Crystals 2013, 3(3), 419-430; doi:10.3390/cryst3030419

Article
Electronic Origin of the Orthorhombic Cmca Structure in Compressed Elements and Binary Alloys
Valentina F. Degtyareva
Institute of Solid State Physics RAS, Moscow district, Chernogolovka 142432, Russia; E-Mail: degtyar@issp.ac.ru; Tel.: +7-496-522-8376; Fax: +7-496-522-8160
Received: 24 May 2013; in revised form: 21 June 2013 / Accepted: 15 July 2013 /
Published: 19 July 2013

Abstract

: Formation of the complex structure with 16 atoms in the orthorhombic cell, space group Cmca (Pearson symbol oC16), was experimentally found under high pressure in the alkali elements (K, Rb, Cs) and polyvalent elements of groups IV (Si, Ge) and V (Bi). Intermetallic phases with this structure form under pressure in binary Bi-based alloys (Bi-Sn, Bi-In, Bi-Pb). Stability of the Cmca-oC16 structure is analyzed within the nearly free-electron model in the frame of Fermi sphere-Brillouin zone interaction. A Brillouin-Jones zone formed by a group of strong diffraction reflections close to the Fermi sphere is the reason for the reduction of crystal energy and stabilization of the structure. This zone corresponds well to the four valence electrons in Si and Ge, and leads to assume an spd-hybridization for Bi. To explain the stabilization of this structure within the same model in alkali metals, that are monovalents at ambient conditions, a possibility of an overlap of the core, and valence band electrons at strong compression, is considered. The assumption of the increase in the number of valence electrons helps to understand sequences of complex structures in compressed alkali elements and unusual changes in their physical properties, such as electrical resistance and superconductivity.
Keywords:
crystal structure; Hume-Rothery phases; structure stability

1. Introduction

Experimental studies of elements under high pressure reveal a great variety of structural transformations, summarized in review papers (see [1,2,3] and literature cited therein). At ambient pressure, the most representative structures for elements are close-packed structures: body-centred cubic (bcc), face-centred cubic (fcc), and hexagonal close-packed (hcp), typical for metals. Elements on the right-hand side of the Periodic table—main group IV-VII semi-metals and non-metals—crystallize in open-packed structures following the 8-N coordination rule. These elements tend to transform under pressure to a metallic state with closely packed structures. On the left-hand side of the Periodic table, the group 1 and II elements (the alkali and alkali-earth elements) are good metals at ambient pressure that crystallize in the closely packed structures. Under pressure, however, they show an anomalous behavior, transforming to open-packed structures.

Two different trends from both sides of the Periodic table are illustrated by the data in Table 1, which show the structural sequences for Si, Ge, and Bi (upper panel), and for the heavy alkali elements (lower panel). These elements are chosen for our consideration because, under pressure, they all go in their pathways through the same structure—orthorhombic with 16 atoms in the cell, space group Cmca, Pearson symbol oC16. This type of structure is unknown for any element or compound at ambient pressure, and was first defined for Cs and Si under pressure [4,5], and then for other elements included in Table 1. Theoretical calculations of the band structure energy for Cmca phases of Si and Cs have demonstrated that “structural similarities in Cs-V and Si-VI are not reflected in similarities of the electronic structures” [6]. For Si, a nearly free-electron behavior has been shown, while for Cs-V, dominate d-orbital components due to s-d electron transfer have been found [6].

Table 1. Sequences of structural transformations on pressure increase for elements with the oC16 structure.

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Table 1. Sequences of structural transformations on pressure increase for elements with the oC16 structure.
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Notes: The numbers above the arrows show the transition pressures in GPa, reported in experimental measurements on pressure increase. The crystal structures of the phases are denoted with their Pearson symbols, apart from the most common metallic structures bcc, fcc, and hcp. “h–g” stands for a host-guest structure. For experimental data see [1,2,3] and literature cited therein.

In this paper, formation and stability of the oC16-Cmca structure is discussed within the Brillouin zone–Fermi sphere interaction with application of the Hume-Rothery mechanism [7,8,9]. A complex structure, like γ-brass Cu5Zn8-cI52, reduces its crystal energy by formation of the Brillouin zone planes close to the Fermi sphere, satisfying the electron concentration rule. Following this model it is necessary to assume for compressed alkali metal, not only s-d transfer, but also further overlap of valence band and upper core electrons [10]. This assumption was made to account for an unusual behavior under pressure of the alkali element sodium [11]. Na transforms above 1 Mbar to the low-symmetry, open structure oP8, which is similar to the phase AuGa with two electrons per atom. It was suggested for Na-oP8, an electronic transfer from core into the valence band. A similar suggestion is necessary to assume for alkali elements in oC16-Cmca phase, as is discussed in this paper.

2. Results and Discussion

The crystal structure oC16-Cmca belongs to the family of structures described by Pearson [12] as a planar square-triangle nets of atoms, assigned as 32434 where “3” specifies a triangle, “4” a square, and the superscript shows a multiplicity. These nets are alternated with square 44 nets. Layers 32434 may be stacked either antisymmetric or with a shift on 1/2 of a basic axis. Examples of this family represent the compounds CuAl2 (tI12), CoGe2 (oC24), PdSn2 (tI48), PdSn3 (oC32), and others [12]. An interesting example is an oC20 phase found for PdSn4, PtSn4, and AuSn4 [13]. This type of structure, with the space group Aba2, has some similarities with the discussed oC16-Cmca structure having nearly same axial ratios but slightly different stacking layers: four 32434 nets alternate by two 44 nets, whereas in oC16-Cmca the numbers of nets are two and four, respectively, as considered below.

2.1. Structural Characteristics of oC16-Cmca Phases

The conventional unit cell contains 16 atoms in two crystallographically non-equivalent positions 8f (0,y,z) and 8d (x,0,0) in Wyckoff notation of the Cmca space group. A feature of the structure oC16-Cmca is 32434 nets, formed by atoms in the 8f position, with squares lying over the cell corners and cell base centers, or over the midpoints of the cell edges, and alternated by two square nets 44 (atoms in the 8d position) shifted with respect to each other on a half of the b axis as shown in Figure 1. The configuration of atoms in the 32434 nets implies a rigid atomic arrangement with atomic positions y and z (8f) close to 0.167 and 0.333, respectively, providing y + z ≈ 0.5.

The data of all oC16-Cmca phases found at present are summarized in Table 2. All the structures have very similar axial ratios (bc ≈ 1, a/ba/c ≈ √3) and very similar atomic positions. This indicates that the structure is defined by certain criteria related to the electronic structure.

Some data for Cmca-oC16 phases in the Table 2 are essentially different, namely volume compression, V/Vo, which is especially significant for alkali metals (indicated in bold). The shortest interatomic distances for alkali metals Cs, Rb, and K (see Table 2, in bold) correspond to atomic radii 1.62, 1.38, and 1.16 Å, respectively. It is interesting to compare these values to the ionic radii given by Kittel [14], 1.67, 1.48, and 1.38 Å, or to the ionic radii for coordination number 10 given by Shannon [15], 1.81, 1.66, and 1.59 Å, respectively. At this degree of compression it is necessary to consider ionic core overleap and a transfer of core electrons into the valence band, as was theoretically proposed earlier [10].

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Figure 1. Crystal structure oC16-Cmca of Si-VI. (a) A perspective view. The atomic positions 8f and 8d are denoted as red and yellow, respectively; (b) A projection along the a-axis for nets at x = 0.5 (red) and x = 0.218 and 0.282 (yellow). The structure can be viewed as an alternating sequence of planar layers formed by square-triangle nets and puckered nearly square layers. The shortest interatomic distances are marked by dark lines (modified from [4]).

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Figure 1. Crystal structure oC16-Cmca of Si-VI. (a) A perspective view. The atomic positions 8f and 8d are denoted as red and yellow, respectively; (b) A projection along the a-axis for nets at x = 0.5 (red) and x = 0.218 and 0.282 (yellow). The structure can be viewed as an alternating sequence of planar layers formed by square-triangle nets and puckered nearly square layers. The shortest interatomic distances are marked by dark lines (modified from [4]).
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Table 2. Structural details of all the known Cmca-oC16 phases, formed under pressure in the pure elements Cs, Rb, Si, Ge, and Bi, and in Bi-alloys with In, Sn, and Pb (experimental data are taken from references indicated for each material).

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Table 2. Structural details of all the known Cmca-oC16 phases, formed under pressure in the pure elements Cs, Rb, Si, Ge, and Bi, and in Bi-alloys with In, Sn, and Pb (experimental data are taken from references indicated for each material).
PhaseSi-VI 38.4 GPa [5]Ge 135 GPa [16]Cs-V 12 GPa [4]Rb-VI 48.1 GPa [17]K-VI 112 GPa [18]Bi-IV 3.2 GPa 465 K [19]Bi40Sn60 5.8 GPa [20]Bi80Pb20 quenched from 1.7 GPa [21]Bi70In30 quenched from 2.0 GPa [21]
a (Å)8.0247.88511.2059.3728.03211.19110.734511.20911.236
b (Å)4.7964.6556.6265.55014.7536.6226.32706.6726.555
c (Å)4.7764.6516.5955.52784.7166.6086.31156.6586.531
Vat3)11.4910.6730.6017.9711.2530.6126.7931.1230.07
V/Vo0.5650.4700.2640.1940.1500.8640.8820.9050.921
a/c1.6801.6951.6991.6891.7031.6931.7011.6841.721
b/c1.0041.0011.0051.0041.0041.0021.0021.0021.004
dshort(Å)2.3402.3153.2352.7642.3173.2752.9853.2423.146
y (8f)0.1730.1730.1640.1700.1730.1700.1670.1720.170
z (8f)0.3270.3280.3130.3180.3270.3200.3330.3280.330
x (8d)0.2160.2180.2180.2110.2160.2100.2120.2140.212

2.2. Electronic Origin of Stability for oC16 Phases: Hume-Rothery Effects

Examination of stability of the oC16 structure is based on the concept of the Hume-Rothery mechanism and consists of construction of the Brillouin planes close to the Fermi sphere defined within the nearly free-electron model [22]. We first consider the oC16 phase in sp-elements and alloys and then in alkali elements.

2.2.1. Group IV Elements Si and Ge with the oC6 Structure

Elements Si and Ge are sp-elements of group IV and therefore have four valence electrons per atom. Figure 2a shows diffraction pattern for Si-oC16 with indication of position 2kF for z = 4 that locates just above a group of strong diffraction peaks selected for construction of the Brillouin-Jones zone (left) [22]. The inscribed Fermi sphere corresponds to 2kF for z = 4 and is in contact with 36 planes; zone filling by electron states VFS/VBZ equals ~93% as for the classical Hume-Rothery phase γ-brass Cu5Zn8. For the spherical Fermi surface, calculated distances to the Bragg planes (131), (113), (421), and (511) are slightly below the value of kF with ratios 1.032, 1.028, 1.014, and 1.004, respectively. In a real case, there is a degree of deformation of the Fermi sphere by the contact with the Brillouin boundary, so-called “truncation” factor. This was initially suggested by Sato and Toth for the electronic nature of long-period superlattices in alloys like Cu-Au, and similar systems [23], where the value of this factor was found to be within 5%.

In the middle of Figure 2a a Brillouin zone is shown, which is constructed by the planes of the first group of the strong reflections lying within the Fermi sphere. It is remarkable, that due to particular ratios of cell axes, this polyhedron is very symmetrical with hexagonal cross-sections ⊥ c* and in planes a*c* and b*c*. The symmetry of the BZ polyhedron formed by first strong Bragg planes is reflected on the electrostatic energy (see by Harrison [24]).

2.2.2. Structure oC16 in Bi and Bi-alloys

Crystal structure of high-pressure, high-temperature phase of bismuth at ~4 GPa and ~500 K was recently solved by single-crystal synchrotron X-ray diffraction [19], with characteristics given in Table 2. Experimental observations of this Bi phase have a long story, since 1958 [25]. Pressure-temperature ranges for this Bi phase, assigned now as Bi-IV, are from ~2.2 GPa to ~5.5 GPa above 450 K. Room temperature phase Bi-III, stable at pressures 2.7–7.7 GPa, has a complex incommensurate host-guest structure [26]. Phase boundary Bi-III-Bi-IV is nearly horizontal (~450 K) and both phases transform to Bi-V with a body-centered cubic structure at higher pressure. There is a small volume difference between Bi phases III and IV, and different structures may be expected from the difference in valence electron bands. Formally, the group V element Bi has outer s2p3 electron configuration. Under pressure-temperature conditions, one may expect that hybridization of s, p, and d levels occur due to lowering of the higher empty d-band, as discussed by Pearson (see Reference [12], pp. 230–232).

For stability of the oC16 structure four valence electrons are necessary, and this count relates to the assumption of spd hybridization. It should be noted that for considerations of the Fermi sphere radius within the model of FS-BZ interactions only sp electrons are taken into account as structure controlled electrons. The same assumption on spd hybridization for Bi in Bi-based alloys with the oC16 structure is necessary to obtain the electron per atom count, equal to four, which stabilizes this structure.

Intermediate phases in Bi-Pb and Bi-In alloys were obtained under pressure-temperature conditions and quenched to ambient pressure at liquid nitrogen temperature [27]. Diffraction patterns of both phases, Bi80Pb20 and Bi70In30, were similar, however, rather complex to be solved 40 years ago. Development of new experimental methods of X-ray diffraction under pressure, and new programs of structure solutions, allowed defining oC16-Cmca structure in Si and Cs, and other elements, as indicated in Table 2. Based on these findings, a description of structure was found for similar phases in Bi80Pb20 and Bi70In30 alloys [21], and was also suggested for the Bi-IV phase. Experimental confirmation of this suggestion was obtained recently [19].

In the Bi-Sn alloys, an intermediate high-pressure phase was observed in situ under pressure [20]. It is remarkable that the X-ray diffraction data of the Bi40Sn60 phase reveals the oC16-Cmca structure with the evidence of site-ordering. Additional diffraction peaks (for example, the difference reflection 111) indicate preferred occupation of the constituent atoms, Sn and Bi, in positions 8f and 8d, respectively. To extend this observation, one can expect formation of ordered oC16-Cmca structures in some binary systems under pressure on the condition that the electron concentration rule will be satisfied.

2.2.3. Structure oC16 in Alkali Elements: Core Ionization

Phases with oC16-Cmca structure appear in Si and Ge under pressure within the sequence сF8 → tI4 → hP1 → oC16 → hcp, which follows an increase in packing density and coordination number (CN) 4 → 6 → 6 + 2 → 10,11 → 12. This pathway is in general tendency, for the elements on the right-hand side of the Periodic table, to adopt the more close-packed structures. The opposite trend was found for the elements on the left-hand side—a transformation under compression to open-packed structures. Alkali elements with the bcc structure at ambient conditions, which transforms to the fcc on pressure increase (CN = 8 and 12, respectively), undergo a transformation to low-coordinated structures. For K, Rb, and Cs the structure before oC16 is tI 4 with CN = (4 + 4), so that there is a turnover at transition tI 4 → oC16 where CN starts to increase again, and for Cs it attains CN = 12 at the transition to the double hexagonal close-packed structure, dhcp.

Unexpected behavior of alkali elements on compression tolerates radical changes in valence electron bonding, and an electronic level overlap and hybridization of upper core electrons and valence band should be considered. This assumption is supported by the large compression and short interatomic distances in oC16 structure, as is analyzed above, in Section 2.1. On Figure 2b diffraction pattern Cs-oC16 is shown (left) with the calculated 2kF positions shown for two possible numbers of valence electrons, z = 1 and 4. The groups of strong reflections near these positions are used for BZ construction (middle and right). The relation of the FS and BZ for the case z = 1 does not satisfy the Hume-Rothery conditions that supports the suggestion in increase of the valence electron counts. The Brillouin zone in Figure 2b (right) for z = 4 is similar to that of Si-oC16 in Figure 2a.

It is remarkable that oC16 structure is found in heavy alkalis, K, Rb, and Cs, but not in light, Na and Li. For Na, transformations from fcc to complex phases started at pressures above 100 GPa, whereas for K, Rb, and Cs, at 20, 13, and 4.3 GPa, respectively (see references [1,2,3]). This different behavior is related to the energetics of the electronic levels. First of all it should be noted that position of the empty d-level for Na is well above the valence s-level comparing to s-d levels for heavy alkalis. The oC16 structure may be expected for Na at higher compression, but it is not expected for Li with its three electrons.

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Figure 2. Simulated diffraction patterns (left) and constructed Brillouin-Jones zones (right) (a) for Si-oC16; and (b) for Cs-oC16 with the data from Table 2. Indices hkl for reflections selected for BZ constructions are indicated on the patterns. The position of 2kF is shown by dotted (red) line. See discussion in the text.

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Figure 2. Simulated diffraction patterns (left) and constructed Brillouin-Jones zones (right) (a) for Si-oC16; and (b) for Cs-oC16 with the data from Table 2. Indices hkl for reflections selected for BZ constructions are indicated on the patterns. The position of 2kF is shown by dotted (red) line. See discussion in the text.
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2.3. Structure Stability and Correlation with Properties within the Hume-Rothery Mechanism

Stability of Hume-Rothery phases in copper-based alloys, and other binary systems of noble-metals, and sp polyvalent metals, have been explained by the mechanism of Brillouin zone–Fermi-sphere interactions [7,8]. Hume-Rothery effects are found to become apparent for a wide variety of material/physical objects, such as for structurally complex alloy phases, quasicrystals and their approximants [28,29]. Liquid and amorphous metals may be ascertained to obey the Hume-Rothery rules [30,31]. Connecting chemical and physical viewpoints on Hume-Rothery electron-counting rules are considered in [32], on the classic example of gamma-brasses structure.

Fermi-sphere–Brillouin zone interactions should increase under compression, providing minimization of electron band energy, which depends on volume as V−2/3, whereas the electrostatic energy depends as V−1/3 (see discussion in [2]). The oC16-Cmca structure considered in this paper satisfies the criteria of Hume-Rothery mechanism for the elements Si and Ge with four valence electrons and there is no satisfaction of the Hume-Rothery mechanism for alkali metals, if considered monovalent. If the oC16 structure in the alkali metals is considered to be stabilized by the Hume-Rothery mechanism, it is essential to assume the increase in the valence electron count to z = 4 in these metals due to the valence band overlap with the outer core electrons.

From another point of view, atomic interactions can be analyzed using the electron localization function (ELF), which describes chemical bonding in real space [33,34]. The result of this approach is that a large amount of valence charge in the open-packed structures resides within the interstitial regions corresponding to the formation of “electrides”, in which the interstitial electrons form the anions. Thus, an elemental phase under pressure is considered as “pseudobinary ionic compound” [35,36]. These papers report the observation of the hexagonal phases of NiAs-hP4 type in Na and K (above 180 GPa and 35 GPa, respectively), the type that is widely occurring in binary phases (see by Pearson [12]). The formation of this phase, formed in a binary system of sp-metals, can be well explained using the Hume-Rothery mechanism with an appropriate number of valence electrons. There are a great variety of complex phases based on hP4 formed by distortions, vacancies, and superlattices to satisfy Hume-Rothery effects [37]. These considerations can help in the understanding of structural variety observed in alkali elements under different pressure-temperature conditions.

Structural properties of materials in many instances correlate with their physical properties. Fermi-sphere–Brillouin zone interactions, and degree of filling of the Brillouin zone by electron states, considerably define the properties of material like electrical resistivity, optical reflectivity, superconductivity, and others. With a high degree of BZ filling the free Fermi surface area becomes small, which is accompanied by an increase in density of state below the kF. The consequences of this FS-BZ configuration are the decrease in reflectivity, increase in resistivity, appearance, and increase in superconductivity, as discussed by Hirsch [38,39].

For the phases with the oC16-Cmca structure in Cs and Si, experiments show a relatively high electrical resistance and an increase in Tc of superconducting state (see discussion in [2]). Electrical resistance measurements under pressure available for Cs found a sharp increase at the transition tI4-oC16 near ~13 GPa. For Cs superconductivity emerges in tI 4 at ~11 GPa and riches Tc ~ 1.3–1.5 K in oC16 at pressure 12–14 GPa [40]. For Si, superconducting state was observed at the transition to the metallic state with β-Sn (tI4), and in the subsequent oI4 and hP1 phases with Tc ~ 7–8 K at pressures 12–20 GPa, with a decrease of Tc with pressure within the existence of the simple hexagonal (hP1) phase. It is noticeable that after reaching the minimum of 3.3 K at 37 GPa, Tc starts to increase again and reaches 4.9 K at 40 GPa in the oC16 phase, followed by a drop in the hcp phase [41]. The observed, relatively high Tc values in the oC16 phases can be attributed to the higher degree of filling of the Brillouin-Jones zone by the electronic states.

The drop of resistance for Bi at the transition of the ambient pressure semimetallic phase to Bi-II-mC4 at 2.5 GPa is well known from its magnitude, sharpness, and reversibility, and makes it an ideal pressure calibration point [25]. Further transition to Bi-III (host-guest) at 2.7 GPa leads to an increase of resistance, and the high temperature phase Bi-IV-oC16 has a resistance that is a little lower than for Bi-III. At higher pressures, the transition IV-V is accompanied by a moderately sharp drop in resistance. This behavior of resistance in Bi can be related now to established crystal structures of high-pressure phases. Relatively high resistance of Bi-IV is in agreement with our considerations of FS-BZ model for oC16 structure. In addition, the relatively high Tc values were observed for quenched oC16 phases in Bi80Pb20 and Bi70In30 alloys, 8.7 K and 7.9 K, respectively [27].

In the Bi-Sn alloys of the composition 40/60 at %, examined in situ under pressure, the initial phase mixture Bi + Sn was transformed to the intermediate phase after annealing the sample at 2.9 GPa and 150 °C for one hour. The diffraction pattern observed after annealing corresponded to the oC16 phase. The superconducting transition temperature (Tc) in BiSn alloy at ambient pressure is 3.7 K, a characteristic of β-Sn in the phase mixture with nonsuperconducting Bi. Under pressure, after the formation of the intermediate phase on the annealing at 363 K and 3.0 GPa, an increase in Tc to 7.4 K was observed (see Reference [20] and references therein).

On the whole, in all three Bi-based systems, intermediate phases formed under pressure-temperature conditions from two-phase mixtures have the same oC16 structure, identical to high-pressure high temperature form of Bi, and these phases can be considered as extended solid solutions based on Bi-oC16. In addition, an atomic ordering within 8f and 8d positions was observed for the nearly equiatomic BiSn-oC16 phase. Structural resemblance of Bi-based phases is supplemented by similar superconducting properties that have its source from the discussed Hume-Rothery mechanism.

3. Method of Analysis

The underlying concept of structural stability in the nearly-free electron model is based on matching of the Fermi sphere (FS) radius, kF, and the distance to the Brillouin zone plane, ½ qhkl, that is half of the reciprocal vector qhkl, kF ≈ ½ qhkl [7,8]. This rule defines boundaries of phase stability by average number of valence electrons per atom for classical Hume-Rothery phases, such as fcc, bcc, and hcp. For complex phases such as γ-brass, Cu5Zn8-cI52, it is necessary to consider the extended zone or Brillouin-Jones zone, assigned here as BZ. For complex phases, it is important as to how well the BZ accommodates the FS, which provides the gain in band structure energy to be enough to compensate the loss in electrostatic energy that arises from the formation of superlattices, vacancies, and distortions.

To analyze complex phases within the FS-BZ interactions, the program BRIZ is used, which allows to consider high symmetry structures, cubic or hexagonal, as well as structures of low symmetry: tetragonal, orthorhombic, monoclinic, or triclinic [22,37]. As an input, the following data are used: lattice parameters, number of atoms in the cell, number of valence electrons per atom, and the hkl indices of the Brillouin planes that are selected from peaks in the diffraction pattern located near kF. The output data are the BZ volume, the FS volume, kF, and distances to the BZ planes. The program gives BZ construction with the inscribed FS as shown in Figure 2. This approach allows qualitative estimations of stability of structure and some physical properties of materials with this structure.

Thus, with the FS-BZ consideration for the phases in compressed alkali metals Li and Na, the appearance of a complex cI16 structure after bcc and fcc is evident to be of electronic origin of Hume-Rothery type, when superlattice 2 × 2 × 2 is formed due to a slight atomic shift to produce a Bragg plane close to kF, at that Li and Na are monovalent [2,11]. When considering the next phase in Na with the oP8 structure, it is essential to assume Na being divalent as for the isostructulal phase AuGa [11].

The same FS-BZ analysis can be applied to the problem of incommensurate structures, by using suitable approximants, as shown for incommensurately modulated phases of phosphorous at pressures 100–137 GPa [42]. Incommensurate host-guest phases are found in alkali metals Na, K, and Rb, and they can be considered in relation to the Hume-Rothery mechanism with the proper approximant extracting the necessary valence electron count from the FS-BZ model, as well as Bi-III host-guest phase [43]. It is important to mention that these host-guest phases in alkali elements are inline among the other high-pressure phases that are suggested to be considered within Hume-Rothery mechanism, as the oC16 phase discussed in this paper.

4. Conclusions

In this paper the oC16-Cmca structure is analyzed for the purpose of understanding the formation and stability of this structure in a number of elements from both sides of the Periodic Table, as well as in some binary alloys, for instance, in Bi alloys with In, Pb, and Sn. Primarily, the Cmca-oC16 structure is a common high-pressure form for polyvalent metals and alloys with the average number of valence electrons ~4, and might well be found in other alloys with the constituents from groups III-VI under pressure. Stability of this rather complex phase is related to the Hume-Rothery mechanism and gaining in the valence electron energy. Construction of Brillouin zone boundaries with the Bragg plains close to the Fermi sphere results in a highly-symmetrical polyhedron with many faces contacting the Fermi sphere, and nearly filled by electron states. This configuration meets well the Hume-Rothery mechanism criteria for phase stability, explaining qualitatively the physical properties of the matter with this structure such as resistivity and superconductivity.

Unexpected formation of the oC16-Cmca structure in compressed alkali elements K, Rb, and Cs brings up the question of the valence electron level hybridization with the upper core electrons. The commonly accepted s-d electron transition is sufficient to explain the first few high-pressure transitions in alkali metals and on further compression it is necessary to extend the degree of electron level hybridization that may account for sequences of complex high pressure phases including discussed in this paper, the oC16 phase.

Acknowledgments

The author gratefully acknowledges Olga Degtyareva for valuable discussion and comments. This work is supported by the Program of Russian Academy of Sciences “The Matter under High Energy Density”.

Conflict of Interest

The author declares no conflict of interest.

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