research papers\(\def\hfill{\hskip 5em}\def\hfil{\hskip 3em}\def\eqno#1{\hfil {#1}}\)

IUCrJ
Volume 3| Part 5| September 2016| Pages 354-366
ISSN: 2052-2525

Cooperative Jahn–Teller effect and the role of strain in the tetragonal-to-cubic phase transition in MgxCu1 − xCr2O4

aDepartment of Earth and Environmental Sciences, University of Pavia, Via Ferrata 9, 27100 Pavia, Italy, bCNR, Institute of Geosciences and Georesources, Via Ferrata 9, 27100 Pavia, Italy, and cDepartment of Earth Sciences, University of Cambridge, Downing Street, Cambridge, Cambridgeshire CB2 3EQ, UK
*Correspondence e-mail: michele.zema@unipv.it

Edited by C. Lecomte, Université de Lorraine, France (Received 29 March 2016; accepted 4 August 2016; online 16 August 2016)

Temperature and composition dependences of the I41/amd[Fd\bar 3m] phase transition in the MgxCu1 − xCr2O4 spinel solid solution, due to the melting of the cooperative Jahn–Teller distortion, have been studied by means of single-crystal X-ray diffraction. Crystals with x = 0, 0.10, 0.18, 0.43, 0.46, 0.53, 1 were grown by flux decomposition methods. All crystals have been refined in the tetragonal I41/amd space group except for the Mg end-member, which has cubic symmetry. In MgxCu1 − xCr2O4 the progressive substitution of the Jahn–Teller, d9 Cu2+ cation with spherical and closed-shell Mg2+ has a substantial effect on the crystal structure, such that there is a gradual reduction of the splitting of a and c unit-cell parameters and flattening of the tetrahedra. Single-crystal diffraction data collected in situ up to T = 1173 K show that the tetragonal-to-cubic transition temperature decreases with increasing Mg content. The strength of the Cu—Cu interaction is, in effect, modulated by varying the Cu/Mg ratio. Structure refinements of diffraction data collected at different temperatures reveal that heating results in a gradual reduction in the tetrahedron compression, which remains significant until near the transition temperature, however, at which point the distortion of the tetrahedra rapidly vanishes. The spontaneous strain arising in the tetragonal phase is large, amounting to 10% shear strain, et, and ∼ 1% volume strain, Vs, in the copper chromite end-member at room temperature. Observed strain relationships are consistent with pseudoproper ferroelastic behaviour ([e_{\rm t}^2]Vs[q_{\rm JT}^2], where qJT is the order parameter). The I41/amd[Fd\bar 3m] phase transition is first order in character for Cu-rich samples and then evolves towards second-order character. Although a third order term is permitted by symmetry in the Landau expansion, this behaviour appears to be more accurately represented by a 246 expansion with a change from negative to positive values of the fourth-order coefficient with progressive dilution of the Jahn–Teller cation.

1. Introduction

Complex AB2O4 oxides with the spinel structure comprise a family of materials, which exhibit a wide range of electronic, magnetic and optical properties through the variation of cations on tetrahedral (A) and octahedral (B) sites. The archetypical spinel structure belongs to the space group [Fd\bar 3m] (No. 227) and is usually described as a pseudocubic close-packed array of O atoms with the A and B cations occupying one eighth of the tetrahedral sites and one half of the octahedral sites, respectively. Such occupancy of the interstitial sites results in an fcc unit cell which is 2 × 2 × 2 times that of the basic ccp oxygen array. One of the characteristics of the spinel structure is its flexibility in the range of possible cations and cation charge combinations, making it a structure adopted by over a hundred compounds. In fact, within the spinel space group, the fractional coordinates of the octahedral and tetrahedral sites are fixed at special positions (A on 8a at 0,0,0; B on 16d at 5/8,5/8,5/8), while the O atoms are on 32e with coordinates uuu. This means that if the relative sizes of the A and B cations change, their positions remain the same but the oxygen array expands or contracts to accommodate them and maintain the same symmetry throughout.

The most common distortion of the spinel structure is by far the tetragonal distortion, whereby one of the cubic axes would become compressed or elongated with respect to the other two. If no additional symmetry breaking occurs, the tetragonal distortion alone decreases the symmetry from [Fd\bar 3m] to I41/amd (No. 141). The c/a ratio is normally used as a parameter of tetragonal distortion. A phase transition from the cubic to the tetragonal structure may be induced by a sufficient concentration of non-spherical, Jahn–Teller (JT) ions, such as Cu2+ or Mn3+, causing a cooperative distortion. Although less common, tetrahedral Cu2+ on the A site can display JT activity. The degeneracy of the partially occupied t2 levels is broken by compressing the tetrahedron and thereby lowering the symmetry, as in copper chromite, CuCr2O4, which is a tetragonally distorted spinel with unit-cell parameters ratio c/a < 1 (Fig. 1[link], left panel). Cu2+ cations can be stabilized in flattened tetrahedral environments because of the preference of Cr3+ ions to occupy the octahedral sites. The cooperative nature of the crystal distortion can be rationalized in terms of elastic interactions among locally distorted tetrahedra, as a consequence of coupling of electronic states to bulk deformation via elastic strain. On heating, CuCr2O4 undergoes a first-order structural transition from the tetragonal distorted spinel structure to the archetypal cubic spinel structure at 853 K (Yé et al., 1994[Yé, Z., Crottaz, O., Vaudano, F., Kubel, F., Tissot, P. & Schmid, H. (1994). Ferroelectrics, 162, 103-118.]; Kennedy & Zhou, 2008[Kennedy, B. & Zhou, Q. (2008). J. Solid State Chem. 181, 2227-2230.]). The structural distortion in CuCr2O4 is large and the transition temperature high, in particular if considering that CuO4 tetrahedra are not directly linked but separated from each other by non-JT ions. Nonetheless, enhancement of the ground-state JT splitting and of lattice distortion have been explained by considering the electronic and elastic coupling of Cu2+ and Cr3+ (Atanasov et al., 1993[Atanasov, M., Kesper, U., Ramakrishna, B. & Reinen, D. (1993). J. Solid State Chem. 105, 1-18.]; Reinen et al., 1988[Reinen, D., Atanasov, M., Nikolov, G. & Steffens, F. (1988). Inorg. Chem. 27, 1678-1686.]). The relevance of strain associated with the Jahn–Teller distortion is curiously showed in NiCr2O4 by the observation that the crystals literally jump off a flat surface when they pass through the transition point (Crottaz et al., 1997[Crottaz, O., Kubel, F. & Schmid, H. (1997). J. Mater. Chem. 7, 143-146.]), due to the large and abrupt change in shear strain.

[Figure 1]
Figure 1
Perspective views of the crystal structures of CuCr2O4 (left) and MgCr2O4 (right) along the a-axis of the I41/amd cell. CuO4 tetrahedra are drawn in green, MgO4 tetrahedra in grey. In CuCr2O4, the contraction along the c direction due to JT flattening of tetrahedral sites is given by a change of tetrahedral angles. Relevant geometrical parameters are reported.

MgCr2O4 forms in the cubic spinel structure (Fig. 1[link], right panel). At room temperature (RT), the Mg-rich (x > 0.6) members of the MgxCu1 − xCr2O4 solid solution are cubic, whereas the Cu-rich members (x < 0.43) are tetragonal. A two-phase region separates the cubic and tetragonal phases (Shoemaker & Seshadri, 2010[Shoemaker, D. P. & Seshadri, R. (2010). Phys. Rev. B, 82, 214107.]; De et al., 1983[De, K. S., Ghose, J. & Murthy, S. R. C. (1983). J. Solid State Chem. 47, 264-277.]).

In this work, the effects on the crystal structure and on the tetragonal-to-cubic phase transition of progressive substitution of the Jahn–Teller and d9 Cu2+ cation with the spherical and closed-shell Mg2+ cation in the MgxCu1 − xCr2O4 solid solution have been studied. Given the relevance of strain in determining the structure-electronic properties relation, in situ high-temperature (HT) single-crystal diffraction data are analysed in terms of the evolution of symmetry-adapted strains for samples with different compositions along the joint MgxCu1 − xCr2O4. Observed variations of spontaneous strains accompanying phase transitions are expected to provide detailed insights into the transition mechanisms.

2. Experimental

2.1. Synthesis and crystal growth

Single crystals of cubic Mg-rich and tetragonal Cu-rich chromites belonging to the series MgxCu1 − xCr2O4 were grown by flux decomposition methods. The synthesis of single crystals of the Mg end-member was conducted on the basis of the strategy reported by Lenaz et al. (2004[Lenaz, D., Skogby, H., Princivalle, F. & Hålenius, U. (2004). Phys. Chem. Miner. 31, 633-642.]). Starting compounds were CuO (Fluka, > 99%), MgO (Carlo Erba, > 99%) and Cr2O3 (Merck, 99%). Na2B4O7 was used as a flux in a weight ratio of 2.2 with respect to the reactive mixture. The mixture was submitted to the following heating cycle: (1) heating from RT to 1473 K at a rate of 100 K h−1; (2) soaking at 1473 K for 24 h; (3) cooling to 1173 K at 6 K h−1; (4) isothermal heating at 1173 K for 9 h; (5) rapid cooling to RT. The residue was then washed with warm HCl 20%.

For the syntheses of the tetragonal Cu-rich members of the MgxCu1 − xCr2O4 solid solution, the method reported by Yé et al. (1994[Yé, Z., Crottaz, O., Vaudano, F., Kubel, F., Tissot, P. & Schmid, H. (1994). Ferroelectrics, 162, 103-118.]) for growing crystals of CuCr2O4 has been adapted to different Cu/Mg stoichiometric ratios. Starting compounds were CuO (Fluka, > 99%), MgO (Carlo Erba, > 99%) and K2Cr2O7 (Carlo Erba, > 99%). K2Cr2O7 transforms into Cr2O3, which, when freshly formed, is highly reactive towards copper oxide. Potassium dichromate acts as a reactive flux for the crystal growth and an excess amount was therefore added according to

[(1 - n) ({\rm CuO + MgO + Cr_2O_3}) + n {\rm K_2Cr_2O_7},]

where n was chosen to be equal to 0.2 mol. B2O3 (1 wt%) was added to the mixture in order to increase the homogeneity of the solution and hence improve the quality of the crystals. Different CuO/MgO stoichiometric ratios were used to obtain spinels with nominal compositions: CuCr2O4 (x = 0), Mg0.05Cu0.95Cr2O4 (x = 0.05), Mg0.1Cu0.9Cr2O4 (x = 0.1), Mg0.4Cu0.6Cr2O4 (x = 0.4). The mixtures were submitted to the following heating cycle: (1) heating from RT to 1093 K at 100 K h−1; (2) soaking at 1093 K for 24 h; (3) cooling at 30 K h−1. Given the high refractory properties of MgO, stage (2) was prolonged for 115 h in the case of the mixture with x = 0.4. After the thermal runs, the residues were washed with boiling water and the single crystals removed from the solidified flux.

2.2. Single-crystal XRD at room temperature

Several crystals were isolated from each synthesis residue. They were checked for crystal quality by analysing X-ray diffraction profiles. The selected crystals, labelled Cu100, Cu90, Cu82, Cu57, Cu47 and Mg100 on the basis of their actual compositions as determined from structure refinements and electron-microprobe analyses (see §§2.4[link] and 2.5[link]), were submitted to single-crystal diffraction analysis at RT using a Bruker-AXS APEX diffractometer equipped with a CCD detector. Data collections were carried out with operating conditions 50 kV and 30 mA and graphite-monochromated Mo Kα radiation (λ = 0.7107 Å). The Bruker SMART system of programs was used for preliminary crystal lattice determination and X-ray data collection. A total of 4800 frames (resolution: 512 × 512 pixels) were collected with eight different goniometer settings using the ω-scan mode (scan width: 0.3°ω; exposure time: 5–20 s per frame, depending on the size and relative scattering power of the crystals analysed; detector–sample distance: 60 mm). Complete data collection was achieved up to sin θ/λ ca 0.95 Å−1.

All the tetragonal crystals of the series were twinned, as expected given the synthesis conditions which imply the use of high temperature, where the cubic phase is stable, and subsequent transformation to tetragonal on cooling. I41/amd is a maximal nonisomorphic t-subgroup of [Fd\bar 3m] and the formation of ferroelastic domains, including transformation twinning, is inevitable during the phase transition. The corresponding ferroelastic species according to Aizu's notation (Aizu, 1969[Aizu, K. (1969). J. Phys. Soc. Jpn, 27, 387-396.]) is [m \bar 3 m{\rm F}4/mmm], where `F' stands for ferroic, and separates the parent point group ([m \bar 3 m]) from the derived point group (4/mmm). As [m \bar 3 m] and 4/mmm are of the order 48 and 16, respectively, there are three possible orientation states in the tetragonal phase. In our study, three twin components were found to be present in crystal Cu100, while two components were detected in the other tetragonal crystals.

The Bruker program SAINT+ was used for the data reduction, including intensity integration, background and Lorentz–polarization corrections. Intensity data from the twin components present in tetragonal crystals were integrated taking into account the superposition affecting some diffraction spots. Final unit-cell parameters were obtained by the Bruker GLOBAL least-squares orientation matrix refinement procedure, based on the positions of all measured reflections. The semi-empirical absorption correction of Blessing (1995[Blessing, R. H. (1995). Acta Cryst. A51, 33-38.]), based on the determination of transmission factors for equivalent reflections, was applied using the Bruker programs SADABS or, for twinned crystals, TWINABS (Sheldrick, 2003[Sheldrick, G. M. (2003). SADABS. University of Göttingen, Germany.]). Details of room-temperature data collection by the CCD diffractometer are reported in Table 1[link].

Table 1
Details of data collections and structure refinements of MgxCu1 − xCr2O4 crystals at RT

Standard deviations are in parentheses and refer to the last significant digits.

  Cu100 Cu90 Cu82 Cu57 Cu47 Mg100
Crystal size (mm) 0.5 × 0.5 × 0.5 0.2 × 0.15 × 0.15 0.2 × 0.2 × 0.2 0.15 × 0.1 × 0.1 0.1 × 0.1 × 0.1 0.15 × 0.15 × 0.1
Space group I41/amd I41/amd I41/amd I41/amd I41/amd [Fd\bar 3m]
a (Å) 6.0287 (2) 6.0163 (1) 6.0045 (1) 5.9523 (1) 5.9435 (1) 8.3288 (1)
c (Å) 7.7803 (2) 7.8279 (1) 7.8778 (1) 8.0752 (2) 8.1379 (2)
Reflns measured 11 427 10 608 10 480 10 314 11 374 19 474
Reflns unique 4312 4375 4372 2400 2700 4570
Reflns independent 295 293 294 120 128 129
Twin fraction (%) 6.6 (3) 14.5 (2) 13.6 (2) 27.0 (3) 22.7 (2)
Rint (%) 2.40 2.04 2.41 1.65 1.93 1.78
Reflns with I > 2σI 3682 3791 3822 2240 2582 4480
R1 (%) 2.50 2.03 2.28 4.38 2.54 1.71
Rall (%) 2.91 2.45 2.75 4.67 2.67 1.76
wR2 (%) 6.58 5.27 5.85 11.99 6.82 4.70
GOF 1.086 1.083 1.060 1.205 1.236 1.169
Δρmax (e Å−3) 0.63 0.49 0.75 0.76 0.44 0.63
Δρmin (e Å−3) −1.14 −0.70 −1.03 −0.88 −0.59 −0.54
†Dataset limited to sin θ/λ = 0.7 Å−1.
‡Three twin components with relative abundances of second and third components 3.7 (3), 2.9 (3).

2.3. Single-crystal XRD at high temperature

Crystals Cu100, Cu90, Cu82, Cu54 (not measured at RT by the CCD diffractometer) and Mg100 were submitted to in situ high-temperature single-crystal diffraction investigations using a Philips PW1100 four-circle diffractometer with point-counter detector. Crystals Cu57 and Cu47 were not used for the HT study due to their low diffracted intensities. Operating conditions were 55 kV and 30 mA with graphite-monochromated Mo Kα radiation (λ = 0.7107 Å). Horizontal and vertical apertures of the point counter detector were 2.0 and 1.5°, respectively. High-temperature measurements were performed by using a home-made U-shaped microfurnace, which has been in use in our laboratory for over 15 years. It makes use of a Pt–Pt/Rh resistance, which allows temperatures up to 1273 K to be achieved, and is equipped with a K-type thermocouple. Temperature calibration (calibration curve R2 = 0.9994) is regularly done by known melting points of several pure compounds and by the transition temperature of quartz (Carpenter, Salje, Graeme-Barber, Wruck et al., 1998[Carpenter, M. A., Salje, E. K. H., Graeme-Barber, A., Wruck, B., Dove, M. T. & Knight, K. S. (1998). Am. Mineral. 83, 2-22.]). Reported temperatures are precise to within ±5 K in the whole temperature range. The design of the furnace limits the angular excursion of the ω circle to ca 27.5° (sin θ/λ ca 0.65 Å−1 with Mo Kα radiation). As routinely done for HT measurements using this system, the selected crystals were inserted into quartz capillaries (0.3–0.5 mm Ø, depending on the dimensions of the crystals) and kept in position by means of quartz wool in order to avoid any mechanical stress. Unit-cell parameters were measured from RT up to 1173 K at regular steps. At each working temperature, the orientation matrix was updated by centring 24 reflections selected in the range of sin θ/λ ca 0.2–0.34 Å−1, and accurate lattice param­eters (reported in Tables 2[link] and 3[link] for tetragonal and cubic phases, respectively) were derived from a least-squares procedure based on the Philips LAT routine over up to 60 d*-spacings, each measured from the positions of all reflection pairs at ±θ in the range of sin θ/λ 0.073–0.628 Å−1.

Table 2
Tetragonal unit-cell parameters of MgxCu1 − xCr2O4 crystals at different temperatures

Standard deviations are in parentheses and refer to the last significant digits.

  Cu100 Cu90 Cu82   Cu54
T (K) a (Å) × [\surd 2] c (Å) a (Å) × [\surd 2] c (Å) a (Å) × [\surd 2] c (Å) T (K) a (Å) × [\surd 2] c (Å)
298 8.5249 (6) 7.7811 (10) 8.5103 (5) 7.8320 (11) 8.4924 (7) 7.8771 (10) 298 8.401 (3) 8.122 (4)
323 8.5264 (6) 7.7826 (10) 8.5128 (4) 7.8335 (6) 8.4914 (6) 7.8810 (8) 323 8.402 (2) 8.140 (2)
348 8.5257 (5) 7.7900 (8) 8.5124 (5) 7.8409 (5) 8.4900 (6) 7.8889 (8) 343 8.397 (2) 8.162 (3)
373 8.5251 (4) 7.7962 (7) 8.5118 (5) 7.8488 (7) 8.4913 (6) 7.8970 (7) 353 8.391 (4) 8.177 (6)
398 8.5252 (4) 7.8026 (7) 8.5117 (5) 7.8564 (5) 8.4899 (6) 7.9053 (7) 363 8.388 (2) 8.204 (4)
423 8.5253 (4) 7.8092 (8) 8.5105 (5) 7.8644 (7) 8.4890 (5) 7.9147 (5) 373 8.385 (3) 8.220 (4)
448 8.5257 (4) 7.8149 (8) 8.5102 (5) 7.8724 (7) 8.4880 (6) 7.9233 (6) 383 8.380 (5) 8.242 (9)
473 8.5249 (6) 7.8222 (9) 8.5094 (5) 7.8804 (5) 8.4849 (6) 7.9340 (8) 393 8.369 (5) 8.276 (9)
498 8.5253 (5) 7.8286 (10) 8.5081 (5) 7.8897 (6) 8.4843 (6) 7.9457 (6) 403 8.362 (4) 8.288 (7)
523 8.5239 (4) 7.8350 (7) 8.5089 (7) 7.8989 (9) 8.4826 (6) 7.9581 (5) 413 8.350 (3) 8.306 (6)
548 8.5237 (5) 7.8444 (9) 8.5058 (5) 7.9093 (6) 8.4789 (7) 7.9716 (7) 423 8.344 (2) 8.320 (3)
573 8.5229 (4) 7.8529 (7) 8.5046 (8) 7.9198 (9) 8.4750 (7) 7.9880 (6) 423 8.338 (3) 8.320 (6)
598 8.5224 (5) 7.8610 (8) 8.5016 (6) 7.9320 (8) 8.4699 (11) 8.0072 (15)
623 8.5215 (5) 7.8706 (8) 8.4981 (8) 7.9467 (9) 8.4590 (10) 8.0337 (15)
648 8.5188 (5) 7.8813 (8) 8.4940 (8) 7.9620 (11)
673 8.5182 (4) 7.8921 (7) 8.4892 (12) 7.9811 (20)
698 8.5155 (5) 7.9043 (8)
723 8.5129 (5) 7.9169 (9)
748 8.5095 (5) 7.9337 (9)
773 8.5055 (4) 7.9479 (8)
788 8.4998 (4) 7.9655 (7)
803 8.4955 (5) 7.9793 (8)
818 8.4899 (5) 7.9964 (7)
†Crystal size: 0.15 × 0.15 × 0.15 mm.
‡On cooling.

Table 3
Cubic unit-cell parameters of MgxCu1 − xCr2O4 crystals at different temperatures

Standard deviations are in parentheses and refer to the last significant digits. Some intermediate data have been omitted in the table but are present in the graphs.

T (K) Cu100 Cu90 Cu82 Cu54 Mg100
298 8.3312 (4)
323 8.3304 (4)
373 8.3342 (4)
423 8.3369 (3)
433 8.337 (4)
473 8.337 (2) 8.3391 (4)
523 8.339 (2) 8.3420 (5)
573 8.340 (2) 8.3458 (4)
623 8.347 (2) 8.3491 (5)
673 8.348 (2) 8.3523 (4)
698 8.3314 (5)
723 8.3333 (5) 8.353 (2) 8.3557 (5)
773 8.3393 (6) 8.3372 (5) 8.356 (2) 8.3571 (5)
823 8.3424 (6) 8.3420 (4) 8.358 (2) 8.3616 (5)
873 8.3411 (5) 8.3448 (6) 8.3446 (4) 8.359 (2) 8.3635 (5)
898 8.3431 (4) 8.3466 (6)
923 8.3465 (7) 8.3492 (5) 8.3502 (5) 8.363 (2) 8.3686 (5)
973 8.3505 (9) 8.3523 (6) 8.3498 (5) 8.366 (2) 8.3711 (5)
1023 8.3546 (11) 8.3564 (6) 8.3545 (5) 8.369 (2) 8.3734 (5)
1073 8.3557 (7) 8.3601 (6) 8.3572 (4) 8.372 (2) 8.3769 (5)
1123 8.3609 (6) 8.3626 (5) 8.374 (2) 8.3797 (5)
1173 8.3622 (4) 8.3667 (6) 8.3665 (5) 8.378 (2) 8.3828 (6)
†Measured at 863 K.

For each crystal, complete datasets of diffracted intensities were collected at different temperatures, both below and above the phase transition temperature, using the same operating conditions as reported above. Intensity data were measured in the sin θ/λ range 0.05–0.628 Å−1 in the ω-scan mode (2.0° θ scan width; 0.05° θ s−1 scan speed). Only diffraction spots belonging to the orientation matrix of the main twin component were measured, thus including overlapping reflections. Three standard reflections were collected every 200 measured reflections. X-ray diffraction intensities were obtained by measuring step-scan profiles and analysing them by the Lehmann & Larsen (1974[Lehmann, M. S. & Larsen, F. K. (1974). Acta Cryst. A30, 580-584.]) σI/I method, as modified by Blessing et al. (1974[Blessing, R. H., Coppens, P. & Becker, P. (1974). J. Appl. Cryst. 7, 488-492.]). Intensities were corrected for absorption using the semi-empirical φ-scan method of North et al. (1968[North, A. C. T., Phillips, D. C. & Mathews, F. S. (1968). Acta Cryst. A24, 351-359.]). Relevant parameters for data collected at different temperatures are reported in Table 4[link]. Some reflections, representative of different classes, were also scanned periodically (ω/2θ scan mode; 2.0° θ scan width; 0.1° θ s−1 scan speed) to check for the crystallinity of the sample.

Table 4
Details on data collections and structure refinements of MgxCu1 − xCr2O4 crystals at HT

  Reflns measured Reflns independent Rint (%) Reflns I > 2σI R1 (%) Rall (%) wR2 (%) GOF Δρmax (e Å−3) Δρmin (e Å−3)
Cu100
298 K 187 89 3.31 76 2.11 2.76 5.41 1.143 0.41 −0.77
373 K 187 89 3.73 77 2.71 3.12 5.71 1.111 0.59 −1.15
473 K 191 91 3.57 79 2.72 3.19 5.93 1.060 0.53 −1.21
573 K 191 91 3.04 78 2.72 3.40 7.01 1.158 0.56 −1.06
673 K 192 92 3.41 78 2.71 3.30 6.10 1.175 0.64 −1.03
773 K 195 93 2.74 78 2.61 3.49 6.21 1.112 0.45 −0.87
803 K 195 93 2.59 78 2.74 3.54 6.84 1.142 0.64 −1.00
863 K 192 45 5.32 41 3.34 3.72 7.47 1.329 0.91 −0.53
973 K 192 45 11.49 37 7.05 7.68 10.50 1.422 3.25 −1.01
1073 K 192 45 19.08 38 8.42 9.26 12.44 1.190 3.70 −0.86
                     
Cu90
298 K 191 91 1.54 78 1.87 2.62 4.86 1.114 0.51 −0.69
373 K 191 91 2.25 75 2.23 3.16 5.84 1.171 0.60 −0.91
473 K 191 91 2.21 74 2.53 3.43 6.70 1.152 0.54 −0.92
573 K 193 92 2.73 74 2.42 3.45 6.15 1.127 0.50 −0.94
673 K 196 93 2.83 79 3.08 3.77 6.84 1.138 0.63 −1.16
773 K 192 45 2.13 37 1.44 2.14 3.41 1.247 0.34 −0.33
873 K 192 45 2.41 36 1.66 2.45 5.41 1.432 0.46 −0.48
973 K 192 45 2.58 38 1.73 2.35 5.17 1.253 0.34 −0.42
1073 K 192 45 2.55 38 1.67 2.65 5.04 1.230 0.43 −0.44
1173 K 192 45 2.67 38 1.82 3.09 5.68 1.304 0.67 −0.61
                     
Cu82
298 K 191 91 2.20 76 3.59 4.16 9.15 1.219 0.65 −1.59
373 K 193 92 2.85 76 3.48 4.61 8.53 1.167 0.70 −1.64
473 K 387 93 3.02 76 3.22 4.36 8.39 1.064 0.89 −1.31
573 K 196 93 3.44 80 3.89 4.53 9.25 1.147 0.71 −1.47
623 K 388 93 3.90 76 3.50 4.36 8.64 1.186 0.82 −1.55
673 K 192 45 14.20 37 6.65 7.96 12.92 1.090 3.03 −1.80
723 K 192 45 2.02 37 1.41 2.11 5.24 1.248 0.39 −0.29
823 K 756 45 2.16 38 1.68 2.43 4.90 1.199 0.34 −0.33
923 K 192 45 2.14 38 1.59 2.40 4.88 1.312 0.26 −0.30
1023 K 192 45 2.54 38 1.67 2.47 5.39 1.298 0.42 −0.30
                     
Cu54
298 K 196 93 6.50 78 4.56 5.49 10.00 1.115 0.85 −0.80
353 K 197 94 11.09 74 4.83 6.00 11.79 1.121 0.98 −0.75
473 K 728 45 2.47 41 2.93 3.25 6.51 1.134 0.62 −0.62
673 K 192 45 2.90 40 3.41 3.76 7.62 1.105 0.52 −0.79
873 K 192 45 3.04 41 3.59 3.79 8.33 1.186 0.47 −0.83
1073 K 192 45 2.97 40 3.35 3.89 7.26 1.210 0.61 −0.77
423 K 201 96 2.51 85 2.31 2.85 6.22 1.114 0.48 −0.47
                     
Mg100
298 K 192 45 1.94 43 2.25 2.27 8.32 1.351 0.44 −0.48
523 K 192 45 2.11 39 2.01 3.00 5.53 1.333 0.62 −0.41
973 K 756 45 2.77 39 2.43 3.38 6.04 1.217 0.69 −0.48
†Cubic.
‡On cooling

2.4. Structure refinements

All structure refinements were carried out by full-matrix least-squares using SHELXL97 (Sheldrick, 2008[Sheldrick, G. M. (2008). Acta Cryst. A64, 112-122.]). Equivalent reflections were averaged, and the resulting internal agreement factors Rint are reported in Table 1[link] for all the datasets collected at RT, and in Table 4[link] for datasets collected at HT. The atomic scattering curves were taken from International Tables for X-ray Crystallography (Ibers & Hamilton, 1974[Ibers, J. A. & Hamilton, W. C. (1974). International Tables for X-ray Crystallography, Vol. 4, pp. 99-101. Birmingham, UK: Kynoch Press.]). For datasets collected at RT by the CCD diffractometer, contributions from the different twin components were taken into account by using the HKLF-5 format in SHELXL97 and including the BASF parameter in the refinement. For all structure refinements, structure factors were weighted according to w = 1/[σ2(Fo2) + (AP)2 + BP], where P = (Fo2 + 2 Fc2)/3, and A and B were chosen for every crystal to produce a flat analysis of variance in terms of Fc2, as suggested by the program. An extinction parameter x was refined to correct the structure factors according to the equation: Fo = [F_{\rm c}\, k [\,1 \,+ \,0.001xF_{\rm c}^{\,2}\,\lambda_3\,/\sin \,2\theta\,]^{-1/4}] (where k is the overall scale factor). In addition to x and k, atomic positions, anisotropic displacement parameters and site occupancy at the A site (for terms with intermediate composition) were refined simultaneously. The Cu/Mg ratios obtained from unconstrained refinements of site occupancy were close to the nominal compositions and were then confirmed by electron microprobe analyses performed on the same crystals at the end of the HT experiments (see §2.5[link]). Final difference-Fourier maps were featureless. Values of the conventional agreement indices, R1 and Rall, as well as the goodness of fit (S) are reported in Tables 1[link] and 4[link] for RT and HT datasets, respectively, whereas interatomic distances and selected geometrical parameters are reported in Table 5[link] for the RT datasets and in Tables 6–10[link][link][link][link][link] for the HT datasets. Atomic fractional coordinates, anisotropic displacement parameters Uij and lists of observed and calculated structure factors are available in the CIF files of supporting information.

Table 5
Electron microprobe analyses and selected geometrical parameters for MgxCu1 − xCr2O4 crystals at RT

Standard deviations are in parentheses and refer to the last significant digits. OAV = Octahedral Angle Variance; OQE = Octahedral Quadratic Elongation; TAV = Tetrahedral Angle Variance; TQE = Tetrahedral Quadratic Elongation (Robinson et al., 1971[Robinson, K., Gibbs, G. V. & Ribbe, P. H. (1971). Science, 172, 567-570.]).

  Cu100 Cu90 Cu82 Cu57 Cu47 Mg100
x (site occupancy) 0 0.103 (1) 0.183 (1) 0.442 (5) 0.504 (2) 1
x (EPMA) 0 (0) 0.103 (21) 0.178 (28) 0.428 (41) 0.527 (7)
a[\surd 2]/c 1.0958 (3) 1.0869 (2) 1.0779 (2) 1.0424 (3) 1.0328 (3) 1
Voctahedron3) 10.31 10.30 10.30 10.33 10.37 10.41
Cr—Oaxial (Å) ×2 1.9854 (5) 1.9852 (4) 1.9865 (4) 1.9807 (13) 1.9872 (6) 1.9927 (1)
Cr—Oequatorial (Å) ×4 1.9884 (3) 1.9875 (2) 1.9870 (3) 1.9911 (9) 1.9915 (4) 1.9927 (1)
Cr—Oaverage (Å) 1.9874 (3) 1.9867 (2) 1.9869 (2) 1.9876 (7) 1.9990 (4) 1.9927 (1)
OAV (°) 37.26 36.99 36.56 34.11 34.10 33.35
OQE 1.0101 1.0100 1.0099 1.0091 1.0091 1.0088
Cr—Cr (Å) 2.8856 (1) 2.8904 (1) 2.8958 (1) 2.9162 (1) 2.9248 (1) 2.9447 (1)
Vtetrahedron3) 3.71 3.74 3.77 3.85 3.87 3.90
(Cu,Mg)—O (Å) 1.9598 (4) 1.9607 (4) 1.9615 (4) 1.9616 (12) 1.9646 (6) 1.9660 (3)
O—(Cu,Mg)—O (°) ×2 103.40 (1) 103.89 (1) 104.39 (1) 106.80 (4) 107.29 (2) 109.47
O—(Cu,Mg)—O (°) ×4 122.45 (3) 121.31 (2) 120.21 (3) 114.97 (8) 113.92 (4) 109.47
O⋯O edge (Å) ×2 3.0760 (5) 3.0879 (4) 3.0994 (5) 3.150 (2) 3.1644 (6) 3.2106 (2)
O⋯O edge (Å) ×4 3.4355 (6) 3.4183 (5) 3.4009 (6) 3.308 (2) 3.2938 (8) 3.2106 (2)
TAV (°) 96.86 80.96 66.78 17.81 11.72 0
TQE 1.0270 1.0223 1.0182 1.0047 1.0031 1.0000
†EPMA for sample Cu54 gave x = 0.460 (71).

Table 6
Selected geometrical parameters for CuCr2O4 (Cu100) at HT

Standard deviations are in parentheses and refer to the last significant digits. OAV = Octahedral Angle Variance; OQE = Octahedral Quadratic Elongation; TAV = Tetrahedral Angle Variance; TQE = Tetrahedral Quadratic Elongation (Robinson et al., 1971[Robinson, K., Gibbs, G. V. & Ribbe, P. H. (1971). Science, 172, 567-570.]).

  298 K 373 K 473 K 573 K 673 K 773 K 803 K 863 K 973 K 1073 K
Voct3) 10.30 10.30 10.33 10.38 10.39 10.33 10.38 10.38 10.25 10.26
Cr—Oaxial (Å) ×2 1.985 (5) 1.983 (5) 1.991 (4) 1.992 (5) 1.991 (5) 1.986 (4) 1.997 (5) 1.992 (4) 1.988 (9) 1.986 (4)
Cr—Oeq. (Å) ×4 1.988 (2) 1.989 (2) 1.988 (2) 1.992 (3) 1.993 (2) 1.990 (2) 1.990 (3) 1.992 (4) 1.985 (4) 1.986 (4)
Cr—Oav. (Å) 1.987 (3) 1.987 (3) 1.989 (3) 1.992 (4) 1.992 (3) 1.989 (3) 1.992 (4) 1.992 (4) 1.985 (4) 1.986 (4)
OAV (°) 37.42 37.71 38.18 36.36 36.69 39.83 38.00 36.60 44.97 45.38
OQE 1.0102 1.0102 1.0103 1.0098 1.0099 1.0107 1.0102 1.0097 1.0118 1.0120
Cr—Cr (Å) 2.8855 (2) 2.8881 (1) 2.8925 (2) 2.8973 (1) 2.9031 (1) 2.9102 (2) 2.9138 (2) 2.9490 (2) 2.9523 (3) 2.9542 (2)
Vtetr.3) 3.71 3.74 3.75 3.76 3.80 3.88 3.87 3.96 4.08 4.09
Cu—O (Å) 1.960 (4) 1.962 (4) 1.965 (4) 1.963 (5) 1.967 (4) 1.977 (4) 1.974 (4) 1.976 (7) 1.996 (7) 1.998 (8)
O—Cu—O (°) ×2 103.4 (1) 103.6 (1) 103.6 (1) 103.9 (1) 104.3 (1) 105.0 (1) 105.0 (1) 109.47 109.47 109.47
O—Cu—O (°) ×4 122.4 (3) 122.0 (3) 121.9 (2) 121.2 (3) 120.3 (3) 118.9 (2) 118.8 (3) 109.47 109.47 109.47
O⋯O edge (Å) ×2 3.077 3.084 3.089 3.093 3.107 3.136 3.132 3.226 3.253 3.252
O⋯O edge (Å) ×4 3.435 3.432 3.436 3.422 3.413 3.406 3.397 3.226 3.253 3.252
TAV (°) 96.52 90.18 89.22 80.05 68.37 52.10 50.37 0 0 0
TQE 1.027 1.0250 1.0247 1.0221 1.0187 1.0141 1.0136 1.0000 1.0000 1.0000

Table 7
Selected geometrical parameters for Mg0.10Cu0.90Cr2O4 (Cu90) at HT

Standard deviations are in parentheses and refer to the last significant digits. OAV = Octahedral Angle Variance; OQE = Octahedral Quadratic Elongation; TAV = Tetrahedral Angle Variance; TQE = Tetrahedral Quadratic Elongation (Robinson et al., 1971[Robinson, K., Gibbs, G. V. & Ribbe, P. H. (1971). Science, 172, 567-570.]).

  298 K 373 K 473 K 573 K 673 K 773 K 873 K 973 K 1073 K 1173 K
Voct.3) 10.31 10.34 10.36 10.36 10.39 10.38 10.36 10.41 10.42 10.46
Cr—Oaxial (Å) ×2 1.990 (4) 1.990 (6) 1.990 (7) 1.990 (6) 1.999 (6) 1.991 (2) 1.991 (3) 1.994 (3) 1.994 (3) 1.997 (3)
Cr—Oeq. (Å) ×4 1.986 (2) 1.989 (2) 1.990 (3) 1.990 (3) 1.989 (3) 1.991 (2) 1.991 (3) 1.994 (3) 1.994 (3) 1.997 (3)
Cr—Oav. (Å) 1.988 1.989 1.990 1.990 1.992 1.991 (2) 1.991 (3) 1.994 (3) 1.994 (3) 1.997 (3)
OAV (°) 37.33 36.51 36.72 37.53 37.17 36.68 38.43 37.42 38.50 37.48
OQE 1.0101 1.0099 1.0099 1.0101 1.0100 1.0097 1.0102 1.0099 1.0102 1.0099
Cr—Cr (Å) 2.8914 (2) 2.8946 (1) 2.8995 (1) 2.9053 (2) 2.9130 (4) 2.9484 (2) 2.9503 (2) 2.9530 (2) 2.9557 (2) 2.9581 (2)
Vtetr.3) 3.74 3.75 3.78 3.82 3.85 3.96 3.99 3.99 4.01 4.01
(Cu,Mg)—O (Å) 1.962 (3) 1.962 (4) 1.965 (5) 1.969 (5) 1.971 (4) 1.976 (5) 1.981 (6) 1.981 (6) 1.985 (6) 1.984 (7)
O—(Cu,Mg)—O (°) ×2 103.8 (1) 104.0 (1) 104.3 (2) 104.6 (2) 105.0 (1) 109.47 109.47 109.47 109.47 109.47
O—(Cu,Mg)—O (°) ×4 121.6 (2) 121.2 (3) 120.5 (4) 119.7 (3) 118.8 (3) 109.47 109.47 109.47 109.47 109.47
O⋯O edge (Å) ×2 3.087 3.091 3.102 3.117 3.128 3.227 3.235 3.234 3.241 3.240
O⋯O edge (Å) ×4 3.424 3.418 3.411 3.405 3.392 3.227 3.235 3.234 3.241 3.240
TAV (°) 84.57 78.94 70.12 60.42 50.54 0 0 0 0 0
TQE 1.0234 1.0217 1.0192 1.0164 1.0136 1.0000 1.0000 1.0000 1.0000 1.0000

Table 8
Selected geometrical parameters for Mg0.18Cu0.82Cr2O4 (Cu82) at HT

Standard deviations are in parentheses and refer to the last significant digits. OAV = Octahedral Angle Variance; OQE = Octahedral Quadratic Elongation; TAV = Tetrahedral Angle Variance; TQE = Tetrahedral Quadratic Elongation (Robinson et al., 1971[Robinson, K., Gibbs, G. V. & Ribbe, P. H. (1971). Science, 172, 567-570.]).

  298 K 373 K 473 K 573 K 623 K 673 K 723 K 823 K 923 K 1023 K
Voct.3) 10.29 10.29 10.37 10.24 10.36 10.44 10.43 10.41 10.43 10.43
Cr—Oaxial (Å) ×2 1.983 (7) 1.989 (8) 1.997 (7) 1.984 (8) 1.986 (7) 1.995 (7) 1.994 (3) 1.993 (3) 1.995 (3) 1.995 (3)
Cr—Oeq. (Å) ×4 1.987 (4) 1.985 (4) 1.988 (4) 1.984 (4) 1.993 (4) 1.995 (7) 1.994 (3) 1.993 (3) 1.995 (3) 1.995 (3)
Cr—Oav. (Å) 1.986 1.986 1.991 1.984 1.990 1.995 (7) 1.994 (3) 1.993 (3) 1.995 (3) 1.995 (3)
OAV (°) 37.22 38.40 35.60 41.73 35.76 34.65 33.39 35.50 36.03 36.65
OQE 1.0100 1.0103 1.0096 1.0111 1.0095 1.0092 1.0089 1.0094 1.0095 1.0097
Cr—Cr (Å) 2.8958 (2) 2.8990 (2) 2.9041 (2) 2.9115 (2) 2.9165 (3) 2.950 (1) 2.9463 (2) 2.9493 (1) 2.9522 (2) 2.9538 (2)
Vtetr.3) 3.78 3.80 3.79 3.92 3.87 3.94 3.91 3.95 3.97 3.98
(Cu,Mg)—O (Å) 1.963 (6) 1.967 (6) 1.962 (6) 1.980 (6) 1.968 (6) 1.973 (13) 1.967 (6) 1.974 (5) 1.977 (6) 1.979 (6)
O—(Cu,Mg)—O (°) ×2 104.5 (2) 104.5 (2) 104.7 (2) 105.4 (2) 106.1 (2) 109.47 109.47 109.47 109.47 109.47
O—(Cu,Mg)—O (°) ×4 120.1 (4) 120.0 (4) 119.6 (4) 117.9 (4) 116.5 (4) 109.47 109.47 109.47 109.47 109.47
O⋯O edge (Å) ×2 3.104 3.110 3.107 3.151 3.145 3.221 3.212 3.224 3.229 3.233
O⋯O edge (Å) ×4 3.402 3.408 3.392 3.391 3.348 3.221 3.212 3.224 3.229 3.233
TAV (°) 64.95 64.79 59.14 41.07 29.37 0 0 0 0 0
TQE 1.0177 1.0177 1.0161 1.0110 1.0078 1.0000 1.0000 1.0000 1.0000 1.0000

Table 9
Selected geometrical parameters for Mg0.46Cu0.54Cr2O4 [Cu54, x (EPMA) = 0.460(71)] at HT

Standard deviations are in parentheses and refer to the last significant digits. OAV = Octahedral Angle Variance; OQE = Octahedral Quadratic Elongation; TAV = Tetrahedral Angle Variance; TQE = Tetrahedral Quadratic Elongation (Robinson et al., 1971[Robinson, K., Gibbs, G. V. & Ribbe, P. H. (1971). Science, 172, 567-570.]).

  298 K 353 K 473 K 673 K 873 K 1073 K 423 K
Voct.3) 10.23 10.32 10.38 10.47 10.45 10.59 10.45
Cr—Oaxial (Å) ×2 1.978 (7) 1.982 (10) 1.992 (3) 1.997 (3) 1.996 (3) 2.004 (3) 1.989 (5)
Cr—Oeq. (Å) ×4 1.985 (5) 1.990 (6) 1.992 (3) 1.997 (3) 1.996 (3) 2.004 (3) 1.998 (3)
Cr—Oav. (Å) 1.983 1.987 1.992 (3) 1.997 (3) 1.996 (3) 2.004 (3) 1.995
OAV (°) 38.76 36.58 36.04 33.79 36.93 32.74 32.00
OQE 1.0103 1.0097 1.0095 1.0090 1.0098 1.0087 1.0085
Cr—Cr (Å) 2.9212 (9) 2.929 (1) 2.9478 (8) 2.9514 (5) 2.9555 (6) 2.9600 (6) 2.945 (1)
Vtetr.3) 3.92 3.92 3.95 3.93 3.99 3.95 3.89
(Cu,Mg)—O (Å) 1.973 (7) 1.971 (9) 1.974 (5) 1.972 (6) 1.981 (6) 1.975 (6) 1.964 (4)
O—(Cu,Mg)—O (°) ×2 107.3 (2) 107.8 (3) 109.47 109.47 109.47 109.47 109.5 (1)
O—(Cu,Mg)—O (°) ×4 114.0 (4) 112.8 (5) 109.47 109.47 109.47 109.47 109.4 (3)
O⋯O edge (Å) ×2 3.177 3.186 3.224 3.220 3.235 3.225 3.205
O⋯O edge (Å) ×4 3.308 3.284 3.224 3.220 3.235 3.225 3.208
TAV (°) 11.86 6.60 0 0 0 0 0.01
TQE 1.0031 1.0017 1.0000 1.0000 1.0000 1.0000 1.0000
†On cooling.

Table 10
Selected geometrical parameters for MgCr2O4 (Mg100) at HT

Standard deviations are in parentheses and refer to the last significant digits.

  298 K 523 K 973 K
Voct.3) 10.41 10.47 10.52
Cr—O (Å) 1.993 (3) 1.996 (3) 2.000 (3)
OAV (°) 33.93 33.10 35.71
OQE 1.0090 1.0088 1.0095
Cr—Cr (Å) 2.9455 (1) 2.9493 (2) 2.9596 (2)
Vtetr.3) 3.91 3.92 3.99
Mg—O (Å) 1.968 (6) 1.969 (5) 1.981 (6)
O⋯O edge (Å) 3.214 3.215 3.236

2.5. Electron probe microanalyses (EPMA)

At the end of the diffraction experiments, all the crystals used in the present study were embedded in epoxy resin, polished and analysed by electron microprobe. The chemical compositions were measured with a Jeol JXA-8200 electron microprobe, fully automated with 5 crystals and 5 wavelength dispersive spectrometers. The polished samples were coated with about 10 nm of amorphous carbon to avoid charging of the surface and studied at acceleration voltages of 15 kV and probe current of 15 nA. The analytical standards used for the calibration of the energy position of the analyzed elements were Cu2O, MgO and Cr2O3 for Cu, Mg and Cr, respectively. For each sample, 10 to 15 points were measured and the averaged chemical compositions, as well as the corresponding standard deviations, are reported in Table 5[link].

3. Results and discussion

3.1. Unit-cell parameters and geometry of tetrahedra at RT

Refinements of X-ray diffraction data reveal a high sensitivity of the crystal structure to the amount of Cu2+ present. The unit-cell parameters are reported as a function of Mg content in Fig. 2[link]. They are expressed in terms of the cubic unit cell itself (MgCr2O4) or of the reduced pseudocubic cell (I41/amd structures of the Cu-rich samples). Samples with x ≤ 0.53 are isostructural with CuCr2O4, thus the tetragonal region seems slightly larger than previously reported by De et al. (1983[De, K. S., Ghose, J. & Murthy, S. R. C. (1983). J. Solid State Chem. 47, 264-277.]), in agreement with recent data of Shoemaker & Seshadri (2010[Shoemaker, D. P. & Seshadri, R. (2010). Phys. Rev. B, 82, 214107.]). Across the solid solution, starting from tetragonal CuCr2O4, replacement of Cu by Mg is accompanied by an increase in the c-axis and a decrease in the a-axis lengths, and hence leads to a gradual decrease of the tetragonal distortion.

[Figure 2]
Figure 2
Variation of unit-cell parameters as a function of composition at room temperature across the MgxCu1 − xCr2O4 join. For ease of comparison, the a parameter in the low-temperature tetragonal phase has been scaled and displayed in the pseudocubic setting [{a_{\rm pc}} = a\sqrt 2]. The vertical size of the symbols exceeds the uncertainties in unit-cell parameters.

The influence of the Jahn–Teller effect can be better estimated by looking at the geometry of the tetrahedra. These are flattened and, with respect to the ideal tetrahedron, display four smaller and two angles larger than 109.47° (see Fig. 1[link] for visual reference). The distortion of the tetrahedra is large, with ΔO—Cu—O = 12.94° in the Cu end-member. The distortion of the tetrahedra in the tetragonal phase is also evident in the behaviour of the O⋯O edges. In Fig. 3[link], O—(Cu,Mg)—O angles and O⋯O edges are plotted as a function of composition. With increasing Mg content, the flattening of the tetrahedra is reduced: the two sets of O—(Cu,Mg)—O tetrahedral angles converge towards 109.47°, as required by the [4 \bar 3 m] site symmetry of the cubic phase. A similar behaviour is shown by the tetrahedral edges. Variation of the (Cu,Mg)—O bond length (Table 5[link]) is related to the difference in ion size between Cu2+ and Mg2+.

[Figure 3]
Figure 3
Variation of (a) tetrahedral O—(Cu,Mg)—O angles and (b) O⋯O edges as a function of Mg content. Error bars are within the symbols.

Homogeneity of the solid solution is quite good. EPMA spot analyses reveal a rather narrow composition range within each sample (Table 5[link]), with Cu54 and Cu47 showing the highest e.s.d.s. When looking at the equivalent atomic displacement parameters (ADPs; Fig. 4[link]a), crystals with intermediate compositions show slightly higher values than those of the two end-members due to some static disorder, with an overall behaviour that is common for solid solutions. Interestingly and as already reported previously (e.g. Kennedy & Zhou, 2008[Kennedy, B. & Zhou, Q. (2008). J. Solid State Chem. 181, 2227-2230.]), in all Cu-bearing crystals, the Cu/Mg site is the one showing the highest displacement parameters. This is mainly due to an elongated displacement ellipsoid towards the c-axis (Fig. 4[link]b). The Rmax/Rmin ratio of the principal axes of the thermal ellipsoid is 2.67 for the tetrahedral cation in Cu100 and decreases almost linearly with increasing Mg content, with Cu47 slightly deviating from this trend likely due to some compositional heterogeneity. However, the behaviour observed for the average structure by XRD does not necessarily allow to differentiate the distinct cation coordinations of Mg2+ and Cu2+ if they are different on the local length scale.

[Figure 4]
Figure 4
Variation of atomic displacement parameters as a function of composition: (a) isotropic ADPs of Cu/Mg (blue diamonds), Cr (green diamonds) and O (red diamonds); (b) anisotropic APDs U11 (circles) and U33 (triangles) for the Cu/Mg site.

3.2. High-temperature behaviour

The temperature dependence of the lattice parameters for CuCr2O4 and all the intermediate compounds of the series MgxCu1 − xCr2O4 is shown in Fig. 5[link]. Heating the samples results in a gradual reduction of the splitting of a and c unit-cell parameters. Variation of the unit-cell parameters with temperature for CuCr2O4 is in good agreement with previously reported data (Kennedy & Zhou, 2008[Kennedy, B. & Zhou, Q. (2008). J. Solid State Chem. 181, 2227-2230.]) and shows (Fig. 5[link]a) a large first-order jump above 818 K, when the tetragonal splitting is abruptly lost. By inspection of the variations of the lattice parameters for the samples of intermediate compositions (Figs. 5[link]bd), it is possible to note how the gradual substitution of Cu for Mg causes a reduction of the initial ac splitting and of the discontinuity at the transition, and a shift of the transition temperature towards lower temperatures.

[Figure 5]
Figure 5
Variation as a function of temperature of unit-cell parameters for spinel samples of different compositions across the MgxCu1 − xCr2O4 join. (a) CuCr2O4; (b) Mg0.10Cu0.90Cr2O4; (c) Mg0.18Cu0.82Cr2O4; (d) Mg0.46Cu0.54Cr2O4. The values of a0 are the lattice parameters of the respective cubic parent phase extrapolated from high temperature into the stability field of the tetragonal phase.

The evolution of lattice parameters of cubic phases have been fitted with straight lines, yielding the following thermal expansion αa coefficients: Cu100: 7.1 (3) × 10−5 K−1; Cu90: 6.9 (3) × 10−5 K−1; Cu82: 7.1 (3) × 10−5 K−1; Cu54: 5.9 (2) × 10−5 K−1. The reported values are all very similar and in good agreement with values reported for most cubic spinels. Variations of the cubic reference parameters, a0, for determination of spontaneous strains of the tetragonal phase were obtained by extrapolation to lower temperatures of these fits. The a and c parameters of the tetragonal phase do not converge symmetrically into the extrapolated values of a0 for the cubic phase because of a volume expansion associated with the transition.

The temperature dependence of the angles within the (Cu,Mg)O4 tetrahedron is illustrated in Fig. 6[link] for all the analysed Cu-rich samples. Heating results in a gradual reduction of the compression of the tetrahedron but, clearly, the compression remains significant until near the transition temperature. The variation with temperature of the O—(Cu,Mg)—O angles for the samples of intermediate composition mimics the change in the lattice parameters, the discontinuity of distortion at the transition decreases when Mg is added.

[Figure 6]
Figure 6
Variation of tetrahedral O—(Cu,Mg)—O angles as a function of temperature. Blue: CuCr2O0; red: Mg0.10Cu0.90Cr2O4; orange: Mg0.18Cu0.82Cr2O4; green: Mg0.46Cu0.54Cr2O4. Error bars are within the symbols.

The nature of JT transitions, cooperative or order–disorder, at the solid state has been debated at length and both scenarios observed in several phases (for a review see, e.g., Kugel & Khomskii, 1982[Kugel, K. I. & Khomskii, D. I. (1982). Sov. Phys. Usp. 25, 231-256.]; Goodenough, 1998[Goodenough, J. (1998). Annu. Rev. Mater. Sci. 28, 1-27.]; Bersuker, 2006[Bersuker, B. I. (2006). The Jahn-Teller Effect, pp. 1-616. Cambridge University Press.]). Similarly, in copper spinel, two mechanisms for the JT transition can be proposed: in the first case, upon increasing T, all tetrahedra transform from flattened in the JT distorted spinel to ideal in the cubic spinel; in the second case, the energy-lowering cation coordination distortions persist above the structural transition temperature and CuO4 tetrahedra are always locally JT distorted. In the latter hypothesis, the structural transition has to be regarded as an order–disorder transition, at which local JT distortions become spatially uncorrelated, although do not disappear; the average crystal structure, which would in turn result in regular tetrahedra, accounts for this disorder through increased thermal displacement parameters.

In the case of JT transitions in systems with octahedrally coordinated cations, as in the case of manganite perovskites, large ADPs for O atoms are observed in the disordered phase along the cation—O bonds, reflecting the largest static bond length distribution (i.e. a mixture of long and short bonds) in these directions. In CuCr2O4, the distortions involve the tetrahedral angles, ADPs of Cu and O atoms are not elongated in a direction parallel to Cu—O bonds. ADPs of O atoms are elongated perpendicularly to the Cu—O bonds, whereas those of Cu atoms are elongated along the c-axis. Both these apparent vibrations affect the tetrahedral angles rather than bond lengths and may indicate the presence of disorder at the Cu sites in the tetragonal phase.

The temperature dependence of the isotropic atomic displacement parameters for Cu, Cr and O atoms in CuCr2O4 and the intermediate compounds of the series MgxCu1 − xCr2O4 is shown in Fig. 7[link]. With increasing temperature up to the transition, the isotropic ADPs of the Cu-rich samples increase linearly, as expected within the harmonic approximation at T far from 0 K. All tetragonal datasets have linear extrapolation to 0 K that are negligible within 3σ. This indicates the absence of a significant static disorder effect. In samples Cu90 and Cu82, this may be interpreted by considering that the ionic radii of both Mg2+ and Cu2+ in coordination 4 is 0.57 Å (Shannon, 1976[Shannon, R. D. (1976). Acta Cryst. A32, 751-767.]). On the other hand, large scatter is displayed at low T by the ADPs of Cu54 sample, which shows a less clear trend in the tetragonal phase, likely due to compositional heterogeneities.

[Figure 7]
Figure 7
Variation as a function of temperature of isotropic atomic displacement parameters of Cu/Mg (blue diamonds), Cr (green diamonds) and O (red diamonds) atoms for spinel samples of different compositions across the MgxCu1 − xCr2O4 join. (a) CuCr2O4; (b) Mg0.10Cu0.90Cr2O4; (c) Mg0.18Cu0.82Cr2O4; (d) Mg0.46Cu0.54Cr2O4.

For all samples, a discontinuity in the temperature evolution of ADPs can be observed at the transition temperature. The observed behaviour of ADPs would suggest the transition to be driven by cooperative distortion, although the presence of an order–disorder component cannot be excluded on the basis of average structure information only.

3.3. Spontaneous strain in CuCr2O4

Instability of the electronic structure is the driving mechanism for a Jahn–Teller transition. However, the change in the structural state appears overtly as changes in lattice parameters, and these can be described formally in terms of macroscopic strains. Variations of spontaneous strains accompanying a phase transition can be used to quantify the associated order parameters and are expected to provide detailed insights into the mechanisms of the transition itself. Strain parameters have been calculated by using the equations given by Carpenter, Salje & Graeme-Barber (1998[Carpenter, M. A., Salje, E. K. H. & Graeme-Barber, A. (1998). Eur. J. Mineral. 10, 621-691.]), who reviewed the use of spontaneous strain to measure order parameters associated with phase transitions in minerals. In this case, there are two strains, the symmetry-breaking tetragonal shear strain, [{e_{\rm t}} = (1 / {\sqrt 3 })(2{e_3} - {e_1} - {e_2})], where e2 = e1 = (a - a0)/a0, e3 = (c - a0)/a0, and the volume strain, Vs = (V - V0)/ V0.

Values for the reference parameter, V0, were obtained by fitting a straight line to data for the unit-cell volume above the transition and extrapolating to lower temperatures. The resulting strains [e_{\rm t}^2] and Vs are reported in Figs. 8[link](a) and 8(b) as a function of T.

[Figure 8]
Figure 8
Symmetry-adapted strains calculated from lattice parameters for MgxCu1 − xCr2O4 with x = 0, 0.10, 0.18, 0.46. (a) The symmetry-adapted tetragonal strains follow the classical pattern of a first-order phase transition driven by a single-order parameter. (b) Volume strain, Vs, data have been fit with standard solutions to a Landau expansion assuming that Vs scales with the square of the order parameter. On this basis the transition is first order in character at x = 0, 0.10, 0.18 and second order at x = 0.46. (c) Strain–strain relationships: tetragonal strains and volume strains vary linearly with each other at each composition and, within experimental uncertainty, extrapolate to the origin. Same symbols as for Fig. 6[link].

Symmetry rules determine the nature of coupling between the strain and order parameters. The order parameter qJT and the tetragonal strain et transform as [\Gamma _3^ +] of [Fd \overline 3 m], the active representation for the transition to I41/amd, giving coupling of the form λetqJT. Vs, which does not break the cubic symmetry of the high-temperature phase, transforms as the identity representation and is proportional to [q_{\rm JT}^2]. Therefore, the expected relationships between strain components are: [{e_{\rm t}} \propto V^{1/2} \propto {q_{\rm JT}}]. Two strains show a linear dependence when plotted as [e_{\rm t}^2] versus Vs (Fig. 8[link]c), consistent with these symmetry considerations.

The simultaneous linear and quadratic coupling of strain components to the Jahn–Teller order parameter implies a renormalization of the Landau expansion in order parameter for free energy (Landau & Lifshitz, 1958[Landau, L. D. & Lifshitz, E. M. (1958). Statistical Physics. Reading, Massachusetts: Addison Wesley.]): the transition temperature is renormalized by coupling between the Jahn–Teller order parameter and the symmetry-breaking strain et, while the fourth-order term of the expansion contains contributions from coupling of the square of qJT with the volume strain.

With increasing Mg content, the magnitudes of the strains all decrease (Figs. 8[link]a and 8b). A decrease in the discontinuity at the transition and a trend towards linear behaviour are also fairly evident.

The [Fd\bar 3m \leftrightarrow I4_1/{amd}] transition is required to be first order in character due to the existence of a third-order term in qJT. However, the strain variations with temperatures are not well represented by the standard solution for the order parameter

[{q_{\rm JT}} = {3 \over 4}{q_{\rm 0,JT}}\left\{ {1 + {{\left [{1 - {4 \over 9}{{T - T_{\rm c}^*} \over {{T_{\rm tr}} - T_{\rm c}^*}}} \right]}^{1/2}}} \right\},]

where Ttr is the transition temperature and Tc* the renormalized critical temperature. Rather, the data for Cu100, Cu90 and Cu82 are well represented by the standard solution for a 246 solution with negative fourth-order coefficient (reported here, from Carpenter, Salje, Graeme-Barber, Wruck et al., 1998[Carpenter, M. A., Salje, E. K. H., Graeme-Barber, A., Wruck, B., Dove, M. T. & Knight, K. S. (1998). Am. Mineral. 83, 2-22.])

[q_{\rm JT}^2 = {3 \over 2}q_{\rm 0,JT}^2\left\{ 1 + \left [1 - {3 \over 4}{{T - T_{\rm c}^*} \over {T_{\rm tr} - T_{\rm c}^*}} \right]^{1/2} \right\}]

as shown in Figs. 8[link](a) and (b). At T = Ttr, the jump in the value of qJT from zero to q0,JT, is

[q_{\rm 0,JT}^2 = - {{4a} \over {{b^*}}}\left({{T_{\rm tr}} - T_c^*} \right),]

where a and b* here are the second- and the renormalized fourth-order terms in the Landau expansion, respectively.

The equilibrium transition temperature Ttr for the three Cu-rich samples, as determined by [e_{\rm t}^2] fits reported in Fig. 8[link], is 834 K (Tc* set to 780 K and q0,JT2 = 4.34 × 10−3) for Cu100, 722 K (Tc* set to 675 K and q0,JT2 = 3.76 × 10−3) for Cu90, and 651 K (Tc* set to 625 K and q0,JT2 = 2.65 × 10−3) for Cu82. Ttr decreases linearly as a function of XMg as evident in Fig. 9[link], where the transition temperature for MgCr2O4 (data from Kemei et al., 2013[Kemei, M. C., Barton, P. T., Moffitt, S. L., Gaultois, M. W., Kurzman, J. A., Seshadri, R., Suchomel, M. R. & Kim, Y.-I. (2013). J. Phys. Condens. Matter, 25, 326001.]) is also shown for comparison. The difference between Ttr and Tc*, which is a measure of the extent of the first-order character of the transition, decreases systematically with increasing Mg content as well.

[Figure 9]
Figure 9
Variation of Ttr and Tc* as a function of Mg content. Magnetic driven structural transition temperature (Nèel temperature) for MgCr2O4 (Kemei et al., 2013[Kemei, M. C., Barton, P. T., Moffitt, S. L., Gaultois, M. W., Kurzman, J. A., Seshadri, R., Suchomel, M. R. & Kim, Y.-I. (2013). J. Phys. Condens. Matter, 25, 326001.]) is also shown for comparison.

At x = 0.46, the transition conforms to [V_{\rm s} \propto e_{\rm t}^2 \propto q_{\rm JT}^2 \propto (T_{\rm c}^* - T)], with Tc* = 407 K, and thus appears to be second order in character.

This is all consistent with the third-order term being small for the Cu–Mg spinel system and the change from first-order to second-order character being due to changes in the value of the fourth-order coefficient. Coupling of the volume strain with the order parameter leads to a renormalization of the fourth-order coefficient and reductions in the strength of this coupling, as appears to occur with increasing Mg content, would contribute to this trend.

4. Summary

Tetragonal distortion of Cu-rich members of the MgxCu1 − xCr2O4 spinel solid solution, due to a cooperative Jahn–Teller effect, can be suppressed either by increasing temperature or by gradually replacing Cu2+ with Mg2+. The effect is to dilute the nearest-neighbour interactions of Cu2+ ions, thus reducing the efficiency of the cooperative distortion. With increasing the Mg content, a gradual reduction of the splitting of a and c unit-cell parameters and of the flattening of the tetrahedra is observed, and the transition temperature also decreases.

Jahn–Teller distortions of individual (Mg,Cu) tetrahedra are accompanied by variations in unit-cell parameters. Large spontaneous strains, coupling with an order parameter which originates physically from an electronic instability, lead to mean-field behaviour. The underlying role of strain in promoting long-range interactions is confirmed by the analysis of strain evolution, which shows that the Jahn–Teller phase transitions in CuCr2O4 conform to mean-field behaviour. Increasing Mg content causes reductions in the magnitude of the strains, and the two coupling coefficients also reduce with increasing Mg content. Reducing the coupling with the volume strain reduces in turn the renormalization of the fourth-term order Landau coefficient so that it goes from negative to positive, hence the tetragonal-to-cubic phase transition evolves from first order for Cu-rich samples towards second order at an intermediate composition.

Supporting information


Computing details top

Program(s) used to solve structure: SHELXS97 (Sheldrick, 1990) for Mg100_RT_CCD_C. Program(s) used to refine structure: SHELXL97 (Sheldrick, 2008) for Cu100_RT_CCD_T; SHELXL97 (Sheldrick, 1997) for Mg100_RT_CCD_C.

(Cu100_RT_CCD_T) top
Crystal data top
Cr2CuO4Z = 4
Mr = 231.54F(000) = 436
Tetragonal, I41/amdDx = 5.439 Mg m3
a = 6.0287 (1) ÅMo Kα radiation, λ = 0.71073 Å
c = 7.7803 (2) ŵ = 14.81 mm1
V = 282.78 (1) Å3T = 293 K
Data collection top
Radiation source: fine-focus sealed tubeRint = 0.000
Graphite monochromatorθmax = 42.7°, θmin = 4.3°
4312 measured reflectionsh = 1111
4312 independent reflectionsk = 1111
3682 reflections with I > 2σ(I)l = 1414
Refinement top
Refinement on F2Primary atom site location: structure-invariant direct methods
Least-squares matrix: fullSecondary atom site location: difference Fourier map
R[F2 > 2σ(F2)] = 0.025 w = 1/[σ2(Fo2) + (0.0361P)2]
where P = (Fo2 + 2Fc2)/3
wR(F2) = 0.066(Δ/σ)max = 0.001
S = 1.09Δρmax = 0.63 e Å3
4312 reflectionsΔρmin = 1.14 e Å3
16 parametersExtinction correction: SHELXL, Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4
0 restraintsExtinction coefficient: 0.0216 (7)
Special details top

Geometry. All s.u.'s (except the s.u. in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell s.u.'s are taken into account individually in the estimation of s.u.'s in distances, angles and torsion angles; correlations between s.u.'s in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell s.u.'s is used for estimating s.u.'s involving l.s. planes.

Refinement. Refinement of F2 against ALL reflections. The weighted R-factor wR and goodness of fit S are based on F2, conventional R-factors R are based on F, with F set to zero for negative F2. The threshold expression of F2 > 2σ(F2) is used only for calculating R-factors(gt) etc. and is not relevant to the choice of reflections for refinement. R-factors based on F2 are statistically about twice as large as those based on F, and R- factors based on ALL data will be even larger.

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top
xyzUiso*/Ueq
Cu010.00000.25000.37500.00847 (4)
Cr020.00000.00000.00000.00445 (4)
O0030.00000.53493 (7)0.25374 (6)0.00545 (8)
Atomic displacement parameters (Å2) top
U11U22U33U12U13U23
Cu010.00544 (5)0.00544 (5)0.01451 (8)0.0000.0000.000
Cr020.00474 (6)0.00372 (6)0.00490 (6)0.0000.0000.00000 (4)
O0030.00552 (17)0.00474 (16)0.00607 (17)0.0000.0000.00050 (14)
Geometric parameters (Å, º) top
Cu01—O003i1.9598 (4)Cr02—O003viii1.9884 (3)
Cu01—O003ii1.9598 (4)Cr02—Cr02ix2.8856
Cu01—O0031.9598 (4)Cr02—Cr02x2.8856
Cu01—O003iii1.9598 (4)Cr02—Cr02xi2.8856
Cr02—O003ii1.9854 (5)Cr02—Cr02xii2.8856
Cr02—O003iv1.9854 (5)O003—Cr02ii1.9854 (5)
Cr02—O003v1.9884 (3)O003—Cr02xiii1.9884 (3)
Cr02—O003vi1.9884 (3)O003—Cr02xiv1.9884 (3)
Cr02—O003vii1.9884 (3)
O003i—Cu01—O003ii103.399 (12)O003v—Cr02—Cr02x87.396 (11)
O003i—Cu01—O003103.399 (12)O003vi—Cr02—Cr02x92.604 (11)
O003ii—Cu01—O003122.45 (3)O003vii—Cr02—Cr02x43.395 (14)
O003i—Cu01—O003iii122.45 (3)O003viii—Cr02—Cr02x136.605 (14)
O003ii—Cu01—O003iii103.399 (12)Cr02ix—Cr02—Cr02x180.0
O003—Cu01—O003iii103.399 (12)O003ii—Cr02—Cr02xi43.475 (8)
O003ii—Cr02—O003iv180.00 (3)O003iv—Cr02—Cr02xi136.525 (8)
O003ii—Cr02—O003v93.774 (18)O003v—Cr02—Cr02xi136.605 (14)
O003iv—Cr02—O003v86.226 (18)O003vi—Cr02—Cr02xi43.395 (14)
O003ii—Cr02—O003vi86.226 (18)O003vii—Cr02—Cr02xi92.604 (11)
O003iv—Cr02—O003vi93.774 (18)O003viii—Cr02—Cr02xi87.396 (11)
O003v—Cr02—O003vi180.0Cr02ix—Cr02—Cr02xi62.975 (1)
O003ii—Cr02—O003vii93.774 (18)Cr02x—Cr02—Cr02xi117.025 (1)
O003iv—Cr02—O003vii86.226 (18)O003ii—Cr02—Cr02xii136.525 (8)
O003v—Cr02—O003vii81.399 (19)O003iv—Cr02—Cr02xii43.475 (8)
O003vi—Cr02—O003vii98.601 (19)O003v—Cr02—Cr02xii43.395 (14)
O003ii—Cr02—O003viii86.226 (18)O003vi—Cr02—Cr02xii136.605 (14)
O003iv—Cr02—O003viii93.774 (18)O003vii—Cr02—Cr02xii87.396 (11)
O003v—Cr02—O003viii98.601 (19)O003viii—Cr02—Cr02xii92.604 (11)
O003vi—Cr02—O003viii81.399 (19)Cr02ix—Cr02—Cr02xii117.025 (1)
O003vii—Cr02—O003viii180.000 (19)Cr02x—Cr02—Cr02xii62.975 (1)
O003ii—Cr02—Cr02ix43.475 (8)Cr02xi—Cr02—Cr02xii180.0
O003iv—Cr02—Cr02ix136.525 (8)Cu01—O003—Cr02ii112.69 (2)
O003v—Cr02—Cr02ix92.604 (11)Cu01—O003—Cr02xiii125.353 (13)
O003vi—Cr02—Cr02ix87.396 (11)Cr02ii—O003—Cr02xiii93.130 (16)
O003vii—Cr02—Cr02ix136.605 (14)Cu01—O003—Cr02xiv125.353 (13)
O003viii—Cr02—Cr02ix43.395 (14)Cr02ii—O003—Cr02xiv93.130 (16)
O003ii—Cr02—Cr02x136.525 (8)Cr02xiii—O003—Cr02xiv98.576 (19)
O003iv—Cr02—Cr02x43.475 (8)
Symmetry codes: (i) y1/4, x+1/4, z+3/4; (ii) x, y+1/2, z; (iii) y+1/4, x+1/4, z+3/4; (iv) x, y1/2, z; (v) y+3/4, x+1/4, z1/4; (vi) y3/4, x1/4, z+1/4; (vii) y3/4, x+1/4, z1/4; (viii) y+3/4, x1/4, z+1/4; (ix) y+1/4, x1/4, z+1/4; (x) y1/4, x+1/4, z1/4; (xi) y1/4, x1/4, z+1/4; (xii) y+1/4, x+1/4, z1/4; (xiii) y+1/4, x+3/4, z+1/4; (xiv) y1/4, x+3/4, z+1/4.
(Mg100_RT_CCD_C) top
Crystal data top
Cr2MgO4F(000) = 736
Mr = 192.31Dx = 4.422 Mg m3
Cubic, Fd3mMo Kα radiation, λ = 0.71073 Å
a = 8.3288 (1) ŵ = 7.55 mm1
V = 577.76 (1) Å3T = 293 K
Z = 8
Data collection top
Radiation source: fine-focus sealed tubeRint = 0.000
Graphite monochromatorθmax = 42.5°, θmin = 4.2°
4570 measured reflectionsh = 1515
4570 independent reflectionsk = 1415
4480 reflections with I > 2σ(I)l = 1515
Refinement top
Refinement on F2Primary atom site location: structure-invariant direct methods
Least-squares matrix: fullSecondary atom site location: difference Fourier map
R[F2 > 2σ(F2)] = 0.017 w = 1/[σ2(Fo2) + (0.0207P)2 + 1.559P]
where P = (Fo2 + 2Fc2)/3
wR(F2) = 0.047(Δ/σ)max = 0.001
S = 1.17Δρmax = 0.63 e Å3
4570 reflectionsΔρmin = 0.54 e Å3
8 parametersExtinction correction: SHELXL, Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4
0 restraintsExtinction coefficient: 0.00248 (11)
Special details top

Geometry. All esds (except the esd in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell esds are taken into account individually in the estimation of esds in distances, angles and torsion angles; correlations between esds in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell esds is used for estimating esds involving l.s. planes.

Refinement. Refinement of F2 against ALL reflections. The weighted R-factor wR and goodness of fit S are based on F2, conventional R-factors R are based on F, with F set to zero for negative F2. The threshold expression of F2 > 2sigma(F2) is used only for calculating R-factors(gt) etc. and is not relevant to the choice of reflections for refinement. R-factors based on F2 are statistically about twice as large as those based on F, and R- factors based on ALL data will be even larger.

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top
xyzUiso*/Ueq
Mg0.37500.37500.37500.00486 (4)
Cr0.00000.00000.00000.00450 (2)
O010.238715 (18)0.238715 (18)0.238715 (18)0.00560 (4)
Atomic displacement parameters (Å2) top
U11U22U33U12U13U23
Mg0.00486 (4)0.00486 (4)0.00486 (4)0.0000.0000.000
Cr0.00450 (2)0.00450 (2)0.00450 (2)0.00021 (1)0.00021 (1)0.00021 (1)
O010.00560 (4)0.00560 (4)0.00560 (4)0.00023 (3)0.00023 (3)0.00023 (3)
Geometric parameters (Å, º) top
Mg—O01i1.9660 (3)Cr—O01xii1.9927 (1)
Mg—O01ii1.9660 (3)Cr—O01xiii1.9927 (1)
Mg—O01iii1.9660 (3)Cr—Crxiii2.9447
Mg—O011.9660 (3)Cr—Crix2.9447
Mg—Mgiv3.6065Cr—Crxiv2.9447
Mg—Mgv3.6065Cr—Crxi2.9447
Mg—Mgvi3.6065Cr—Crxv2.9447
Mg—Mgvii3.6065Cr—Crxvi2.9447
Cr—O01viii1.9927 (1)O01—Crix1.9927 (1)
Cr—O01ix1.9927 (1)O01—Crxiii1.9927 (1)
Cr—O01x1.9927 (1)O01—Crxi1.9927 (1)
Cr—O01xi1.9927 (1)
O01i—Mg—O01ii109.471 (1)O01ix—Cr—Crix86.175 (6)
O01i—Mg—O01iii109.5O01x—Cr—Crix137.636 (4)
O01ii—Mg—O01iii109.5O01xi—Cr—Crix42.364 (4)
O01i—Mg—O01109.471 (1)O01xii—Cr—Crix137.636 (4)
O01ii—Mg—O01109.471 (1)O01xiii—Cr—Crix42.364 (4)
O01iii—Mg—O01109.471 (1)Crxiii—Cr—Crix60.0
O01i—Mg—Mgiv70.5O01viii—Cr—Crxiv86.175 (6)
O01ii—Mg—Mgiv70.5O01ix—Cr—Crxiv93.825 (6)
O01iii—Mg—Mgiv70.5O01x—Cr—Crxiv42.364 (4)
O01—Mg—Mgiv180.000 (3)O01xi—Cr—Crxiv137.636 (4)
O01i—Mg—Mgv180.000 (3)O01xii—Cr—Crxiv42.364 (4)
O01ii—Mg—Mgv70.529 (1)O01xiii—Cr—Crxiv137.636 (4)
O01iii—Mg—Mgv70.529 (1)Crxiii—Cr—Crxiv120.0
O01—Mg—Mgv70.5Crix—Cr—Crxiv180.0
Mgiv—Mg—Mgv109.5O01viii—Cr—Crxi137.636 (4)
O01i—Mg—Mgvi70.5O01ix—Cr—Crxi42.364 (4)
O01ii—Mg—Mgvi70.5O01x—Cr—Crxi93.825 (6)
O01iii—Mg—Mgvi180.000 (3)O01xi—Cr—Crxi86.175 (6)
O01—Mg—Mgvi70.529 (1)O01xii—Cr—Crxi137.636 (4)
Mgiv—Mg—Mgvi109.5O01xiii—Cr—Crxi42.364 (4)
Mgv—Mg—Mgvi109.5Crxiii—Cr—Crxi60.0
O01i—Mg—Mgvii70.5Crix—Cr—Crxi60.0
O01ii—Mg—Mgvii180.000 (3)Crxiv—Cr—Crxi120.0
O01iii—Mg—Mgvii70.5O01viii—Cr—Crxv42.364 (4)
O01—Mg—Mgvii70.5O01ix—Cr—Crxv137.636 (4)
Mgiv—Mg—Mgvii109.5O01x—Cr—Crxv86.175 (6)
Mgv—Mg—Mgvii109.5O01xi—Cr—Crxv93.825 (6)
Mgvi—Mg—Mgvii109.5O01xii—Cr—Crxv42.364 (4)
O01viii—Cr—O01ix180.000 (8)O01xiii—Cr—Crxv137.636 (4)
O01viii—Cr—O01x84.471 (9)Crxiii—Cr—Crxv120.0
O01ix—Cr—O01x95.529 (9)Crix—Cr—Crxv120.0
O01viii—Cr—O01xi95.529 (9)Crxiv—Cr—Crxv60.0
O01ix—Cr—O01xi84.471 (9)Crxi—Cr—Crxv180.0
O01x—Cr—O01xi180.000 (17)O01viii—Cr—Crxvi42.364 (4)
O01viii—Cr—O01xii84.471 (9)O01ix—Cr—Crxvi137.636 (4)
O01ix—Cr—O01xii95.529 (9)O01x—Cr—Crxvi42.364 (4)
O01x—Cr—O01xii84.471 (9)O01xi—Cr—Crxvi137.636 (4)
O01xi—Cr—O01xii95.529 (9)O01xii—Cr—Crxvi86.175 (6)
O01viii—Cr—O01xiii95.529 (9)O01xiii—Cr—Crxvi93.825 (6)
O01ix—Cr—O01xiii84.471 (9)Crxiii—Cr—Crxvi180.0
O01x—Cr—O01xiii95.529 (9)Crix—Cr—Crxvi120.0
O01xi—Cr—O01xiii84.471 (9)Crxiv—Cr—Crxvi60.0
O01xii—Cr—O01xiii180.0Crxi—Cr—Crxvi120.0
O01viii—Cr—Crxiii137.636 (4)Crxv—Cr—Crxvi60.0
O01ix—Cr—Crxiii42.364 (4)Mg—O01—Crix121.439 (6)
O01x—Cr—Crxiii137.636 (4)Mg—O01—Crxiii121.439 (6)
O01xi—Cr—Crxiii42.364 (4)Crix—O01—Crxiii95.273 (8)
O01xii—Cr—Crxiii93.825 (6)Mg—O01—Crxi121.439 (6)
O01xiii—Cr—Crxiii86.175 (6)Crix—O01—Crxi95.273 (8)
O01viii—Cr—Crix93.825 (6)Crxiii—O01—Crxi95.273 (8)
Symmetry codes: (i) x+3/4, y, z+3/4; (ii) x+3/4, y+3/4, z; (iii) x, y+3/4, z+3/4; (iv) x+1, y+1, z+1; (v) x+1/2, y+1, z+1/2; (vi) x+1, y+1/2, z+1/2; (vii) x+1/2, y+1/2, z+1; (viii) x1/4, y, z1/4; (ix) x+1/4, y, z+1/4; (x) x1/4, y1/4, z; (xi) x+1/4, y+1/4, z; (xii) x, y1/4, z1/4; (xiii) x, y+1/4, z+1/4; (xiv) x1/4, y, z1/4; (xv) x1/4, y1/4, z; (xvi) x, y1/4, z1/4.
 

Footnotes

Present address: Laboratoire de Réactivité et Chimie des Solides CNRS UMR 7314, 33 rue Saint-Leu, 80039 Amiens, France.

Acknowledgements

The authors thank Professor Paolo Ghigna (University of Pavia, Italy) for his help with the synthesis of some compounds. The Bayerisches Geoinstitut (University of Bayreuth, Germany) and Mr Detlef Krausse are acknowledged for making microprobe time available and for helping with the analyses.

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Volume 3| Part 5| September 2016| Pages 354-366
ISSN: 2052-2525