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

IUCrJ
Volume 13| Part 1| January 2026| Pages 116-125
ISSN: 2052-2525

Phase transitions in rutile-related V0.92O2 synthesized at high pressures and tem­per­a­tures

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aJülich Centre for Neutron Science, Research Center Jülich, Jülich, 52425, Germany, bInstitute of Crystallography, RWTH Aachen University, Aachen, 52066, Germany, cInstitute of Physics, Academy of Sciences of the Czech Republic, Praha, 162 00, Czech Republic, dQuantum Materials Department, Max Planck Institute for Solid State Research, Stuttgart, 70569, Germany, and eSwiss-Norwegian Beamlines, European Synchrotron Radiation Facility, Grenoble, 38043, France
*Correspondence e-mail: [email protected]

Edited by X. Zhang, Tsinghua University, China (Received 29 July 2025; accepted 30 November 2025)

Structural phase transitions in metastable rutile-related V0.92O2 synthesized at 10 GPa and 1273 K were studied with single-crystal X-ray diffraction in the tem­per­a­ture range 110–500 K and at pressures up to 9.2 GPa. V0.92O2 starts to decom­pose at 470 K and atmospheric pressure. When heated to tem­per­a­tures above about 350 K, the material transforms to an incommensurate phase. The oxygen sublattice is essentially rigid and it is mostly the V atoms that are affected by the modulation. An anharmonic description of the displacement parameters and their corresponding modulation is used for the V atoms to reach satisfactory agreement factors for main and first-order satellite reflections, indicating substantial disorder in the modulated structure. Measurements of electronic transport properties provide evidence that the incommensurate phase is insulating. On com­pression at room tem­per­a­ture, V0.92O2 reaches the ideal rutile structure at about 5.0 GPa. Both structural and electronic phase transitions are of the first-order character. The results of this work demonstrate that the structural and electronic behaviour of V0.92O2 at extreme conditions is distinctly different from that of stoichiometric VO2.

1. Introduction

Vanadium dioxide (VO2) undergoes a first-order metal–insulator phase transition (MIT) from the rutile (phase R, P42/mnm, Z = 2) to the monoclinic (phase M1, P21/c, Z = 4) polymorphs at about TMIT = 341 K (Qazilbash et al., 2007View full citation; Shao et al., 2018View full citation; Liu et al., 2020View full citation; Pouget, 2021View full citation; Xue & Yin, 2022View full citation; Joshi et al., 2023View full citation). The metallic R phase is built of chains of edge-sharing VO6 octa­hedra connected by common corners. The V—V distance of 2.85 Å along the chains is equal to the c lattice parameter. The structure of the insulating M1 phase is also made of two VO6 chains, but with V–V dimers in a zigzag pattern due to displacement of the V atoms from the ideal rutile positions (Longo et al., 1970View full citation). The RM1 structural instability gives rise to pre-transitional diffuse scattering (Pouget, 2021View full citation). MIT, which is an improper ferroelastic phase transition, is associated with a magnetic susceptibility drop (Pouget, 2021View full citation) and a change in thermochromic properties (Mamakhel et al., 2022View full citation).

Doping with low-valence cations (e.g. Al3+, Cr3+ and Fe3+) stabilizes two additional insulating polymorphs, which are monoclinic (phase M2, C2/m, Z = 8) and triclinic (phase T, P[\overline{1}], Z = 4). In M2, there are alternate short and long distances in the linear V—V chain, while the V atoms are equidistant in the other zigzag V—V chain (Marezio et al., 1972View full citation; Ghedira et al., 1977View full citation). The distortion in T with respect to M2 is mainly due to breaking of the linearity and pairing of the V atoms in the zigzag chain (Ghedira et al., 1977View full citation). The stabilities of phases R, M1, M2 and T are affected by stoichiometry, electric field, strain or pressure (Marezio et al., 1972View full citation, Ghedira et al., 1977View full citation; Atkin et al., 2012View full citation; Liu et al., 2018View full citation; Pouget, 2021View full citation; Wilson et al., 2022View full citation; Bouvier et al., 2023View full citation; Joshi et al., 2023View full citation). M1 and M2 can transform into one another, with T as an inter­mediate (Marezio et al., 1972View full citation). M2 could also be an inter­mediate in the M1→R transformation (Liu et al., 2020View full citation; Bleu et al., 2023View full citation). The three insulating phases may co-exist and form domains (Lu et al., 2014View full citation). The high-valence dopants (e.g. Nb5+, Mo6+ and W6+) lower the TMIT, while the low-valence dopants (e.g. Al3+, Cr3+ and Fe3+) increase it (Pouget, 2021View full citation; Xue & Yin, 2022View full citation; Joshi et al., 2023View full citation). In the first case, the charge is com­pensated by the presence of the V3+ cations. In the latter, it is com­pensated by the V5+ cations.

51V NMR studies of the metallic and insulating phases of VO2 provide contradictory results. Boyarsky et al. (2000View full citation) suggested that MIT is accom­panied by the change of the electronic state 2V4+ ↔ V3+ + V5+, with the presence of two structurally and chemically different vanadium cations V3+ and V5+ in M1. On the other hand, the data by Gro Nielsen et al. (2002View full citation) show the presence of only V4+ cations in the insulating phase. Electrical and photoemission investigations by Joshi et al. (2023View full citation) demonstrated that the V3+ and V5+ cations co-exist in the metallic state of stoichiometric VO2 due to charge fluctuations of the V4+ cations. The insulating phase is sup­pressed in VO2–x, while the metallic phase is suppressed in VO2+y. However, Joshi et al. (2023View full citation) did not present structural data for any of the VO2–x and VO2+y phases across MIT.

The pressure–tem­per­a­ture phase diagram of VO2 was determined by Chen et al. (2017View full citation). In addition to the R and M1 polymorphs, one insulating M1′ (monoclinic) phase and two metallic phases X (triclinic) and O (ortho­rhom­bic) were identified. When M1 is com­pressed at room tem­per­a­ture, it transforms to M1′ at 13.9 GPa (Bouvier et al., 2023View full citation). X co-exists with M1′ in the pressure range 32–42 GPa. Upon decom­pression, X transforms to another (unidentified) phase between 20 and 3 GPa. The sequence of phase transitions in VO2 under strong com­pression was examined by Xie et al. (2018View full citation).

Apart from VO2, the experimentally determined equilibrium phases in the central part of the V–O phase diagram (VOx, 1.5 ≤ x ≤ 2.5) at atmospheric pressure are V2O3, VnO2n–1 (n = 3 ÷ 8), V3O7, V6O13 and V2O5 (Wriedt, 1989View full citation). The calculated phase diagram for 1.5 ≤ x ≤ 2.5 includes only V2O3, V3O5, VO2, V3O7 and V2O5 (Hu et al., 2023View full citation). The oxides VnO2n–1 (n = 3 ÷ 9) form a Magnéli homologous series (Schwingenschlögl & Eyert, 2004View full citation; Allred & Cava, 2013View full citation) according to the formula VnO2n–1 = V2O3 + (n − 2)VO2. With respect to the com­position of vanadium dioxide, they are anion deficient and can also be expressed as VO2–y. The end members of this series are corundum V2O3 (R[\overline{3}]c, Z = 6) and rutile VO2 (phase R), both with a hexa­gonal close-packed array of O atoms (Katzke et al., 2003View full citation). One oxygen layer is removed at every nth vanadium layer in the direction perpendicular to the (211) plane of the parent rutile structure. Magnéli phases are also known for the titanium, niobium and tungsten oxides (Wu et al., 2023View full citation).

The homologous series of vanadium oxides VnO2n+1 in the V2O5–VO2 system was predicted by Wadsley (1957View full citation). Its formula can be written as VnO2n+1 = V2O5 + (n − 2)VO2 for 2 ≤ n. With respect to the chemical com­position of VO2, the Wadsley oxides are cation deficient, i.e. V1–xO2. The end members of this series are α-V2O5 and VO2(B) (Katzke et al., 2003View full citation). These materials have structures derived from VOx (Fm[\overline{3}]m, Z = 4), where x ≃ 1, by introducing different ordered vacancies in the oxygen cubic close-packing array. Shear deformations break symmetry and cause the collapse of the face-centred cubic layers along the cubic c axis. The cations partially fill out the available voids in the oxygen sublattice in a commensurate way.

Metal-deficient V1–xO2 material, synthesized at 6.5 GPa and 1273 K by substituting V5+ into VO2 (Chamberland, 1973View full citation), has a distorted rutile structure (P2/m, Z = 2), with the V—V distances in both chains equal to the b lattice parameter (Galy & Miehe, 1999View full citation). Up to 10 wt% of V2O5 was accommodated in V1–xO2 at these conditions. Based on the resistivity data, the tem­per­a­tures for MIT depend on the actual com­position (Chamberland, 1973View full citation). They increase from 353 to 361 K for 2 wt% (V0.995O2) and 10 wt% of V2O5 (V0.976O2), respectively. No structural details of the metallic phase were provided.

Recently, we have grown single crystals of rutile-related V0.92O2 at 10 GPa and 1273 K from a polycrystalline starting material of the Wadsley phase V6O13 (Grzechnik et al., 2024View full citation) corresponding in terms of its com­position to V1–xO2 (Chamberland, 1973View full citation) or VO2+y (Joshi et al., 2023View full citation) with 35 wt% of V2O5. In situ synchrotron measurements revealed that this new phase forms above 500 K in the pressure range 4–17.5 GPa and can be recovered to ambient conditions. The characteristic feature of its crystal structure (C2/m, Z = 4) is the presence of disorder affecting the V atoms, which occupy the two split-atom positions V1 and V2. The V1 atoms in one of the octa­hedral chains are displaced along the b axis, while the V2 atoms in the other are fourfold split in the bc plane. This results in two zigzag V—V chains, one with equidistant V1 atoms and the other with short and long V2—V2 distances. Disregarding the split V-atom positions, the average structure (P2/m, Z = 2) of this new phase (Fig. 1[link]) is like that for the V1–xO2 material (Chamberland, 1973View full citation; Galy & Miehe, 1999View full citation). Pseudosymmetry considerations (Grzechnik et al., 2024View full citation) indicate that it is the ordered variant of M2. The transformation of the Wadsley phase V6O13 into rutile-related V0.92O2 involves the transition from cubic to hexa­gonal close-packing of the O atoms.

[Figure 1]
Figure 1
The average crystal structure in the space group P2/m (Z = 2), as well as the tem­per­a­ture dependence of its lattice parameters and unit-cell volumes. The octa­hedra around the V1 and V2 atoms are drawn in yellow and cyan, respectively. The O1 and O2 atoms are labelled. The symbols in the plots of the lattice parameters and unit-cell volumes are larger than the estimated standard deviations.

The physical properties of different structural forms of V1–xO2 are closely correlated with the formation and spatial arrangement of the short V—V distances (Liu et al., 2018View full citation; Joshi et al., 2023View full citation). Detailed experimental characterization of new types of structural ordering, such as the (in)commensurate long- or short-range order, are a necessary step towards the better understanding of structure–property relationships and the further control of the physical properties of vanadium oxides. While browsing the literature on (non)stoichiometric vanadium dioxides, one can readily see that most of the articles are somewhat incom­plete in the sense that either the structural or electronic properties and transformations of VOx are investigated. In this article, we combine both approaches (i) to determine whether metastable V0.92O2 undergoes any tem­per­a­ture- or pressure-induced phase transitions using single-crystal X-ray diffraction, and (ii) to examine its electronic transport properties at atmospheric pressure for further elucidation of the structure–property relationships in vanadium dioxides.

2. Experimental methods

Single-crystal growth of V0.92O2 from the Wadsley phase V6O13 was described previously (Grzechnik et al., 2024View full citation).

Synchrotron single-crystal diffraction measurements (λ = 0.72044 Å) were performed on the BM01 station of the Swiss–Norwegian Beamlines (SNBL) at the European Synchrotron Radiation Facility (Grenoble, France) (Dyadkin et al., 2016View full citation). The data (a full rotation of 360°) were collected using a Pilatus 2M detector. After several tests on various crystals at room tem­per­a­ture to check for their quality and for any radiation damage (Grzechnik et al., 2023View full citation), our data collection strategy was to measure frames with a fine angular slicing of 0.1° and the exposure time of 0.1 s/frame. The chosen crystal was mounted on a glass pin and placed in the stream of nitro­gen from an Oxford Cryostream 700+. It was cooled to 100 K and the data were collected on heating to 500 K with a step of 10 K.

High-pressure single-crystal X-ray data at room tem­per­a­ture were measured on a STOE IPDS-II (Stoe & Cie GmbH, Darmstadt, Germany; λ = 0.71073 Å) equipped with an image plate, as well as on a 4-circle Huber diffractometer with an Ag microfocus Incoatec source (λ = 0.5608 Å) and a Pilatus 300k detector. A crystal of V0.92O2 was loaded into the Ahsbahs diamond anvil cell (Ahsbahs, 2012View full citation), together with a 4:1 (v/v) methanol–ethanol pressure medium and a ruby ball as a pressure marker (Mao et al., 1986View full citation).

All the laboratory and synchrotron data collected with the Pilatus detectors were analysed with the program CrysAlis PRO (Rigaku Oxford Diffraction, 2024View full citation). The data from the IPDS-II diffractometer were processed with the program X-AREA (Stoe & Cie, 1998View full citation). Solution and refinement of the structures were carried out with the programs JANA2006 (Petříček et al., 2014View full citation) and JANA2020 (Petříček et al., 2023View full citation).

Electronic transport measurements were carried out between 250 and 400 K inside a Quantum Design PPMS system, employing the electrical transport option (ETO). We used a standard four-wire measurement technique with a low AC excitation current of 100 µA to avoid parasitic sample heating and a frequency around 57 Hz. Good electronic contacts were made by attaching 10 µm Au wires to a single crystal of approximate dimensions 0.15 mm × 0.10 mm × 0.08 mm using an Ag paint. We confirmed a negligible phase angle of less than 1° over the tem­per­a­ture range.

3. Results and discussion

3.1. Single-crystal X-ray diffraction in the tem­per­a­ture range 110–500 K and under ambient pressure

On heating from 110 K to about 460 K, all the main reflections in the synchrotron data are indexed and integrated with the primitive monoclinic lattice corresponding to the average structure (P2/m, Z = 2) determined previously (Galy & Miehe, 1999View full citation; Grzechnik et al., 2024View full citation). Metastable V0.92O2 starts to collapse at above 460 K as the reflections become smeared out. Also, new additional reflections appear. Above 470 K, the observed reflections cannot be indexed as originating from a single phase, indicating decom­position of the V0.92O2 material.

From the abrupt changes of the lattice parameters and unit-cell volumes (Fig. 1[link]), it is seen that the material undergoes a first-order iso-symmetrical P2/mP2/m phase transition at about 350 K. The b lattice parameter of the high-tem­per­a­ture phase is smaller than that for the low-tem­per­a­ture phase. The drop in this lattice parameter at the phase transition is correlated with an abrupt shortening of the V—V distances in the octa­hedral chains. The a and c lattice parameters exhibit the same evolution in the entire tem­per­a­ture range studied here. The β angle, which is a measure of a monoclinic distortion of the tetra­gonal rutile structure, increases with elevated tem­per­a­ture and has a drastic change of slope at about 350 K. It is remarkable that the tem­per­a­ture of the phase transition observed in V0.92O2 is very similar to that observed in V1–xO2, depending on the com­positional variable x (Chamberland, 1973View full citation; Qazilbash et al., 2007View full citation; Liu et al., 2020View full citation; Pouget, 2021View full citation; Joshi et al., 2023View full citation).

The V—O distances in the average structure of V0.92O2 (P2/m, Z = 2) as a function of tem­per­a­ture are shown in Fig. 2[link]. There is no obvious anomaly that could be associated with the phase transition at about 350 K. However, the O—O distances in both chains of octa­hedra exhibit clear changes in their tem­per­a­ture dependencies at the phase transition (Fig. 3[link]). The equatorial planes of the octa­hedra are defined by the atoms involved in edge sharing in the chains. The apical atoms in V1O6 and V2O6 are O1 and O2, respectively. The shortest and longest O—O distances are in the equatorial planes of both polyhedra, i.e. the O2—O2 distances in the V1O6 octa­hedra and the O1—O1 distances in the V2O6 octa­hedra. The shortest distances correspond to the shared edges of the octa­hedra. The most affected O—O distances at the phase transition are those in the respective equatorial planes. The average O—O distances abruptly change at the phase transition – they increase in V1O6, while they decrease in V2O6 (Fig. 4[link]). The octa­hedron around the V1 atom at the site with the higher occupancy is less distorted than that around the V2 atom and becomes more regular above the phase transition.

[Figure 2]
Figure 2
Temperature dependence of the V—O distances in the V1O6 (full symbols) and V2O6 (open symbols) octa­hedra in the average structure (P2/m, Z = 2).
[Figure 3]
Figure 3
Temperature dependence of the O—O distances in the average structure (P2/m, Z = 2). The error bars are shown when larger than the symbols.
[Figure 4]
Figure 4
Average O—O distances and Δ〈O—O〉 deviation parameter in the V1O6 (full symbols) and V2O6 (open symbols) octa­hedra of the average structure (P2/m, Z = 2). The deviation parameter is defined as Δ〈O—O〉 = [ \left( \sum _{i=1}^{12} \left\vert {\rm OO}_i - {\rm OO}_m \right\vert \right) / 12 {\rm OO}_m].

Diffuse scattering is not observed in the laboratory data measured either on the IPDS-II diffractometer (image plate, Mo Kα radiation) or on the 4-circle diffractometer (Pilatus 300k detector, Ag microfocus source). However, the analysis of the reconstructions of the reciprocal space based on the synchrotron measurements reveals the presence of diffuse scattering at all tem­per­a­tures (Figs. 5[link] and 6[link]). The intensity of the diffuse scattering increases close to the transition tem­per­a­ture. Above the phase transition, the diffuse features start to condense to well-defined satellite reflections. The strongest diffuse scattering is between the nearest satellites, which could be indexed with one incommensurate wave vector q = ([1 \over 2], β, [1 \over 2]), where β ≃ 0.234. This vector, which is essentially constant as a function of tem­per­a­ture, can only be precisely determined above 400 K (Fig. 7[link]).1 All these observations indicate that metastable V0.92O2 does not transform to the ideal rutile structure (R) at high tem­per­a­tures and ambient pressure.

[Figure 5]
Figure 5
Reconstructions of the reciprocal space in the (0kl) and ([1 \over 2]kl) planes (the upper and lower row, respectively) from the synchrotron data at selected tem­per­a­tures.
[Figure 6]
Figure 6
Reconstructions of the reciprocal space in the (hk0) and (hk[1 \over 2]) planes (the upper and lower row, respectively) from the synchrotron data at selected tem­per­a­tures.
[Figure 7]
Figure 7
Temperature dependence of the qβ com­ponent of the incommensurate vector.

All the main and satellite reflections in the diffraction pattern at 460 K can be indexed and integrated with monoclinic lattice parameters a = 4.5995 (4), b = 2.8746 (2), c = 4.6014 (4) Å and β = 92.49 (1)° in combination with the vector q = [[1 \over 2], 0.2328 (9), [1 \over 2]]. Only first-order satellites were detected. Satellites of the second order do not show any significant intensity in the integration and are also not visible in the reconstructions of reciprocal space. For all the refinements, the overall stoichiometry and occupancies for V1 and V2 were fixed to the values reported by Grzechnik et al. (2024View full citation), as a free refinement of the occupation parameters showed only minor deviations from this stoichiometry.

The refinement of the average structure at 460 K was carried out in the space groups P2/m, P2, Pm, P[\overline{1}] and P1. For the triclinic space groups, additional twinning via a twofold axis in the direction [010] was included. For none of the last four space groups were the overall agreement factors significantly better than for P2/m, considering the higher number of parameters in the refinements.

For the refinements of the incommensurate structure, the structure was transformed according to a′ = a + c, b′ = b and c′ = −a + c, with a resulting q vector of [0, 0.2328 (9), 0] to a pseudo-ortho­rhom­bic X-centred cell with X = ([1 \over 2], 0, [1 \over 2], [1 \over 2]) and an angle of 90.02° (Table 1[link]). Several trial refinements were performed in monoclinic and triclinic superspace groups. Considering the agreement factors and the number of parameters in the refinement, the best result was obtained in superspace group X2/m(0β0)s0. Additional twinning with a twofold axis in the direction [001] was included. The introduction of the twinning led to a significant decrease in the agreement factors for the satellite reflections. In this model, initially only the first harmonics of the Fourier coefficients of a displacive modulation of the V and O atoms were considered. This led to an unsatisfactory R(obs) agreement factor of approximately 25% for the satellite reflections and high difference density in the difference Fourier map around the V atoms. When the second harmonic of the displacive modulation function for the V atoms was added, a substantial decrease in the overall agreement factors for the satellite and main reflections was achieved, while introducing higher harmonics for oxygen or an occupational modulation wave for vanadium did not result in better agreement factors (while leading to an increased data-to-parameter ratio). However, a trial calculation of the intensities of the second-order satellites showed that, assuming this model, their intensities would be substantial so that they should be clearly observed. As this is not the case, it is obvious that this model cannot be the correct one. Also, an inspection of the de Wolff sections and the refined modulation functions around the V-atom positions clearly showed a very bad agreement. We therefore discarded the model with higher harmonics of the displacive modulation.

Table 1
Experimental and refinement details at 460 K (λ = 0.72044 Å)

Space group X2/m(0β0)s0
Centring X = [1 \over 2], 0, [1 \over 2], [1 \over 2]
Z 4
a (Å) 6.6458 (6)
b (Å) 2.8746 (2)
c (Å) 6.3631 (6)
β (°) 90.024 (10)
V3) 121.562 (18)
q vector 0, 0.2328 (9), 0
ρ (g cm−3) 4.3091
μ (mm−1) 6.934
   
No. measured reflns 1297
Range of hkl −8 ≤ h ≤ 8
  −4 ≤ k ≤ 4
  −8 ≤ l ≤ 84
  −1 ≤ m ≤ 1
θ (min/max) 3.53/32.52
No. symmetry independent reflns (all) 445
No. symmetry independent reflns (obs)a 302
Rint(obs/all) 0.75/0.76
   
All reflns R(obs)/wR(all)b 5.60/7.28
Main reflns R(obs)/wR(all) 5.08/6.44
Satellite reflns R(obs)/wR(all) 9.44/11.74
GoF (obs/all) 5.71/4.44
Twin law (−100, 0−10, 001)
Twin volumes I/II 0.86 (4)/0.14 (4)
Δρmax, Δρmin (e Å−3) 0.72, −0.79
No. parameters 92
Symmetry operations: (1) x1, x2, x3, x4; (2) −x1, x2, −x3, x4 + [1 \over 2]; (3) −x1, −x2, −x3, −x4; (4) x1, −x2, x3, −x4 + [1 \over 2]. Notes: (a) criterion for the observed reflections is |F(obs)| > 3σ; (b) all agreement factors are given in percent (%) and the weighing scheme is 1/{σ2F(obs) + [0.01F(obs)]2}.

Instead, we started from the assumption of a modulation of the displacement parameters. The electron density around the V atoms in the average structure (Fig. S1 in the supporting information) was best described using an anharmonic tensor. As the com­ponents of the third-order tensor for V are fixed to zero by the symmetry, we introduced a fourth-order anharmonic tensor in the average structure. This led to a substantial decrease in the agreement factors for the main reflections. Introducing a modulation of the anharmonic displacement parameters also led to a significant decrease of the agreement factor for the satellite reflections of first order, while the intensities of the second-order satellites were very small, in accordance with our observations.2

According to an earlier chemical analysis, the overall com­position of the com­pound is V0.92O2 (Grzechnik et al., 2024View full citation), suggesting vacancies in the V sublattice. However, neither of the de Wolff sections showed any indication of a significant modulation of the height of maxima in the electron density, nor did the introduction and subsequent refinement of occupational modulation lead to better agreement factors. From these observations, we deduced that the V vacancies are randomly distributed within the V sublattice.

In the disordered room-tem­per­a­ture structure, the oxygen sublattice does not substanti­ally deviate from the ideal positions. This observation correlates very well with the fact that the O-atom positions and their displacement parameters are hardly affected by the modulation functions in the incommensurate structure (Table 2[link]). Consequently, the O—O distances do not essentially vary as a function of the inter­nal parameter t if the standard deviations are considered (Table S1 in the supporting information). All these observations imply that the oxygen sublattice is nearly rigid (see animation S1 in the supporting information).

Table 2
Positional and isotropic displacement parameters of the atoms, as well as Fourier coefficients of the modulation amplitudes at 460 K

  Occupancy x y z Uiso  
V1 0.492 (4) 0.0 0.0 0.0 0.0318 (11)  
V2 0.428 (4) 0.0 0.5 0.5 0.0283 (13)  
O1 0.5 −0.2003 (2) 0.0 0.5002 (4) 0.0155 (7)  
O2 0.5 0.0005 (3) 0.5 0.2000 (2) 0.0128 (6)  
             
  xsin1 ysin1 zsin1 xcos1 ycos1 zcos1
V1 0.0065 (4) 0.0 0.0003 (6) 0.0 0.0 0.0
V2 −0.0059 (4) 0.0 0.0001 (6) 0.0 0.0 0.0
O1 −0.0004 (3) 0.0 −0.0004 (6) 0.0 −0.0039 (8) 0.0
O2 0.0008 (3) 0.0 0.0001 (5) 0.0 0.0003 (10) 0.0
             
  u11 u22 u33 u12 u13 u23
V1 0.0693 (14) 0.0155 (18) 0.010 (2) 0.0 0.0068 (16) 0.0
V2 0.051 (2) 0.027 (2) 0.007 (3) 0.0 0.0025 (18) 0.0
O1 0.0147 (11) 0.0171 (9) 0.0147 (14) 0.0 0.0009 (12) 0.0
O2 0.0186 (13) 0.0112 (8) 0.0085 (12) 0.0 0.0059 (16) 0.0
             
V1/V2 uijsin1 = 0.0
             
  u11sin1 u22sin1 u33sin1 u12sin1 u13sin1 u23sin1
O1 −0.0009 (11) −0.0002 (10) −0.0004 (13) 0.0 0.0012 (15) 0.0
O2 0.0006 (17) −0.0001 (13) 0.0020 (17) 0.0 −0.0004 (9) 0.0
  u11cos1 u22cos1 u33cos1 u12cos1 u13cos1 u23cos1
             
V1 For i = j uijcos1 = 0.0 0.0007 (9) 0.0 0.0012 (14)
V2       −0.0001 (11) 0.0 −0.0004 (16)
O1       0.0012 (7) 0.0 −0.0024 (15)
O2       −0.0008 (7) 0.0. −0.0005 (12)
             
  D1111 D1113 D1122 D1133 D1223 D1333
V1 −0.0975 (13) 0.0019 (12) −0.006 (3) −0.0009 (8) −0.005 (3) −0.0007 (19)
V2 −0.019 (2) −0.0022 (18) −0.017 (3) 0.0017 (12) −0.007 (3) −0.003 (2)
             
  D2222 D2233 D3333 D1112 = D1123 = D1222 = D1233 = D2223 = D2333 = 0.0
V1 0.07 (4) −0.009 (3) 0.000 (3)      
V2 −0.10 (4) −0.012 (3) −0.002 (3)      
             
  C111sin1 C113sin1 C122sin1 C133sin1 C223sin1 C333sin1
V1 −0.048 (2) 0.006 (2) −0.015 (4) −0.0037 (13) −0.000 (5) 0.002 (3)
V2 0.022 (3) −0.004 (2) 0.016 (5) 0.0020 (12) 0.000 (6) 0.000 (4)
             
V1/V2 C112sin1 = C123sin1 = C222sin1 = C233sin1 = 0.0
V1/V2 Cijkcos1 = 0.0
             
  D1112cos1 D1123cos1 D1222cos1 D1233cos1 D2223cos1 D2333cos1
V1 −0.000 (3) 0.002 (2) 0.008 (9) −0.0002 (12) 0.007 (11) −0.000 (4)
V2 0.006 (3) −0.002 (3) −0.004 (10) 0.0004 (15) 0.005 (13) −0.002 (4)
             
V1/V2 D1111cos1 = D1113cos1 = D1122cos1 = D1133cos1 = D1223cos1 = D1333cos1 = D2222cos1 = D2233cos1 = D3333cos1 = 0.0
V1/V2 Dijklsin1 = 0.0

Amplitudes of the displacive modulation of the V atoms are also hardly significant and V—V distances are almost constant in the modulated structure (Table S2). We attribute the absence of significant displacements to the fact that the atoms are disordered over several split atom positions. In our structural model, the anharmonic displacement parameters and their corresponding modulations describe such a disorder of the atoms. While it is thus difficult to qu­antify the absolute displacements of the V atoms from their average positions, an inspection of the anharmonic displacement parameters reveals that the largest displacements are in the direction of a (animation S1). This is also clearly visible in animations S2 and S3, which show the joint probability density function (j.p.d.f.) around the V-atom positions in the modulated structure. Animations S4 and S5 show the j.p.d.f. around the O atoms. A complete animation of the incommensurate phase, including the j.p.d.f. for all the atoms in the unit cell, is in animation S6.

In the disordered room-tem­per­a­ture structure, the V1 atoms are arranged in a zigzag pattern, with a V1—V1 dis­tance of 2.9020 (2) Å. In the modulated structure, the average V1—V1 and V2—V2 distances are slightly smaller at 2.87489 (3) and 2.87484 (3) Å, respectively. Thus, surprisingly, the V—V distances are smaller at higher tem­per­a­tures. How­ever, the true positions of vanadium in the modulated structure are difficult to determine due to the additional disorder modelled by the anharmonic displacement parameters and their modulation.

Considering the V1O6 octa­hedra, in the modulated structures there are four shorter V—O bonds, plus two longer ones (Table S3). On the other hand, within the V2O6 octa­hedra, the situation is reversed and there are four longer and two shorter V—O bonds (Table S3).

In the disordered structure at room tem­per­a­ture, the bond valence sums (BVSs) of V1 and V2 are basically equal and amount to about 4.0 v.u. (with the BVS parameters for V4+) or about 4.4 v.u. (with the BVS parameters for V5+). In the modulated structure, the bond valence sums are smaller, with values of around 3.80 for both V atoms assuming a bond valence parameter of V4+ and 4.15 for a bond-valence parameter of V5+. Again, one must consider that these parameters are based on the average V-atom coordinates and do not really reflect the deviations from these average positions described by the anharmonic parameters.

3.2. Measurements of electronic transport properties at atmospheric pressure

Fig. 8[link] shows qualitatively the evolution of resistance measured on a single crystal of V0.92O2 on heating and cooling in the range 275–400 K. The onset of a first-order phase transition is at about 330 K. A hysteresis of about 10 K is observed on cooling the crystal from 400 K to room tem­per­a­ture. The data clearly show that both phases are non-metallic. V0.92O2 becomes even more insulating above the phase transition. Such a behaviour is different from that of (nearly) stoichiometric VO2, in which the high-tem­per­a­ture phases are metallic (Chamberland, 1973View full citation; Joshi et al., 2023View full citation).

[Figure 8]
Figure 8
Resistance versus tem­per­a­ture on heating (black line) and cooling (red line) in the range 275–400 K.

3.3. Single-crystal X-ray diffraction to 9.2 GPa at room tem­per­a­ture

The high-pressure single-crystal data measured on both laboratory diffractometers up to 9.2 GPa at room tem­per­a­ture were analyzed in the average structure in P2/m (Z = 2). The β angle decreases on com­pression, and it becomes equal to 90° at 4.9 GPa (Fig. 9[link]). All the reflections at this and higher pressures can be indexed with the tetra­gonal lattice: a ≃ 4.5 Å and c ≃ 2.8 Å. There is also a discontinuity in the lattice parameters bmct, which are determined by the V—V distances in the octa­hedral chains. This implies a first-order phase transition from the monoclinic to tetra­gonal phases at about 3.7–4.9 GPa. The data measured at 6.35 GPa and room tem­per­a­ture on the 4-circle diffractometer could be integrated and refined with the ideal rutile structure (Tables S4–S6). The P2/mP42/mnm phase transition is reversible on decom­pression. All these observations agree with our previous observations about the fact that, on quenching to ambient conditions, rutile V0.92O2 transforms to a range of its distorted variants depending on the actual highest pressure and tem­per­a­ture reached during the synthesis (Grzechnik et al., 2024View full citation). The behaviour of metal-deficient V0.92O2 at high pressures and room tem­per­a­ture is therefore different from that of the M1 phase of stoichiometric VO2, which transforms to a series of low-symmetry polymorphs but not to ideal rutile (Chen et al., 2017View full citation; Bouvier et al., 2023View full citation).

[Figure 9]
Figure 9
Lattice parameters, β angles and unit-cell volumes for the monoclinic (m, full symbols) and tetra­gonal (t, open symbols) phases on com­pression at room tem­per­a­ture. The estimated standard deviations are smaller than the size of the symbols. The solid lines are the fits of the third-order Murnaghan equations of state.

The monoclinic phase is much more com­pressible than the tetra­gonal one. The PV data up to 3.66 GPa can be fitted with the third-order Murnaghan equation of state (EoS): V0 = 60.24 (2) Å3, B0 = 66 (3) GPa and B0′ = 29 (3). Since the zero-pressure volume V0 for the tetra­gonal polymorph cannot be determined from the EoS fit, a modified third-order Murnaghan EoS in terms of (PPtr), where Ptr = 4.91 GPa in the transition pressure, was used. Consequently, Vtr = 57.80 (2) Å3, Btr = 143 (13) GPa and Btr′ = 16 (8) are obtained at Ptr = 4.91 GPa. The B0/Btr and B0′/Btr′ parameters can be com­pared with those for the different polymorphs of stoichiometric VO2. The bulk modulus B0 for the phase M1 determined theoretically (Dong & Liu, 2013View full citation) is 237 GPa, while the reported experimental values are 213 (2) (Bai et al., 2015View full citation) and 194 (7) GPa (Bouvier et al., 2023View full citation). The theoretical B0 for M2 is 241 GPa (Dong & Liu, 2013View full citation). According to the calculations by Dong & Liu (2013View full citation), B0 for rutile VO2 is 243 GPa. The experimental B0 for rutile at 383 K is 190 (2) GPa (Bai et al., 2015View full citation). The most com­pressible polymorph of stoichiometric vanadium dioxide is VO2(B), with B0 = 129 (4) GPa (Wang et al., 2016View full citation), which is com­parable to V0.92O2. The first derivatives of the bulk moduli for V0.92O2 are higher than all those for VO2, which are in the range 4–7 (Dong & Liu, 2013View full citation; Bai et al., 2015View full citation; Wang et al., 2016View full citation; Bouvier et al., 2023View full citation).

4. Conclusions

Structural modulations are usually stabilized at low tem­per­a­tures as a disordered structure transforms into a more ordered one on cooling. Notable exceptions are brownmillerites Ca2Fe2O5 (Krüger et al., 2005View full citation) and Ca2Al2O5 (Lazic et al., 2008View full citation), as well as inter­metallic PdBi (Folkers et al., 2020View full citation). In the brownmillerites at about 1000 K, the modulation arises from the incommensurate sequence of enanti­omorphic left- and right-handed tetra­hedral BO4 chains (B = Fe or Al). In PdBi with the structure related to TlI, the incommensurability on heating to above 473 K originates from the presence of nearly regular TlI-type slabs in a distorted TlI superstructure with Pd–Pd dimers. Folkers et al. (2020View full citation) inter­preted the TlI-type slabs as the regions of higher vibrational freedom that are entropically favoured at high tem­per­a­tures. Metastable V0.92O2, which is investigated in this study, undergoes a phase transition to an incommensurate phase above about 350 K. Our inter­pretation is that such behaviour is a consequence of an incommensurate way of disordering of V4+ and V5+ cations, which are chemically and structurally distinct with different ionic radii, in a rigid hexa­gonal close-packing oxygen sublattice. Eventually, V0.92O2 starts to decom­pose above 460 K at atmospheric pressure. In other words, decom­position is preceded by incommensurability. Such a phenomenon could possibly be found in other materials, not necessarily metastable and synthesized at high pressures.

V0.92O2, which contains 35 wt% of V2O5, is insulating. It demonstrates the capacity of the rutile-type framework to accommodate a wide series of VO2–V2O5 com­positions. It also suggests that by varying stoichiometries and pressure–tem­per­a­ture conditions one would synthesize rutile-related V1–xO2 materials with transport properties ranging from metallic to insulating. Since the com­pound with 10 wt% of V2O5 (V0.976O2) is indeed metallic (Chamberland, 1973View full citation), it remains to be seen for which higher V2O5 contents V1–xO2 oxides become insulating. In addition, 35 wt% of V2O5 does not need to be a com­positional limit for the stability of the rutile-related structure that has one important feature common to all the known (non-)stochiometric VO2 phases: the hexa­gonal close-packing oxygen sublattice is rigid, while the cation sublattice is flexible, allowing for various schemes of cation (dis)order. Therefore, incommensurate phases could also be expected for other V1–xO2 com­positions, apart from V0.92O2.

Metal-deficient V0.92O2 reversibly transforms to the ideal rutile structure (P42/mnm, Z = 2) at about 5 GPa and room tem­per­a­ture. Altogether, the results of this work demonstrate that its structural behaviour under extreme conditions is distinctly different from that of stoichiometric VO2.

Our findings imply then that the structural and electronic (in)stabilities of the non-stoichiometric vanadium dioxides warrant detailed investigations since the occurrence of the metallic R phases (P42/mnm, Z = 2) in the mixed-valence VOx materials for different x ≠ 0 is not certain. As our work was focused on Bragg diffraction, further insight into the mechanism of the unusual phase transition observed in V0.92O2 on increasing the tem­per­a­ture could be obtained by a future detailed investigation of the diffuse scattering, which seems to occur as a precursor effect to the formation of the modulated structure.

Supporting information


Computing details top

Vanadium dioxide (V0.92O2tetragonal) top
Crystal data top
O2V0.92Dx = 4.576 Mg m3
Mr = 78.9Ag Kα radiation, λ = 0.5608 Å
Tetragonal, P42/mnmCell parameters from 127 reflections
Hall symbol: -P 4n;-2nθ = 3.5–24.5°
a = 4.5050 (19) ŵ = 3.73 mm1
c = 2.8200 (13) ÅT = 293 K
V = 57.23 (4) Å3Irregular, black
Z = 20.05 × 0.03 × 0.03 × 0.03 (radius) mm
F(000) = 74
Data collection top
Esperanto-CrysAlisPro-abstract goniometer imported esperanto images
diffractometer
45 independent reflections
Radiation source: X-ray tube30 reflections with I > 3σ(I)
Synchrotron monochromatorRint = 0.109
Detector resolution: 5.8140 pixels mm-1θmax = 25.0°, θmin = 5.0°
φ scansh = 55
Absorption correction: multi-scan
(CrysAlis PRO; Rigaku OD, 2024)
k = 66
Tmin = 0.937, Tmax = 1l = 33
328 measured reflections
Refinement top
Refinement on F0 restraints
R[F2 > 2σ(F2)] = 0.0600 constraints
wR(F2) = 0.057Weighting scheme based on measured s.u.'s w = 1/(σ2(F) + 0.0001F2)
S = 2.14(Δ/σ)max = 0.0002
45 reflectionsExtinction correction: B-C type 1 Gaussian isotropic (Becker & Coppens, 1974)
5 parametersExtinction coefficient: 400 (200)
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top
xyzUiso*/UeqOcc. (<1)
V10.50.500.0280 (18)*0.92
O10.2026 (11)0.2026 (11)00.009 (2)*
Atomic displacement parameters (Å2) top
U11U22U33U12U13U23
???????
Geometric parameters (Å, º) top
V1—V1i2.820 (3)O1—O1viii2.582 (7)
V1—V1ii2.820 (3)O1—O1ix2.691 (6)
V1—O11.895 (5)O1—O1x2.691 (6)
V1—O1iii1.895 (5)O1—O1iv2.691 (6)
V1—O1iv1.912 (4)O1—O1v2.691 (6)
V1—O1v1.912 (4)O1—O1xi2.691 (6)
V1—O1vi1.912 (4)O1—O1xii2.691 (6)
V1—O1vii1.912 (4)O1—O1vi2.691 (6)
O1—O1i2.820 (3)O1—O1vii2.691 (6)
O1—O1ii2.820 (3)
V1i—V1—V1ii180V1x—O1—O1xi93.6 (2)
V1i—V1—O190V1x—O1—O1xii44.74 (13)
V1i—V1—O1iii90V1x—O1—O1vi149.5 (2)
V1i—V1—O1iv42.48 (11)V1x—O1—O1vii95.10 (11)
V1i—V1—O1v137.52 (11)O1i—O1—O1ii180
V1i—V1—O1vi42.48 (11)O1i—O1—O1viii90.00 (14)
V1i—V1—O1vii137.52 (11)O1i—O1—O1ix58.41 (13)
V1ii—V1—O190O1i—O1—O1x121.6 (2)
V1ii—V1—O1iii90O1i—O1—O1iv58.41 (13)
V1ii—V1—O1iv137.52 (11)O1i—O1—O1v121.6 (2)
V1ii—V1—O1v42.48 (11)O1i—O1—O1xi58.41 (13)
V1ii—V1—O1vi137.52 (11)O1i—O1—O1xii121.6 (2)
V1ii—V1—O1vii42.48 (11)O1i—O1—O1vi58.41 (13)
O1—V1—O1iii180O1i—O1—O1vii121.6 (2)
O1—V1—O1iv90.00 (18)O1ii—O1—O1viii90.00 (14)
O1—V1—O1v90.00 (18)O1ii—O1—O1ix121.6 (2)
O1—V1—O1vi90.00 (18)O1ii—O1—O1x58.41 (13)
O1—V1—O1vii90.00 (18)O1ii—O1—O1iv121.6 (2)
O1iii—V1—O1iv90.00 (18)O1ii—O1—O1v58.41 (13)
O1iii—V1—O1v90.00 (18)O1ii—O1—O1xi121.6 (2)
O1iii—V1—O1vi90.00 (18)O1ii—O1—O1xii58.41 (13)
O1iii—V1—O1vii90.00 (18)O1ii—O1—O1vi121.6 (2)
O1iv—V1—O1v95.05 (16)O1ii—O1—O1vii58.41 (13)
O1iv—V1—O1vi84.95 (16)O1viii—O1—O1ix61.34 (17)
O1iv—V1—O1vii180O1viii—O1—O1x61.34 (17)
O1v—V1—O1vi180O1viii—O1—O1iv134.74 (19)
O1v—V1—O1vii84.95 (16)O1viii—O1—O1v134.74 (19)
O1vi—V1—O1vii95.05 (16)O1viii—O1—O1xi61.34 (17)
V1—O1—V1ix132.48 (11)O1viii—O1—O1xii61.34 (17)
V1—O1—V1x132.48 (11)O1viii—O1—O1vi134.74 (19)
V1—O1—O1i90.00 (14)O1viii—O1—O1vii134.74 (19)
V1—O1—O1ii90.00 (14)O1ix—O1—O1x63.19 (14)
V1—O1—O1viii180O1ix—O1—O1iv113.63 (11)
V1—O1—O1ix118.7 (2)O1ix—O1—O1v161.8 (3)
V1—O1—O1x118.7 (2)O1ix—O1—O1xi89.48 (17)
V1—O1—O1iv45.26 (13)O1ix—O1—O1xii122.7 (2)
V1—O1—O1v45.26 (13)O1ix—O1—O1vi74.07 (17)
V1—O1—O1xi118.7 (2)O1ix—O1—O1vii105.9 (2)
V1—O1—O1xii118.7 (2)O1x—O1—O1iv161.8 (3)
V1—O1—O1vi45.26 (13)O1x—O1—O1v113.63 (11)
V1—O1—O1vii45.26 (13)O1x—O1—O1xi122.7 (2)
V1ix—O1—V1x95.0 (2)O1x—O1—O1xii89.48 (17)
V1ix—O1—O1i42.48 (10)O1x—O1—O1vi105.9 (2)
V1ix—O1—O1ii137.5 (2)O1x—O1—O1vii74.07 (17)
V1ix—O1—O1viii47.52 (11)O1iv—O1—O1v63.19 (14)
V1ix—O1—O1ix44.74 (13)O1iv—O1—O1xi74.07 (17)
V1ix—O1—O1x93.6 (2)O1iv—O1—O1xii105.9 (2)
V1ix—O1—O1iv95.10 (11)O1iv—O1—O1vi57.33 (17)
V1ix—O1—O1v149.5 (2)O1iv—O1—O1vii90.5 (2)
V1ix—O1—O1xi44.74 (13)O1v—O1—O1xi105.9 (2)
V1ix—O1—O1xii93.6 (2)O1v—O1—O1xii74.07 (17)
V1ix—O1—O1vi95.10 (11)O1v—O1—O1vi90.5 (2)
V1ix—O1—O1vii149.5 (2)O1v—O1—O1vii57.33 (17)
V1x—O1—O1i137.5 (2)O1xi—O1—O1xii63.19 (14)
V1x—O1—O1ii42.48 (10)O1xi—O1—O1vi113.63 (11)
V1x—O1—O1viii47.52 (11)O1xi—O1—O1vii161.8 (3)
V1x—O1—O1ix93.6 (2)O1xii—O1—O1vi161.8 (3)
V1x—O1—O1x44.74 (13)O1xii—O1—O1vii113.63 (11)
V1x—O1—O1iv149.5 (2)O1vi—O1—O1vii63.19 (14)
V1x—O1—O1v95.10 (11)
Symmetry codes: (i) x, y, z1; (ii) x, y, z+1; (iii) x+1, y+1, z; (iv) y+1/2, x+1/2, z1/2; (v) y+1/2, x+1/2, z+1/2; (vi) y+1/2, x+1/2, z1/2; (vii) y+1/2, x+1/2, z+1/2; (viii) x, y, z; (ix) y+1/2, x1/2, z1/2; (x) y+1/2, x1/2, z+1/2; (xi) y1/2, x+1/2, z1/2; (xii) y1/2, x+1/2, z+1/2.
(V0.92O2modulated) top
Crystal data top
O2V0.92V = 121.56 (2) Å3
Mr = 78.9Z = 4
Monoclinic, F(000) = 149
a = 6.6458 (6) ÅDx = 4.309 Mg m3
b = 2.8746 (2) ÅX-ray radiation, λ = 0.72044 Å
c = 6.3631 (6) ŵ = 6.93 mm1
β = 90.024 (10)°T = 293 K
Data collection top
1297 measured reflectionsθmax = 35.4°, θmin = 3.5°
445 independent reflectionsh = 88
302 reflections with I > 3σ(I)k = 44
Rint = 0.007l = 88
Refinement top
Refinement on F1 constraint
R[F2 > 2σ(F2)] = 0.056Weighting scheme based on measured s.u.'s w = 1/(σ2(F) + 0.01F2)
wR(F2) = 0.073(Δ/σ)max = 0.006
S = 4.44Δρmax = 0.72 e Å3
445 reflectionsΔρmin = 0.78 e Å3
92 parametersExtinction correction: B-C type 1 Gaussian isotropic (Becker & Coppens, 1974)
0 restraintsExtinction coefficient: 3800 (400)
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top
xyzUiso*/UeqOcc. (<1)
V10000.0318 (11)0.983 (8)
V200.50.50.0283 (13)0.857 (8)
O10.2003 (2)00.5002 (4)0.0155 (7)
O20.0005 (3)0.50.2000 (2)0.0128 (6)
Atomic displacement parameters (Å2) top
U11U22U33U12U13U23
V10.0693 (14)0.0155 (18)0.010 (2)00.0068 (16)0
V20.051 (2)0.027 (2)0.007 (3)00.0025 (18)0
O10.0147 (11)0.0171 (9)0.0147 (14)00.0008 (12)0
O20.0186 (13)0.0112 (8)0.0085 (12)00.0059 (16)0
Experimental and refinement details at 460 K (λ = 0.72044 Å) top
Space groupX 2/m(0β0)s0
CenteringX = 1/2, 0, 1/2, 1/2
Z4
a (Å)6.6458 (6)
b (Å)2.8746 (2)
c (Å)6.3631 (6)
β (°)90.024 (10)
V (Å3)121.562 (18)
q vector0, 0.2328 (9), 0
ρ (g cm-3)4.3091
µ (mm-1)6.934
No. measured reflns1297
Range of hkl-8 h 8
-4 k 4
-8 l 84
-1 m 1
θ (min/max)3.53/32.52
No. symmetry independent reflns (all)445
No. symmetry independent reflns (obs)a302
Rint(obs/all)0.75/0.76
All reflns R(obs)/wR(/all)b5.60/7.28
Main reflns R(obs)/wR(/all)5.08/6.44
Satellite reflns R(obs)/wR(/all)9.44/11.74
GoF (obs/all)5.71/4.44
Twin law(-1 0 0, 0 -1 0, 0 0 1)
Twin volumes I/II0.86 (4)/0.14 (4)
ρ(min/max) (e Å-3)0.72/-0.79
No. parameters92
Symmetry operations: (1) x1, x2, x3, x4; (2) -x1, x2, -x3, x4 + 1/2; (3) -x1, -x2, -x3, -x4; (4) x1, -x2, x3, -x4 + 1/2' (a) Criterion for the observed reflections is |F(obs)| > 3σ. (b) All agreement factors are given in %, weighing scheme is 1/{σ2F(obs) + [0.01F(obs)]2}.
Positional and displacement parameters of the atoms as well as Fourier coefficients of the modulation amplitudes at 460 K top
OccupancyxyzUiso
V10.492 (4)0.00.00.00.0318 (11)
V20.428 (4)0.00.50.50.0283 (13)
O10.5-0.2003 (2)0.00.5002 (4)0.0155 (7)
O20.50.0005 (3)0.50.2000 (2)0.0128 (6)
xsin1ysin1zsin1xcos1ycos1zcos1
V10.0065 (4)0.00.0003 (6)0.00.00.0
V2-0.0059 (4)0.00.0001 (6)0.00.00.0
O1-0.0004 (3)0.0-0.0004 (6)0.0-0.0039 (8)0.0
O20.0008 (3)0.00.0001 (5)0.00.0003 (10)0.0
u11u22u33u12u13u23
V10.0693 (14)0.0155 (18)0.010 (2)0.00.0068 (16)0.0
V20.051 (2)0.027 (2)0.007 (3)0.00.0025 (18)0.0
O10.0147 (11)0.0171 (9)0.0147 (14)0.00.0009 (12)0.0
O20.0186 (13)0.0112 (8)0.0085 (12)0.00.0059 (16)0.0
V1/V2uijsin1 = 0.0
u11sin1u22sin1u33sin1u12sin1u13sin1u23sin1
O1-0.0009 (11)-0.0002 (10)-0.0004 (13)0.00.0012 (15)0.0
O20.0006 (17)-0.0001 (13)0.0020 (17)0.0-0.0004 (9)0.0
u11cos1u22cos1u33cos1u12cos1u13cos1u23cos1
V1For ii = j uijcos1 = 0.00.0007 (9)0.00.0012 (14)
V2-0.0001 (11)0.0-0.0004 (16)
O10.0012 (7)0.0-0.0024 (15)
O2-0.0008 (7)0.0.-0.0005 (12)
D1111D1113D1122D1133D1223D1333
V1-0.0975 (13)0.0019 (12)-0.006 (3)-0.0009 (8)-0.005 (3)-0.0007 (19)
V2-0.019 (2)-0.0022 (18)-0.017 (3)0.0017 (12)-0.007 (3)-0.003 (2)
D2222D2233D3333D1112 = D1123 = D1222 = D1233 = D2223 = D2333 = 0.0
V10.07 (4)-0.009 (3)0.000 (3)
V2-0.10 (4)-0.012 (3)-0.002 (3)
C111sin1C113sin1C122sin1C133sin1C223sin1C333sin1
V1-0.048 (2)0.006 (2)-0.015 (4)-0.0037 (13)-0.000 (5)0.002 (3)
V20.022 (3)-0.004 (2)0.016 (5)0.0020 (12)0.000 (6)0.000 (4)
V1/V2C112sin1 = C123sin1 = C222sin1 = C233sin1 = 0.0
V1/V2Cijkcos1 = 0.0
D1112cos1D1123cos1D1222cos1D1233cos1D2223cos1D2333cos1
V1-0.000 (3)0.002 (2)0.008 (9)-0.0002 (12)0.007 (11)-0.000 (4)
V20.006 (3)-0.002 (3)-0.004 (10)0.0004 (15)0.005 (13)-0.002 (4)
V1/V2D1111cos1 = D1113cos1 = D1122cos1 = D1133cos1 = D1223cos1 = D1333cos1 = D2222cos1 = D2233cos1 = D3333cos1 = 0.0
V1/V2Dijklsin1 = 0.0
 

Footnotes

1The incommensurate vector would be q = (0, 0, γ), where γ ≈ 0.234, in the pseudo-ortho­rhom­bic C-centred cell derived from the primitive monoclinic one using the transformation a′ = a + c, b′ = −a + c and c′ = −b.

2It is noteworthy that part of the elements of the anharmonic tensor and the coefficients of the modulation function of the anharmonic tensor elements refined to values below 3σ. If one restricts these parameters to 0, the overall number of parameters is halved (approximately 40). At the same time, the agreement factors for the satellite reflections increase by approximately 2% [R(obs) = 11.54% and wR(all) = 13.84%].

Acknowledgements

Charlie McMonagle assisted us with setting up the low-tem­per­a­ture measurements at the SNBL. We thank Micha Hölzle, Fabian Beule, Robert Swaczyna and Roman Schäfer for their help with configuring our laboratory 4-circle diffractometer. This work was supported by the Helmholtz InnoPool Project MATHIPE (MATerials under HIgh PrEssure). Crystallog­raphy at the Institute of Physics was supported by MGML (mgml.eu) as part of the Czech Research Infrastructures program (project no. LM2023065).

Conflict of interest

There are no conflicts of inter­est.

Data availability

The data supporting the results reported here can be accessed within the article and supporting information.

References

Return to citationAhsbahs, H. (2012). Z. Kristallogr. 219, 305.  Web of Science CrossRef Google Scholar
Return to citationAllred, J. M. & Cava, R. J. (2013). J. Solid State Chem. 198, 10–17.  Web of Science CrossRef ICSD CAS Google Scholar
Return to citationAtkin, J. M., Berweger, S., Chavez, E. K., Raschke, M. B., Cao, J., Fan, W. & Wu, J. (2012). Phys. Rev. B 85, 020101.  Web of Science CrossRef Google Scholar
Return to citationBai, L., Li, Q., Corr, S. A., Meng, Y., Park, C., Sinogeikin, S. V., Ko, C., Wu, J. & Shen, G. (2015). Phys. Rev. B 91, 104110.  Web of Science CrossRef Google Scholar
Return to citationBleu, Y., Bourquard, F., Misdanitis, K., Poulet, A., Loir, A.-S., Garrelie, F. & Donnet, C. (2023). Mater. Today Commun. 35, 105564.  Web of Science CrossRef Google Scholar
Return to citationBouvier, P., Bussmann, L., Machon, D., Breslavetz, I., Garbarino, G., Strobel, P. & Dmitriev, V. (2023). Phys. Rev. B 108, 144106.  Web of Science CrossRef Google Scholar
Return to citationBoyarsky, L. A., Gabuda, S. P. & Kozlova, S. G. (2000). Physica B 284–288, 1454–1455.  Web of Science CrossRef CAS Google Scholar
Return to citationChamberland, B. L. (1973). J. Solid State Chem. 7, 377–384.  CrossRef CAS Google Scholar
Return to citationChen, Y., Zhang, S., Ke, F., Ko, C., Lee, S., Liu, K., Chen, B., Ager, J. W., Jeanloz, R., Eyert, V. & Wu, J. (2017). Nano Lett. 17, 2512–2516.  Web of Science CrossRef CAS PubMed Google Scholar
Return to citationDong, H. & Liu, H. (2013). Solid State Commun. 167, 1–4.  Web of Science CrossRef CAS Google Scholar
Return to citationDyadkin, V., Pattison, P., Dmitriev, V. & Chernyshov, D. (2016). J. Synchrotron Rad. 23, 825–829.  Web of Science CrossRef CAS IUCr Journals Google Scholar
Return to citationFolkers, L. C., Mitchell Warden, H. E., Fredrickson, D. C. & Lidin, S. (2020). Inorg. Chem. 59, 4936–4949.  Web of Science CrossRef ICSD CAS PubMed Google Scholar
Return to citationGaly, J. & Miehe, G. (1999). Solid State Sci. 1, 433–448.  Web of Science CrossRef ICSD CAS Google Scholar
Return to citationGhedira, G., Vincent, H., Marezio, M. & Launay, J. C. (1977). J. Solid State Chem. 22, 423–438.  CrossRef ICSD CAS Web of Science Google Scholar
Return to citationGro Nielsen, U., Skibsted, J. & Jakobsen, H. J. (2002). Chem. Phys. Lett. 356, 73–78.  CrossRef CAS Google Scholar
Return to citationGrzechnik, A., Hakala, B. V., Kurig, S., Walte, N., Tsujino, N., Kakizawa, S., Higo, Y., Zagorac, D., Zagorac, J., Dronskowski, R., Schön, J. C. & Friese, K. (2024). Cryst. Growth Des. 24, 5582–5592.  Web of Science CrossRef ICSD CAS Google Scholar
Return to citationGrzechnik, A., Petříček, V., Chernyshov, D., McMonagle, C., Geise, T., Shahed, H. & Friese, K. (2023). Acta Cryst. B 79, 103–113.  Web of Science CrossRef ICSD IUCr Journals Google Scholar
Return to citationHu, P., Hu, P., Vu, T. D., Li, M., Wang, S., Ke, Y., Zeng, X., Mai, L. & Long, Y. (2023). Chem. Rev. 123, 4353–4415.  Web of Science CrossRef CAS PubMed Google Scholar
Return to citationJoshi, S., Smieszek, N. & Chakrapani, V. (2023). Sci. Rep. 10, 17121.  Web of Science CrossRef Google Scholar
Return to citationKatzke, H., Tolédano, P. & Depmeier, W. (2003). Phys. Rev. B 68, 024109.  Web of Science CrossRef Google Scholar
Return to citationKrüger, H. & Kahlenberg, V. (2005). Acta Cryst. B61, 656–662.  Web of Science CrossRef ICSD IUCr Journals Google Scholar
Return to citationLazic, B., Krüger, H., Kahlenberg, V., Konzett, J. & Kaindl, R. (2008). Acta Cryst. B64, 417–425.  Web of Science CrossRef ICSD CAS IUCr Journals Google Scholar
Return to citationLiu, K., Lee, S., Yang, S., Delaire, O. & Wu, J. (2018). Mater. Today 21, 875–896.  Web of Science CrossRef CAS Google Scholar
Return to citationLiu, M., Xie, S., Wei, L., Galluzzi, M., Li, Y., Wang, Q., Zhou, X., Wang, Y. & Li, J. (2020). Acta Mater. 195, 720–727.  Web of Science CrossRef CAS Google Scholar
Return to citationLongo, J. M., Kierkegaard, P., Ballhausen, C. J., Ragnarsson, U., Rasmussen, S. E., Sunde, E. & Sørensen, N. A. (1970). Acta Chem. Scand. 24, 420–426.  CrossRef ICSD CAS Web of Science Google Scholar
Return to citationLu, P., Zhou, J., Liu, X., Zhang, Z., Xu, F., Zhang, L., Mou, X., Feng, J., Gao, Y. & Zhao, J. (2014). J. Appl. Cryst. 47, 732–738.  Web of Science CrossRef CAS IUCr Journals Google Scholar
Return to citationMamakhel, A., Gjørup, F. H., Kløve, M., Borup, K. & Iversen, B. B. (2022). Inorg. Chem. 61, 8760–8766.  Web of Science CrossRef CAS PubMed Google Scholar
Return to citationMao, H. K., Xu, J. & Bell, P. M. (1986). J. Geophys. Res. 91, 4673–4676.  CrossRef CAS Web of Science Google Scholar
Return to citationMarezio, M., McWhan, D. B., Remeika, J. P. & Dernier, P. D. (1972). Phys. Rev. B 5, 2541–2551.  CrossRef ICSD Web of Science Google Scholar
Return to citationPetříček, V., Dušek, M. & Palatinus, L. (2014). Z. Kristallogr. 229, 345–352.  Google Scholar
Return to citationPetříček, V., Palatinus, L., Plášil, J. & Dušek, M. (2023). Z. Kristallogr. 238, 271–282.  Google Scholar
Return to citationPouget, J.-P. (2021). C. R. Phys. 22, 37–87.  Web of Science CrossRef CAS Google Scholar
Return to citationQazilbash, M. M., Brehm, M., Chae, B.-G., Ho, P.-C., Andreev, G. O., Kim, B.-J., Yun, S. J., Balatsky, A. V., Maple, M. B., Keilmann, F., Kim, H.-T. & Basov, D. N. (2007). Science 318, 1750–1753.  Web of Science CrossRef PubMed CAS Google Scholar
Return to citationRigaku Oxford Diffraction (2024). CrysAlis PRO. Rigaku Oxford Diffraction Ltd, Yarnton, Oxfordshire, England.  Google Scholar
Return to citationSchwingenschlögl, U. & Eyert, V. (2004). Ann. Phys. 13, 475–510.  Google Scholar
Return to citationShao, Z., Cao, X., Luo, H. & Jin, P. (2018). NPG Asia Mater. 10, 581–605.  Web of Science CrossRef Google Scholar
Return to citationStoe & Cie (1998). X-AREA. Stoe & Cie GmbH, Darmstadt, Germany.  Google Scholar
Return to citationWadsley, A. D. (1957). Acta Cryst. 10, 261–267.  CrossRef ICSD IUCr Journals Web of Science Google Scholar
Return to citationWang, Y., Zhu, J., Yang, W., Wen, T., Pravica, M., Liu, Z., Hou, M., Fei, Y., Kang, L., Lin, Z., Jin, C. & Zhao, Y. (2016). Nat. Commun. 7, 12214.  Web of Science CrossRef PubMed Google Scholar
Return to citationWilson, C. E., Gibson, A. E., Cuillier, P. M., Li, C.-H., Crosby, P. H. N., Trigg, E. B., Najmr, S., Murray, C. B., Jinschek, J. R. & Doan-Nguyen, V. (2022). Sci. Rep. 12, 14767.  Web of Science CrossRef PubMed Google Scholar
Return to citationWriedt, H. A. (1989). Bull. Alloy Phase Diagrams 10, 271–277.  CrossRef CAS Google Scholar
Return to citationWu, X., Wang, H. & Wang, Y. (2023). Materials 16, 6874.  Web of Science CrossRef PubMed Google Scholar
Return to citationXie, S.-Y., Wang, L., Liu, F., Li, X.-B., Bai, L., Prakapenka, V. B., Cai, Z., Mao, H.-K., Zhang, S. & Liu, H. (2018). J. Phys. Chem. Lett. 9, 2388–2393.  Web of Science CrossRef CAS PubMed Google Scholar
Return to citationXue, Y. & Yin, S. (2022). Nanoscale 14, 11054–11097.  Web of Science CrossRef CAS PubMed Google Scholar

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