Abstract
For the first time, the ternary Zintl phases RbCaBi and CsCaBi have been synthesized and structurally characterized via single-crystal X-ray diffraction methods. These two compounds, alongside KCaBi, are confirmed to crystallize in a tetragonal crystal system with the space group P4/nmm (no. 129) with two formula units per cell. The lattice constants increase monotonically from a = 5.3812(10) Å and c = 8.410(3) Å for KCaBi, to a = 5.4139(7) Å and c = 8.6180(17) Å for RbCaBi, and to a = 5.4709(11) Å and c = 8.914(3) Å for CsCaBi. The crystal structure can be visualized as an array of square prisms formed of Bi atoms, which are centered by alkali metal atoms, while the Ca atoms fill tetrahedra formed of Bi atoms. There are no direct Bi–Bi interactions in the crystal structure; therefore, with full cation ordering present, the chemical bonding in the ACaBi compounds can be rationalized within the fully ionic approximation as A+Ca2+Bi3− (A = K, Rb, Cs). This suggests the opening of an (narrow) energy gap between the valence and conduction bands, i.e., semiconducting behavior.
1. Introduction
Quantum materials as a whole represent a large category of materials that consist of materials like superconductors, topological materials, spin liquids, qubits, etc. Among this large group of material systems, this study focused on the field of topological materials, which in recent years have seen perhaps one of the largest expansions in interest [1,2,3,4,5,6]. Attempts to understand topological behavior predate the classification of quantum materials or even the term topological materials. The intellectual precursor of topological phases is the integer quantum Hall effect which was discovered in 1980 [7]. This effect is observed in two-dimensional electron systems that are subjected to strong magnetic fields and low temperatures, causing them to exhibit precise quantized steps in Hall resistivity, which allows for an investigation into a material’s transport properties. The integer quantum Hall effect is based on Landau levels, which are essentially the eigenstates of a charge particle (an electron) moving in a uniform magnetic field in free space. A more modern view of topological phases takes into account spin–orbit coupling. When electrons with opposite spin angular momentums move in opposing directions, non-trivial electronic topology is achieved [8].
Perhaps the most common and researched type of topological material is the topological insulator. Topological insulators cannot be classified as pure insulators/semiconductors or as metals. Instead, they lie somewhere in between. Most recent research focuses on three-dimensional (3D) topological insulators. These topological insulators begin to stray from the 2D model described above and must be thought of slightly differently. There are two general classes of 3D topological insulators—weak and strong—with the latter having more convoluted connection to their 2D counterparts compared to weak topological insulators. Strong topological insulators have a bulk that is insulating, but the entire surface exhibits topological surface states, i.e., it is conductive. Strong topological insulators occur when spin–orbit coupling causes inversion between the valence and conduction bands. If this band inversion occurs but the bulk remains gapped, then the material becomes a topological insulator. A key point is that through this process time-reversal symmetry is preserved, which protects the topological surface states [9]. This spin–orbit coupling, which is crucial to the formation of topological insulators, is most commonly observed in the presence of heavy metals [10]. Some examples of strong topological insulators include Bi2Se3 and Bi2Te3 [11], as well as the first experimentally realized strong 3D topological insulator Bi1–xSbx [12].
Recently, a new category of topological materials have received much interest: topological semimetals. These consist of Weyl and Dirac semimetals, which exhibit band crossing in the bulk of the material rather than just the surface, as in topological insulators. Essentially one can image Dirac semimetals through the lens of Weyl semimetals as a combination of two Weyl points with opposite chiralities. Dirac semimetals were experimentally realized, not long ago, in materials like Na3Bi [13] and Cd3As2 [14].
As evident from the above, perhaps the most prominent heavy metal in many topologically relevant compounds is Bi. Often, Bi is found in a reduced state (viz. Na3Bi = 3 × Na+ + Bi3−), forming compounds known as Zintl phases. They are made from metals from groups 1 and 2 along with the more electronegative elements from groups 13 through 15. The crystal structures of these unique materials display the characteristics of both ionic-like and covalent-like bonding, satisfying the valence requirements according to the Zintl–Klemm concept [15].
Traditionally, Zintl phases have been studied as candidate materials for thermoelectric energy conversion [16,17]. More recently, they have come under renewed investigation for their potential as topological materials [2]. Density functional theory (DFT) computations, which have provided accelerated means for the exploration of yet unknown chemical compositions and structures, have also shown promise of Zintl phases as topological materials [18,19].
Our research team has had a long-standing interest in compounds of Bi within the realm of Zintl phases [20,21,22,23]. With the interest in Bi-based Zintl phases skyrocketing, we renewed our exploratory work aimed at the discovery of such new materials. Specifically, we targeted the equiatomic AAEBi general compositions (A = alkali metal, AE = alkaline–earth metal), several of which have been computationally predicted to be topologically non-trivial [24,25,26].
In this paper, we report the synthesis and structural characterization of KCaBi, RbCaBi, and CsCaBi via single-crystal X-ray diffraction methods. The structures are new additions to the large family of compounds that are isotypic to the Cu2Sb structure and commonly referred to as being of the anti-PbFCl structure type. In all three cases, a full cation ordering is observed, indicating that the structures obey the valence rules and the materials are expected to be semiconductors following the formula breakdown K+Ca2+Bi3−, Rb+Ca2+Bi3−, and Cs+Ca2+Bi3−, i.e., they are typical Zintl phases.
2. Results
Among the structures of the three compounds presented below, only two are new; the structure of KCaBi has been previously reported [27]. We include it again in this paper since the original determination was performed at ambient temperature, while the structures of ACaBi (A = K, Rb, Cs) discussed here are all established at 200 K. Details of data collection and selected crystallographic parameters are summarized in Table 1.
Table 1.
Selected single-crystal data collection and structure refinement parameters for KCaBi, RbCaBi and CsCaBi. All three data sets were collected at 200(2) K with monochromated Mo Kα radiation, λ = 0.71073 Å.
The structure of ACaBi (A = K, Rb, Cs) is tetragonal and has the centrosymmetric space group P4/nmm (no. 129). The prototype anti-PbFCl structure has been discussed in many other published works [28,29]; therefore, we will only briefly cover it. A schematic representation of the structure, drawn with thermal ellipsoids, can be found in Figure 1.
Figure 1.
The tetragonal crystal structure of CsCaBi, projected approximately down the a-axis. The representation emphasizes the arrangement of Na-centered tetrahedra of Bi and Cs-centered square pyramids of Bi. The unit cell is outlined. Thermal ellipsoids are drawn at the 90% probability level. One should notice that Ueq for the A atoms vs. the average Ueq values for the Ca and Bi atoms shows a trend with Ueq (Cs):Ueq (Bi,Ca) = 1.4; Ueq (Rb):Ueq (Bi,Ca) = 2.3; and Ueq (K):Ueq (Bi,Ca) = 2.7, which could indicate that the smaller K+ cation is not able to fit very well in the coordination environment of five Bi3− anions.
There are three independent crystallographic positions in the asymmetric unit (Table 2), including one alkali metal, one calcium, and one bismuth site, all in special positions (Pearson symbol tP6, Wyckoff c2a). The structure can be described in multiple ways and related to other simpler structures, which are commonly derived from close-packed ions [30,31]. One such way of relating the ACaBi (A = K, Rb, Cs) structure to that of the ubiquitous cubic MgAgAs structure (also known as half-Heusler, a variant of the rock salt and zinc blende patterns) is depicted schematically in Figure 2. In essence, if one considers a cubic close-packed array of Bi3− anions and fills the interstices with A+ and Ca2+ cations as depicted in the left panel, the MgAgAs structure is realized. Such an arrangement of large ions is unlikely to be stable, and in fact, most other equiatomic AAEBi compounds crystallize with different structures; only LiMgBi from the latter family is reported with the cubic MgAgAs-type structure [32]. Following a rearrangement of half of the alkali and alkaline-–earth metal atoms, and subsequent unit cell expansion, the actual tetragonal PbFCl arrangement can be obtained.
Table 2.
The atomic coordinates of the atoms and their equivalent isotropic displacement parameters Ueq a for KCaBi, RbCaBi and CsCaBi.
Figure 2.
A schematic diagram showing how the tetragonal ACaBi (A = K, Rb, Cs) crystal structure can be derived from the cubic MgAgAs structure (close relative of the rock salt and zinc blende structures).
Another easy way of visualizing the crystal structure is as an array of square prisms of Bi atoms, centered by alkali metal atoms and Bi atom tetrahedra filled with Ca atoms, organized as shown in Figure 1. Alternating layers of prisms and tetrahedra are stacked along the c-direction. The much larger (relative to Ca) alkali metal atoms expand the stacking sequence, which is evident from the large increase in the c-axis from ca. 8.4 Å for KCaBi to ca. 8.9 Å for CsCaBi (Table 1). There also is a small elongation of the a-axis ongoing from KCaBi to CsCaBi, but the unit cell expansion is clearly anisotropic; the c/a ratios presented in Table 1 are a testament to that. The reason for the much smaller effect of the alkali metal on the bonding in the ab-plane is rooted in the fact that Ca coordination by the Bi atoms should remain nearly constant in the series. Table 3 shows selected interatomic distances, with dCa–Bi varying within less that 0.5%.
Table 3.
Selected interatomic distances (Å) in KCaBi, RbCaBi and CsCaBi.
With regards to distances, it is noted that the smaller Ca atom favors “tighter” 4-fold tetrahedral coordination with dCa–Bi values on the order of 3.2 Å; these are on par with the sum of the Pauling single-bonded radii of Ca (1.736 Å) and Bi (1.51 Å) [33]. At the same time, the larger alkali metal atoms are pyramidally (CN 5) coordinated but only the axial dA–Bi contacts come close to the sum of the Pauling single-bonded radii (dK–Bi = 3.57 Å vs. 2.025 + 1.51 = 3.535 Å; dRb–Bi = 3.73 Å vs. 2.16 + 1.51 = 3.67 Å; dCs–Bi = 3.94 Å vs. 2.35 + 1.51 = 3.86 Å). The equatorial dA–Bi contacts between the A atoms that are square–pyramidally coordinated by the Bi atoms are much longer (Table 3), indicating that these interactions might be more electrostatic than covalent in nature. The larger equivalent displacement parameters Ueq for K in KCaBi, Rb in RbCaBi, and Cs in CsCaBi (Table 2) are all systematically larger compared to the Ueq values for Ca and Bi, suggesting that the alkali metal atoms may have more “room” to move about their equilibrium positions in the referenced structures.
There are no direct Bi–Bi interactions, with the Bi atoms being over 5 Å apart from each other. Thus, ACaBi (A = K, Rb, Cs) can be thought of as salt-like A+Ca2+Bi3− compounds, i.e., a Zintl phase. Such partitioning of the valence electrons is indicative of the opening of an (narrow) energy gap between the valence and the conduction bands, which is sought after in both thermoelectrics and topological insulators [2].
Along that line of thought, we also mention that the ACaBi materials could be conceptually derived from the Dirac semimetal Na3Bi, discussed previously, the structure of which can also be rationalized as made of closed-shell Na+ and Bi3− ions. Na3Bi crystallizes hexagonally with the centrosymmetric space group P63/mmc (no. 194), where the majority of the Na atoms are arranged in a nearly perfect tetrahedral network with the topology of lonsdaleite [13]. The heavier alkali metals tend to form cubic A3Bi (A = K, Rb, Cs) compounds with the full Heusler (CuMn2Al) structure, which is related to the already discussed MgAgAs (Figure 2). One can then envision the substitution of two monovalent A+ cations with one divalent AE2+ cation to arrive at the salt-like formulation A+AE2+Bi3−. Also of note is the fact that in such a gedanken experiment, the parent A3Bi structure would be expected to undergo substantial reconstruction to accommodate the loss of one per formula unit atom and optimize the crystal packing based on the two types of cations with differing charges and ionic sizes (Figure 2). An expansion of these ideas, taking a deeper look into the current landscape of structural data pertaining to such compounds follows in the next section.
3. Discussion
Many equiatomic A–AE–Pn phases (A = alkali metal, AE = alkaline–earth metal, Pn = pnictogen, i.e., P, As, Sb, Bi) are already known, with the first structural reports dating back over 50 years ago [32,33,34,35]. The nominally divalent Eu and Yb from the lanthanide family can also be included here since the atomic radius of Eu is close to that of Sr and the atomic radius of Yb is close to that of Ca [36]. Hence, Eu and Yb often form compounds that are isostructural to those of Sr and Ca.
If we consider all the elements (Li, Na, K, Rb, Cs; Be, Mg, Ca, Sr, Ba, Eu, Yb; P, As, Sb, Bi) that could possibly make up a ternary equiatomic A–AE–Pn phase, there will exist nearly 150 possible combinations. However, out of them, only 48 (roughly ⅓) have been experimentally confirmed, with the corresponding structures reported in the literature (see Appendix A, where a complete list of experimentally reported AAEPn compounds is given). There are almost no indications that the rest of the possibilities are not synthesizable; the gaps in knowledge are likely due to the increased chemical reactivity and increased difficulty in synthesizing and analyzing the compounds with K, Rb and Cs. In fact, this article marks the first compound from this family containing Cs that has been successfully synthesized and characterized. Furthermore, modern computational approaches have predicted what the crystal structures of the many yet-to-be-discovered compounds ought to be [37,38,39], and it is satisfying to see partial agreement between theory and experiment with regards to CsCaBi (vide infra).
From the structures that are experimentally established to date, the most recurring types are schematically depicted in Figure 3. A relatively straightforward dependence on the structures with the atomic sizes has been proposed [20].
Figure 3.
Schematic representations of the crystal structures of the most typical experimentally observed A–AE–Pn phases (A = alkali metal, AE = alkaline–earth metal, Pn = P, As, Sb, Bi). The A atoms are drawn in blue, AE atoms are the green spheres, and Pn atoms are shown in red.
Although there is lack of experimental reports on compounds composed of the heaviest alkali metals, some prominent trends begin to emerge. For example, when A = Li, the orthorhombic TiNiSi structure (also known as MgSrSi or Co2Si) is the dominating one. By comparison, when A = Na, the hexagonal ZrNiAl structure type is favored. The cubic MgAgAs structure type, as already mentioned, has only been observed for the composition MgLiPn, which can be attributed to the smallest ionic radii of Li+ (r = 0.59 Å) and Mg2+ (r = 0.57 Å) [36] compared to the rest of the alkali and alkaline–earth metals (with the exception of Be2+, which is even smaller). In addition, Li+ and Mg2+ are quite similar to each other and probably best suited for highly symmetric coordination by Pn3− anions.
When looking at other patterns in the current literature, it is observed that compounds with heavier alkali metals K and Rb tend to crystallize into the tetragonal anti-PbFCl structure type; however, it must be noted that this is the structure type with the widest range of chemical composition. The ZrBeSi structure type is largely made up of Li and Be-containing compositions. In this case, the very small Li+ and Be2+ cations are able to adopt a trigonal–planar coordination environment. The LiGaGe structure is just a non-centrosymmetric variant of the ZrBeSi structure, where the 3-fold coordinated position “almost” attains a higher coordination number 4 (Figure 4). Curiously, one can envision additional structural reconstruction, whereby the structure transitions to an ordered TiNiSi-like arrangement with 4- and 5-fold coordination of the cations.
Figure 4.
Schematic representations of how the AAEPn crystal structures of the ZrBeSi, LiGaGe, and TiNiSi types are related to each other. The honeycomb layers in the ZrBeSi-like structure (emphasized with the gray cylinders) become slightly puckered in the LiGaGe-like structure. Additional distortion allows neighboring layers to come close together and the coordination environment to become distorted tetrahedral. The coordination number of the larger cation, an alkali metal in the chosen examples, is reduced from 6 to 5 since one of the vertices of the octahedron becomes too distant.
We would be remiss here if we do not mention that there are several curious cases in the published structural data which show “swapped” positions of alkali and alkaline–earth metals, or flat-out “violations” of bonding principles established from analogous compounds. One such recent exception to the rules is KBaBi, which was found to crystallize in the ZrBeSi-type structure [40]. This is the first AAEPn compound in the ZrBeSi structure type that contains an alkali metal heavier than Li or Na. Contrary to the trend mentioned above, Ba and K both have large atomic radii (1.981 Å and 2.025 Å, respectively) [33], making it difficult to explain the trigonal–planar coordination of Ba. This suggests that the parameters for crystallization in this structure type, and possibly other structure types too, are not understood as well as anticipated.
With machine learning and various computational algorithms for structure assessment rapidly becoming mainstream approaches, one could anticipate rapid advances in this area. However, the scarcity of experimental structural information for the heavy alkali metal (Rb and Cs)-based compositions contributes to incomplete training sets, and as a result, predictive modeling may not arrive at the correct ground state structure. For example, there are predictions that RbCaBi will crystallize in the hexagonal ZrNiAl [41] as well as the ZrBeSi [25] structure types, while the experiment indicates that the correct structure is tetragonal. Similarly, CsCaBi has also been predicted to crystallize in the ZrNiAl structure by one study [41], while other models correctly identify it as being a part of the anti-PbFCl structural tree [42,43]. Clearly, further experimental investigation into all yet-to-be-synthesized compositions is warranted.
4. Materials and Methods
Maintaining inert atmosphere every step of the way is critical, because most of the complications with the synthesis and crystallographic studies arose from their extreme air and moisture sensitivity. Therefore, all synthetic and post-synthetic manipulations were carried out in an argon gas-filled glove box with O2/H2O levels below 1 ppm, or under vacuum (typically ca. 20 mTorr).
The synthesis procedure for KCaBi, RbCaBi and CsCaBi was adapted from the protocols used for synthesizing the previously reported Na–AE–Pn phases [44,45]. Briefly, the elements were purchased from Alfa or Sigma-Aldrich (St. Louis, MO, USA) with stated purity 99.9 wt% and used without additional purification. The elements were weighed and put in Nb tubes in the glove box. The Nb tubes were then welded shut under argon. The welded Nb tubes were subsequently placed in fused silica tubes, which were then evacuated and flame-sealed. The reactions were carried out at temperatures ranging from 600 to 800 °C (ramp rate: 300 °C/h) for 24h, and subsequently cooled to room temperature (rate −10 °C/h). Then, the tubes were put back in the glove box and cut open.
Caution: Alkali metals react quickly with air, even more so at high temperature where the reaction could be violent. Extreme care must be exercised, and to mitigate the risk, the silica jackets in such reactions should be made sufficiently long so that one of the ends of the tube protrudes outside the furnace; this is essential for the condensation of vapors in the event of a leak from the niobium ampoules into the silica tube.
X-ray powder diffraction data were collected using a Rigaku MiniFlex powder diffractometer (Rigaku Americas, The Woodlands, TX, USA), which was operated inside a nitrogen-filled glove box. Regardless of the steps taken to prevent contact of the samples with air and moisture, the X-ray powder diffraction patterns showed very high background and weak Bragg peaks, which is an indication that the samples are extremely air-sensitive and have partially decomposed in the preparation/transfer steps or during the actual experiments. The best results were obtained when the powdered samples were covered with Kapton polyimide tape. A representative powder diffraction pattern from such an experiment is shown in Figure 5.
Figure 5.
Experimental (blue) and simulated (red) powder diffraction patterns of CsCaBi. The high background at a low angle is contributed by the polyimide tape that protects the extremely air-sensitive material.
All additional structural characterization was performed via single-crystal X-ray diffraction. The crystals of KCaBi, RbCaBi and CsCaBi were generally small and did not have well-defined morphologies. As expected, air stability is an issue for samples with such high alkali metal contents (vide supra); therefore, single crystals had to be selected in the glove box. This was carried out under a microscope, with the crystals cut to dimensions of 0.10–0.20 mm. The procedure was carried out with a scalpel in a droplet of dry oil and was easily performed because the crystals were very brittle. After that, the crystals were taken out of the glove box, quickly “scooped” from the oil droplet by using MiteGen plastic loops (Ithaca, NY, USA), and transferred to the goniometer head of a Bruker APEX III CCD-based diffractometer.
For the intensity data collection, supplying nitrogen gas flow was needed to alleviate the problem of air sensitivity. Temperature was maintained at 200 K throughout the experiments via a nitrogen stream from boiled liquid N2. The software package provided by Bruker (Madison, WI, USA) [46] was used to manage data collection and for the integration of the measured reflections. Absorption correction was applied using SADABS (version 2.03) [47]. Refinements by least-square minimizations on F2 were carried out with the aid of the SHELXL program [48]. The atomic coordinates from the previous report on KCaBi [27] were used to create a starting model. Very reasonable conventional residual factors were obtained only after a few refinement cycles. Site occupancies were checked for each atom (for each structure) and no deviations from the unit were found. In the last refinement cycles, the atoms were refined anisotropically with SHELXL [48]. The final difference Fourier maps, in all cases, are featureless (Table 1).
5. Conclusions
Although ternary Zintl phases have been explored in the past and have provided some of the earliest topological materials, there remain large gaps in the literature as far as Zintl AAEPn is concerned. This is due to the increasing chemical reactivity and difficulty in synthesizing and analyzing such compounds. The lack of precise structural information and inconsistencies in knowledge are the primary reasons for the failure of some of the computational methodologies used to date to help close these gaps. Further experimental work is called for to allow for better synergy between theory and experiment and to improve the future accuracy of DFT calculations.
Author Contributions
Conceptualization, A.S. and S.B.; methodology, formal analysis, A.S. and S.B.; investigation, A.S. and S.B.; resources, S.B.; data curation, S.B.; writing—original draft preparation, S.B.; writing—review and editing, S.B.; supervision, S.B.; project administration, S.B.; funding acquisition, S.B. All authors have read and agreed to the published version of the manuscript.
Funding
This research was funded by the US Department of Energy through a grant DE-SC0008885.
Institutional Review Board Statement
Not applicable.
Informed Consent Statement
Not applicable.
Data Availability Statement
The corresponding crystallographic information files (CIFs) for all structures have been deposited with CSD, and the data for this paper can be obtained free of charge via https://www.ccdc.cam.ac.uk/structures/ (accessed on 2 March 2026) (or from the CCDC, 12 Union Road, Cambridge CB2 1 EZ, UK; Fax: +44-1223-336033; E-mail: deposit@ccdc.cam.ac.uk). Depository numbers are 2529379 (KCaBi), 2529380 (RbCaBi) and 2529381 (CsCaBi).
Acknowledgments
The authors are indebted to Salina Rahman for their help with single-crystal X-ray diffraction data collection and Daniel Tortorella for assisting with the preliminary exploratory work on A–AE–Pn phases.
Conflicts of Interest
The authors declare no conflicts of interest.
Abbreviations
The following abbreviations are used in this manuscript:
| A | alkali metal |
| AE | Alkaline–earth metal |
| Pn | pnictogen, i.e., P, As, Sb, Bi |
Appendix A
Table A1.
Experimentally reported AAEPn compositions with their respective structure types and geometric data used to group them in the main text.
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