Mg(H₂O)₂[TeO₂(OH)₄]: a polytypic structure with a two-mode disordered stacking arrangement

Crystals of the hydrous magnesium orthotellurate(VI) Mg(H₂O)₂[TeO₂(OH)₄] were grown by slow diffusion of an aqueous MgCl₂ solution into a KOH/Te(OH)₆ solution immobilized in gelatin. The crystal structure is built of sheets of nearly regular corner-sharing [MgO₆] and [TeO₆] octahedra. Half of the bridging O atoms are connected to disordered H atoms, which are located in rhomboidal voids (long and short diameters of ∼5.0 and ∼2.5 Å, respectively) of these layers. Moreover, the Te^VI atom connects to two OH⁻ ions and the Mg^II atom to two H₂O molecules. The OH⁻ ions and H₂O molecules connect adjacent layers forming a disordered hydrogen-bonding network. In a given layer, an adjacent layer may be positioned in four ways, which can be characterized by one of two origin shifts and one of two orientations with respect to [100]. The crystals feature a disordered stacking arrangement, leading to rods of diffuse scattering in the diffraction pattern. The polytypism is explained by application of the order–disorder (OD) theory. Different refinement models are compared and the diffuse scattering is evaluated with structure factor calculations. The correlation coefficient of subsequent origin shifts is ∼ −0.33, whereas the orientation of the layers is essentially random. Determining the latter is particularly difficult owing to a small contribution to the diffraction pattern and virtually indistinguishable diffraction patterns for pairs of correlations with the same absolute value. On longer standing in a glass vial, an ordered polytype forms.

1. Introduction

Orthotellurates(VI) of alkaline earth metals with general formula M₂M′[Te^VIO₆] bear interesting crystal-chemical and physico-chemical aspects, and a number of these phases and their solid solutions are structurally well characterized (Prior et al., 2005; Fu et al., 2008). The structures of nearly all alkaline earth metal tellurates (except Be) with a single M^II cation and the general formula M^II₃[Te^VIO₆] have been elucidated [M = Mg: Schulz & Bayer (1971); M = Ca: Hottentot & Loopstra (1981); M = Sr, Ba: Stöger et al. (2010)]. The structures of these tellurates are characterized by rigid, practically regular, octahedral [TeO₆]⁶⁻ units. Ca₃[TeO₆] (P2₁/n, Z = 2), Sr₃[TeO₆] (, Z = 32) and Ba₃[TeO₆] (I4₁/a, Z = 80) are hettotypes of the double perovskite structure type, where the M^II atom occupies two positions with distinctly different coordination spheres. The ionic radius of Mg^II, on the other hand, is incompatible with the large voids required by the double perovskite aristotype and therefore Mg₃[TeO₆] (, Z = 2) crystallizes in a different structure type, isotypic with Mn₃[TeO₆] (Weil, 2006).

During our ongoing studies of hydrous derivatives of M₃[TeO₆] phases with M = Mg, Ca, Sr, Ba we obtained single crystals of the title compound, Mg(H₂O)₂[TeO₂(OH)₄], with a unique crystal structure. So far, hydrous alkaline earth tellurates have only been described for Ba (Weil et al., 2016). We report here on the structure determination and description of the polytypic structure as well as on thermal behavior of Mg(H₂O)₂[TeO₂(OH)₄].

Symbols used are summarized in Appendix A.

2. Experimental

2.1. Synthesis and crystal growth

Crystals of Mg(H₂O)₂[TeO₂(OH)₄] were grown in gelatin using a gel diffusion technique (Heinisch, 1996). Three gelatin sheets (∼4.5 g) were dissolved in a solution of KOH (4.34 g, 85%wt) and Te(OH)₆ (7.89 g) in water (300 ml). From this mixture, 25 ml of the solution were introduced into a large test tube. After solidification, the gel was covered with 10 ml of a neutral gelatin solution, prepared by dissolving one gelatin sheet (∼1.5 g) in water (100 ml). After solidification of the second gelatin layer, it was covered with Mg^II solution (10 ml, 0.5%wt) which was obtained by dissolving MgCl₂·6H₂O (4.16 g) in water (100 ml). The test tube was sealed with wrapping film and kept at 295 K for one month. Square-bipyramidal crystals of Mg(H₂O)₂[TeO₂(OH)₄] had formed at the interface of both gelatin layers. The gel was cut with a scalpel and crystals with an adequate size for single-crystal diffraction were isolated under a polarizing microscope.

2.2. Data collection

Diffraction intensities for structure refinements were collected at room temperature using fine-sliced ω- and φ-scans on a Bruker KAPPA APEX II diffractometer equipped with a CCD camera (Mo radiation, graphite-monochromated). Bragg intensities were reduced using the SAINT-Plus software (Bruker, 2017). An absorption correction was applied using a multi-scan approach with SADABS (Bruker, 2017) using the 4/mmm Laue group.

Inspection of the diffraction pattern (reconstructed reciprocal space layers) revealed lines with pronounced diffuse scattering. For the quantitative analysis of the diffuse scattering, a second crystal was measured with special attention paid to minimization of artifacts on a Stoe IPDS-II image-plate diffractometer using graphite-monochromated Mo radiation produced by a conventional sealed X-ray tube operated at 50 kV and 40 mA. A 0.5 mm fiber optic collimator and beam stop were positioned in such a way that the free beam path in air was 30 mm long, with the crystal in the center. Compared to the default setup, this arrangement has a significant shorter air beam path and the background caused by air-scattering is reduced. The sample-to-detector distance was set to 100 mm. For further background correction, 46 frames were collected under the same conditions without the sample. These frames were averaged and used as background in further processing. The data collection was run as a 180° ω-scan using 0.2° rotation and 2 min exposure times, resulting in 900 measured frames. Reference frames were collected every 2 h using 1 min exposures over a 10° ω rotation. Evaluation of the 29 reference frames did not show any significant change of the intensities.

The experimentally determined background was subtracted from all measured raw data frames. Furthermore, a masking procedure was applied to flag overexposed spots. XDS (Kabsch, 2010) was used to determine the orientation matrix for further processing with a modified version of Xcavate (Estermann & Steurer, 1998; Estermann, 2001). Intensity scaling of the original 32-bit images was obtained with Xcavate, and shading of non-measured areas and extraction of line profiles were performed with ImageJ (Abràmoff et al., 2004). One-dimensional streak profiles were extracted by manually determining the lateral center of the streaks and summing over 20 pixels segments perpendicular to the streaks.

Further diffraction experiments on a crystal (70 µm × 70 µm × 80 µm) kept for six years in gelatin at room conditions have been performed at the X06DA beamline of the Swiss Light Source (Paul Scherrer Institute, Villigen, Switzerland). Monochromated radiation of 0.7085 Å was utilized to collect 1800 data frames during a 180° rotation of the crystal (0.3 seconds per frame) using a Pilatus 2M-F detector. Data collection was controlled by DA+ (Wojdyla et al., 2018), evaluation of the orientation matrix and reconstruction of the reciprocal space layers were performed using XDS and Xcavate.

Details of the data collections are summarized in Table 1.

Table 1
Crystal data and integration details of Mg(H₂O)₂[TeO₂(OH)₄]

	Data collection 1	Data collection 2	Data collection 3
Crystal data
Sum formula	MgTeO8H8	MgTeO8H8	MgTeO8H8
Mr	486.46	486.46	486.46
Crystal system	Tetragonal	Tetragonal	Tetragonal
Crystal form	Square bipyramid	Square bipyramid	Square bipyramid
Crystal color	Colorless	Colorless	Colorless
Crystal size (mm)	0.15 × 0.15 × 0.22	0.16 × 0.16 × 0.25	0.07 × 0.07 × 0.08
Data collection
Diffractometer	Bruker KAPPA APEX II	Stoe IPDS-II	X06DA beamline
Radiation type, λ (Å)	Mo , 0.71073	Mo , 0.71073 Å	0.7085
Temperature (K)	293	293	293
Data collection method	ω- and φ-scans	ω-scan	ω-scan
θmax(°)	39.1	29.7	30.0
No. of measured reflections	7344	^†	^†
a, c (Å)	5.32820 (10), 20.6725 (4)	5.334 (2), 20.808 (5)	5.316 (2), 20.791 (4)
V (Å^3)	586.886 (11)	592 (3)	587 (3)
Dx (Mg m^−3)	3.166	†	†
μ (mm^−1)	5.167	†	†
Absorption correction	Multi-scan (SADABS)	†	†
Tmin, Tmax	0.32, 0.46	†	†
Rint (Laue class)	0.040 (4/mmm)	†	†

†No data reduction or refinement performed.

2.3. Refinement

The crystal structure of Mg(H₂O)₂[TeO₂(OH)₄] was solved using the charge flipping method implemented in SUPERFLIP (Palatinus & Chapuis, 2007) and refined against F² in Jana2006 (Petříček et al., 2014). Owing to disorder, the H atoms could not be located reliably and thus were not considered in the refinements. All atoms were refined using anisotropic atomic displacement parameters (ADPs). More details on different modeling and refinement attempts are given below (§3.8).

2.4. Calculation of diffuse scattering

Experimental peak broadening of the one-dimensional intensity profiles was estimated by fitting Gaussian distributions to sharp reflections using the least squares (LS) solver Ceres (Agarwal et al., 2020) refining the origin, reciprocal basis vector length, variance σ (all in pixels) and the individual intensities (in arbitrary units). The overall peak shape of the sharp reflections was well described by a Gaussian, only the base was better described by a Lorentz (Cauchy) distribution. One-dimensional diffuse scattering was calculated using the analytical expressions derived below. Atomic coordinates and ADPs of single layers were taken from the single-crystal refinements. The atomic form factors were calculated using polynomial approximations tabulated in International Tables for Crystallography (Brown et al., 2006). Calculations were performed on a one-dimensional grid with four times the resolution of experimental data and later downsampled to the experimental grid.

Correlation parameters were estimated using a simple coordinate-descent algorithm optimizing in turn the origin (in pixels), the length of the reciprocal basis vector (in pixels) and the correlation parameter (unitless). Each variable was determined using a golden-section search. When multiple rods were refined concurrently, a hierarchical coordinate-descent was performed. In an outer loop, the correlation parameter was refined, in an inner loop the origin and basis vector length of each rod.

The validity of such a trivial search was confirmed by noting that the loss function possesses a single local minimum in each coordinate. The process was stopped when the change in all variables fell below a threshhold of 0.001 in the respective unit. The scale factor was determined after each cycle using a simple linear least-squares regression with unit weight, which also provided the loss function . Refinements using the weighting functions w = 1/(I_obs)^e (e = 1,2), which are used in powder diffraction (Toraya, 1998), led to unreasonable peak shapes owing to an exaggerated emphasis on the intensities of `valleys' (local minima between peaks).

2.5. Thermal analysis

Simultaneous thermal analysis (STA) measurements in the temperature range 30–900°C were performed with a ∼50 mg sample in a corundum crucible on a NETZSCH STA 449 C Jupiter system coupled with a Aeolos quadrupole mass analyzer. The quartz capillary was kept at 250°C. The measured mass signals were 2 (H₂), 12 (C), 14 (N), 15 (CH₃), 16 (CH₄, O), 17 (OH), 18 (H₂O), 28 (N₂, CO), 32 (O₂) and 44 (CO₂). All measurements were performed under a flowing argon atmosphere (20 ml min⁻¹) and heating rates of 10 K min⁻¹. Base line corrections of the TG curves were carried out by measuring the empty alumina crucible prior to each measurement. Temperature-dependent powder X-ray diffraction measurements (PXRD) were performed on a PANalytical X'Pert PRO diffractometer using a HTK1200 Anton-Paar high-temperature oven chamber mounted on the diffractometer. Prior to the measurement, the sample was finely ground and placed on a glass ceramic (Marcor) sample holder (depth 0.5 mm). The zero point was calibrated with a LaB₆ standard and automatically adjusted during the measurements with a PC-controllable alignment stage. The samples were heated under atmospheric conditions at 10 K min⁻¹ to the respective measurement temperature and kept for 5 min before measurement of each step to ensure temperature stability.

3. Results and discussion

3.1. Crystal chemistry

Mg(H₂O)₂[TeO₂(OH)₄] crystallizes as polytypes composed of distinct crystallo-chemical layers, designated as L_n, where n is a sequential number (Fig. 1). The L_n layers possess (idealized) p4/m symmetry (Kopsky & Litvin, 2006) with a square lattice spanned by (a, b). c₀ is the vector perpendicular to the layer planes with the length of one layer width. Henceforth, all directions and Miller indices will be given with respect to the basis (a, b, c₀). The L_n layers are composed of close to regular [MO₆] (M = Mg, Te) octahedra, which are connected by corners forming sheets (Fig. 2).

Figure 1 A polytype of Mg(H2O)2[TeO2(OH)4] [MDO2 (see §3.4), Pcnm, c = 2c0] viewed down [010]. Layer names according to the crystallo-chemical and the OD description are indicated to the right and left, respectively.

Figure 2 Idealized Ln layer in Mg(H2O)2[TeO2(OH)4] with p4/m symmetry viewed down [001]. Color codes as in Fig. 1. Crosses indicate the possible origins of the adjacent layers up to layer translation.

Both octahedra are located on sites with symmetry 4/m and are tilted by ∼26° in opposite directions about [001], thus leaving rhomboidal voids with a long and a short diameter of ≃5.0 and ≃2.5 Å, respectively. The M positions are alternately occupied with Te and Mg atoms in a checkerboard pattern. The O atoms connected only to Te and Mg are labeled O1 and O2, respectively. The shared O atom is O3 (Fig. 2). The [MgO₆] octahedron is slightly larger than the [TeO₆] octahedron with an average Mg—O distance of 2.056 Å compared to the average Te—O distance of 1.929 Å. Selected distances and angles are compiled in Table 2.

Table 2
Selected interatomic distances d (Å) and angles (°) in Mg(H₂O)₂[TeO₂(OH)₄]

The data are derived from the refinement of §3.8.

Atoms	d	Atoms	Angle
Te—O1	1.972 (2) (2×)	O1—Te—O1	180
Te—O3	1.906 (2) (4×)	O1—Te—O3	90.97 (6)
Mg—O2	2.044 (3) (2×)	O3—Te—O3	90.02 (10)
Mg—O3	2.064 (2) (4×)	O3—Te—O3	178.07 (8)
O1⋯O1	2.9316 (14) (2×)	O2—Mg—O2	180
O1⋯O2	2.9024 (14) (2×)	O2—Mg—O3	90.89 (5)
O2⋯O2	2.8746 (14) (2×)	O3—Mg—O3	90.01 (9)
O3⋯O3	2.525 (3)	O3—Mg—O3	178.21 (7)

The rigid conformation of the octahedral [TeO₆]⁶⁻ anion and the Te—O distances are characteristic for oxotellurates(VI). Reviews on the crystal chemistry of these compounds were given by Kratotochvíl & Jenšovský (1986), Loub (1993), Levason (1997) and Christy et al. (2016). An octahedral coordination is the most common coordination for Mg^II cations, and the average Mg—O distance of 2.057 Å compares well to the maximum of the distribution of Mg—O distances of 2.1 Å given in a survey on Mg—O coordination polyhedra (Blatov et al., 1999; Gagné & Hawthorne, 2016).

Bond valence sums (BVSs) are a useful tool to assign H atoms, in particular for those cases where H atoms cannot be located, e.g. in the presence of heavy atoms, from X-ray diffraction data (Donnay & Allmann, 1970). Neglecting the contributions of H atoms, in the ideal case, the O atoms of H₂O molecules, OH⁻ ions and O²⁻ ions have total BVS of 0, 1 and 2 valence units (v.u.), respectively. Bond valence calculations based on the model of §3.8 with (Brown, 2002) using the parameters R_o = 1.693 Å, b = 0.37 for Mg—O and R_o = 1.917 Å, b = 0.37 for Te—O (Brese & O'Keeffe, 1991) result in BVSs of 0.84 v.u. (O1), 0.36 v.u. (O2) and 1.34 v.u. (O3). It has to be noted that these BVS calculations are slightly skewed by substitutional disorder of the Te and Mg atoms as well as positional disorder of the O atoms, showed by enlarged ADPs.

According to these BVSs, the Te atoms are bonded to two OH⁻ anions (O1) and the Mg atoms to two H₂O molecules (O2). The remaining two H atoms per formula unit are connected to two out of four bridging O3 atoms, amounting to one per rhomboidal void. Thus, the structural arrangement of the compound can be expressed with the connectivity formula . This is in agreement with crystallo-chemical considerations and corresponds to an electronically neutral structure. Moreover, the Te—O bond lengths distribution in the [TeO₂(OH)₄]²⁻ octahedron is in good agreement with those of other structures comprising this type of anion (Weil, 2004, 2007; Weil et al., 2017).

The larger and smaller than ideal BVSs of the H₂O molecules and OH⁻ anions (0.36 and 0.83 versus 0 and 1 v.u.) can be explained by the H atoms being involved in hydrogen-bonding. Indeed, the distances between close O atoms [O1⋯O1 2.9316 (14) Å; O1⋯O2 2.9024 (14) Å; O2⋯O2 2.8746 (14) Å; O3⋯O3 2.525 (3) Å] strongly suggest formation of intra- and interlayer O—H⋯O hydrogen bonds.

3.2. Polytypism

The origin of the L_n+1 layer is related to the origin of the adjacent L_n layer by a translation of or , as indicated in Fig. 2. In these two different stacking possibilities the locations of the Te and Mg atoms are exchanged. An alternation of the two will henceforth be called Te/Mg exchange. Moreover, every L_n layer can appear in two orientations related by m_〈100〉 operations. A change in orientation will be called orientation inversion. The four resulting stacking possibilities are shown in Fig. 3.

Figure 3 The four kinds of (Ln,Ln+1) layer pairs in Mg(H2O)2[TeO2(OH)4], viewed down [001]. The Ln layers are marked by brighter colors and dotted lines. In (c) and (d) the Te and Mg atoms in Ln+1 are exchanged with respect to (a) and (b). In (d) and (c) the Ln and Ln+1 layers do not, in (b) and (d) they do feature orientation inversion. Note that under the idealization of equal Mg—O and Te—O distances, the oxygen substructures are identical in the (a) and (d) as well as the (b) and (c) layer pairs.

3.3. Order–disorder description

The order–disorder (OD) theory (Dornberger-Schiff & Grell-Niemann, 1961) has been devised to explain the common occurrence of polytypism in all classes of compounds. It is based on layers, which do not necessarily correspond to layers in the crystallo-chemical sense (Grell, 1984). The crucial point in an OD description is that pairs of adjacent layers are equivalent, which corresponds to the vicinity condition (VC). However, pairs of adjacent layers without [Figs. 3(a) and 3(c)] and with orientation inversion [Figs. 3(b) and 3(d)] are not equivalent and therefore violate the VC. The particular layer choice as described here is therefore not of the OD type.

An OD description can nevertheless be achieved by `slicing' the structure into two kinds of layers, designated as A¹ and A² (Fig. 1, left). The structure then belongs to a tetragonal category IV OD family built of two kinds of non-polar (with respect to the stacking direction) layers.

The OD groupoid family symbol reads as

according to the notation of Grell & Dornberger-Schiff (1982).

The first line of the symbol gives the name of the layers, the second their symmetry and the third one possible arrangement of adjacent layers. Note that in OD theory, layer group symbols with five directions are sometimes necessary to describe tetragonal OD groupoid families. Here, because it is not necessary to distinguish between the [100] and [010] directions, as well as the [110] and directions, the usual symbols can be used.

The A¹ layers possess p4/m symmetry. They are built of the [MgO₆] and [TeO₆] octahedra [Fig. 4(a)] and the disordered hydrogen atom belonging to O²⁻/OH⁻ in the rhombohedral void. The A² layers are built of the OH⁻ anions (O1) and H₂O molecules (O2) that connect the L_n layers [Fig. 5(a)]. Thus, the O1 and O2 atoms are located at the layer interfaces and belong to both OD layers. The layer symmetries were deduced under the assumption of a disordered hydrogen-bonding network.

Figure 4 (a) OD layer A^1 of Mg(H2O)2[TeO2(OH)4] and (b) superposition of four A^1 layers in the family structure. Te, Mg and O atoms are represented by yellow, blue and red spheres of arbitrary radius. The O1 and O2 atoms above Te and Mg (with respect to [001]) are omitted for clarity. Disordered 1:1 Te:Mg positions are represented by gray spheres. In (b) the coordinates of the O3 atom have been idealized to fulfill the equation x + y = ½.

Figure 5 (a) OD layer A^2 of Mg(H2O)2[TeO2(OH)4] and (b) superposition of four A^2 layers in the family structure. OH^− anions and H2O molecules are represented by black and white spheres of arbitrary radius. A gray sphere is an equal superposition (assuming equal Te—O and Mg—O distances), where + and − symbols mark groups located above and below the drawing plane, respectively.

The third line of the symbol indicates that, in one possible arrangement, the origins of the A¹_n and A²_n+1 layers are spaced by ra + sb + c₀/2. According to the stacking rules described above, (r, s) adopt the values or equivalently , i.e. the 4_[001] and 2_[001] axes of the A¹ and A² layers coincide. Note that in contrast to many other OD families, here the parameters adopt a precise value because adjacent layers share common atoms (O1 and O2) located on special positions.

The NFZ relationship (Ďurovič, 1997) is a formalism to determine the alternative stacking possibilities in a family of OD structures. It is based on the groups of those operations of the A_n layers that do not reverse the orientation with respect to the stacking direction (λ-τ-POs according to the OD terminology). For the A¹ and A² layers, is p4 and pmm2, respectively. Because the adjacent layers are not equivalent, the NFZ relationship reads as , where designates the index of the subgroup of . For any pair of adjacent layers, .

For an contact, Z = N/F = [p4 : p112] = 2. Thus, given an A_n¹ layer, the adjacent A_n+1² layer can appear in two orientations (with pmma and pmmb symmetry), which are related by the fourfold rotation of the A_n¹ layer. For an contact, Z = N/F = [pmm2 : p112] = 2. Given an A_n² layer, the adjacent A_n+1¹ layer can likewise appear in two positions, which in this case are related by the m_〈100〉 reflections of the A_n² layer.

By following these stacking rules, an infinity of polytypes can be constructed, which are equivalent to the non-OD polytypes described in the previous section. The usefulness of the OD description does not only lie in the concise symmetry classification. It also sheds light on the crystallo-chemical reasons of the polytypism by splitting them into two distinct contributions. On the one hand (), the orientations of the hydrogen-bonding network to both sides of the [TeO₆] and [MgO₆] octahedra may be the same, or different. On the other hand (), the inter-layer hydrogen bonding independent of the orientation of the octahedral sheets.

3.4. Maximum degree of order polytypes

Polytypes of a maximum degree of order (MDO) are a central concept of OD theory (Dornberger-Schiff, 1982; Dornberger-Schiff & Grell, 1982). MDO polytypes cannot be decomposed into simpler polytypes, i.e. into polytypes composed only of a selection of pairs, triples or any n-tuples of adjacent layers. Experience shows that the majority of macroscopically ordered polytypes are of the MDO type.

There are two kinds of triples, namely with and without orientation inversion. Moreover, there are two kinds of triples, namely with and without Te/Mg exchange.

The combination of these triples results in four MDO polytypes:

MDO₁: never orientation inversion, never Te/Mg exchange, B112/m, c = 2c₀;

MDO₂: always orientation inversion, never Te/Mg exchange, Pcnm, c = 2c₀;

MDO₃: never orientation inversion, always Te/Mg exchange, I4₁/a, c = 4c₀;

MDO₄: always orientation inversion, always Te/Mg exchange, , c = 4c₀.

All other stacking arrangements can be divided into fragments of MDO polytypes, which therefore represent the `alphabet' of an OD family.

Atomic coordinates for all four MDO polytypes are listed in Table 3.

Table 3
Fractional coordinates, multiplicity, Wyckoff letter and site symmetry in the four MDO polytypes and the family structure of Mg(H₂O)₂[TeO₂(OH)₄]

The coordinates were derived from the I4₁/a (MDO₁ and MDO₃), (MDO₂ and MDO₄) and family structure refinements described in §3.8.

Atom	x	y	z	Multiplicity, Wyckoff letter, site symmetry
MDO1 (B112/m, c = 2c0)
Te	0	0	0	2, a, 2/m
Mg	½	½	0	2, d, 2/m
O1	0	0	0.19082	2, g, ..2
O2	½	½	0.19786	2, g, ..2
O3	−0.1563	−0.3211	0	4, i, ..m
O3′	−0.3211	0.1563	0	4, i, ..m
MDO2 (Pcnm, c = 2c0)
Te	0	0	0	2, a,
Mg	½	½	0	2, c,
O1	0	0	0.19074	4, e, ..2
O2	½	½	0.19780	4, f, ..2
O3	−0.1563	−0.3214	0	4, h, ..m
O3′	−0.3214	0.1563	0	4, h, ..m
MDO3 (I41/a, c = 4c0)
Te	0	0	0	4, a,
Mg	½	½	0	4, b,
O1	0	0	0.09541	8, e, 2..
O2	½	½	0.09893	8, e, 2..
O3	−0.3211	−0.1563	−0.0020	16, f, 1
MDO4 (, c = 4c0)
Te	0	0	0	4, a,
Mg	½	½	0	4, b,
O1	0	0	0.09537	8, c, 2..
O2	½	½	0.09890	8, c, 2..
O3	−0.3214	−0.1563	−0.0015	16, e, 1
Family (F4/mmm, c = 2c0)
Te/Mg	0	0	0	2, a, 4/mmm
O1/O2	0	0	0.19445	4, e, 4mm
O3	0.3318	0.1682	0	8, i, m2m.

3.5. Family structure

The family structure of an OD family is a fictitious structure in which all stacking possibilities are realized to the same degree. It plays an important role in the elucidation of OD structures. The family structure of Mg(H₂O)₂[TeO₂(OH)₄] has F4/mmm symmetry (non-standard setting of I4/mmm) with c = 2c₀ (coordinates in Table 3).

For a fixed A¹_n layer, the adjacent A²_n+1 layer can appear in two orientations related by the 4_[001] operation. Each of these two orientations gives rise to two orientations of the A¹_n+2 layer, which are related by the m_〈100〉 operations of the A²_n+1 layer. Thus, in the family structure the A¹ layers are an equal superposition of four positions (Te/Mg disorder and orientation disorder) with c4/mmm (non-standard setting of p4/mmm) symmetry [Fig. 4(b)].

According to analogous reasoning in the A² layers of the family structure, the OH⁻ anions and H₂O molecules are disordered in a 1:1 ratio [Fig. 5(b)]. These disordered layers possess c4/emm (non-standard setting of p4/nmm) symmetry.

3.6. Diffraction pattern

The diffraction pattern of Mg(H₂O)₂[TeO₂(OH)₄] features rods with sharp reflections and rods with broader reflections on top of prominent one-dimensional diffuse scattering (Fig. 6). Such diffraction patterns are characteristic for polytypes with translationally equivalent layers (Jeffery, 1953; Ferraris et al., 2008), and were the inspiration for the name `OD' (Bragg reflections: order; streaks: disorder).

Figure 6 The h = 0…3 planes of reciprocal space of Mg(H2O)2[TeO2(OH)4] reconstructed from image-plate data. (a) h = 0, (b) h=1, (c)h =2, (d) h = 3.

In Mg(H₂O)₂[TeO₂(OH)₄], the L_n layers are not translationally equivalent, since they can appear in two orientations. As will be shown below, in this case the reason of the rods lacking diffuse scattering lies in the particular makeup of the L_n layers, namely the similar size of the [MgO₆] and the [TeO₆] octahedra.

In the reciprocal basis , the structure factor F(hkν) of a polytype can be calculated as the sum of the structure factors F_n(hkν) of the individual L_n layers:

Since the translation lattices of all layers are spanned by (a, b), F_n(hkν) is only non-zero for . The structure factor F_n(hkν) can be decomposed into the contributions of the O3 atom and of the remaining atoms (Te, Mg, O1, O2):

The origin of the L_n layer can be written as

with and α₀ = β₀ = 0. Since the origin shift from L_n to L_n+1 is either a/2 + c₀ or b/2 + c₀, α_n + β_n is even, if and only if, n is even, which can be expressed by

with .

The Mg, Te, O1 and O2 atoms are not affected by orientation inversion, since the eigensymmetry of their (layer group) orbits is p4/mmm, which contains the reflection relating both orientations. These parts of the layers are therefore obtained from the L₀ layer by translation along o_n. According to equations (3) and (4), F^M_n can therefore be written in terms of F^M₀ as

Note that since Mg, Te, O1 and O2 are located on fourfold rotation axes, their displacements are isotropic in the (001) plane and, therefore, disregarding desymmetrization, the reflection at [100] has no influence on their (harmonic) ADPs.

The orientation of the L_n layer will be described by ω_n = 0, 1, . If O3 is located on the line, which is perfectly realized if d(Te—O3) = d(Mg—O3), ω_n = 1 corresponds to an additional translation of (a + b)/2 with respect to o_n. If the displacement of the O3 atom is likewise isotropic in the (001) plane, F^O_n can be written in terms of F^O₀ as

If h + k is even, then (h + k)β_n and (h + k)(β_n + ω_n) are likewise even and equations (5) and (7) simplify to

and

and therefore

and

where δ is the Dirac delta distribution. Note that the last equals sign represents an abuse of notation as the given function series does not converge at any point [technically, the series converges in the distributional sense (Bricogne, 2010)].

In summary, on rods h + k even only sharp reflections are observed at ν = l/2, , where h, k and l are all even or all odd. This corresponds to the diffraction pattern of a crystal with a tetragonal F-centered (tF) lattice with the centered reciprocal basis . These reflections correspond to the diffraction pattern of the family structure (§3.5) and are called the family reflections. All stacking arrangements, ordered or disordered, contribute equally (proportional to their volume fraction) to these reflections, since neither α_n, β_n nor ω_n contribute to equation (12).

On rods h + k odd the simplifications above do not apply and diffraction intensities can appear at arbitrary positions. Bragg reflections on these rods are called characteristic reflections, because they are generated only by certain polytypes. The characteristic reflections of MDO_1/2 are located at ν = l/2, , those of MDO_3/4 at , .

The calculations above were derived under the assumption that d(Te—O3) = d(Mg—O3), whereas the actual structure deviates from this assumption [1.906 (3) versus 2.064 (2) Å]. Moreover, ordered polytypes typically feature desymmetrization (Ďurovič, 1979). For example, in the MDO_3/4 polytypes, the O3 atom is located slightly off the z = 0 reflection plane of the p4/m layer symmetry (Table 3). Distinctly enlarged ADPs of the O1 and O2 atoms show that they are located on the fourfold axis (which is a twofold axis in the actual MDO_3/4 polytypes) only on average (Fig. 7). These deviations may lead to violations of the systematic non-crystallographic absences, namely faint streaking and very weak characteristic reflections on h + k even rods.

Figure 7 Fragment of the Mg(H2O)2[TeO2(OH)4] structure, showing the ADPs as ellipsoids drawn at the 75% probability level (Te: yellow, Mg: blue, O: red). Data taken from the refinement.

3.7. Rods with insignificant contribution of O3

To differentiate between the effects of orientation inversion and Te/Mg exchange on the diffraction pattern, it is useful to note that the fractional coordinates x and y of the O3 atom, which is essentially the only atom affected by orientation inversion, are close to and , respectively. If the O3 atom is idealized as being located on such a position, the L₀ layer contains up to translation two O3 atoms at and the two atoms obtained by inversion at the origin. If, moreover, the displacements of the O3 atom are considered as being isotropic in the (001) plane [], then the structure factor F^O₀ is

where f^O(hkν) is the atomic form factor of O. Note that the structure factor is real and contains only cos terms owing to the inversion at the origin. If h is divisible by three, i.e. h = 3h′, , this expression simplifies for rods h + k odd to

(h′ is even, if and only if, h is even and therefore k − h′ is odd). The same argument can be applied to rods with k divisible by three. Thus for h or k divisible by three, equation (2) simplifies to

and equation (1) can ultimately be written as

The variable ω_n, which describes the orientation of the octahedra, does not affect rods h + k odd with either h or k divisible by three, and any significant diffuse scattering or Bragg reflections on these rods are due to the arrangement of the Te and Mg atoms.

To illustrate the effect in absolute terms, plots of and against ν are given in Fig. 8 for the 10ν and 12ν rods. Indeed, for 10ν the contribution of F^O₀ is negligible when compared to F^M₀. On the other hand, 12ν features significant contribution at low scattering angles. In particular, this rod (including symmetry equivalents) has the highest relative contribution of F^O₀.

Figure 8 Plots of and against ν for the 10ν and 12ν rods. Only ν ≥ 0 are shown, because the structure factors are essentially symmetric by reflection at the ν = 0 plane. is practically 0 and therefore barely to be seen at the bottom of the chart.

3.8. Classical refinements

To determine atomic coordinates and ADPs, classical independent atom model refinements were performed. In a first refinement, only the family reflections were considered. Excellent reliability factors are thus obtained (Table 4). In the family structure, Te/Mg exchange and orientation inversion are realized in 50% of the layers. In principle, the O3 atom is disordered over four positions. Nevertheless, only two positions could be resolved, because the Te—O3 and Mg—O3 distances are nearly equal. Likewise, the O1 and O2 atoms could not be separated without introduction of distance restraints and therefore were refined as a single O1/O2 position.

Table 4
Comparison of the refinements

The MDO₃:MDO₄ ratio was derived from the occupancy of the O3/O3′ positions. The (MDO_1/2):(MDO_3/4) ratio was determined from the occupancy ratio of the Te/Mg positions.

	Family	1:1 MDO3/4	MDO3	MDO4
Space group	F4/mmm	I41/amd	I41/a
MDO3:MDO4	1:1	1:1	64:35 (3)	52.8:47.2 (12)
MDO1/2:MDO3/4	1:1	9.2:90.8 (12)	15.4:84.6 (8)	13.6:86.4 (6)
R[F^2 > 3σ(F^2)], wR(F)	0.0121, 0.0313	0.0204, 0.0782	0.0176, 0.0678	0.0166, 0.0581
S	1.33	1.61	1.34	1.17
Δρmin, Δρmax (eÅ^−3)	−0.45, 0.27	−0.90, 1.23	−0.71, 0.93	−0.70, 0.80
Coefficient of extinction (Becker & Coppens, 1974)	490 (110)	800 (200)	960 (170)	750 (140)
No. of parameters	11	24	28	27
Twin operation	–	–	m[100]
Twin volume fractions	–	–	50.4:49.6 (6)	51:49 (9)

On top of the lines of diffuse scattering at h + k odd are located elongated peaks where the characteristic reflections of MDO_3/4 are expected (Fig. 6). No peaks corresponding to MDO_1/2 were observed (though see §3.13). One has to realize that treating these peaks as Bragg reflections in classical refinements will inevitably introduce systematic errors.

Owing to the systematic non-space group absences (§3.6), reflection conditions cannot differentiate between MDO₃ (I4₁/a) and MDO₄ (). Moreover, owing to diffuse scattering on rods h + k odd, intensities in violation of the I-centring are observed. Thus, classical space group determination is unreliable and the diffractometer software strongly suggests the space group I4₁/amd (c = 4c₀), which is the space group of a 1:1 superposition of MDO₃ and MDO₄.

The first model was generated and refined using this I4₁/amd symmetry, where the O3 atom is disordered with a 1:1 occupation ratio about the m_[100] reflection plane. To achieve satisfying residuals, occupational disorder of the Te and Mg atoms (with Mg′ and Te′) had to be introduced, corresponding to a contribution of MDO_1/2 fragments.

Based on the refined model in I4₁/amd, the symmetry was reduced by an index of 2 to I4₁/a (MDO₃) and (MDO₄), respectively. The linear parts of the lost operations were retained as the twin law and the twin volume ratio was refined. The disordered O3 position was split in both cases into two distinct positions (O3 and O3′). The coordinates and ADPs of O3 and O3′ were constrained to be equal with respect to the m_[100] operation and the occupancies were refined and constrained to a sum of 1. A comparison of the refinements is given in Table 4. The volume fraction of MDO_3/4 (as opposed to MDO_1/2) was derived from the occupancy of Te as |2occ(Te) − 1|. Likewise, the volume fraction of the major domain of the MDO₃/MDO₄ pair was derived as |2occ(O3) − 1| (see Appendix B).

According to these refinements, there was ∼10–15% of MDO_1/2 present in the crystal under investigation. Estimating the MDO₃:MDO₄ ratio is more difficult. According to the refinement with the best reliability factors (), there are approximately equal amounts of MDO₃ and MDO₄, which would correspond to a 50% chance of orientation inversion. The I4₁/a refinement on the other hand suggests an MDO₃:MDO₄ ratio of ∼2:1, which shows the difficulty of deriving these values from routine refinements. The fundamental problem is that a disordered stacking is in general not equivalent to a superposition of MDO polytypes.

Allotwinning, i.e. the association of macroscopic domains of distinct polytypes (Nespolo et al., 1999), was ruled out owing to diffuse scattering. Indeed, such models did not lead to improved reliability factors. Likewise, placing the characteristic and family reflections on different scales to avoid the Ďurovič effect (Nespolo & Ferraris, 2001) led to unreliable refinements because the ratio of polytypes and the ratio of the scales correlate (Hans et al., 2015). As will be shown below (§3.10) Te/Mg exchange does occur and thus the single-scale refinements are preferred, even though the quantification of Te/Mg exchange is inaccurate.

In summary, neither the amount of MDO_1/2 nor the MDO₃:MDO₄ ratio can be quantified reliably with routine refinements, demonstrating the inherent difficulties of structurally characterizing such compounds. Nevertheless, these refinements are crucial to determine Mg—O and Te—O distances.

3.9. Disorder model

To quantify the diffuse scattering, a simple growth model was derived from the OD interpretation given in §3.3. The crystal is described as an alternating succession of A¹ and A² OD layers. According to the OD description, pairs of adjacent OD layers are geometrically equivalent, but triples may differ. Therefore, in the simplest growth model the A_n layer depends on the A_n−1 and A_n−2 layers. Since there are two kinds of triples and two kinds of triples (§3.4), this model is fully determined by two parameters. P_MgTe describes the probability of without Mg/Te-inversion and P_orient the probability of triples without orientation inversion. In some cases, it will be more convenient to express these probabilities in terms of the correlation coefficients

This two-parameter model is sufficient to describe all four MDO polytypes and also of equal overlays of MDO polytypes, as listed in Table 5.

Table 5
Extreme growth model parameters and the corresponding polytypes. Note that the statistical stackings (P_MgTe = 0 or P_orient = 0) are strictly speaking not overlays or the family structure, but behave as such

Polytype	PMgTe	cMgTe	Porient	corient
MDO1	1	1	1	1
MDO2	1	1	0	−1
MDO3	0	−1	1	1
MDO4	0	−1	0	−1
MDO1/2	1	1	½	0
MDO3/4	0	−1	½	0
Family structure	½	0	½	0

In this trivial model, each layer triple is considered independent of the previous triple. In more refined models, the orientation–inversion probability could depend on the occurrence of Mg/Te inversion and vice versa. Additional parameters would then be required.

Growth models are conveniently expressed as Markov chains (Welberry, 2010). The above model corresponds to the four-state Markov chain

where each step corresponds to a new triple of OD layers, which has two OD layers in common with the previous triple. This Markov chain has a period of two since an A¹ layer is only added after every second step (and likewise for A²). Such chains are developed into two (or more for higher periods) independent chains, here from the nth triple to the n+2nd triple. These two Markov chains are most conveniently expressed in terms of the crystal-chemical L_n layers:

The first Markov chain describes the relation of the origin of the L_n and L_n+1 layers and the second chain the orientation of the L_n layer. The chains are independent, because one OD layer triple does not depend on the previous triple. Each chain can be considered as an independent nearest-neighbor model, since the o_n depends only on o_n−1 and ω_n on ω_n–1.

For P_MgTe, P_orient ≠ 0,1, the Markov chains converge to the equilibrium states P(Δo_n = a/2) = P(Δo_n = b/2) = P(ω_n = 0) = P(ω_n = 1) = ½, i.e. after an infinity of layers, both origin shifts and both layer orientations are equally likely. In the following only this general case will be considered.

3.10. Diffuse scattering

To calculate the diffraction pattern of disordered structures, it is advantageous to directly calculate the intensity I(hkν) = |F(hkν)|² in terms of pair correlations between layers (Welberry, 2010):

where an overline designates the complex conjugate. The orientation of the L_n layer is flipped with respect to the L₀ layer if ω_n = 1. To express the structure factor of such a layer, it will be related to the structure factor of the mirrored L₀ layer:

The hkν argument of F will henceforth be omitted for brevity.

The diffraction intensity can then be expressed in terms of probabilities:

where expresses the probability that the origins of the L_n and L_n+Δn layers are separated by Δα_na/2 + Δβ_nb/2 + Δnc (up to a full layer lattice translation). and are the probabilities that the L_n and L_n+Δn layers possess the same, respectively opposite, orientation. , the sum over Δα and Δβ, is the pair-correlation function of layers spaced by . It should be stressed that equation (29) is only valid for an equal probability of both layer orientations (P_orient ≠ 0, 1, large domain size) and independence of both Markov chains. On the flip side, it is valid for more complex growth models with interactions over more than one layer width.

From the stacking rules it follows that = = 0 for Δn even and = = 0 for Δn odd. Since, as has been shown above, significant diffuse scattering is only observed on rods h + k odd, let us concentrate on these. Then, the exponential factor of the Δα = Δβ = 1 terms in equation (29) is = . Factoring out the probabilities, for Δn even we thus obtain

In analogy, for Δn odd and h + k odd, = (if k is odd h is even and vice-versa) and therefore

Let us now derive the `pair distribution' probabilities. Obviously, the starting state of the growth model is P^0,0₀ = 1 and P^1,1₀ = 0. As has been noted above, in non-degenerate cases (P_MgTe ≠ 0,1), the equation (23) converges to an equilibrium state where the origin shifts Δo_n = a/2+ c₀ and Δo_n = b/2 + c₀ are equally likely and therefore P^1,0₁ = P^0,1₁ = ½. Repeated application of equation (23) to theses initial states gives the general case (see Appendix C):

Note that for negative Δn, the same reasoning applies and therefore the absolute value of Δn is used in the exponents. In analogy, according to the Markov chain equation (24) the probabilities describing the orientations are

By substituting equation (35) into equation (32) it follows that s_Δn = 0 for odd Δn. Note that this is only valid for the simple nearest-neighbor model of equation (23). In more general growth models, these terms adopt non-zero values.

For even Δn, from equations (33) and (34) it follows that − = (c_MgTe)^|Δn|/2 and equation (31) becomes

Ultimately, the intensity on rods h + k odd therefore is [see equation (30)]

where m = Δn/2 and

By identifying two geometric series (see Appendix D), an analytical expression of I(hkν) can be given as

To avoid the unwieldy expressions in the parentheses, we will introduce the function family

which describes the shape of one-dimensional diffuse scattering produced by a structure with a simple nearest-neighbor correlation of −1 < c < 1 (Welberry, 2010). d_c(x) is generally (except for c = 0) a function with periodicity 1, featuring peaks which are sharper for increasing |c|. For |c| approaching 1, d_c(x) converges to a Dirac comb with sharp reflections for integer x (c → 1) or half-integer x (c → −1). For c = 0, d_c is the constant function d₀(x) = 1.

Using d_c, equation (42) simplifies to

which shows that the diffuse scattering is the sum of two independent shape-functions of the nearest-neighbor correlation c_MgTe and c′. The factor corresponds to the (hypothetical) intensity of an superposition of both orientations of the L₀ layer and to the intensity of the difference of the electron density of these two orientations.

Since c′ depends on the square of c_orient [equation (41)], c_MgTe and c′ are of the same sign [sgn(c_MgTe) = sgn(c′)]. Thus, the location of the peaks depends only on c_MgTe, but not on c_orient. For c_MgTe > 0, I(hkν) has peaks at ν = l/2, and for c_MgTe < 0 at ν = l/2 + , as is expected for MDO_1/2-like and MDO_3/4-like stacking arrangements, respectively.

Moreover, note that from |c_orient| < 1 follows that |c′| < |c_MgTe| and therefore ordering of the orientation inversion can never lead to sharper peaks for a given c_MgTe, whereas its disorder can lead to more diffuse peaks.

But most remarkably, under the given assumptions (nearest-neighbor model, negligible desymmetrization, c_MgTe, c_orient ≠ ± 1) the diffuse scattering is identical for pairs of c_orient with the same absolute value.

3.11. Estimation of the correlation coefficients

Assuming the idealization d(Te—O3) = d(Mg—O3), orientation inversion corresponds to a translation of O3 by (a + b)/2 (see § 3.6). Using the decomposition F₀ = F₀^M+F₀^O, then is

which for h + k odd becomes and consequently

Thus, equation (44) becomes

Conveniently, as has been shown above, is negligible for rods h + k odd with h or k divisible by three (Fig. 8). Thus, these rods can be used to estimate c_MgTe with only a negligible contribution of c_orient.

Fig. 9(a) gives I(10ν) plots for different values of c_MgTe calculated using only the term of equation (48). To estimate c_MgTe, a simultaneous LS optimization was performed on the rods listed in Table 6. Fig. 9(b) shows the result of the LS optimization without convolution of the experimental peak shape for the 01ν rod. As expected, an additional convolution with the experimental peak shape results in a slightly more negative correlation c_MgTe (−0.353 versus −0.338). Since the refinements without convolution result generally in better fits (Table 6), we will henceforth assume the latter value.

Table 6
Residuals of the concurrent refinement of the h + k even rods with h or k divisible by three

Rod	Rp with convolution	Rp without convolution
All	0.022	0.019
01ν	0.025	0.021
03ν	0.020	0.018
05ν	0.016	0.014
10ν	0.020	0.016
16ν	0.014	0.013
23ν	0.017	0.014
30ν	0.022	0.019
32ν	0.018	0.016
34ν	0.019	0.017
36ν	0.018	0.017
43ν	0.018	0.016

Figure 9 Intensity I(10ν) of the 10ν rod (a) calculated for various cMgTe values and (b) with cMgTe optimized against experimental data. Intensity is absolute, i.e. zero intensity is at the bottom of the chart.

The agreement of the experimental and calculated curves is reasonable, though not perfect as the experimental peaks are somewhat narrower. Even though a stronger negative correlation c_MgTe leads to narrower peaks, it is in disagreement with the strong diffuse scattering between the peaks. We suppose that the sample is composed of domains with different c_MgTe values, some with stronger and some with weaker correlations. A model taking into account interactions over more than the nearest-neighbor can be ruled out, since such models produce valleys of different shapes (Welberry, 2010).

Given c_MgTe, |c_orient| can be determined from the h + k odd rods with neither h nor k divisible by three. Fig. 10(a) gives I(12ν) plots with c_MgTe = −0.338 derived from the 10ν rod and |c_orient| = 0, 0.9, where the contribution of the term is shown separately. The 12ν rod features the highest relative contribution of the O3 atom to the scattering intensity (§3.6). Even on this rod and with the extreme values of |c_orient|, the effect on the peak shape is rather subtle.

Figure 10 Intensity I(12ν) of the 12ν rod with fixed cMgTe = −0.338 (a) calculated for |corient| = 0.9 and |corient| = 0.0 and (b) with |corient| = 0 optimized against experimental data. Intensity is absolute. Additionally, the contributions of (a) the term and (b) the and terms are shown.

Independent LS optimization with fixed c_MgTe yielded a zero correlation of |c_orient| for all rods listed in Table 7. The refinement of the 12ν rod is displayed in Fig. 10(b). Again, without convolution of the experimental peak broadening slightly improved residuals are obtained. However, in both cases a zero c_orient is derived. We conclude that the orientation of the [MgO₆] and [TeO₆] octahedra is mostly random, which means that the problem of identical diffraction for pairs of structures becomes a moot point, since the sign of c_orient ≈ 0 is irrelevant.

Table 7
Residuals of the individual refinements of the h + k even rods with h or k divisible by three

Rod	Rp with convolution	Rp without convolution
12ν	0.014	0.013
14ν	0.010	0.008
21ν	0.016	0.014
25ν	0.016	0.016
41ν	0.017	0.016
45ν	0.013	0.013

3.12. Diffuse scattering on h + k even rods

As has been argued above, pairs of structures with c_orient of the same absolute value produce the same diffraction intensity on h + k odd rods. Moreover, under the idealization of d(Te—O3) = d(Mg—O3) the h + k even rods are identical for all stacking arrangements. Thus, such pairs of idealized structures can be considered as homometric.

Since these assumptions are not perfectly realized, very weak diffuse scattering is likewise observed on rods h + k even (Fig. 11). In principle, this could be used to determine the sign of c_orient.

Figure 11 1kl layer with intensities scaled to make weakest effects visible.

The diffuse scattering on these rods can be derived in analogy to §3.10. However, for h + k even the equalities exp[2πi(h/2+k/2+Δnν)] = exp[2πiΔnν] and exp[2πi(h/2+Δnν)] = exp[2πi(k/2+Δnν)] hold, since h and k are either both even or both odd. Conveniently, these terms can be generalized to exp[2πi(Δnh/2+Δnν)] for even and odd Δn (see §3.6). Factoring out the probabilities of equation (29), the leading factors in the equations analogous to equations (31) and (32) are = = 1. Ultimately, the general expression for s_Δn on rods h + k even is

which also holds for more general growth models. Substituting the probabilities of equations (36) and (37), the intensity I(hkν) is (setting m = Δn)

The first term corresponds to the Bragg peaks of the family structure, again committing the abuse of notation. For h + k even, equation (45) becomes and therefore

Thus, as shown in §3.6, under the assumption d(Te—O3) = d(Mg—O3), only family reflections are observed on rods h + k even. Non-equal Te—O and Mg—O distances lead to a non-vanishing and thus diffuse scattering as described in the second term of equation (51). For distinctly positive c_orient one would expect additional peaks on top of the family reflections and valleys between the family reflections. For negative c_orient, additional peaks would be observed between the family reflections. This is consistent with the MDO₁ and MDO₂ polytypes: the lattice of the former (c_orient = 1) does not allow for reflections between family reflections owing to the B-centering, whereas the latter (c_orient = −1) has a primitive Bravais lattice and features systematic non-space group absences in the idealized case, which should be observable for noticeable deviations therefrom.

In the actual diffraction pattern (Fig. 11), the minute streaks are basically structureless, confirming the low correlation c_orient ≈ 0. Tiny sharp spots are observed, which can however be explained by λ/2 radiation. To prove this assignment, a Mg(H₂O)₂[TeO₂(OH)₄] crystal was quickly scanned using synchrotron radiation, which confirmed the structureless diffuse scattering on rods h + k even (Fig. 12).

Figure 12 11ν rod extracted from synchrotron data. The intensity was scaled up to show the minute diffuse scattering base line. Intensities are absolute.

It has to be noted that equation (51) does not allow for a simple quantitative estimation of the diffuse scattering in cases where c_orient ≠ 0, because the |F₀ − factor does not only represent the deviation of the equidistance of O3 from Mg and Te, but also generally the deviation from the idealized p4/m symmetry, which certainly exists as shown by enlarged ADPs. Moreover, the origin difference between adjacent layers might deviate slightly from the ideal Δo = a/2 + c₀/2 or Δo = b/2 + c₀/2, which would likewise invalidate the reasoning in §3.5 and lead to faint diffuse scattering.

All these deviations from the idealized model can not be simply derived from single-crystal experiments, since they will differ depending on the adjacent layers. Owing to missing structural data of all MDO polytypes, these would have to be derived by relaxation, for example with DFT methods.

In any case, this is of no concern here, since there appears to be no significant c_orient.

In summary, we propose a model with a negative correlation of the Mg/Te stacking c_MgTe ≈ −0.34 and a c_orient ≈ 0 correlation of the orientation, with the caveat that the peak shape is not described perfectly, as the crystals might be composed of domains with varying c_MgTe.

3.13. Rearrangement of the crystal structure over time

The synchrotron measurement described in the previous section was performed on a newly isolated crystal seasoned for six years at 15–35°C in a closed glass vial containing residual gel from the synthesis. Much to our surprise, in this experiment additional sharp characteristic reflections were observed on rods h + k odd at integer and half-integer ν-values [Fig. 13(a)], as would be expected for MDO_1/2 polytypes. To confirm the appearance of ordered domains, a different crystal was measured in-house and likewise featured sharp reflections with h + k odd [Fig. 13(b)], though only half as many.

Figure 13 1kν plane of crystals seasoned for six years collected (a) at the X06DA beamline and (b) the IPDS in-house system.

For ordered MDO_1/2 polytypes (c_MgTe = 1), the simplifications of §3.10 do not apply and therefore macroscopic MDO₁ and MDO₂ polytypes produce distinctly different intensities on rods h + k odd. The sharp reflections of the second crystal can be indexed with the B-centered cell of the MDO₁ polytype [h + 2ν even, Fig. 14(a)]. The location of the sharp reflections of the first crystals could in principle be explained by the MDO₂ polytype. According to structure factor calculations, for MDO₂ one would expect alternately strong and weak characteristic reflections at opposite positions on 12ν and rods. In the actual crystal though, the strong and weak characteristic reflections appear at the same ν-values [Fig. 14(b)], which means that the characteristic reflections are probably due to two MDO₁ orientation states, related by a fourfold rotation.

Figure 14 Comparison of the 12ν and ν rods of crystals seasoned for six years measured at (a) the IPDS in-house system and (b) the X06DA beamline.

The shape of the diffuse scattering essentially stays the same during seasoning of the crystals (Fig. 15). We conclude that the disordered domains slowly convert to ordered MDO₁ polytypes.

Figure 15 Comparison of the 12ν rods of a freshly synthesized crystal and a crystal seasoned for six years, both measured at the IPDS in-house system.

We recently measured three newly isolated crystals of the same synthesis batch after an additional one year time-period and all of them clearly contained ordered MDO₁ fragments. One of the crystals was twinned by fourfold rotation. The amount of diffuse scattering did not decrease significantly compared to the previous year. Thus, the kinetics and preconditions of the transition are not yet understood.

3.14. Thermal behavior

The thermal decomposition of Mg(H₂O)₂[TeO₂(OH)₄] is connected with a multi-step mechanism between 30–900°C. The hydrous phase is stable up to a temperature of ∼160°C in the oven chamber (Fig. 16; PXRD), followed by an amorphization. According to the TG/DTA curves (Fig. 17; STA), the onsets of the associated mass loss and the endothermic effect due to dehydration are at ∼195°C. We ascribe the different temperatures of the Mg(H₂O)₂[TeO₂(OH)₄] stability field to the different timescales of the two measurement techniques. Whereas the temperature-dependent PXRD measurement is slow due to stepwise heating rates and long measurement times, the STA measurement is much faster with continuous heating rates and much shorter measurement times. The mass loss of ∼25% up to a temperature of 500°C is due to release of water and oxygen according to the mass spectra. The amorphous phase remains up to 510°C where first reflections appear, indicating a crystallization of new phases as shown by a two-step exothermal effect at ∼550°C, also associated with a release of small amounts of water (onset DTA first step 545°C, second step 575°C). The diffuse nature of the reflections in the stability field between ∼510°C and 570°C makes a clear assignment difficult. Besides weak reflections that could be unambiguously assigned to the formation of Mg₃[TeO₆], a relationship with trirutile-type Co[Sb₂O₆] (Reimers et al., 1989) could be derived from the strong reflections. Given the very similar ionic radii for Co²⁺/Mg²⁺ and Sb⁵⁺/Te⁶⁺, respectively, this could point to possible existence of a mixed-valent Te⁴⁺/Te⁶⁺ compound with composition Mg[Te₂O₆]. The assumption of the existence of such a mixed-valent phase is supported by the detection of oxygen in the mass analyzer during the preceding decomposition step. The assumed mixed-valent phase transforms above 570°C into a phase for which the diffraction pattern could be related to Mg[TeO₄] (Sleight et al., 1972), which is stable until ∼660°C. Above this temperature another phase is formed for which a relation to a known phase could not be made. Above ∼710°C only the reflections of Mg₃[TeO₆] are visible, associated with another small mass loss of ∼3% in the TG curve under further release of oxygen. Above this temperature no further mass loss is observed until 900°C. We currently cannot interpret the significant endothermal effect in the DTA curve in this temperature interval (onset 824°C). Since no further mass loss is observed here, this effect could be related either to a structural phase transition of (parts of) the remaining material or to a melting of an amorphous content thereof. Both effects cannot be related with the temperature-dependent diffraction pattern, e.g. by splitting or vanishing of reflections or a significantly broader background. It should be noted that the same material heated up to 1000°C in another experiment similar to the STA study resulted in the complete formation of a glass.

Figure 16 Temperature-dependent X-ray diffraction pattern of Mg(H2O)2[TeO2(OH)4].

Figure 17 STA measurement of Mg(H2O)2[TeO2(OH)4] with the TG curve in black and the DTA curve in grey.

In summary, the decomposition mechanism of Mg(H₂O)₂[TeO₂(OH)₄] can be formulated as:

I. Mg(H₂O)₂[TeO₂(OH)₄]_(s) → amorphous material_(s) + H₂O_(g), O_(g)

II. Amorphous material_(s) → `Mg[Te₂O₆]'_(s)+ Mg₃[TeO₆]_(s) + H₂O_(g)

IIIa. `Mg[Te₂O₆]'_(s) + Mg₃[TeO₆]_(s) → Mg[TeO₄]_(s) + Mg₃[TeO₆]_(s)

IIIb. Mg[TeO₄]_(s) + Mg₃[TeO₆]_(s) → unknown phase_(s) + Mg₃[TeO₆]_(s)

IV. Unknown phase_(s) + Mg₃[TeO₆]_(s) → Mg₃[TeO₆]_(s) + O_2(g)

4. Conclusion and outlook

The correlated disorder of Mg(H₂O)₂[TeO₂(OH)₄] is notable because it can be decomposed into two modes, which can be treated separately. It demonstrates the difficulties of a quantitative structure determination inherent to data sets with a significant diffuse scattering. In such cases, refinements against Bragg reflections are not sufficient and information on correlated disorder has to be derived from diffuse scattering. But even such descriptions can be ambiguous. Here, pairs of entirely different structures with opposite sign of c_orient produce virtually indistinguishable diffraction patterns. Using a small degree of idealization, simple analytical expressions describing the diffuse scattering can be derived, which allow for extremely fast calculations and a more thorough insight on the observed diffraction phenomena.

A crucial feature in the polytypism of Mg(H₂O)₂[TeO₂(OH)₄] is the hydrogen-bonding network that connects adjacent layers. Its role has been ignored in this X-ray study owing to disorder and the weak scattering power of the hydrogen atoms. A study using neutron diffraction might reveal a very different picture, possibly even necessitating the introduction of a third correlation parameter and different OD-layer symmetries.

APPENDIX A

Symbols used

    ∝ : Proportional to.

≈ : Almost equal to.

σ : Variance of Gaussian distribution.

n, m, h, k, l : Integers.

x : Real.

w, e : Weighting function and exponent in weighting function.

L_n : Crystal-chemical layer with sequential index n.

A¹_n, A²_n+1 : OD layers ( A¹_n: octahedra, A²_n+1: hydrogen-bonding network).

 : Group of operations of the OD layer A_n not inverting the layer orientation.

 : Index of the subgroup of .

a, b : Layer lattice basis vectors.

c₀ : Vector perpendicular to layer plane with the length of one L_n layer width.

c : Basis vector of a specific polytype.

a, b, c₀ : Lengths of the vectors a, b, c₀.

r, s : Metric parameters describing the relative positions of adjacent OD layers.

a*, b*,  : Basis vectors of the dual basis to a, b, c₀.

h, k, ν : Reciprocal coordinates with respect to (a*, b*, ) (h, k: integers; ν: real).

F, I : Structure factor and intensity (I = |F|²) of a polytype or disordered stacking arrangement.

s_Δn : Sum term in the calculation of I.

F_n : Structure factor of the L_n layer.

F^M_n, F^O_n : Contributions of the non-O3 atoms and the O3 atom to F_n = F^M+F^O_n, respectively.

 : Structure factor of the L₀ layer reflected at (100).

T_O3 : Displacement parameter of the O3 atom.

f^O : Atomic form factor of O.

d(O1—O2) : Distance between atoms O1 and O2.

o_n : Origin of the L_n layer.

Δo_n : Origin shift from the L_n to the L_n+1 layer.

α_n, β_n : Origin of the L_n layer in coordinates: Δo_n = α_na/2 + β_nb/2.

ω_n : Orientation of the L_n layer (ω = 0,1).

Δα, Δβ, Δn : Relative origin shift between two layers Δαa + Δβb + Δ nc₀ up to layer lattice translation (Δα, Δβ = 0, 1).

P(…) : Probability that the expression … holds.

P_MgTe : Probability that the origin shifts o_n and o_n+1 are equal.

P_orient : Probability that the orientation of two adjacent layers is the same (ω_n equals ω_n+1).

c_MgTe, c_orient : Nearest-neighbor correlations c_MgTe = 2P_MgTe − 1 and c_orient = 2P_orient −1.

d_c(x) : Shape of the diffuse scattering with nearest-neighbor correlation c.

 : Probability that the origin shift of the (L_n, L_n+Δn) layer pair is Δαa + Δβb + Δnc₀.

,  : Probabilities that the L_n and L_n+Δn possess the (ω_n = ω_n+Δn) or opposite (ω_n ≠ ω_n+Δn) orientation, respectively.

R_p : Residuals for fitting one-dimensionally diffuse scattering: .

APPENDIX B

Derivation of volume fractions from occupancies

The volume fraction of polytypes were derived from refinements using expressions of the type |2occ − 1|, where occ is the occupancy of an atom. This may seem surprising and is due to the symmetry used in the refinements.

Consider a superposition of MDO₃ and MDO₄, which conveniently possess the same unit-cell parameters. Both polytypes differ in the position of the O3 atoms, which will be considered up to fourfold rotation and translation. Representative O3 atoms of MDO₃ and MDO₄ are listed in the first and second row of Table 8, respectively. A 1 − x : x MDO_3/4 superposition then possesses the O3 occupancies shown in the third row. However, when refined using the MDO₄ symmetry (), the O3 positions equivalent in MDO₄ are averaged, leading to the occupancies listed in the last row.

Table 8
Occupancy of O3 atoms in MDO_3/4 superpositions

Atom positions are idealized and given with respect to the MDO_3/4 cell (c = 4c₀).

Polytype	(x,y,0)^T	(−x,y,0)^T	(x,y,)^T	(−x,y,)^T
MDO3	1	0	1	0
MDO4	1	0	0	1
MDO3/4 (1 − x : x)	1	0	1 − x	x
MDO3/4 (1 − x : x) refined in	(1+ x)/2	(1 − x)/2	(1 − x)/2	(1 + x)/2

Thus, such a refinement features two O3 positions with the occupancies occ(O3) = (1± x)/2 which leads to x = |2occ(O3) − 1|. Note that an occupancy of occ(O3) = 0 likewise corresponds to MDO₄, but with a different origin. An analoguous argument can be made for the Mg/Te sites.

APPENDIX C

General pair distribution probabilities

For Δn even and = = 0. Double application of equation (23) then gives

Repeated substitution of equation (57) into itself leads to

Substituting the initial term P₀⁰⁰ = 1:

which can be expressed in terms of Δn = 2m as

An analoguous reasoning applies to Δn odd, though with the initial terms P₁¹⁰ = P₁⁰¹ = ½.

APPENDIX D

Derivation of the peak shape induced by nearest-neighbor growth models

The shape of the diffuse scattering due to nearest-neighbor correlated stacking arrangements is long known [see Welberry (2010), and references therein]. It will be briefly derived here for a general nearest-neighbor correlation c using geometric series.

designates the real part.

Supporting information

Computing details

For all structures, data collection: Apex 3 (Bruker, 2016); cell refinement: SAINT-Plus (Bruker, 2016); data reduction: SAINT-Plus (Bruker, 2016); program(s) used to solve structure: SHELXT (Sheldrick, 2015); program(s) used to refine structure: Jana 2006 (Petříček et al., 2014); molecular graphics: Mercury (Macrae et al., 2008).

(family)

Crystal data

H8MgO8Te	Dx = 3.259 Mg m^−3
Mr = 288	Mo Kα radiation, λ = 0.71073 Å
Tetragonal, F4/mmm	Cell parameters from 5981 reflections
Hall symbol: -f_4_2	θ = 4.0–39.1°
a = 5.3282 (1) Å	µ = 5.17 mm^−1
c = 10.3363 (2) Å	T = 293 K
V = 293.45 (1) Å^3	Block, colorless
Z = 2	0.22 × 0.15 × 0.15 mm
F(000) = 256

Data collection

Bruker KAPPA APEX II CCD diffractometer	140 reflections with I > 3σ(I)
Radiation source: X-ray tube	Rint = 0.029
ω– and φ–scans	θmax = 38.8°, θmin = 5.8°
Absorption correction: multi-scan SADABS	h = −8→8
Tmin = 0.32, Tmax = 0.46	k = −5→8
1970 measured reflections	l = −17→16
140 independent reflections

Refinement

Refinement on F^2	H-atom parameters constrained
R[F^2 > 2σ(F^2)] = 0.012	Weighting scheme based on measured s.u.'s w = 1/(σ^2(I) + 0.0004I^2)
wR(F^2) = 0.031	(Δ/σ)max = 0.008
S = 1.33	Δρmax = 0.27 e Å^−3
140 reflections	Δρmin = −0.45 e Å^−3
11 parameters	Extinction correction: B-C type 1 Gaussian isotropic (Becker & Coppens, 1974)
0 restraints	Extinction coefficient: 490 (110)
2 constraints

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Ų)

	x	y	z	Uiso*/Ueq	Occ. (<1)
Te	0	0	0	0.00996 (8)	0.5
Mg	0	0	0	0.00996 (8)	0.5
O1	0	0	0.19444 (18)	0.0237 (3)
O3	−0.3318 (3)	−0.1682 (3)	0	0.0199 (5)	0.5

Atomic displacement parameters (Ų)

	U^11	U^22	U^33	U^12	U^13	U^23
Te	0.00842 (14)	0.00842 (14)	0.01304 (14)	0	0	0
Mg	0.00842 (14)	0.00842 (14)	0.01304 (14)	0	0	0
O1	0.0269 (6)	0.0269 (6)	0.0174 (6)	0	0	0
O3	0.0118 (7)	0.0118 (7)	0.0362 (11)	0.0034 (8)	0	0

Geometric parameters (Å, º)

Te—Mg	0	Mg—O1^viii	2.0098 (18)
Te—O3	1.9820 (17)	Mg—O3	1.9820 (17)
Te—O3^i	1.9820 (17)	Mg—O3^i	1.9820 (17)
Te—O3^ii	1.9820 (17)	Mg—O3^ii	1.9820 (17)
Te—O3^iii	1.9820 (17)	Mg—O3^iii	1.9820 (17)
Te—O3^iv	1.9820 (17)	Mg—O3^iv	1.9820 (17)
Te—O3^v	1.9820 (17)	Mg—O3^v	1.9820 (17)
Te—O3^vi	1.9820 (17)	Mg—O3^vi	1.9820 (17)
Te—O3^vii	1.9820 (17)	Mg—O3^vii	1.9820 (17)
Mg—O1	2.0098 (18)	O3—O3^iii	1.232 (2)
Mg—Te—O3	0	O1—Mg—O3^iv	90
Mg—Te—O3^i	0	O1—Mg—O3^v	90
Mg—Te—O3^ii	0	O1—Mg—O3^vi	90
Mg—Te—O3^iii	0	O1—Mg—O3^vii	90
Mg—Te—O3^iv	0	O1^viii—Mg—O3	90
Mg—Te—O3^v	0	O1^viii—Mg—O3^i	90
Mg—Te—O3^vi	0	O1^viii—Mg—O3^ii	90
Mg—Te—O3^vii	0	O1^viii—Mg—O3^iii	90
O3—Te—O3^i	143.78 (7)	O1^viii—Mg—O3^iv	90
O3—Te—O3^ii	180	O1^viii—Mg—O3^v	90
O3—Te—O3^iii	36.22 (7)	O1^viii—Mg—O3^vi	90
O3—Te—O3^iv	90.00 (7)	O1^viii—Mg—O3^vii	90
O3—Te—O3^v	53.78 (7)	O3—Mg—O3^i	143.78 (7)
O3—Te—O3^vi	90.00 (7)	O3—Mg—O3^ii	180
O3—Te—O3^vii	126.22 (7)	O3—Mg—O3^iii	36.22 (7)
O3^i—Te—O3^ii	36.22 (7)	O3—Mg—O3^iv	90.00 (7)
O3^i—Te—O3^iii	180	O3—Mg—O3^v	53.78 (7)
O3^i—Te—O3^iv	126.22 (7)	O3—Mg—O3^vi	90.00 (7)
O3^i—Te—O3^v	90.00 (7)	O3—Mg—O3^vii	126.22 (7)
O3^i—Te—O3^vi	53.78 (7)	O3^i—Mg—O3^ii	36.22 (7)
O3^i—Te—O3^vii	90.00 (7)	O3^i—Mg—O3^iii	180
O3^ii—Te—O3^iii	143.78 (7)	O3^i—Mg—O3^iv	126.22 (7)
O3^ii—Te—O3^iv	90.00 (7)	O3^i—Mg—O3^v	90.00 (7)
O3^ii—Te—O3^v	126.22 (7)	O3^i—Mg—O3^vi	53.78 (7)
O3^ii—Te—O3^vi	90.00 (7)	O3^i—Mg—O3^vii	90.00 (7)
O3^ii—Te—O3^vii	53.78 (7)	O3^ii—Mg—O3^iii	143.78 (7)
O3^iii—Te—O3^iv	53.78 (7)	O3^ii—Mg—O3^iv	90.00 (7)
O3^iii—Te—O3^v	90.00 (7)	O3^ii—Mg—O3^v	126.22 (7)
O3^iii—Te—O3^vi	126.22 (7)	O3^ii—Mg—O3^vi	90.00 (7)
O3^iii—Te—O3^vii	90.00 (7)	O3^ii—Mg—O3^vii	53.78 (7)
O3^iv—Te—O3^v	143.78 (7)	O3^iii—Mg—O3^iv	53.78 (7)
O3^iv—Te—O3^vi	180	O3^iii—Mg—O3^v	90.00 (7)
O3^iv—Te—O3^vii	36.22 (7)	O3^iii—Mg—O3^vi	126.22 (7)
O3^v—Te—O3^vi	36.22 (7)	O3^iii—Mg—O3^vii	90.00 (7)
O3^v—Te—O3^vii	180	O3^iv—Mg—O3^v	143.78 (7)
O3^vi—Te—O3^vii	143.78 (7)	O3^iv—Mg—O3^vi	180
Te—Mg—O1	0	O3^iv—Mg—O3^vii	36.22 (7)
Te—Mg—O1^viii	0	O3^v—Mg—O3^vi	36.22 (7)
Te—Mg—O3	0	O3^v—Mg—O3^vii	180
Te—Mg—O3^i	0	O3^vi—Mg—O3^vii	143.78 (7)
Te—Mg—O3^ii	0	Te—O3—Te^ix	143.78 (9)
Te—Mg—O3^iii	0	Te—O3—Mg	0
Te—Mg—O3^iv	0	Te—O3—Mg^ix	143.78 (9)
Te—Mg—O3^v	0	Te—O3—O3^iii	71.89 (11)
Te—Mg—O3^vi	0	Te^ix—O3—Mg	143.78 (9)
Te—Mg—O3^vii	0	Te^ix—O3—Mg^ix	0
O1—Mg—O1^viii	180	Te^ix—O3—O3^iii	71.89 (11)
O1—Mg—O3	90	Mg—O3—Mg^ix	143.78 (9)
O1—Mg—O3^i	90	Mg—O3—O3^iii	71.89 (11)
O1—Mg—O3^ii	90	Mg^ix—O3—O3^iii	71.89 (11)
O1—Mg—O3^iii	90

Symmetry codes: (i) x+1/2, y+1/2, z; (ii) −x, −y, z; (iii) −x−1/2, −y−1/2, z; (iv) −y, x, z; (v) −y−1/2, x+1/2, z; (vi) y, −x, z; (vii) y+1/2, −x−1/2, z; (viii) y, x, −z; (ix) x−1/2, y−1/2, z.

(mdo34)

Crystal data

H8MgO8Te	Dx = 3.260 Mg m^−3
Mr = 288	Mo Kα radiation, λ = 0.71073 Å
Tetragonal, I41/amd	Cell parameters from 5981 reflections
Hall symbol: -I 4bd;-2	θ = 4.0–39.1°
a = 5.3268 (1) Å	µ = 5.18 mm^−1
c = 20.6747 (4) Å	T = 293 K
V = 586.64 (1) Å^3	Block, colorless
Z = 4	0.22 × 0.15 × 0.15 mm
F(000) = 512

Data collection

Bruker KAPPA APEX II CCD diffractometer	409 reflections with I > 3σ(I)
Radiation source: X-ray tube	Rint = 0.040
ω– and φ–scans	θmax = 39.1°, θmin = 4.0°
Absorption correction: multi-scan SADABS	h = −5→8
Tmin = 0.32, Tmax = 0.46	k = −8→8
7123 measured reflections	l = −35→33
461 independent reflections

Refinement

Refinement on F^2	H-atom parameters constrained
R[F^2 > 2σ(F^2)] = 0.020	Weighting scheme based on measured s.u.'s w = 1/(σ^2(I) + 0.0016I^2)
wR(F^2) = 0.078	(Δ/σ)max = 0.040
S = 1.61	Δρmax = 1.23 e Å^−3
461 reflections	Δρmin = −0.90 e Å^−3
24 parameters	Extinction correction: B-C type 1 Gaussian isotropic (Becker & Coppens, 1974)
0 restraints	Extinction coefficient: 800 (200)
7 constraints

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Ų)

	x	y	z	Uiso*/Ueq	Occ. (<1)
Te	0	0	0	0.00979 (11)	0.954 (6)
Mg'	0	0	0	0.00979 (11)	0.046 (6)
Mg	0.5	0.5	0	0.0096 (6)	0.954 (6)
Te'	0.5	0.5	0	0.0096 (6)	0.046 (6)
O1	0	0	−0.0955 (2)	0.0242 (10)
O2	0.5	0.5	−0.0989 (2)	0.0230 (9)
O3	−0.3215 (8)	−0.1569 (8)	−0.00124 (16)	0.0171 (9)	0.5

Atomic displacement parameters (Ų)

	U^11	U^22	U^33	U^12	U^13	U^23
Te	0.00852 (19)	0.00852 (19)	0.0123 (2)	0	0	0
Mg'	0.00852 (19)	0.00852 (19)	0.0123 (2)	0	0	0
Mg	0.0077 (10)	0.0077 (10)	0.0133 (10)	0	0	0
Te'	0.0077 (10)	0.0077 (10)	0.0133 (10)	0	0	0
O1	0.0150 (14)	0.046 (2)	0.0114 (12)	0	0	0
O2	0.0141 (14)	0.038 (2)	0.0170 (14)	0	0	0
O3	0.0078 (14)	0.0089 (15)	0.034 (2)	−0.0021 (13)	−0.0018 (9)	−0.0010 (9)

Geometric parameters (Å, º)

Te—Mg'	0	Mg'—O3^iv	1.906 (4)
Te—O1	1.975 (4)	Mg'—O3^v	1.906 (4)
Te—O1^i	1.975 (4)	Mg'—O3^vi	1.906 (4)
Te—O3	1.906 (4)	Mg'—O3^vii	1.906 (4)
Te—O3^ii	1.906 (4)	Mg—Te'	0
Te—O3^i	1.906 (4)	Mg—O2	2.046 (4)
Te—O3^iii	1.906 (4)	Mg—O2^i	2.046 (4)
Te—O3^iv	1.906 (4)	Mg—O3^viii	2.060 (4)
Te—O3^v	1.906 (4)	Mg—O3^ii	2.060 (4)
Te—O3^vi	1.906 (4)	Mg—O3^ix	2.060 (4)
Te—O3^vii	1.906 (4)	Mg—O3^iii	2.060 (4)
Mg'—O1	1.975 (4)	Mg—O3^x	2.060 (4)
Mg'—O1^i	1.975 (4)	Mg—O3^xi	2.060 (4)
Mg'—O3	1.906 (4)	Mg—O3^xii	2.060 (4)
Mg'—O3^ii	1.906 (4)	Mg—O3^xiii	2.060 (4)
Mg'—O3^i	1.906 (4)	O3—O3^i	1.241 (6)
Mg'—O3^iii	1.906 (4)
Mg'—Te—O1	0	O3—Mg'—O3^v	90.01 (18)
Mg'—Te—O1^i	0	O3—Mg'—O3^vi	52.02 (18)
Mg'—Te—O3	0	O3—Mg'—O3^vii	127.95 (18)
Mg'—Te—O3^ii	0	O3^ii—Mg'—O3^i	142.03 (18)
Mg'—Te—O3^i	0	O3^ii—Mg'—O3^iii	38.00 (18)
Mg'—Te—O3^iii	0	O3^ii—Mg'—O3^iv	90.01 (18)
Mg'—Te—O3^iv	0	O3^ii—Mg'—O3^v	90.01 (18)
Mg'—Te—O3^v	0	O3^ii—Mg'—O3^vi	127.95 (18)
Mg'—Te—O3^vi	0	O3^ii—Mg'—O3^vii	52.02 (18)
Mg'—Te—O3^vii	0	O3^i—Mg'—O3^iii	178.46 (14)
O1—Te—O1^i	180	O3^i—Mg'—O3^iv	127.95 (18)
O1—Te—O3	89.23 (10)	O3^i—Mg'—O3^v	52.02 (18)
O1—Te—O3^ii	89.23 (10)	O3^i—Mg'—O3^vi	90.01 (18)
O1—Te—O3^i	90.77 (10)	O3^i—Mg'—O3^vii	90.01 (18)
O1—Te—O3^iii	90.77 (10)	O3^iii—Mg'—O3^iv	52.02 (18)
O1—Te—O3^iv	90.77 (10)	O3^iii—Mg'—O3^v	127.95 (18)
O1—Te—O3^v	90.77 (10)	O3^iii—Mg'—O3^vi	90.01 (18)
O1—Te—O3^vi	89.23 (10)	O3^iii—Mg'—O3^vii	90.01 (18)
O1—Te—O3^vii	89.23 (10)	O3^iv—Mg'—O3^v	178.46 (14)
O1^i—Te—O3	90.77 (10)	O3^iv—Mg'—O3^vi	38.00 (18)
O1^i—Te—O3^ii	90.77 (10)	O3^iv—Mg'—O3^vii	142.03 (18)
O1^i—Te—O3^i	89.23 (10)	O3^v—Mg'—O3^vi	142.03 (18)
O1^i—Te—O3^iii	89.23 (10)	O3^v—Mg'—O3^vii	38.00 (18)
O1^i—Te—O3^iv	89.23 (10)	O3^vi—Mg'—O3^vii	178.46 (14)
O1^i—Te—O3^v	89.23 (10)	Te'—Mg—O2	0
O1^i—Te—O3^vi	90.77 (10)	Te'—Mg—O2^i	0
O1^i—Te—O3^vii	90.77 (10)	Te'—Mg—O3^viii	0
O3—Te—O3^ii	178.46 (14)	Te'—Mg—O3^ii	0
O3—Te—O3^i	38.00 (18)	Te'—Mg—O3^ix	0
O3—Te—O3^iii	142.03 (18)	Te'—Mg—O3^iii	0
O3—Te—O3^iv	90.01 (18)	Te'—Mg—O3^x	0
O3—Te—O3^v	90.01 (18)	Te'—Mg—O3^xi	0
O3—Te—O3^vi	52.02 (18)	Te'—Mg—O3^xii	0
O3—Te—O3^vii	127.95 (18)	Te'—Mg—O3^xiii	0
O3^ii—Te—O3^i	142.03 (18)	O2—Mg—O2^i	180
O3^ii—Te—O3^iii	38.00 (18)	O2—Mg—O3^viii	89.29 (9)
O3^ii—Te—O3^iv	90.01 (18)	O2—Mg—O3^ii	89.29 (9)
O3^ii—Te—O3^v	90.01 (18)	O2—Mg—O3^ix	90.71 (9)
O3^ii—Te—O3^vi	127.95 (18)	O2—Mg—O3^iii	90.71 (9)
O3^ii—Te—O3^vii	52.02 (18)	O2—Mg—O3^x	90.71 (9)
O3^i—Te—O3^iii	178.46 (14)	O2—Mg—O3^xi	90.71 (9)
O3^i—Te—O3^iv	127.95 (18)	O2—Mg—O3^xii	89.29 (9)
O3^i—Te—O3^v	52.02 (18)	O2—Mg—O3^xiii	89.29 (9)
O3^i—Te—O3^vi	90.01 (18)	O2^i—Mg—O3^viii	90.71 (9)
O3^i—Te—O3^vii	90.01 (18)	O2^i—Mg—O3^ii	90.71 (9)
O3^iii—Te—O3^iv	52.02 (18)	O2^i—Mg—O3^ix	89.29 (9)
O3^iii—Te—O3^v	127.95 (18)	O2^i—Mg—O3^iii	89.29 (9)
O3^iii—Te—O3^vi	90.01 (18)	O2^i—Mg—O3^x	89.29 (9)
O3^iii—Te—O3^vii	90.01 (18)	O2^i—Mg—O3^xi	89.29 (9)
O3^iv—Te—O3^v	178.46 (14)	O2^i—Mg—O3^xii	90.71 (9)
O3^iv—Te—O3^vi	38.00 (18)	O2^i—Mg—O3^xiii	90.71 (9)
O3^iv—Te—O3^vii	142.03 (18)	O3^viii—Mg—O3^ii	178.57 (13)
O3^v—Te—O3^vi	142.03 (18)	O3^viii—Mg—O3^ix	35.06 (17)
O3^v—Te—O3^vii	38.00 (18)	O3^viii—Mg—O3^iii	144.97 (17)
O3^vi—Te—O3^vii	178.46 (14)	O3^viii—Mg—O3^x	90.01 (17)
Te—Mg'—O1	0	O3^viii—Mg—O3^xi	90.01 (17)
Te—Mg'—O1^i	0	O3^viii—Mg—O3^xii	125.01 (17)
Te—Mg'—O3	0	O3^viii—Mg—O3^xiii	54.97 (17)
Te—Mg'—O3^ii	0	O3^ii—Mg—O3^ix	144.97 (17)
Te—Mg'—O3^i	0	O3^ii—Mg—O3^iii	35.06 (17)
Te—Mg'—O3^iii	0	O3^ii—Mg—O3^x	90.01 (17)
Te—Mg'—O3^iv	0	O3^ii—Mg—O3^xi	90.01 (17)
Te—Mg'—O3^v	0	O3^ii—Mg—O3^xii	54.97 (17)
Te—Mg'—O3^vi	0	O3^ii—Mg—O3^xiii	125.01 (17)
Te—Mg'—O3^vii	0	O3^ix—Mg—O3^iii	178.57 (13)
O1—Mg'—O1^i	180	O3^ix—Mg—O3^x	54.97 (17)
O1—Mg'—O3	89.23 (10)	O3^ix—Mg—O3^xi	125.01 (17)
O1—Mg'—O3^ii	89.23 (10)	O3^ix—Mg—O3^xii	90.01 (17)
O1—Mg'—O3^i	90.77 (10)	O3^ix—Mg—O3^xiii	90.01 (17)
O1—Mg'—O3^iii	90.77 (10)	O3^iii—Mg—O3^x	125.01 (17)
O1—Mg'—O3^iv	90.77 (10)	O3^iii—Mg—O3^xi	54.97 (17)
O1—Mg'—O3^v	90.77 (10)	O3^iii—Mg—O3^xii	90.01 (17)
O1—Mg'—O3^vi	89.23 (10)	O3^iii—Mg—O3^xiii	90.01 (17)
O1—Mg'—O3^vii	89.23 (10)	O3^x—Mg—O3^xi	178.57 (13)
O1^i—Mg'—O3	90.77 (10)	O3^x—Mg—O3^xii	35.06 (17)
O1^i—Mg'—O3^ii	90.77 (10)	O3^x—Mg—O3^xiii	144.97 (17)
O1^i—Mg'—O3^i	89.23 (10)	O3^xi—Mg—O3^xii	144.97 (17)
O1^i—Mg'—O3^iii	89.23 (10)	O3^xi—Mg—O3^xiii	35.06 (17)
O1^i—Mg'—O3^iv	89.23 (10)	O3^xii—Mg—O3^xiii	178.57 (13)
O1^i—Mg'—O3^v	89.23 (10)	Te—O1—Mg'	0
O1^i—Mg'—O3^vi	90.77 (10)	Te—O3—Mg'	0
O1^i—Mg'—O3^vii	90.77 (10)	Te—O3—Mg^xiv	143.5 (2)
O3—Mg'—O3^ii	178.46 (14)	Te—O3—O3^i	71.0 (3)
O3—Mg'—O3^i	38.00 (18)	Mg'—O3—Mg^xiv	143.5 (2)
O3—Mg'—O3^iii	142.03 (18)	Mg'—O3—O3^i	71.0 (3)
O3—Mg'—O3^iv	90.01 (18)	Mg^xiv—O3—O3^i	72.5 (3)

Symmetry codes: (i) y, x, −z; (ii) −x, −y, z; (iii) −y, −x, −z; (iv) y, −x, −z; (v) −y, x, −z; (vi) x, −y, z; (vii) −x, y, z; (viii) x+1, y+1, z; (ix) y+1, x+1, −z; (x) y+1, −x, −z; (xi) −y, x+1, −z; (xii) x+1, −y, z; (xiii) −x, y+1, z; (xiv) x−1, y−1, z.

(mdo3)

Crystal data

MgTeO8H8	Dx = 3.259 Mg m^−3
Mr = 288	Mo Kα radiation, λ = 0.71073 Å
Tetragonal, I41/a	Cell parameters from 5981 reflections
Hall symbol: -I 4ad	θ = 4.0–39.1°
a = 5.3282 (1) Å	µ = 5.17 mm^−1
c = 20.6725 (4) Å	T = 293 K
V = 586.89 (1) Å^3	Block, colorless
Z = 4	0.22 × 0.15 × 0.15 mm
F(000) = 512

Data collection

Bruker KAPPA APEX II CCD diffractometer	773 independent reflections
Radiation source: X-ray tube	651 reflections with I > 3σ(I)
Graphite monochromator	Rint = 0.032
ω– and φ–scans	θmax = 39.1°, θmin = 4.0°
Absorption correction: multi-scan SADABS	h = −5→8
Tmin = 0.32, Tmax = 0.46	k = −8→8
7853 measured reflections	l = −35→33

Refinement

Refinement on F^2	H-atom parameters constrained
R[F^2 > 2σ(F^2)] = 0.018	Weighting scheme based on measured s.u.'s w = 1/(σ^2(I) + 0.0016I^2)
wR(F^2) = 0.068	(Δ/σ)max = 0.007
S = 1.34	Δρmax = 0.93 e Å^−3
773 reflections	Δρmin = −0.71 e Å^−3
28 parameters	Extinction correction: B-C type 1 Gaussian isotropic (Becker & Coppens, 1974)
0 restraints	Extinction coefficient: 960 (170)
17 constraints

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Ų)

	x	y	z	Uiso*/Ueq	Occ. (<1)
Te	0	0	0	0.00998 (8)	0.923 (4)
Mg'	0	0	0	0.00998 (8)	0.077 (4)
Mg	0.5	0.5	0	0.0121 (4)	0.923 (4)
Te'	0.5	0.5	0	0.0121 (4)	0.077 (4)
O1	0	0	0.09543 (14)	0.0247 (7)
O2	0.5	0.5	0.09889 (15)	0.0232 (6)
O3	−0.3216 (5)	−0.1563 (5)	−0.00202 (9)	0.0183 (6)	0.822 (14)
O3'	−0.3216 (5)	0.1563 (5)	−0.00202 (9)	0.0183 (6)	0.178 (14)

Atomic displacement parameters (Ų)

	U^11	U^22	U^33	U^12	U^13	U^23
Te	0.00867 (14)	0.00867 (14)	0.01258 (14)	0	0	0
Mg'	0.00867 (14)	0.00867 (14)	0.01258 (14)	0	0	0
Mg	0.0097 (6)	0.0097 (6)	0.0169 (7)	0	0	0
Te'	0.0097 (6)	0.0097 (6)	0.0169 (7)	0	0	0
O1	0.0316 (14)	0.0298 (13)	0.0128 (9)	−0.011 (3)	0	0
O2	0.0234 (11)	0.0276 (12)	0.0185 (10)	−0.003 (3)	0	0
O3	0.0082 (9)	0.0094 (10)	0.0374 (14)	−0.0022 (9)	−0.0056 (4)	−0.0053 (5)
O3'	0.0082 (9)	0.0094 (10)	0.0374 (14)	0.0022 (9)	−0.0056 (4)	0.0053 (5)

Geometric parameters (Å, º)

Te—Mg'	0	Mg'—O3'	1.906 (3)
Te—O1	1.973 (3)	Mg'—O3'^ii	1.906 (3)
Te—O1^i	1.973 (3)	Mg'—O3'^i	1.906 (3)
Te—O3	1.906 (3)	Mg'—O3'^iii	1.906 (3)
Te—O3^ii	1.906 (3)	Mg—Te'	0
Te—O3^i	1.906 (3)	Mg—O2	2.044 (3)
Te—O3^iii	1.906 (3)	Mg—O2^iv	2.044 (3)
Te—O3'	1.906 (3)	Mg—O3^v	2.064 (3)
Te—O3'^ii	1.906 (3)	Mg—O3^ii	2.064 (3)
Te—O3'^i	1.906 (3)	Mg—O3^vi	2.064 (3)
Te—O3'^iii	1.906 (3)	Mg—O3^vii	2.064 (3)
Mg'—O1	1.973 (3)	Mg—O3'^viii	2.064 (3)
Mg'—O1^i	1.973 (3)	Mg—O3'^ix	2.064 (3)
Mg'—O3	1.906 (3)	Mg—O3'^i	2.064 (3)
Mg'—O3^ii	1.906 (3)	Mg—O3'^x	2.064 (3)
Mg'—O3^i	1.906 (3)	O3—O3'^iii	1.248 (4)
Mg'—O3^iii	1.906 (3)
Mg'—Te—O1	0	O3^ii—Mg'—O3^i	90.03 (12)
Mg'—Te—O1^i	0	O3^ii—Mg'—O3^iii	90.03 (12)
Mg'—Te—O3	0	O3^ii—Mg'—O3'	128.10 (12)
Mg'—Te—O3^ii	0	O3^ii—Mg'—O3'^ii	51.83 (12)
Mg'—Te—O3^i	0	O3^ii—Mg'—O3'^i	38.24 (12)
Mg'—Te—O3^iii	0	O3^ii—Mg'—O3'^iii	141.85 (12)
Mg'—Te—O3'	0	O3^i—Mg'—O3^iii	177.49 (8)
Mg'—Te—O3'^ii	0	O3^i—Mg'—O3'	38.24 (12)
Mg'—Te—O3'^i	0	O3^i—Mg'—O3'^ii	141.85 (12)
Mg'—Te—O3'^iii	0	O3^i—Mg'—O3'^i	51.83 (12)
O1—Te—O1^i	180	O3^i—Mg'—O3'^iii	128.10 (12)
O1—Te—O3	91.25 (5)	O3^iii—Mg'—O3'	141.85 (12)
O1—Te—O3^ii	91.25 (5)	O3^iii—Mg'—O3'^ii	38.24 (12)
O1—Te—O3^i	88.75 (5)	O3^iii—Mg'—O3'^i	128.10 (12)
O1—Te—O3^iii	88.75 (5)	O3^iii—Mg'—O3'^iii	51.83 (12)
O1—Te—O3'	91.25 (5)	O3'—Mg'—O3'^ii	177.49 (8)
O1—Te—O3'^ii	91.25 (5)	O3'—Mg'—O3'^i	90.03 (12)
O1—Te—O3'^i	88.75 (5)	O3'—Mg'—O3'^iii	90.03 (12)
O1—Te—O3'^iii	88.75 (5)	O3'^ii—Mg'—O3'^i	90.03 (12)
O1^i—Te—O3	88.75 (5)	O3'^ii—Mg'—O3'^iii	90.03 (12)
O1^i—Te—O3^ii	88.75 (5)	O3'^i—Mg'—O3'^iii	177.49 (8)
O1^i—Te—O3^i	91.25 (5)	Te'—Mg—O2	0
O1^i—Te—O3^iii	91.25 (5)	Te'—Mg—O2^iv	0
O1^i—Te—O3'	88.75 (5)	Te'—Mg—O3^v	0
O1^i—Te—O3'^ii	88.75 (5)	Te'—Mg—O3^ii	0
O1^i—Te—O3'^i	91.25 (5)	Te'—Mg—O3^vi	0
O1^i—Te—O3'^iii	91.25 (5)	Te'—Mg—O3^vii	0
O3—Te—O3^ii	177.49 (8)	Te'—Mg—O3'^viii	0
O3—Te—O3^i	90.03 (12)	Te'—Mg—O3'^ix	0
O3—Te—O3^iii	90.03 (12)	Te'—Mg—O3'^i	0
O3—Te—O3'	51.83 (12)	Te'—Mg—O3'^x	0
O3—Te—O3'^ii	128.10 (12)	O2—Mg—O2^iv	180
O3—Te—O3'^i	141.85 (12)	O2—Mg—O3^v	91.16 (5)
O3—Te—O3'^iii	38.24 (12)	O2—Mg—O3^ii	91.16 (5)
O3^ii—Te—O3^i	90.03 (12)	O2—Mg—O3^vi	88.84 (5)
O3^ii—Te—O3^iii	90.03 (12)	O2—Mg—O3^vii	88.84 (5)
O3^ii—Te—O3'	128.10 (12)	O2—Mg—O3'^viii	91.16 (5)
O3^ii—Te—O3'^ii	51.83 (12)	O2—Mg—O3'^ix	91.16 (5)
O3^ii—Te—O3'^i	38.24 (12)	O2—Mg—O3'^i	88.84 (5)
O3^ii—Te—O3'^iii	141.85 (12)	O2—Mg—O3'^x	88.84 (5)
O3^i—Te—O3^iii	177.49 (8)	O2^iv—Mg—O3^v	88.84 (5)
O3^i—Te—O3'	38.24 (12)	O2^iv—Mg—O3^ii	88.84 (5)
O3^i—Te—O3'^ii	141.85 (12)	O2^iv—Mg—O3^vi	91.16 (5)
O3^i—Te—O3'^i	51.83 (12)	O2^iv—Mg—O3^vii	91.16 (5)
O3^i—Te—O3'^iii	128.10 (12)	O2^iv—Mg—O3'^viii	88.84 (5)
O3^iii—Te—O3'	141.85 (12)	O2^iv—Mg—O3'^ix	88.84 (5)
O3^iii—Te—O3'^ii	38.24 (12)	O2^iv—Mg—O3'^i	91.16 (5)
O3^iii—Te—O3'^i	128.10 (12)	O2^iv—Mg—O3'^x	91.16 (5)
O3^iii—Te—O3'^iii	51.83 (12)	O3^v—Mg—O3^ii	177.68 (7)
O3'—Te—O3'^ii	177.49 (8)	O3^v—Mg—O3^vi	90.02 (11)
O3'—Te—O3'^i	90.03 (12)	O3^v—Mg—O3^vii	90.02 (11)
O3'—Te—O3'^iii	90.03 (12)	O3^v—Mg—O3'^viii	125.09 (11)
O3'^ii—Te—O3'^i	90.03 (12)	O3^v—Mg—O3'^ix	54.85 (11)
O3'^ii—Te—O3'^iii	90.03 (12)	O3^v—Mg—O3'^i	144.87 (11)
O3'^i—Te—O3'^iii	177.49 (8)	O3^v—Mg—O3'^x	35.21 (11)
Te—Mg'—O1	0	O3^ii—Mg—O3^vi	90.02 (11)
Te—Mg'—O1^i	0	O3^ii—Mg—O3^vii	90.02 (11)
Te—Mg'—O3	0	O3^ii—Mg—O3'^viii	54.85 (11)
Te—Mg'—O3^ii	0	O3^ii—Mg—O3'^ix	125.09 (11)
Te—Mg'—O3^i	0	O3^ii—Mg—O3'^i	35.21 (11)
Te—Mg'—O3^iii	0	O3^ii—Mg—O3'^x	144.87 (11)
Te—Mg'—O3'	0	O3^vi—Mg—O3^vii	177.68 (7)
Te—Mg'—O3'^ii	0	O3^vi—Mg—O3'^viii	35.21 (11)
Te—Mg'—O3'^i	0	O3^vi—Mg—O3'^ix	144.87 (11)
Te—Mg'—O3'^iii	0	O3^vi—Mg—O3'^i	125.09 (11)
O1—Mg'—O1^i	180	O3^vi—Mg—O3'^x	54.85 (11)
O1—Mg'—O3	91.25 (5)	O3^vii—Mg—O3'^viii	144.87 (11)
O1—Mg'—O3^ii	91.25 (5)	O3^vii—Mg—O3'^ix	35.21 (11)
O1—Mg'—O3^i	88.75 (5)	O3^vii—Mg—O3'^i	54.85 (11)
O1—Mg'—O3^iii	88.75 (5)	O3^vii—Mg—O3'^x	125.09 (11)
O1—Mg'—O3'	91.25 (5)	O3'^viii—Mg—O3'^ix	177.68 (7)
O1—Mg'—O3'^ii	91.25 (5)	O3'^viii—Mg—O3'^i	90.02 (11)
O1—Mg'—O3'^i	88.75 (5)	O3'^viii—Mg—O3'^x	90.02 (11)
O1—Mg'—O3'^iii	88.75 (5)	O3'^ix—Mg—O3'^i	90.02 (11)
O1^i—Mg'—O3	88.75 (5)	O3'^ix—Mg—O3'^x	90.02 (11)
O1^i—Mg'—O3^ii	88.75 (5)	O3'^i—Mg—O3'^x	177.68 (7)
O1^i—Mg'—O3^i	91.25 (5)	Te—O1—Mg'	0
O1^i—Mg'—O3^iii	91.25 (5)	Te—O3—Mg'	0
O1^i—Mg'—O3'	88.75 (5)	Te—O3—Mg^xi	143.28 (16)
O1^i—Mg'—O3'^ii	88.75 (5)	Te—O3—O3'^iii	70.88 (18)
O1^i—Mg'—O3'^i	91.25 (5)	Mg'—O3—Mg^xi	143.28 (16)
O1^i—Mg'—O3'^iii	91.25 (5)	Mg'—O3—O3'^iii	70.88 (18)
O3—Mg'—O3^ii	177.49 (8)	Mg^xi—O3—O3'^iii	72.39 (18)
O3—Mg'—O3^i	90.03 (12)	Te—O3'—Mg'	0
O3—Mg'—O3^iii	90.03 (12)	Te—O3'—Mg^xii	143.28 (16)
O3—Mg'—O3'	51.83 (12)	Te—O3'—O3^i	70.88 (18)
O3—Mg'—O3'^ii	128.10 (12)	Mg'—O3'—Mg^xii	143.28 (16)
O3—Mg'—O3'^i	141.85 (12)	Mg'—O3'—O3^i	70.88 (18)
O3—Mg'—O3'^iii	38.24 (12)	Mg^xii—O3'—O3^i	72.39 (18)

Symmetry codes: (i) y, −x, −z; (ii) −x, −y, z; (iii) −y, x, −z; (iv) y, −x+1, −z; (v) x+1, y+1, z; (vi) y+1, −x, −z; (vii) −y, x+1, −z; (viii) x+1, y, z; (ix) −x, −y+1, z; (x) −y+1, x+1, −z; (xi) x−1, y−1, z; (xii) x−1, y, z.

(mdo4)

Crystal data

MgTeO8H8	Dx = 3.259 Mg m^−3
Mr = 288	Mo Kα radiation, λ = 0.71073 Å
Tetragonal, I42d	Cell parameters from 5981 reflections
Hall symbol: I -4;2bw	θ = 4.0–39.1°
a = 5.3282 (1) Å	µ = 5.17 mm^−1
c = 20.6725 (4) Å	T = 293 K
V = 586.89 (1) Å^3	Block, colorless
Z = 4	0.22 × 0.15 × 0.15 mm
F(000) = 512

Data collection

Bruker KAPPA APEX II CCD diffractometer	786 independent reflections
Radiation source: X-ray tube	676 reflections with I > 3σ(I)
Graphite monochromator	Rint = 0.032
ω– and φ–scans	θmax = 39.1°, θmin = 4.0°
Absorption correction: multi-scan SADABS	h = −5→8
Tmin = 0.32, Tmax = 0.46	k = −8→8
7371 measured reflections	l = −35→33

Refinement

Refinement on F^2	Weighting scheme based on measured s.u.'s w = 1/(σ^2(I) + 0.0016I^2)
R[F^2 > 2σ(F^2)] = 0.017	(Δ/σ)max = 0.034
wR(F^2) = 0.058	Δρmax = 0.80 e Å^−3
S = 1.17	Δρmin = −0.70 e Å^−3
786 reflections	Extinction correction: B-C type 1 Gaussian isotropic (Becker & Coppens, 1974)
28 parameters	Extinction coefficient: 750 (140)
0 restraints	Absolute structure: 314 of Friedel pairs used in the refinement
17 constraints	Absolute structure parameter: 0.51 (9)
H-atom parameters constrained

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Ų)

	x	y	z	Uiso*/Ueq	Occ. (<1)
Te	0	0	0	0.00987 (6)	0.932 (3)
Mg'	0	0	0	0.00987 (6)	0.068 (3)
Mg	0.5	0.5	0	0.0111 (3)	0.932 (3)
Te'	0.5	0.5	0	0.0111 (3)	0.068 (3)
O1	0	0	0.09541 (12)	0.0246 (7)
O2	0.5	0.5	0.09888 (13)	0.0231 (6)
O3	−0.3217 (4)	−0.1561 (4)	−0.00156 (9)	0.0173 (5)	0.736 (6)
O3'	−0.3217 (4)	0.1561 (4)	−0.00156 (9)	0.0173 (5)	0.264 (6)

Atomic displacement parameters (Ų)

	U^11	U^22	U^33	U^12	U^13	U^23
Te	0.00857 (11)	0.00857 (11)	0.01248 (12)	0	0	0
Mg'	0.00857 (11)	0.00857 (11)	0.01248 (12)	0	0	0
Mg	0.0087 (5)	0.0087 (5)	0.0158 (6)	0	0	0
Te'	0.0087 (5)	0.0087 (5)	0.0158 (6)	0	0	0
O1	0.0316 (14)	0.0298 (14)	0.0125 (7)	0.010 (6)	0	0
O2	0.0236 (10)	0.0275 (11)	0.0182 (8)	0.001 (11)	0	0
O3	0.0092 (8)	0.0103 (8)	0.0325 (10)	−0.0016 (7)	−0.0055 (4)	−0.0056 (4)
O3'	0.0092 (8)	0.0103 (8)	0.0325 (10)	0.0016 (7)	−0.0055 (4)	0.0056 (4)

Geometric parameters (Å, º)

Te—Mg'	0	Mg'—O3'	1.906 (2)
Te—O1	1.972 (2)	Mg'—O3'^ii	1.906 (2)
Te—O1^i	1.972 (2)	Mg'—O3'^i	1.906 (2)
Te—O3	1.906 (2)	Mg'—O3'^iii	1.906 (2)
Te—O3^ii	1.906 (2)	Mg—Te'	0
Te—O3^i	1.906 (2)	Mg—O2	2.044 (3)
Te—O3^iii	1.906 (2)	Mg—O2^iv	2.044 (3)
Te—O3'	1.906 (2)	Mg—O3^v	2.064 (2)
Te—O3'^ii	1.906 (2)	Mg—O3^ii	2.064 (2)
Te—O3'^i	1.906 (2)	Mg—O3^vi	2.064 (2)
Te—O3'^iii	1.906 (2)	Mg—O3^vii	2.064 (2)
Mg'—O1	1.972 (2)	Mg—O3'^viii	2.064 (2)
Mg'—O1^i	1.972 (2)	Mg—O3'^ix	2.064 (2)
Mg'—O3	1.906 (2)	Mg—O3'^i	2.064 (2)
Mg'—O3^ii	1.906 (2)	Mg—O3'^x	2.064 (2)
Mg'—O3^i	1.906 (2)	O3—O3'^iii	1.250 (3)
Mg'—O3^iii	1.906 (2)
Mg'—Te—O1	0	O3^ii—Mg'—O3^i	90.02 (10)
Mg'—Te—O1^i	0	O3^ii—Mg'—O3^iii	90.02 (10)
Mg'—Te—O3	0	O3^ii—Mg'—O3'	128.20 (10)
Mg'—Te—O3^ii	0	O3^ii—Mg'—O3'^ii	51.75 (10)
Mg'—Te—O3^i	0	O3^ii—Mg'—O3'^i	38.28 (10)
Mg'—Te—O3^iii	0	O3^ii—Mg'—O3'^iii	141.77 (10)
Mg'—Te—O3'	0	O3^i—Mg'—O3^iii	178.07 (8)
Mg'—Te—O3'^ii	0	O3^i—Mg'—O3'	38.28 (10)
Mg'—Te—O3'^i	0	O3^i—Mg'—O3'^ii	141.77 (10)
Mg'—Te—O3'^iii	0	O3^i—Mg'—O3'^i	51.75 (10)
O1—Te—O1^i	180	O3^i—Mg'—O3'^iii	128.20 (10)
O1—Te—O3	90.97 (6)	O3^iii—Mg'—O3'	141.77 (10)
O1—Te—O3^ii	90.97 (6)	O3^iii—Mg'—O3'^ii	38.28 (10)
O1—Te—O3^i	89.03 (6)	O3^iii—Mg'—O3'^i	128.20 (10)
O1—Te—O3^iii	89.03 (6)	O3^iii—Mg'—O3'^iii	51.75 (10)
O1—Te—O3'	90.97 (6)	O3'—Mg'—O3'^ii	178.07 (8)
O1—Te—O3'^ii	90.97 (6)	O3'—Mg'—O3'^i	90.02 (10)
O1—Te—O3'^i	89.03 (6)	O3'—Mg'—O3'^iii	90.02 (10)
O1—Te—O3'^iii	89.03 (6)	O3'^ii—Mg'—O3'^i	90.02 (10)
O1^i—Te—O3	89.03 (6)	O3'^ii—Mg'—O3'^iii	90.02 (10)
O1^i—Te—O3^ii	89.03 (6)	O3'^i—Mg'—O3'^iii	178.07 (8)
O1^i—Te—O3^i	90.97 (6)	Te'—Mg—O2	0
O1^i—Te—O3^iii	90.97 (6)	Te'—Mg—O2^iv	0
O1^i—Te—O3'	89.03 (6)	Te'—Mg—O3^v	0
O1^i—Te—O3'^ii	89.03 (6)	Te'—Mg—O3^ii	0
O1^i—Te—O3'^i	90.97 (6)	Te'—Mg—O3^vi	0
O1^i—Te—O3'^iii	90.97 (6)	Te'—Mg—O3^vii	0
O3—Te—O3^ii	178.07 (8)	Te'—Mg—O3'^viii	0
O3—Te—O3^i	90.02 (10)	Te'—Mg—O3'^ix	0
O3—Te—O3^iii	90.02 (10)	Te'—Mg—O3'^i	0
O3—Te—O3'	51.75 (10)	Te'—Mg—O3'^x	0
O3—Te—O3'^ii	128.20 (10)	O2—Mg—O2^iv	180
O3—Te—O3'^i	141.77 (10)	O2—Mg—O3^v	90.89 (5)
O3—Te—O3'^iii	38.28 (10)	O2—Mg—O3^ii	90.89 (5)
O3^ii—Te—O3^i	90.02 (10)	O2—Mg—O3^vi	89.11 (5)
O3^ii—Te—O3^iii	90.02 (10)	O2—Mg—O3^vii	89.11 (5)
O3^ii—Te—O3'	128.20 (10)	O2—Mg—O3'^viii	90.89 (5)
O3^ii—Te—O3'^ii	51.75 (10)	O2—Mg—O3'^ix	90.89 (5)
O3^ii—Te—O3'^i	38.28 (10)	O2—Mg—O3'^i	89.11 (5)
O3^ii—Te—O3'^iii	141.77 (10)	O2—Mg—O3'^x	89.11 (5)
O3^i—Te—O3^iii	178.07 (8)	O2^iv—Mg—O3^v	89.11 (5)
O3^i—Te—O3'	38.28 (10)	O2^iv—Mg—O3^ii	89.11 (5)
O3^i—Te—O3'^ii	141.77 (10)	O2^iv—Mg—O3^vi	90.89 (5)
O3^i—Te—O3'^i	51.75 (10)	O2^iv—Mg—O3^vii	90.89 (5)
O3^i—Te—O3'^iii	128.20 (10)	O2^iv—Mg—O3'^viii	89.11 (5)
O3^iii—Te—O3'	141.77 (10)	O2^iv—Mg—O3'^ix	89.11 (5)
O3^iii—Te—O3'^ii	38.28 (10)	O2^iv—Mg—O3'^i	90.89 (5)
O3^iii—Te—O3'^i	128.20 (10)	O2^iv—Mg—O3'^x	90.89 (5)
O3^iii—Te—O3'^iii	51.75 (10)	O3^v—Mg—O3^ii	178.21 (7)
O3'—Te—O3'^ii	178.07 (8)	O3^v—Mg—O3^vi	90.01 (9)
O3'—Te—O3'^i	90.02 (10)	O3^v—Mg—O3^vii	90.01 (9)
O3'—Te—O3'^iii	90.02 (10)	O3^v—Mg—O3'^viii	125.17 (9)
O3'^ii—Te—O3'^i	90.02 (10)	O3^v—Mg—O3'^ix	54.79 (9)
O3'^ii—Te—O3'^iii	90.02 (10)	O3^v—Mg—O3'^i	144.80 (9)
O3'^i—Te—O3'^iii	178.07 (8)	O3^v—Mg—O3'^x	35.24 (9)
Te—Mg'—O1	0	O3^ii—Mg—O3^vi	90.01 (9)
Te—Mg'—O1^i	0	O3^ii—Mg—O3^vii	90.01 (9)
Te—Mg'—O3	0	O3^ii—Mg—O3'^viii	54.79 (9)
Te—Mg'—O3^ii	0	O3^ii—Mg—O3'^ix	125.17 (9)
Te—Mg'—O3^i	0	O3^ii—Mg—O3'^i	35.24 (9)
Te—Mg'—O3^iii	0	O3^ii—Mg—O3'^x	144.80 (9)
Te—Mg'—O3'	0	O3^vi—Mg—O3^vii	178.21 (7)
Te—Mg'—O3'^ii	0	O3^vi—Mg—O3'^viii	35.24 (9)
Te—Mg'—O3'^i	0	O3^vi—Mg—O3'^ix	144.80 (9)
Te—Mg'—O3'^iii	0	O3^vi—Mg—O3'^i	125.17 (9)
O1—Mg'—O1^i	180	O3^vi—Mg—O3'^x	54.79 (9)
O1—Mg'—O3	90.97 (6)	O3^vii—Mg—O3'^viii	144.80 (9)
O1—Mg'—O3^ii	90.97 (6)	O3^vii—Mg—O3'^ix	35.24 (9)
O1—Mg'—O3^i	89.03 (6)	O3^vii—Mg—O3'^i	54.79 (9)
O1—Mg'—O3^iii	89.03 (6)	O3^vii—Mg—O3'^x	125.17 (9)
O1—Mg'—O3'	90.97 (6)	O3'^viii—Mg—O3'^ix	178.21 (7)
O1—Mg'—O3'^ii	90.97 (6)	O3'^viii—Mg—O3'^i	90.01 (9)
O1—Mg'—O3'^i	89.03 (6)	O3'^viii—Mg—O3'^x	90.01 (9)
O1—Mg'—O3'^iii	89.03 (6)	O3'^ix—Mg—O3'^i	90.01 (9)
O1^i—Mg'—O3	89.03 (6)	O3'^ix—Mg—O3'^x	90.01 (9)
O1^i—Mg'—O3^ii	89.03 (6)	O3'^i—Mg—O3'^x	178.21 (7)
O1^i—Mg'—O3^i	90.97 (6)	Te—O1—Mg'	0
O1^i—Mg'—O3^iii	90.97 (6)	Te—O3—Mg'	0
O1^i—Mg'—O3'	89.03 (6)	Te—O3—Mg^xi	143.24 (13)
O1^i—Mg'—O3'^ii	89.03 (6)	Te—O3—O3'^iii	70.86 (15)
O1^i—Mg'—O3'^i	90.97 (6)	Mg'—O3—Mg^xi	143.24 (13)
O1^i—Mg'—O3'^iii	90.97 (6)	Mg'—O3—O3'^iii	70.86 (15)
O3—Mg'—O3^ii	178.07 (8)	Mg^xi—O3—O3'^iii	72.38 (15)
O3—Mg'—O3^i	90.02 (10)	Te—O3'—Mg'	0
O3—Mg'—O3^iii	90.02 (10)	Te—O3'—Mg^xii	143.24 (13)
O3—Mg'—O3'	51.75 (10)	Te—O3'—O3^i	70.86 (15)
O3—Mg'—O3'^ii	128.20 (10)	Mg'—O3'—Mg^xii	143.24 (13)
O3—Mg'—O3'^i	141.77 (10)	Mg'—O3'—O3^i	70.86 (15)
O3—Mg'—O3'^iii	38.28 (10)	Mg^xii—O3'—O3^i	72.38 (15)

Symmetry codes: (i) y, −x, −z; (ii) −x, −y, z; (iii) −y, x, −z; (iv) y, −x+1, −z; (v) x+1, y+1, z; (vi) y+1, −x, −z; (vii) −y, x+1, −z; (viii) x+1, y, z; (ix) −x, −y+1, z; (x) −y+1, x+1, −z; (xi) x−1, y−1, z; (xii) x−1, y, z.