si1—O1^xii	65.05 (16)
Ca2^vii—Ca1—Si1^viii	68.80 (3)	Ca1^xvii—Si1—O1^xi	155.77 (18)
Ca2^vii—Ca1—Si1ⁱⁱⁱ	168.65 (4)	Ca1^xvii—Si1—O2^v	100.9 (7)
Ca2^vii—Ca1—Si1ⁱⁱ	75.24 (4)	Ca1^xvii—Si1—O2^xiii	93.9 (7)
Ca2^vii—Ca1—O2	102.35 (10)	Ca1^xvii—Si1—O3	72.36 (17)
Ca2^vii—Ca1—O2^ix	102.35 (10)	Ca1^xvii—Si1—O3^xiv	45.93 (17)
Ca2^vii—Ca1—O3	87.43 (9)	Ca1^xvii—Si1—O1_2^xii	48.4 (4)
Ca2^vii—Ca1—O3^ix	87.43 (9)	Ca1^xvii—Si1—O1_2^xi	139.1 (3)
Si1—Ca1—Si1^viii	118.15 (5)	Ca1—Si1—Ca1^xv	118.58 (3)
Si1—Ca1—Si1ⁱⁱⁱ	115.24 (3)	Ca1—Si1—Ca1ⁱ	74.88 (3)
Si1—Ca1—Si1ⁱⁱ	105.12 (3)	Ca1—Si1—Ca2^v	73.03 (4)
Si1—Ca1—O2	76.3 (5)	Ca1—Si1—O1^xii	155.77 (18)
Si1—Ca1—O2^ix	71.3 (5)	Ca1—Si1—O1^xi	65.05 (16)
Si1—Ca1—O3	29.82 (9)	Ca1—Si1—O2^v	93.9 (7)
Si1—Ca1—O3^ix	147.80 (10)	Ca1—Si1—O2^xiii	100.9 (7)
Si1^viii—Ca1—Si1ⁱⁱⁱ	115.24 (3)	Ca1—Si1—O3	45.93 (17)
Si1^viii—Ca1—Si1ⁱⁱ	105.12 (3)	Ca1—Si1—O3^xiv	72.36 (17)
Si1^viii—Ca1—O2	71.3 (5)	Ca1—Si1—O1_2^xii	139.1 (3)
Si1^viii—Ca1—O2^ix	76.3 (5)	Ca1—Si1—O1_2^xi	48.4 (4)
Si1^viii—Ca1—O3	147.80 (10)	Ca1^xv—Si1—Ca1ⁱ	99.07 (5)
Si1^viii—Ca1—O3^ix	29.82 (9)	Ca1^xv—Si1—Ca2^v	146.04 (5)
Si1ⁱⁱⁱ—Ca1—Si1ⁱⁱ	93.41 (5)	Ca1^xv—Si1—O1^xii	53.57 (17)
Si1ⁱⁱⁱ—Ca1—O2	88.98 (10)	Ca1^xv—Si1—O1^xi	53.57 (17)
Si1ⁱⁱⁱ—Ca1—O2^ix	88.98 (10)	Ca1^xv—Si1—O2^v	96.81 (15)
Si1ⁱⁱⁱ—Ca1—O3	92.35 (9)	Ca1^xv—Si1—O2^xiii	96.81 (15)
Si1ⁱⁱⁱ—Ca1—O3^ix	92.35 (9)	Ca1^xv—Si1—O3	151.87 (14)
Si1ⁱⁱ—Ca1—O2	176.3 (4)	Ca1^xv—Si1—O3^xiv	151.87 (14)
Si1ⁱⁱ—Ca1—O2^ix	176.3 (4)	Ca1^xv—Si1—O1_2^xii	73.4 (4)
Si1ⁱⁱ—Ca1—O3	88.51 (7)	Ca1^xv—Si1—O1_2^xi	73.4 (4)
Si1ⁱⁱ—Ca1—O3^ix	88.51 (7)	Ca1ⁱ—Si1—Ca2^v	114.89 (6)
O2—Ca1—O2^ix	5.7 (8)	Ca1ⁱ—Si1—O1^xii	83.60 (17)
O2—Ca1—O3	94.2 (6)	Ca1ⁱ—Si1—O1^xi	83.60 (17)
O2—Ca1—O3^ix	88.6 (6)	Ca1ⁱ—Si1—O2^v	163.6 (2)
O2^ix—Ca1—O3	88.6 (6)	Ca1ⁱ—Si1—O2^xiii	163.6 (2)
O2^ix—Ca1—O3^ix	94.2 (6)	Ca1ⁱ—Si1—O3	56.90 (11)
O3—Ca1—O3^ix	174.58 (13)	Ca1ⁱ—Si1—O3^xiv	56.90 (11)
Ca1—Ca2—Ca1^xv	101.61 (3)	Ca1ⁱ—Si1—O1_2^xii	64.4 (3)
Ca1—Ca2—Ca1^xvi	101.61 (3)	Ca1ⁱ—Si1—O1_2^xi	64.4 (3)
Ca1—Ca2—Ca1^v	98.46 (3)	Ca2^v—Si1—O1^xii	127.49 (17)
Ca1—Ca2—Ca1^vi	98.46 (3)	Ca2^v—Si1—O1^xi	127.49 (17)
Ca1—Ca2—Ca1^x	155.44 (4)	Ca2^v—Si1—O2^v	49.34 (15)
Ca1—Ca2—Ca2^vii	61.72 (3)	Ca2^v—Si1—O2^xiii	49.34 (15)
Ca1—Ca2—Ca2^x	146.01 (4)	Ca2^v—Si1—O3	59.92 (12)
Ca1—Ca2—Si1^vi	69.86 (4)	Ca2^v—Si1—O3^xiv	59.92 (12)
Ca1—Ca2—O1	137.87 (11)	Ca2^v—Si1—O1_2^xii	120.5 (4)
Ca1—Ca2—O1^vii	57.17 (12)	Ca2^v—Si1—O1_2^xi	120.5 (4)
Ca1—Ca2—O1^xi	57.17 (12)	O1^xii—Si1—O1^xi	102.0 (2)
Ca1—Ca2—O1^ix	137.87 (11)	O1^xii—Si1—O2^v	109.3 (7)
Ca1—Ca2—O2	39.84 (9)	O1^xii—Si1—O2^xiii	102.8 (7)
Ca1—Ca2—O2^ix	39.84 (9)	O1^xii—Si1—O3	128.0 (2)
Ca1—Ca2—O1_2	140.9 (2)	O1^xii—Si1—O3^xiv	105.1 (2)
Ca1—Ca2—O1_2^ix	140.9 (2)	O1^xii—Si1—O1_2^xii	24.0 (4)
Ca1^xv—Ca2—Ca1^xvi	98.07 (3)	O1^xii—Si1—O1_2^xi	111.9 (4)
Ca1^xv—Ca2—Ca1^v	79.78 (2)	O1^xi—Si1—O2^v	102.8 (7)
Ca1^xv—Ca2—Ca1^vi	159.82 (4)	O1^xi—Si1—O2^xiii	109.3 (7)
Ca1^xv—Ca2—Ca1^x	63.74 (3)	O1^xi—Si1—O3	105.1 (2)
Ca1^xv—Ca2—Ca2^vii	62.99 (2)	O1^xi—Si1—O3^xiv	128.0 (2)
Ca1^xv—Ca2—Ca2^x	100.48 (3)	O1^xi—Si1—O1_2^xii	111.9 (4)
Ca1^xv—Ca2—Si1^vi	130.93 (2)	O1^xi—Si1—O1_2^xi	24.0 (4)
Ca1^xv—Ca2—O1	61.81 (11)	O2^v—Si1—O2^xiii	8.1 (11)
Ca1^xv—Ca2—O1^vii	104.94 (12)	O2^v—Si1—O3	106.7 (3)
Ca1^xv—Ca2—O1^xi	44.45 (12)	O2^v—Si1—O3^xiv	108.7 (3)
Ca1^xv—Ca2—O1^ix	118.26 (12)	O2^v—Si1—O1_2^xii	124.8 (8)
Ca1^xv—Ca2—O2	126.1 (5)	O2^v—Si1—O1_2^xi	117.0 (8)
Ca1^xv—Ca2—O2^ix	121.2 (5)	O2^xiii—Si1—O3	108.7 (3)
Ca1^xv—Ca2—O1_2	48.9 (2)	O2^xiii—Si1—O3^xiv	106.7 (3)
Ca1^xv—Ca2—O1_2^ix	107.0 (3)	O2^xiii—Si1—O1_2^xii	117.0 (8)
Ca1^xvi—Ca2—Ca1^v	159.82 (4)	O2^xiii—Si1—O1_2^xi	124.8 (8)
Ca1^xvi—Ca2—Ca1^vi	79.78 (2)	O3—Si1—O3^xiv	26.4 (2)
Ca1^xvi—Ca2—Ca1^x	63.74 (3)	O3—Si1—O1_2^xii	104.0 (4)
Ca1^xvi—Ca2—Ca2^vii	62.99 (2)	O3—Si1—O1_2^xi	82.2 (4)
Ca1^xvi—Ca2—Ca2^x	100.48 (3)	O3^xiv—Si1—O1_2^xii	82.2 (4)
Ca1^xvi—Ca2—Si1^vi	130.93 (2)	O3^xiv—Si1—O1_2^xi	104.0 (4)
Ca1^xvi—Ca2—O1	118.26 (12)	O1_2^xii—Si1—O1_2^xi	111.6 (5)
Ca1^xvi—Ca2—O1^vii	44.45 (12)	Ca2—O1—Ca2^x	95.64 (16)
Ca1^xvi—Ca2—O1^xi	104.94 (12)	Ca2—O1—Si1^xviii	145.2 (3)
Ca1^xvi—Ca2—O1^ix	61.81 (11)	Ca2—O1—O1_2	75.3 (9)
Ca1^xvi—Ca2—O2	121.2 (5)	Ca2^x—O1—Si1^xviii	114.6 (2)
Ca1^xvi—Ca2—O2^ix	126.1 (5)	Ca2^x—O1—O1_2	122.3 (9)
Ca1^xvi—Ca2—O1_2	107.0 (3)	Si1^xviii—O1—O1_2	74.0 (9)
Ca1^xvi—Ca2—O1_2^ix	48.9 (2)	Ca1—O2—Ca2	97.45 (15)
Ca1^v—Ca2—Ca1^vi	95.30 (3)	Ca1—O2—Si1^vi	160.5 (5)
Ca1^v—Ca2—Ca1^x	98.02 (3)	Ca1—O2—O2^ix	87.2 (14)
Ca1^v—Ca2—Ca2^vii	130.438 (18)	Ca2—O2—Si1^vi	100.5 (2)
Ca1^v—Ca2—Ca2^x	60.69 (2)	Ca2—O2—O2^ix	87.3 (15)
Ca1^v—Ca2—Si1^vi	55.49 (2)	Si1^vi—O2—O2^ix	85.9 (15)
Ca1^v—Ca2—O1	43.13 (11)	Ca1—O3—Si1	104.3 (2)
Ca1^v—Ca2—O1^vii	155.58 (12)	Ca1—O3—O3^xiv	177.3 (4)
Ca1^v—Ca2—O1^xi	87.68 (11)	Si1—O3—O3^xiv	76.8 (4)
Ca1^v—Ca2—O1^ix	101.30 (11)	Ca2—O1_2—Si1^xviii	160.7 (6)
Ca1^v—Ca2—O2	74.2 (4)	Ca2—O1_2—O1	88.4 (10)
Ca1^v—Ca2—O2^ix	70.0 (4)	Si1^xviii—O1_2—O1	81.9 (9)

Symmetry codes: (i) −x, y−1/2, −z+1; (ii) −x, y+1/2, −z+1; (iii) −x+1/2, −y+1, z−1/2; (iv) −x+1/2, −y+2, z−1/2; (v) −x+1, y−1/2, −z+1; (vi) −x+1, y+1/2, −z+1; (vii) x−1/2, −y+3/2, −z+3/2; (viii) x, y+1, z; (ix) x, −y+3/2, z; (x) x+1/2, −y+3/2, −z+3/2; (xi) x−1/2, y, −z+3/2; (xii) x−1/2, −y+1/2, −z+3/2; (xiii) −x+1, −y+1, −z+1; (xiv) x, −y+1/2, z; (xv) −x+1/2, −y+1, z+1/2; (xvi) −x+1/2, −y+2, z+1/2; (xvii) x, y−1, z; (xviii) x+1/2, −y+1/2, −z+3/2.

(2p5K_modulated_dyn) top

Crystal data top

Ca₈O₁₆Si₄	Z = 1
M_r = 689	F(000) = 344
Orthorhombic, Pnma(α00)0ss†	D_x = 3.316 Mg m⁻³
q = 0.379500a*	Electron radiation, λ = 0.0197 Å
a = 6.765 Å	µ = 0 mm⁻¹
b = 5.514 Å	T = 293 K
c = 9.25 Å	Nanocrystals of up to 500 nm in size
V = 345.05 Å³

Data collection top

TEM diffractometer	θ_max = 0.8°, θ_min = 0.1°
18230 measured reflections	h = −8→8
6997 independent reflections	k = −7→7
3076 reflections with I > 3σ(I)	l = −11→12

Refinement top

Refinement on F	129 parameters
R[F² > 2σ(F²)] = 0.096	0 restraints
wR(F²) = 0.105	0 constraints
S = 2.22	Weighting scheme based on measured s.u.'s w = 1/(σ²(F) + 0.0001F²)
6997 reflections	(Δ/σ)_max = 0.025

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å²) top

	x	y	z	U_iso*/U_eq	Occ. (<1)
Ca1	0.49106 (12)	0.75	0.20467 (11)	0.0091 (2)*
Ca2	0.83234 (13)	0.75	−0.07067 (11)	0.0169 (3)*
Si1	0.21886 (16)	0.25	0.41267 (15)	0.0101 (3)*
O1	0.2760 (3)	0.4818 (4)	0.3217 (2)	0.0278 (5)*
O2	0.6575 (3)	0.8153 (5)	0.4402 (3)	0.0261 (6)*	0.5
O3	0.5086 (3)	0.8056 (5)	−0.0482 (3)	0.0270 (7)*	0.5

Geometric parameters (Å, º) top

	Average	Minimum	Maximum
Ca1—Ca1ⁱ	3.4900 (11)	3.4849 (11)	3.4952 (11)
Ca1—Ca1ⁱⁱ	3.4901 (11)	3.4849 (11)	3.4952 (11)
Ca1—Ca2	3.4394 (13)	3.4375 (13)	3.4412 (13)
Ca1—Ca2ⁱⁱⁱ	3.654 (2)	3.637 (2)	3.670 (2)
Ca1—Ca2^iv	3.653 (2)	3.637 (2)	3.670 (2)
Ca1—Ca2^v	3.734 (2)	3.549 (2)	3.922 (2)
Ca1—Ca2^vi	3.733 (2)	3.549 (2)	3.922 (2)
Ca1—Ca2ⁱ	3.5531 (14)	3.5517 (14)	3.5545 (14)
Ca1—Si1^vii	3.0568 (16)	3.0515 (16)	3.0622 (16)
Ca1—Si1^viii	3.342 (3)	3.195 (3)	3.487 (3)
Ca1—Si1ⁱⁱ	3.339 (3)	3.195 (3)	3.487 (3)
Ca1—O1	2.357 (4)	2.318 (4)	2.420 (4)
Ca1—O1ⁱⁱ	2.464 (4)	2.359 (4)	2.595 (4)
Ca1—O1^ix	2.463 (4)	2.359 (4)	2.595 (4)
Ca1—O1^x	2.357 (4)	2.318 (4)	2.420 (4)
Ca1—O3	2.377 (3)	2.358 (3)	2.388 (3)
Ca1—O3^x	2.377 (3)	2.358 (3)	2.388 (3)
Ca2—Ca2^xi	3.804 (2)	3.688 (2)	3.920 (2)
Ca2—Ca2^xii	3.802 (2)	3.688 (2)	3.920 (2)
Ca2—Si1^xiii	3.0413 (14)	3.0401 (14)	3.0425 (14)
Ca2—Si1^vi	3.1844 (17)	3.1824 (17)	3.1864 (17)
Ca2—Si1^viii	3.214 (3)	3.181 (3)	3.246 (3)
Ca2—Si1ⁱⁱ	3.213 (3)	3.181 (3)	3.246 (3)
Ca2—O1^vi	2.755 (4)	2.340 (4)	3.173 (4)
Ca2—O1ⁱⁱ	2.767 (4)	2.415 (4)	3.130 (4)
Ca2—O1^xiv	2.752 (4)	2.340 (4)	3.173 (4)
Ca2—O1^ix	2.771 (4)	2.415 (4)	3.130 (4)
Ca2—O2^xv	2.481 (4)	2.309 (4)	2.559 (4)
Ca2—O2^xvi	2.479 (4)	2.309 (4)	2.559 (4)
Ca2—O3	2.228 (2)	2.206 (2)	2.249 (2)
Ca2—O3^x	2.228 (2)	2.206 (2)	2.249 (2)
Si1—O1	1.606 (5)	1.579 (5)	1.638 (5)
Si1—O1^xvii	1.606 (5)	1.579 (5)	1.638 (5)
Si1—O2^xviii	1.627 (3)	1.613 (3)	1.663 (3)
Si1—O2^xix	1.628 (3)	1.613 (3)	1.663 (3)
Si1—O3^xx	1.609 (2)	1.590 (3)	1.641 (3)
Si1—O3^xxi	1.609 (2)	1.590 (3)	1.641 (3)

Ca1ⁱ—Ca1—Ca1ⁱⁱ	151.70 (4)	151.24 (4)	152.18 (4)
Ca1ⁱ—Ca1—Ca2	145.96 (4)	145.77 (4)	146.15 (4)
Ca1ⁱ—Ca1—Ca2ⁱⁱⁱ	100.39 (4)	97.05 (4)	103.73 (4)
Ca1ⁱ—Ca1—Ca2^iv	100.40 (4)	97.05 (4)	103.73 (4)
Ca1ⁱ—Ca1—Ca2^v	60.65 (4)	58.48 (4)	62.70 (4)
Ca1ⁱ—Ca1—Ca2^vi	60.66 (4)	58.48 (4)	62.70 (4)
Ca1ⁱ—Ca1—Ca2ⁱ	58.45 (3)	58.40 (3)	58.50 (3)
Ca1ⁱ—Ca1—Si1^vii	76.05 (3)	75.91 (3)	76.19 (3)
Ca1ⁱ—Ca1—Si1^viii	121.75 (6)	117.02 (6)	126.47 (6)
Ca1ⁱ—Ca1—Si1ⁱⁱ	121.79 (6)	117.02 (6)	126.47 (6)
Ca1ⁱ—Ca1—O1	44.82 (10)	42.43 (10)	48.02 (10)
Ca1ⁱ—Ca1—O1ⁱⁱ	142.03 (12)	128.52 (11)	154.78 (11)
Ca1ⁱ—Ca1—O1^ix	141.85 (12)	128.52 (11)	154.78 (11)
Ca1ⁱ—Ca1—O1^x	44.86 (10)	42.43 (10)	48.02 (10)
Ca1ⁱ—Ca1—O3	106.16 (6)	105.61 (6)	107.06 (6)
Ca1ⁱ—Ca1—O3^x	106.16 (6)	105.61 (6)	107.06 (6)
Ca1ⁱⁱ—Ca1—Ca2	61.69 (3)	61.63 (3)	61.75 (3)
Ca1ⁱⁱ—Ca1—Ca2ⁱⁱⁱ	62.95 (4)	59.38 (4)	66.62 (4)
Ca1ⁱⁱ—Ca1—Ca2^iv	63.02 (4)	59.38 (4)	66.62 (4)
Ca1ⁱⁱ—Ca1—Ca2^v	130.47 (6)	124.97 (6)	136.03 (6)
Ca1ⁱⁱ—Ca1—Ca2^vi	130.56 (6)	124.97 (6)	136.03 (6)
Ca1ⁱⁱ—Ca1—Ca2ⁱ	93.68 (3)	93.59 (3)	93.76 (3)
Ca1ⁱⁱ—Ca1—Si1^vii	131.39 (4)	131.07 (4)	131.70 (4)
Ca1ⁱⁱ—Ca1—Si1^viii	68.24 (4)	65.30 (4)	71.17 (4)
Ca1ⁱⁱ—Ca1—Si1ⁱⁱ	68.30 (4)	65.30 (4)	71.17 (4)
Ca1ⁱⁱ—Ca1—O1	119.23 (11)	110.32 (10)	128.31 (11)
Ca1ⁱⁱ—Ca1—O1ⁱⁱ	42.40 (10)	41.51 (10)	43.77 (10)
Ca1ⁱⁱ—Ca1—O1^ix	42.42 (10)	41.51 (10)	43.77 (10)
Ca1ⁱⁱ—Ca1—O1^x	119.24 (11)	110.32 (10)	128.31 (11)
Ca1ⁱⁱ—Ca1—O3	100.37 (6)	99.95 (6)	101.12 (6)
Ca1ⁱⁱ—Ca1—O3^x	100.37 (6)	99.95 (6)	101.12 (6)
Ca2—Ca1—Ca2ⁱⁱⁱ	101.62 (4)	99.54 (5)	103.72 (4)
Ca2—Ca1—Ca2^iv	101.66 (4)	99.54 (5)	103.72 (4)
Ca2—Ca1—Ca2^v	98.48 (4)	96.51 (4)	100.45 (4)
Ca2—Ca1—Ca2^vi	98.52 (4)	96.51 (4)	100.45 (4)
Ca2—Ca1—Ca2ⁱ	155.36 (3)	155.29 (3)	155.42 (3)
Ca2—Ca1—Si1^vii	69.97 (3)	69.85 (3)	70.09 (3)
Ca2—Ca1—Si1^viii	56.54 (5)	55.48 (5)	57.58 (5)
Ca2—Ca1—Si1ⁱⁱ	56.56 (5)	55.48 (5)	57.58 (5)
Ca2—Ca1—O1	139.05 (12)	133.66 (12)	144.86 (12)
Ca2—Ca1—O1ⁱⁱ	53.00 (10)	44.53 (10)	62.08 (10)
Ca2—Ca1—O1^ix	53.10 (10)	44.53 (10)	62.08 (10)
Ca2—Ca1—O1^x	139.15 (12)	133.66 (12)	144.86 (12)
Ca2—Ca1—O3	40.06 (6)	39.45 (6)	40.58 (6)
Ca2—Ca1—O3^x	40.06 (6)	39.45 (6)	40.58 (6)
Ca2ⁱⁱⁱ—Ca1—Ca2^iv	97.99 (4)	97.99 (4)	97.99 (4)
Ca2ⁱⁱⁱ—Ca1—Ca2^v	79.87 (5)	77.57 (5)	82.30 (5)
Ca2ⁱⁱⁱ—Ca1—Ca2^vi	159.68 (3)	158.88 (4)	160.31 (3)
Ca2ⁱⁱⁱ—Ca1—Ca2ⁱ	63.69 (4)	61.66 (4)	65.72 (4)
Ca2ⁱⁱⁱ—Ca1—Si1^vii	130.96 (8)	126.26 (8)	135.68 (8)
Ca2ⁱⁱⁱ—Ca1—Si1^viii	53.93 (4)	52.81 (4)	55.12 (4)
Ca2ⁱⁱⁱ—Ca1—Si1ⁱⁱ	131.03 (4)	130.27 (4)	131.74 (4)
Ca2ⁱⁱⁱ—Ca1—O1	57.56 (10)	49.65 (10)	65.37 (10)
Ca2ⁱⁱⁱ—Ca1—O1ⁱⁱ	104.71 (10)	100.92 (10)	108.58 (10)
Ca2ⁱⁱⁱ—Ca1—O1^ix	48.59 (10)	38.78 (10)	58.18 (10)
Ca2ⁱⁱⁱ—Ca1—O1^x	114.46 (11)	107.92 (11)	120.84 (11)
Ca2ⁱⁱⁱ—Ca1—O3	132.30 (9)	129.63 (9)	133.57 (9)
Ca2ⁱⁱⁱ—Ca1—O3^x	114.42 (9)	113.10 (9)	117.21 (10)
Ca2^iv—Ca1—Ca2^v	159.68 (3)	158.88 (4)	160.31 (3)
Ca2^iv—Ca1—Ca2^vi	79.88 (5)	77.57 (5)	82.30 (5)
Ca2^iv—Ca1—Ca2ⁱ	63.68 (4)	61.66 (4)	65.72 (4)
Ca2^iv—Ca1—Si1^vii	130.99 (8)	126.26 (8)	135.68 (8)
Ca2^iv—Ca1—Si1^viii	131.04 (4)	130.27 (4)	131.74 (4)
Ca2^iv—Ca1—Si1ⁱⁱ	53.95 (4)	52.81 (4)	55.12 (4)
Ca2^iv—Ca1—O1	114.54 (11)	107.92 (11)	120.84 (11)
Ca2^iv—Ca1—O1ⁱⁱ	48.74 (10)	38.78 (10)	58.18 (10)
Ca2^iv—Ca1—O1^ix	104.78 (10)	100.92 (10)	108.58 (10)
Ca2^iv—Ca1—O1^x	57.52 (10)	49.65 (10)	65.37 (10)
Ca2^iv—Ca1—O3	114.43 (9)	113.10 (9)	117.21 (10)
Ca2^iv—Ca1—O3^x	132.31 (9)	129.63 (9)	133.57 (9)
Ca2^v—Ca1—Ca2^vi	95.14 (4)	95.01 (4)	95.27 (4)
Ca2^v—Ca1—Ca2ⁱ	97.99 (4)	95.89 (4)	100.02 (4)
Ca2^v—Ca1—Si1^vii	55.39 (5)	52.99 (5)	57.70 (5)
Ca2^v—Ca1—Si1^viii	63.50 (4)	60.95 (4)	66.08 (5)
Ca2^v—Ca1—Si1ⁱⁱ	140.49 (4)	138.88 (4)	142.09 (4)
Ca2^v—Ca1—O1	47.37 (11)	40.25 (10)	54.78 (11)
Ca2^v—Ca1—O1ⁱⁱ	151.10 (11)	141.55 (10)	160.46 (11)
Ca2^v—Ca1—O1^ix	88.80 (11)	81.24 (10)	96.11 (10)
Ca2^v—Ca1—O1^x	104.91 (10)	99.80 (10)	110.21 (10)
Ca2^v—Ca1—O3	79.63 (7)	78.11 (8)	80.46 (7)
Ca2^v—Ca1—O3^x	65.13 (7)	64.24 (7)	66.74 (7)
Ca2^vi—Ca1—Ca2ⁱ	97.98 (4)	95.89 (4)	100.02 (4)
Ca2^vi—Ca1—Si1^vii	55.41 (5)	52.99 (5)	57.70 (5)
Ca2^vi—Ca1—Si1^viii	140.49 (4)	138.88 (4)	142.09 (4)
Ca2^vi—Ca1—Si1ⁱⁱ	63.53 (4)	60.95 (4)	66.08 (5)
Ca2^vi—Ca1—O1	104.87 (10)	99.80 (10)	110.21 (10)
Ca2^vi—Ca1—O1ⁱⁱ	88.92 (11)	81.24 (10)	96.11 (10)
Ca2^vi—Ca1—O1^ix	151.24 (11)	141.55 (10)	160.46 (11)
Ca2^vi—Ca1—O1^x	47.46 (11)	40.25 (10)	54.78 (11)
Ca2^vi—Ca1—O3	65.13 (7)	64.24 (7)	66.74 (7)
Ca2^vi—Ca1—O3^x	79.65 (7)	78.11 (8)	80.46 (7)
Ca2ⁱ—Ca1—Si1^vii	134.44 (4)	134.20 (4)	134.67 (4)
Ca2ⁱ—Ca1—Si1^viii	116.72 (6)	114.66 (6)	118.72 (6)
Ca2ⁱ—Ca1—Si1ⁱⁱ	116.73 (6)	114.66 (6)	118.72 (6)
Ca2ⁱ—Ca1—O1	51.09 (11)	42.40 (11)	59.67 (10)
Ca2ⁱ—Ca1—O1ⁱⁱ	109.26 (11)	100.18 (11)	117.59 (10)
Ca2ⁱ—Ca1—O1^ix	109.17 (11)	100.18 (11)	117.59 (10)
Ca2ⁱ—Ca1—O1^x	51.00 (11)	42.40 (11)	59.67 (10)
Ca2ⁱ—Ca1—O3	162.04 (8)	160.60 (8)	164.68 (7)
Ca2ⁱ—Ca1—O3^x	162.05 (8)	160.60 (8)	164.68 (7)
Si1^vii—Ca1—Si1^viii	85.80 (6)	81.89 (6)	89.73 (6)
Si1^vii—Ca1—Si1ⁱⁱ	85.82 (6)	81.89 (6)	89.73 (6)
Si1^vii—Ca1—O1	96.85 (11)	89.48 (11)	104.58 (11)
Si1^vii—Ca1—O1ⁱⁱ	105.90 (11)	104.55 (10)	106.78 (12)
Si1^vii—Ca1—O1^ix	105.91 (11)	104.55 (10)	106.78 (12)
Si1^vii—Ca1—O1^x	96.95 (11)	89.48 (11)	104.58 (11)
Si1^vii—Ca1—O3	31.40 (6)	30.86 (6)	32.12 (6)
Si1^vii—Ca1—O3^x	31.40 (6)	30.86 (6)	32.12 (6)
Si1^viii—Ca1—Si1ⁱⁱ	111.20 (5)	111.13 (5)	111.28 (5)
Si1^viii—Ca1—O1	85.18 (11)	81.51 (11)	88.89 (11)
Si1^viii—Ca1—O1ⁱⁱ	96.03 (10)	87.56 (10)	105.13 (10)
Si1^viii—Ca1—O1^ix	26.84 (10)	23.47 (10)	30.24 (9)
Si1^viii—Ca1—O1^x	162.25 (12)	159.42 (12)	167.31 (12)
Si1^viii—Ca1—O3	77.80 (8)	74.94 (8)	79.07 (8)
Si1^viii—Ca1—O3^x	61.46 (8)	60.25 (8)	64.28 (8)
Si1ⁱⁱ—Ca1—O1	162.32 (12)	159.42 (12)	167.31 (12)
Si1ⁱⁱ—Ca1—O1ⁱⁱ	26.90 (10)	23.47 (10)	30.24 (9)
Si1ⁱⁱ—Ca1—O1^ix	96.17 (10)	87.56 (10)	105.13 (10)
Si1ⁱⁱ—Ca1—O1^x	85.24 (11)	81.51 (11)	88.89 (11)
Si1ⁱⁱ—Ca1—O3	61.46 (8)	60.25 (8)	64.28 (8)
Si1ⁱⁱ—Ca1—O3^x	77.80 (8)	74.94 (8)	79.07 (8)
O1—Ca1—O1ⁱⁱ	155.20 (14)	149.29 (14)	164.00 (14)
O1—Ca1—O1^ix	98.29 (15)	84.53 (14)	111.90 (15)
O1—Ca1—O1^x	79.40 (14)	78.42 (14)	80.38 (14)
O1—Ca1—O3	126.33 (12)	116.84 (12)	133.44 (13)
O1—Ca1—O3^x	111.77 (13)	106.32 (12)	120.92 (14)
O1ⁱⁱ—Ca1—O1^ix	75.30 (13)	74.51 (13)	76.07 (13)
O1ⁱⁱ—Ca1—O1^x	98.45 (15)	84.53 (14)	111.90 (14)
O1ⁱⁱ—Ca1—O3	79.39 (12)	75.58 (11)	81.14 (12)
O1ⁱⁱ—Ca1—O3^x	83.60 (11)	81.55 (11)	88.45 (12)
O1^ix—Ca1—O1^x	155.10 (14)	149.29 (15)	164.00 (14)
O1^ix—Ca1—O3	83.60 (11)	81.55 (11)	88.45 (12)
O1^ix—Ca1—O3^x	79.38 (12)	75.58 (11)	81.14 (12)
O1^x—Ca1—O3	111.86 (13)	106.32 (12)	120.92 (14)
O1^x—Ca1—O3^x	126.43 (12)	116.84 (12)	133.44 (13)
Ca1—Ca2—Ca1^xiii	129.90 (6)	127.46 (7)	132.28 (6)
Ca1—Ca2—Ca1^xv	129.85 (6)	127.46 (7)	132.28 (6)
Ca1—Ca2—Ca1^v	81.48 (4)	79.85 (4)	83.02 (4)
Ca1—Ca2—Ca1^vi	81.45 (4)	79.85 (4)	83.02 (4)
Ca1—Ca2—Ca1ⁱⁱ	59.86 (3)	59.78 (3)	59.94 (3)
Ca1—Ca2—Ca2^xi	98.42 (4)	96.59 (4)	100.23 (4)
Ca1—Ca2—Ca2^xii	98.39 (4)	96.59 (4)	100.23 (4)
Ca1—Ca2—Si1^xiii	135.08 (4)	135.03 (4)	135.13 (4)
Ca1—Ca2—Si1^vi	131.41 (4)	131.27 (4)	131.56 (4)
Ca1—Ca2—Si1^viii	60.20 (5)	57.41 (5)	62.93 (5)
Ca1—Ca2—Si1ⁱⁱ	60.14 (5)	57.41 (5)	62.93 (5)
Ca1—Ca2—O1^vi	116.74 (9)	111.63 (8)	122.45 (10)
Ca1—Ca2—O1ⁱⁱ	45.11 (8)	41.84 (7)	48.88 (9)
Ca1—Ca2—O1^xiv	116.82 (9)	111.63 (8)	122.45 (10)
Ca1—Ca2—O1^ix	45.08 (8)	41.84 (7)	48.88 (9)
Ca1—Ca2—O2^xv	89.57 (8)	86.74 (8)	91.94 (8)
Ca1—Ca2—O2^xvi	89.61 (8)	86.74 (8)	91.94 (8)
Ca1—Ca2—O3	43.37 (8)	42.78 (8)	43.69 (8)
Ca1—Ca2—O3^x	43.37 (8)	42.78 (8)	43.69 (8)
Ca1^xiii—Ca2—Ca1^xv	97.99 (4)	97.99 (4)	97.99 (4)
Ca1^xiii—Ca2—Ca1^v	56.37 (3)	54.89 (3)	57.94 (4)
Ca1^xiii—Ca2—Ca1^vi	124.04 (4)	122.29 (4)	125.67 (4)
Ca1^xiii—Ca2—Ca1ⁱⁱ	116.30 (5)	114.27 (5)	118.35 (5)
Ca1^xiii—Ca2—Ca2^xi	56.87 (4)	55.75 (3)	58.04 (4)
Ca1^xiii—Ca2—Ca2^xii	123.18 (3)	122.24 (3)	124.09 (3)
Ca1^xiii—Ca2—Si1^xiii	69.17 (5)	67.40 (5)	70.96 (5)
Ca1^xiii—Ca2—Si1^vi	58.03 (5)	55.34 (5)	60.69 (5)
Ca1^xiii—Ca2—Si1^viii	71.90 (5)	71.36 (5)	72.46 (5)
Ca1^xiii—Ca2—Si1ⁱⁱ	169.83 (6)	169.29 (6)	170.37 (6)
Ca1^xiii—Ca2—O1^vi	87.42 (9)	83.96 (10)	90.46 (8)
Ca1^xiii—Ca2—O1ⁱⁱ	157.01 (10)	154.43 (10)	158.98 (9)
Ca1^xiii—Ca2—O1^xiv	41.83 (8)	39.34 (10)	44.00 (7)
Ca1^xiii—Ca2—O1^ix	96.50 (10)	94.30 (11)	98.37 (9)
Ca1^xiii—Ca2—O2^xv	140.07 (7)	139.95 (8)	140.33 (7)
Ca1^xiii—Ca2—O2^xvi	42.21 (7)	42.09 (7)	42.47 (7)
Ca1^xiii—Ca2—O3	119.32 (9)	115.62 (9)	121.84 (9)
Ca1^xiii—Ca2—O3^x	105.07 (9)	102.40 (9)	108.92 (10)
Ca1^xv—Ca2—Ca1^v	124.02 (4)	122.29 (4)	125.67 (4)
Ca1^xv—Ca2—Ca1^vi	56.35 (3)	54.89 (3)	57.94 (4)
Ca1^xv—Ca2—Ca1ⁱⁱ	116.33 (5)	114.27 (5)	118.35 (5)
Ca1^xv—Ca2—Ca2^xi	123.19 (3)	122.24 (3)	124.09 (3)
Ca1^xv—Ca2—Ca2^xii	56.88 (4)	55.75 (3)	58.04 (4)
Ca1^xv—Ca2—Si1^xiii	69.19 (5)	67.40 (5)	70.96 (5)
Ca1^xv—Ca2—Si1^vi	57.99 (5)	55.34 (5)	60.69 (5)
Ca1^xv—Ca2—Si1^viii	169.82 (6)	169.29 (6)	170.37 (6)
Ca1^xv—Ca2—Si1ⁱⁱ	71.91 (5)	71.36 (5)	72.46 (5)
Ca1^xv—Ca2—O1^vi	41.84 (8)	39.34 (10)	44.00 (7)
Ca1^xv—Ca2—O1ⁱⁱ	96.47 (10)	94.30 (11)	98.37 (9)
Ca1^xv—Ca2—O1^xiv	87.36 (9)	83.96 (10)	90.46 (8)
Ca1^xv—Ca2—O1^ix	157.05 (10)	154.43 (10)	158.98 (9)
Ca1^xv—Ca2—O2^xv	42.21 (7)	42.09 (7)	42.47 (7)
Ca1^xv—Ca2—O2^xvi	140.07 (7)	139.95 (8)	140.33 (7)
Ca1^xv—Ca2—O3	105.05 (9)	102.40 (9)	108.92 (10)
Ca1^xv—Ca2—O3^x	119.29 (9)	115.62 (9)	121.84 (9)
Ca1^v—Ca2—Ca1^vi	95.14 (4)	95.01 (4)	95.27 (3)
Ca1^v—Ca2—Ca1ⁱⁱ	119.63 (5)	117.36 (5)	121.82 (5)
Ca1^v—Ca2—Ca2^xi	85.99 (5)	83.09 (5)	88.88 (5)
Ca1^v—Ca2—Ca2^xii	177.99 (5)	176.02 (5)	179.71 (4)
Ca1^v—Ca2—Si1^xiii	124.70 (7)	121.96 (7)	127.39 (7)
Ca1^v—Ca2—Si1^vi	66.76 (5)	65.57 (5)	67.85 (5)
Ca1^v—Ca2—Si1^viii	51.55 (4)	49.61 (4)	53.57 (4)
Ca1^v—Ca2—Si1ⁱⁱ	130.08 (4)	128.10 (4)	131.99 (4)
Ca1^v—Ca2—O1^vi	84.62 (9)	81.67 (8)	87.64 (10)
Ca1^v—Ca2—O1ⁱⁱ	126.53 (9)	122.38 (8)	131.25 (10)
Ca1^v—Ca2—O1^xiv	39.09 (9)	36.24 (8)	42.56 (10)
Ca1^v—Ca2—O1^ix	78.67 (9)	76.33 (8)	81.29 (10)
Ca1^v—Ca2—O2^xv	139.66 (7)	137.36 (7)	142.72 (7)
Ca1^v—Ca2—O2^xvi	44.60 (6)	42.38 (6)	47.72 (7)
Ca1^v—Ca2—O3	64.66 (8)	61.88 (9)	65.98 (8)
Ca1^v—Ca2—O3^x	48.45 (8)	47.14 (8)	51.12 (8)
Ca1^vi—Ca2—Ca1ⁱⁱ	119.63 (5)	117.36 (5)	121.82 (5)
Ca1^vi—Ca2—Ca2^xi	177.97 (5)	176.02 (5)	179.71 (4)
Ca1^vi—Ca2—Ca2^xii	85.97 (5)	83.09 (5)	88.88 (5)
Ca1^vi—Ca2—Si1^xiii	124.70 (7)	121.96 (7)	127.39 (7)
Ca1^vi—Ca2—Si1^vi	66.73 (5)	65.57 (5)	67.85 (5)
Ca1^vi—Ca2—Si1^viii	130.11 (4)	128.10 (4)	131.99 (4)
Ca1^vi—Ca2—Si1ⁱⁱ	51.52 (4)	49.61 (4)	53.57 (4)
Ca1^vi—Ca2—O1^vi	39.04 (9)	36.24 (8)	42.56 (10)
Ca1^vi—Ca2—O1ⁱⁱ	78.69 (9)	76.33 (8)	81.29 (10)
Ca1^vi—Ca2—O1^xiv	84.65 (9)	81.67 (8)	87.64 (10)
Ca1^vi—Ca2—O1^ix	126.46 (9)	122.38 (8)	131.25 (10)
Ca1^vi—Ca2—O2^xv	44.55 (6)	42.38 (6)	47.72 (7)
Ca1^vi—Ca2—O2^xvi	139.71 (7)	137.36 (7)	142.72 (7)
Ca1^vi—Ca2—O3	48.44 (8)	47.14 (8)	51.12 (8)
Ca1^vi—Ca2—O3^x	64.66 (8)	61.88 (9)	65.98 (8)
Ca1ⁱⁱ—Ca2—Ca2^xi	59.43 (4)	58.52 (4)	60.31 (4)
Ca1ⁱⁱ—Ca2—Ca2^xii	59.44 (4)	58.52 (4)	60.31 (4)
Ca1ⁱⁱ—Ca2—Si1^xiii	75.27 (3)	75.24 (4)	75.31 (3)
Ca1ⁱⁱ—Ca2—Si1^vi	168.49 (4)	168.32 (4)	168.66 (4)
Ca1ⁱⁱ—Ca2—Si1^viii	68.80 (5)	66.94 (5)	70.70 (5)
Ca1ⁱⁱ—Ca2—Si1ⁱⁱ	68.83 (5)	66.94 (5)	70.70 (5)
Ca1ⁱⁱ—Ca2—O1^vi	152.21 (11)	150.68 (10)	153.59 (12)
Ca1ⁱⁱ—Ca2—O1ⁱⁱ	41.18 (9)	40.50 (10)	41.93 (8)
Ca1ⁱⁱ—Ca2—O1^xiv	152.21 (11)	150.68 (10)	153.59 (12)
Ca1ⁱⁱ—Ca2—O1^ix	41.19 (9)	40.50 (10)	41.93 (8)
Ca1ⁱⁱ—Ca2—O2^xv	86.02 (8)	85.00 (8)	88.33 (8)
Ca1ⁱⁱ—Ca2—O2^xvi	86.00 (8)	85.00 (8)	88.33 (8)
Ca1ⁱⁱ—Ca2—O3	101.77 (8)	101.53 (8)	102.16 (8)
Ca1ⁱⁱ—Ca2—O3^x	101.77 (8)	101.53 (8)	102.16 (8)
Ca2^xi—Ca2—Ca2^xii	92.91 (4)	92.86 (4)	92.96 (4)
Ca2^xi—Ca2—Si1^xiii	54.63 (5)	53.80 (5)	55.42 (5)
Ca2^xi—Ca2—Si1^vi	114.03 (6)	111.88 (6)	116.10 (6)
Ca2^xi—Ca2—Si1^viii	50.52 (4)	49.15 (4)	51.95 (4)
Ca2^xi—Ca2—Si1ⁱⁱ	127.44 (4)	126.31 (4)	128.50 (4)
Ca2^xi—Ca2—O1^vi	141.62 (9)	137.44 (11)	145.13 (8)
Ca2^xi—Ca2—O1ⁱⁱ	100.44 (9)	98.88 (10)	101.78 (8)
Ca2^xi—Ca2—O1^xiv	96.36 (10)	95.49 (11)	97.19 (9)
Ca2^xi—Ca2—O1^ix	53.43 (8)	48.77 (9)	57.44 (8)
Ca2^xi—Ca2—O2^xv	132.93 (7)	132.21 (7)	134.54 (7)
Ca2^xi—Ca2—O2^xvi	40.04 (6)	39.38 (6)	41.63 (6)
Ca2^xi—Ca2—O3	132.29 (10)	127.47 (10)	135.01 (9)
Ca2^xi—Ca2—O3^x	115.69 (10)	112.73 (10)	120.81 (10)
Ca2^xii—Ca2—Si1^xiii	54.64 (5)	53.80 (5)	55.42 (5)
Ca2^xii—Ca2—Si1^vi	114.00 (6)	111.88 (6)	116.10 (6)
Ca2^xii—Ca2—Si1^viii	127.43 (4)	126.31 (4)	128.50 (4)
Ca2^xii—Ca2—Si1ⁱⁱ	50.54 (4)	49.15 (4)	51.95 (4)
Ca2^xii—Ca2—O1^vi	96.38 (10)	95.49 (11)	97.19 (9)
Ca2^xii—Ca2—O1ⁱⁱ	53.35 (8)	48.77 (9)	57.44 (8)
Ca2^xii—Ca2—O1^xiv	141.57 (9)	137.44 (11)	145.13 (8)
Ca2^xii—Ca2—O1^ix	100.46 (9)	98.88 (10)	101.78 (8)
Ca2^xii—Ca2—O2^xv	40.05 (6)	39.38 (6)	41.63 (6)
Ca2^xii—Ca2—O2^xvi	132.92 (7)	132.21 (7)	134.54 (7)
Ca2^xii—Ca2—O3	115.66 (10)	112.73 (10)	120.81 (10)
Ca2^xii—Ca2—O3^x	132.27 (10)	127.47 (10)	135.01 (9)
Si1^xiii—Ca2—Si1^vi	93.36 (4)	93.30 (4)	93.41 (4)
Si1^xiii—Ca2—Si1^viii	105.15 (7)	102.95 (7)	107.37 (7)
Si1^xiii—Ca2—Si1ⁱⁱ	105.18 (7)	102.95 (7)	107.37 (7)
Si1^xiii—Ca2—O1^vi	102.67 (9)	98.58 (10)	106.26 (8)
Si1^xiii—Ca2—O1ⁱⁱ	100.03 (9)	95.94 (10)	103.64 (8)
Si1^xiii—Ca2—O1^xiv	102.61 (9)	98.58 (10)	106.26 (8)
Si1^xiii—Ca2—O1^ix	100.10 (9)	95.94 (10)	103.64 (8)
Si1^xiii—Ca2—O2^xv	87.16 (8)	86.23 (8)	89.28 (8)
Si1^xiii—Ca2—O2^xvi	87.15 (8)	86.23 (8)	89.28 (8)
Si1^xiii—Ca2—O3	169.54 (12)	166.21 (12)	175.67 (12)
Si1^xiii—Ca2—O3^x	169.57 (12)	166.21 (12)	175.67 (12)
Si1^vi—Ca2—Si1^viii	115.24 (7)	112.56 (8)	117.87 (8)
Si1^vi—Ca2—Si1ⁱⁱ	115.20 (7)	112.56 (8)	117.87 (8)
Si1^vi—Ca2—O1^vi	29.72 (10)	29.47 (11)	29.94 (9)
Si1^vi—Ca2—O1ⁱⁱ	144.31 (12)	142.00 (12)	146.86 (12)
Si1^vi—Ca2—O1^xiv	29.72 (10)	29.47 (11)	29.94 (9)
Si1^vi—Ca2—O1^ix	144.34 (12)	142.00 (12)	146.86 (12)
Si1^vi—Ca2—O2^xv	92.44 (9)	89.61 (9)	95.52 (9)
Si1^vi—Ca2—O2^xvi	92.49 (9)	89.61 (9)	95.52 (9)
Si1^vi—Ca2—O3	89.27 (8)	88.73 (8)	89.50 (8)
Si1^vi—Ca2—O3^x	89.28 (8)	88.73 (8)	89.50 (8)
Si1^viii—Ca2—Si1ⁱⁱ	118.17 (5)	118.17 (5)	118.18 (5)
Si1^viii—Ca2—O1^vi	136.01 (10)	134.63 (9)	137.62 (11)
Si1^viii—Ca2—O1ⁱⁱ	92.82 (10)	90.69 (9)	95.12 (11)
Si1^viii—Ca2—O1^xiv	85.68 (10)	83.10 (9)	88.57 (12)
Si1^viii—Ca2—O1^ix	29.67 (9)	29.29 (9)	30.32 (10)
Si1^viii—Ca2—O2^xv	147.46 (8)	147.33 (8)	147.77 (8)
Si1^viii—Ca2—O2^xvi	29.47 (7)	29.34 (7)	29.78 (7)
Si1^viii—Ca2—O3	81.37 (9)	77.39 (9)	84.32 (9)
Si1^viii—Ca2—O3^x	66.09 (9)	63.17 (9)	70.01 (9)
Si1ⁱⁱ—Ca2—O1^vi	85.64 (10)	83.10 (9)	88.57 (12)
Si1ⁱⁱ—Ca2—O1ⁱⁱ	29.67 (9)	29.29 (9)	30.32 (10)
Si1ⁱⁱ—Ca2—O1^xiv	136.01 (10)	134.63 (9)	137.62 (11)
Si1ⁱⁱ—Ca2—O1^ix	92.78 (10)	90.69 (9)	95.12 (11)
Si1ⁱⁱ—Ca2—O2^xv	29.47 (7)	29.34 (7)	29.78 (7)
Si1ⁱⁱ—Ca2—O2^xvi	147.46 (8)	147.33 (8)	147.77 (8)
Si1ⁱⁱ—Ca2—O3	66.06 (9)	63.17 (9)	70.01 (9)
Si1ⁱⁱ—Ca2—O3^x	81.35 (9)	77.39 (9)	84.32 (9)
O1^vi—Ca2—O1ⁱⁱ	114.87 (14)	112.29 (12)	117.91 (15)
O1^vi—Ca2—O1^xiv	55.57 (13)	55.41 (12)	55.72 (13)
O1^vi—Ca2—O1^ix	156.64 (11)	150.69 (10)	162.08 (12)
O1^vi—Ca2—O2^xv	65.46 (11)	63.68 (11)	66.96 (13)
O1^vi—Ca2—O2^xvi	120.67 (12)	118.50 (13)	122.13 (12)
O1^vi—Ca2—O3	75.89 (11)	70.46 (10)	82.01 (12)
O1^vi—Ca2—O3^x	83.63 (11)	77.99 (10)	89.21 (11)
O1ⁱⁱ—Ca2—O1^xiv	156.76 (11)	150.69 (10)	162.08 (12)
O1ⁱⁱ—Ca2—O1^ix	65.16 (12)	64.68 (12)	65.64 (13)
O1ⁱⁱ—Ca2—O2^xv	56.24 (11)	54.81 (11)	56.89 (10)
O1ⁱⁱ—Ca2—O2^xvi	120.68 (12)	119.63 (11)	121.13 (13)
O1ⁱⁱ—Ca2—O3	70.04 (10)	67.89 (10)	75.34 (11)
O1ⁱⁱ—Ca2—O3^x	85.90 (11)	79.78 (11)	88.78 (11)
O1^xiv—Ca2—O1^ix	114.90 (14)	112.29 (12)	117.91 (15)
O1^xiv—Ca2—O2^xv	120.64 (12)	118.50 (13)	122.13 (12)
O1^xiv—Ca2—O2^xvi	65.49 (11)	63.68 (11)	66.96 (13)
O1^xiv—Ca2—O3	83.68 (11)	77.99 (10)	89.21 (11)
O1^xiv—Ca2—O3^x	75.94 (11)	70.46 (10)	82.01 (12)
O1^ix—Ca2—O2^xv	120.67 (12)	119.63 (11)	121.13 (13)
O1^ix—Ca2—O2^xvi	56.25 (11)	54.81 (11)	56.89 (10)
O1^ix—Ca2—O3	85.90 (11)	79.78 (11)	88.78 (11)
O1^ix—Ca2—O3^x	70.04 (10)	67.89 (10)	75.34 (11)
O2^xv—Ca2—O3	81.68 (11)	79.37 (10)	85.87 (11)
O2^xv—Ca2—O3^x	95.98 (11)	95.38 (11)	96.74 (11)
O2^xvi—Ca2—O3	95.98 (11)	95.38 (11)	96.74 (11)
O2^xvi—Ca2—O3^x	81.75 (11)	79.37 (10)	85.87 (11)
Ca1^xx—Si1—Ca1^xxii	94.11 (6)	89.99 (6)	98.23 (6)
Ca1^xx—Si1—Ca1ⁱ	94.18 (6)	89.99 (6)	98.23 (6)
Ca1^xx—Si1—Ca2ⁱⁱⁱ	114.81 (5)	114.71 (5)	114.90 (5)
Ca1^xx—Si1—Ca2^v	145.64 (5)	145.25 (5)	146.02 (4)
Ca1^xx—Si1—Ca2^xxii	73.03 (5)	68.80 (5)	77.34 (6)
Ca1^xx—Si1—Ca2ⁱ	73.10 (5)	68.80 (5)	77.34 (6)
Ca1^xx—Si1—O1	125.38 (19)	117.17 (18)	134.07 (19)
Ca1^xx—Si1—O1^xvii	125.22 (19)	117.17 (18)	134.07 (19)
Ca1^xx—Si1—O2^xviii	59.90 (10)	59.24 (9)	60.70 (10)
Ca1^xx—Si1—O2^xix	59.90 (10)	59.24 (9)	60.70 (10)
Ca1^xx—Si1—O3^xx	50.32 (11)	49.80 (10)	50.65 (11)
Ca1^xx—Si1—O3^xxi	50.31 (11)	49.80 (10)	50.65 (11)
Ca1^xxii—Si1—Ca1ⁱ	111.21 (4)	111.13 (4)	111.28 (5)
Ca1^xxii—Si1—Ca2ⁱⁱⁱ	118.53 (8)	116.97 (8)	120.05 (8)
Ca1^xxii—Si1—Ca2^v	68.05 (5)	66.48 (5)	69.55 (5)
Ca1^xxii—Si1—Ca2^xxii	63.27 (6)	61.45 (6)	65.18 (6)
Ca1^xxii—Si1—Ca2ⁱ	165.02 (5)	164.23 (5)	165.67 (5)
Ca1^xxii—Si1—O1	127.16 (16)	112.61 (16)	141.61 (16)
Ca1^xxii—Si1—O1^xvii	44.18 (14)	36.77 (14)	52.79 (14)
Ca1^xxii—Si1—O2^xviii	131.75 (16)	127.96 (16)	138.09 (15)
Ca1^xxii—Si1—O2^xix	110.58 (15)	104.14 (15)	114.57 (16)
Ca1^xxii—Si1—O3^xx	58.42 (13)	54.56 (12)	62.24 (13)
Ca1^xxii—Si1—O3^xxi	77.77 (13)	73.85 (13)	81.70 (12)
Ca1ⁱ—Si1—Ca2ⁱⁱⁱ	118.55 (8)	116.97 (8)	120.05 (8)
Ca1ⁱ—Si1—Ca2^v	68.06 (5)	66.48 (5)	69.55 (5)
Ca1ⁱ—Si1—Ca2^xxii	165.01 (5)	164.23 (5)	165.67 (5)
Ca1ⁱ—Si1—Ca2ⁱ	63.29 (6)	61.45 (6)	65.18 (6)
Ca1ⁱ—Si1—O1	44.17 (14)	36.77 (14)	52.79 (14)
Ca1ⁱ—Si1—O1^xvii	127.28 (16)	112.61 (16)	141.61 (16)
Ca1ⁱ—Si1—O2^xviii	110.65 (15)	104.14 (15)	114.57 (16)
Ca1ⁱ—Si1—O2^xix	131.82 (16)	127.96 (16)	138.09 (15)
Ca1ⁱ—Si1—O3^xx	77.84 (13)	73.85 (13)	81.70 (12)
Ca1ⁱ—Si1—O3^xxi	58.49 (13)	54.56 (12)	62.24 (13)
Ca2ⁱⁱⁱ—Si1—Ca2^v	99.19 (4)	99.14 (4)	99.24 (4)
Ca2ⁱⁱⁱ—Si1—Ca2^xxii	74.83 (5)	72.64 (5)	77.04 (5)
Ca2ⁱⁱⁱ—Si1—Ca2ⁱ	74.84 (5)	72.64 (5)	77.04 (5)
Ca2ⁱⁱⁱ—Si1—O1	77.47 (14)	64.81 (14)	90.05 (14)
Ca2ⁱⁱⁱ—Si1—O1^xvii	77.40 (14)	64.81 (14)	90.05 (14)
Ca2ⁱⁱⁱ—Si1—O2^xviii	56.56 (9)	55.82 (9)	57.41 (9)
Ca2ⁱⁱⁱ—Si1—O2^xix	56.57 (9)	55.82 (9)	57.41 (9)
Ca2ⁱⁱⁱ—Si1—O3^xx	159.92 (14)	156.82 (15)	163.08 (13)
Ca2ⁱⁱⁱ—Si1—O3^xxi	159.98 (14)	156.82 (15)	163.08 (13)
Ca2^v—Si1—Ca2^xxii	118.55 (8)	115.56 (8)	121.56 (9)
Ca2^v—Si1—Ca2ⁱ	118.57 (8)	115.56 (8)	121.56 (9)
Ca2^v—Si1—O1	59.77 (16)	45.10 (16)	74.68 (16)
Ca2^v—Si1—O1^xvii	59.88 (16)	45.10 (16)	74.68 (16)
Ca2^v—Si1—O2^xviii	152.09 (12)	148.70 (13)	154.05 (11)
Ca2^v—Si1—O2^xix	152.06 (12)	148.70 (13)	154.05 (11)
Ca2^v—Si1—O3^xx	97.16 (11)	96.60 (11)	97.37 (11)
Ca2^v—Si1—O3^xxi	97.16 (11)	96.60 (11)	97.37 (11)
Ca2^xxii—Si1—Ca2ⁱ	118.17 (5)	118.17 (5)	118.18 (5)
Ca2^xxii—Si1—O1	150.30 (15)	141.75 (14)	157.55 (15)
Ca2^xxii—Si1—O1^xvii	59.44 (17)	48.03 (16)	71.31 (17)
Ca2^xxii—Si1—O2^xviii	69.57 (13)	66.88 (13)	75.19 (13)
Ca2^xxii—Si1—O2^xix	48.70 (13)	43.15 (12)	51.45 (13)
Ca2^xxii—Si1—O3^xx	88.54 (14)	83.94 (13)	92.08 (14)
Ca2^xxii—Si1—O3^xxi	106.10 (14)	102.63 (14)	110.72 (14)
Ca2ⁱ—Si1—O1	59.57 (17)	48.03 (16)	71.31 (17)
Ca2ⁱ—Si1—O1^xvii	150.28 (15)	141.75 (14)	157.55 (15)
Ca2ⁱ—Si1—O2^xviii	48.76 (13)	43.15 (12)	51.45 (13)
Ca2ⁱ—Si1—O2^xix	69.63 (13)	66.88 (13)	75.19 (13)
Ca2ⁱ—Si1—O3^xx	106.17 (14)	102.63 (14)	110.72 (14)
Ca2ⁱ—Si1—O3^xxi	88.61 (14)	83.94 (13)	92.08 (14)
O1—Si1—O1^xvii	109.2 (2)	108.1 (2)	110.3 (2)
O1—Si1—O2^xviii	108.6 (2)	97.0 (2)	114.7 (2)
O1—Si1—O2^xix	109.21 (19)	103.27 (19)	121.4 (2)
O1—Si1—O3^xx	113.86 (19)	110.62 (19)	119.91 (18)
O1—Si1—O3^xxi	106.2 (2)	99.0 (2)	109.7 (2)
O1^xvii—Si1—O2^xviii	109.21 (19)	103.27 (19)	121.4 (2)
O1^xvii—Si1—O2^xix	108.6 (2)	97.0 (2)	114.7 (2)
O1^xvii—Si1—O3^xx	106.2 (2)	99.0 (2)	109.7 (2)
O1^xvii—Si1—O3^xxi	113.94 (19)	110.62 (19)	119.91 (18)
O2^xviii—Si1—O3^xx	109.91 (15)	109.59 (15)	110.08 (15)
O2^xviii—Si1—O3^xxi	107.07 (15)	106.78 (15)	107.17 (15)
O2^xix—Si1—O3^xx	107.06 (15)	106.78 (15)	107.17 (15)
O2^xix—Si1—O3^xxi	109.91 (15)	109.59 (15)	110.08 (15)
Ca1—O1—Ca1ⁱ	92.77 (15)	90.18 (14)	94.72 (15)
Ca1—O1—Ca2^v	93.57 (14)	88.02 (12)	99.11 (14)
Ca1—O1—Ca2ⁱ	87.72 (13)	78.52 (11)	97.09 (16)
Ca1—O1—Si1	151.8 (2)	135.7 (2)	165.7 (2)
Ca1ⁱ—O1—Ca2^v	89.54 (12)	77.83 (10)	101.84 (14)
Ca1ⁱ—O1—Ca2ⁱ	81.83 (12)	76.02 (11)	86.63 (13)
Ca1ⁱ—O1—Si1	108.96 (18)	96.97 (16)	119.6 (2)
Ca2^v—O1—Ca2ⁱ	170.43 (16)	163.23 (14)	176.13 (18)
Ca2^v—O1—Si1	90.51 (18)	75.46 (15)	105.4 (2)
Ca2ⁱ—O1—Si1	90.76 (18)	79.23 (16)	101.72 (18)
Ca2^iv—O2—Si1^xxiii	101.78 (16)	98.99 (16)	107.34 (16)
Ca1—O3—Ca2	96.57 (10)	95.87 (10)	97.77 (10)
Ca1—O3—Si1^vii	98.29 (13)	97.68 (13)	99.26 (13)
Ca2—O3—Si1^vii	153.47 (19)	152.99 (19)	154.15 (19)

Symmetry codes: (i) x₁−1/2, −x₂+3/2, −x₃+1/2, x₄; (ii) x₁+1/2, −x₂+3/2, −x₃+1/2, x₄; (iii) −x₁+3/2, −x₂+1, x₃+1/2, −x₄+1/2; (iv) −x₁+3/2, −x₂+2, x₃+1/2, −x₄+1/2; (v) −x₁+1, x₂−1/2, −x₃, −x₄+1/2; (vi) −x₁+1, x₂+1/2, −x₃, −x₄+1/2; (vii) −x₁+1/2, −x₂+1, x₃−1/2, −x₄+1/2; (viii) x₁+1/2, −x₂+1/2, −x₃+1/2, x₄; (ix) x₁+1/2, x₂, −x₃+1/2, x₄+1/2; (x) x₁, −x₂+3/2, x₃, x₄+1/2; (xi) −x₁+2, x₂−1/2, −x₃, −x₄+1/2; (xii) −x₁+2, x₂+1/2, −x₃, −x₄+1/2; (xiii) −x₁+3/2, −x₂+1, x₃−1/2, −x₄+1/2; (xiv) −x₁+1, −x₂+1, −x₃, −x₄; (xv) −x₁+3/2, −x₂+2, x₃−1/2, −x₄+1/2; (xvi) −x₁+3/2, x₂−1/2, x₃−1/2, −x₄; (xvii) x₁, −x₂+1/2, x₃, x₄+1/2; (xviii) −x₁+1, x₂−1/2, −x₃+1, −x₄+1/2; (xix) −x₁+1, −x₂+1, −x₃+1, −x₄; (xx) −x₁+1/2, −x₂+1, x₃+1/2, −x₄+1/2; (xxi) −x₁+1/2, x₂−1/2, x₃+1/2, −x₄; (xxii) x₁−1/2, −x₂+1/2, −x₃+1/2, x₄; (xxiii) −x₁+1, x₂+1/2, −x₃+1, −x₄+1/2.

Acknowledgements

Open access funding enabled and organized by Projekt DEAL.

Funding information

The following funding is acknowledged: Bundesministerium für Wirtschaftliche Zusammenarbeit und Entwicklung (grant No. 0324244A).

References

Barnard, J. S., Johnstone, D. N. & Midgley, P. A. (2017). Ultramicroscopy, 174, 79–88. CrossRef CAS PubMed Google Scholar
Bragg, S. W. L. & Claringbull, G. F. (1965). The Crystalline State: Crystal Structures of Minerals. Cornell University Press. Google Scholar
Bredig, M. A. (1950). J. Am. Ceram. Soc. 33, 188–192. CrossRef CAS Google Scholar
Burla, M. C., Caliandro, R., Carrozzini, B., Cascarano, G. L., Cuocci, C., Giacovazzo, C., Mallamo, M., Mazzone, A. & Polidori, G. (2015). J. Appl. Cryst. 48, 306–309. Web of Science CrossRef CAS IUCr Journals Google Scholar
Cascarano, G. L., Giacovazzo, C. & Carrozzini, B. (2010). Ultramicroscopy, 111, 56–61. Web of Science PubMed Google Scholar
De la Torre, A. G. & Aranda, M. A. G. (2003). J. Appl. Cryst. 36, 1169–1176. Web of Science CrossRef CAS IUCr Journals Google Scholar
Dunstetter, F., de Noirfontaine, M.-N. & Courtial, M. (2006). Cem. Concr. Res. 36, 39–53. CrossRef CAS Google Scholar
Fukuda, K. & Maki, I. (1989). J. Am. Ceram. Soc. 72, 2204–2207. CrossRef CAS Web of Science Google Scholar
Gemmi, M., Mugnaioli, E., Gorelik, T. E., Kolb, U., Palatinus, L., Boullay, P., Hovmöller, S. & Abrahams, J. P. (2019). ACS Cent. Sci. 5, 1315–1329. Web of Science CrossRef CAS PubMed Google Scholar
Il'inets, A. M. & Bikbau, M. Ya. (1990). Soviet Phys. Crystallogr. (Engl. Translation), 35, 54–56. Google Scholar
Jelenić, I. & Bezjak, A. (1982). Cem. Concr. Res. 12, 785–788. Google Scholar
Jost, K. H., Ziemer, B. & Seydel, R. (1977). Acta Cryst. B33, 1696–1700. CrossRef ICSD CAS IUCr Journals Web of Science Google Scholar
Kim, Y. J., Nettleship, I. & Kriven, W. M. (1992). J. Am. Ceram. Soc. 75, 2407–2419. CrossRef CAS Google Scholar
Kolb, U., Gorelik, T., Kübel, C., Otten, M. T. & Hubert, D. (2007). Ultramicroscopy, 107, 507–513. Web of Science CrossRef PubMed CAS Google Scholar
Kolb, U., Gorelik, T. & Otten, M. T. (2008). Ultramicroscopy, 108, 763–772. Web of Science CrossRef PubMed CAS Google Scholar
Kolb, U., Krysiak, Y. & Plana-Ruiz, S. (2019). Acta Cryst. B75, 463–474. Web of Science CSD CrossRef IUCr Journals Google Scholar
Mahasenan, N., Smith, S. & Humphreys, K. (2003). Greenhouse Gas Control Technologies, 6th International Conference, Vol. II, edited by J. Gale & Y. Kaya, pp. 995–1000. Oxford: Pergamon. Google Scholar
Midgley, C. M. (1952). Acta Cryst. 5, 307–312. CrossRef ICSD CAS IUCr Journals Web of Science Google Scholar
Momma, K. & Izumi, F. (2011). J. Appl. Cryst. 44, 1272–1276. Web of Science CrossRef CAS IUCr Journals Google Scholar
Morsli, K., De La Torre, G., Stöber, S., Cuberos, A. J. M., Zahir, M. & Aranda, M. A. G. (2007). J. Am. Ceram. Soc. 90, 3205–3212. CrossRef CAS Google Scholar
Mugnaioli, E., Andrusenko, I., Schüler, T., Loges, N., Dinnebier, R. E., Panthöfer, M., Tremel, W. & Kolb, U. (2012). Angew. Chem. Int. Ed. 51, 7041–7045. Web of Science CSD CrossRef CAS Google Scholar
Mumme, W. G., Hill, R. J., Bushnell-Wye, G. & Segnit, E. R. (1995). Neues Jahrb. Mineral. Abh. 169, 35–68. CAS Google Scholar
Olivier, J., Janssens-Maenhout, G., Muntean, M. & Peters, J. (2016). Trends in Global CO₂ Emissions. 2016 Report. The Hague: PBL Netherlands Environmental Assessment Agency. Google Scholar
Palatinus, L. (2013). Acta Cryst. B69, 1–16. CrossRef CAS IUCr Journals Google Scholar
Palatinus, L. (2017). Acta Cryst. A73, C810. CrossRef IUCr Journals Google Scholar
Palatinus, L., Brázda, P., Jelínek, M., Hrdá, J., Steciuk, G. & Klementová, M. (2019). Acta Cryst. B75, 512–522. Web of Science CrossRef IUCr Journals Google Scholar
Palatinus, L. & Chapuis, G. (2007). J. Appl. Cryst. 40, 786–790. Web of Science CrossRef CAS IUCr Journals Google Scholar
Palatinus, L., Corrêa, C. A., Steciuk, G., Jacob, D., Roussel, P., Boullay, P., Klementová, M., Gemmi, M., Kopeček, J., Domeneghetti, M. C., Cámara, F. & Petříček, V. (2015). Acta Cryst. B71, 740–751. Web of Science CrossRef IUCr Journals Google Scholar
Palatinus, L., Petříček, V. & Corrêa, C. A. (2015). Acta Cryst. A71, 235–244. Web of Science CrossRef IUCr Journals Google Scholar
Petříček, V., Dušek, M. & Palatinus, L. (2014). Z. Kristallogr. Cryst. Mater. 229, 345–352. Google Scholar
Plana-Ruiz, S., Krysiak, Y., Portillo, J., Alig, E., Estradé, S., Peiró, F. & Kolb, U. (2020). Ultramicroscopy, 211, 112951. Web of Science PubMed Google Scholar
Plana-Ruiz, S., Portillo, J., Estradé, S., Peiró, F., Kolb, U. & Nicolopoulos, S. (2018). Ultramicroscopy, 193, 39–51. Web of Science CAS PubMed Google Scholar
Prince, E. (2004). Editor. International Tables for Crystallography, Vol. C, Mathematical, physical and chemical tables, 3rd ed. Dordrecht: Kluwer Academic Publishers. Google Scholar
Redhammer, G. J., Tippelt, G., Roth, G. & Amthauer, G. (2004). Am. Mineral. 89, 405–420. Web of Science CrossRef ICSD CAS Google Scholar
Regourd, M., Bigaré, M., Forest, J. & Guinier, A. (1968). Proceedings of the 5th International Symposium on the Chemistry of Cement, 7–11 October 1968, Tokyo, Japan, pp. 44–48. Tokyo: Japan Cement Association. Google Scholar
Remy, C., Guyot, F. & Madon, M. (1995). Phys. Chem. Miner. 22, 419–427. CrossRef CAS Google Scholar
Richardson, I. G., Hall, C. & Groves, G. W. (1993). Adv. Cem. Res. 5, 15–21. CrossRef CAS Google Scholar
Saalfeld, H. (1975). Am. Mineral. 60, 824–827. CAS Google Scholar
Sarkar, S. L. (1980). J. Mater. Sci. 15, 1324–1325. CrossRef CAS Google Scholar
Scrivener, K. L., John, V. M. & Gartner, E. M. (2018). Cem. Concr. Res. 114, 2–26. CrossRef CAS Google Scholar
Smith, D. K., Majumdar, A. & Ordway, F. (1965). Acta Cryst. 18, 787–795. CrossRef ICSD CAS IUCr Journals Web of Science Google Scholar
Smyth, J. R. & Hazen, R. M. (1973). Am. Mineral. 58, 588–593. CAS Google Scholar
Taylor, H. F. W. (1997). Cement Chemistry. London: T. Telford. Google Scholar
Thompson, J. G., Withers, R. L. & Hyde, B. G. (1987). J. Am. Ceram. Soc. 70, C-383–C-386. Google Scholar
Toraya, H. & Yamazaki, S. (2002). Acta Cryst. B58, 613–621. Web of Science CrossRef ICSD CAS IUCr Journals Google Scholar
Udagawa, S., Urabe, K., Natsume, M. & Yano, T. (1980). Cem. Concr. Res. 10, 139–144. CrossRef ICSD CAS Web of Science Google Scholar
Wagner, T. & Schönleber, A. (2009). Acta Cryst. B65, 249–268. Web of Science CSD CrossRef CAS IUCr Journals Google Scholar
Wolff, P. M. de (1974). Acta Cryst. A30, 777–785. CrossRef Web of Science IUCr Journals Google Scholar

This is an open-access article distributed under the terms of the Creative Commons Attribution (CC-BY) Licence, which permits unrestricted use, distribution, and reproduction in any medium, provided the original authors and source are cited.

STRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS

ISSN: 2052-5206

Volume 80| Part 2| April 2024| Pages 105-116

https://doi.org/10.1107/S205252062400146X

Open

access