Abstract
Clathrate hydrates are a class of ordered structures that are stabilized via the delicate balance of hydrophobic interactions between water and guest molecules, of which the space-filling network of hydrogen-bonded (H-bonded) water molecules are closely related to tetrahedrally close-packed structures, known as Frank-Kasper (FK) phases. Here we report an alternative way to understand the intricate structures of clathrate hydrates, which unveils the diverse crystalline H-bonded networks that can be generated via assembly of one common building block. In addition to the intrinsic relations and pathways linking these crystals, we further illustrate the rich structural possibilities of clathrate hydrates. Given that the topological dual relations between networks of clathrate hydrates and tetrahedral close-packed structures, the descriptors presented for clathrate hydrates can be directly extended to other ordered materials for a more thorough understanding of their nucleation, phases transition, and co-existence mechanisms.
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Introduction
The science of water and ice still brings surprises to this day. As such, it is expected that the science of clathrate hydrates, which are solid solutions of water and gas, reveals even more intricacies from the delicate balance of hydrophobic interactions for the space-filling networks of hydrogen-bonded water molecules1. Among them, three structures are the cornerstones of clathrate hydrates, denoted as Type I, II, and H2,3,4. However, the known crystalline structures of clathrate hydrate are not unique. A majority of clathrate hydrates structures are closely related to a class of intermetallic structures, known as FK phases.
FK phases are tetrahedrally close-packed (TCP) structures, which are observed in a broad range of physical scales, from a few angstroms in alloys5,6 to mesoscopic-scale in various self-assembly of soft matter7,8,9,10,11,12,13,14,15. Generally, the TCP networks are described by the combination of four polyhedrons with only triangular faces16 (see Fig. 1). The icosahedron with coordination number 12 (CN12) interweaves with at least one of CN14, CN15, or CN16 forming diverse crystalline networks (27 types known17) that contains exclusively tetrahedral interstices. Instead of directly considering the densely packed framework as for the FK phases, the clathrate hydrate community focuses on its topological dual (Wigner–Seitz or Voronoi cells), that is, the network formed of H-bonded water molecules. Considering clathrate hydrates from the close packing perspective, the guest molecules at the center of the cages, or just the center position for empty cages, correspond to the TCP nodes in the FK phases, while the water molecules fill the tetrahedral interstices and are connected through H-bond forming a complex network (Fig. 1a–c). The network of H-bonded water molecules partition the space into a series of cavities (denoted H-bond cages) where guest molecules encaged, in principle, are the topological dual of CN polyhedrons (Fig. 1c–d). However, it is not uncommon for cages in clathrate hydrates to be empty which renders the non-stoichiometric characteristic of clathrate hydrates1, that is, the non-integer number of guest molecules to the number of water molecules in the clathrate structure. This unusual fact means that even though the guest molecules are insufficient to define the TCP, the H-bonded water network still remains stable and has FK ordered structure in the form of topological duals. The collective structural stabilization not entirely relied on TCP differs clathrate hydrates from other conventional FK phases, which is one of the unique and beneficial aspect for structural diverse based on clathrate hydrate structures. Nevertheless, from the perspective of topological duality, clathrate hydrate is a valuable platform for structurally probing relations among FK phases, since their diverse crystals appear on the same physical scale, which was previously only considered mathematically (Yarmolyuk-Kripyakevich’s empirical formula for describing FK phases18,19,20). Moreover, H-bond cages have an advantage over the CN polyhedrons when understanding detailed 3D structures, as the connectivity between the former is simpler and more defined than the latter – see a detailed discussion in Supplementary Note 1. We also note that the topological duals of the Type H clathrate hydrate follow the CaCU5 prototype21 in the intermetallic structures (some studies classify it as quasi-FK phase22), which indicates clathrate hydrates may provide more insight into the densely-packed structures, not limited to TCP.
In this work, based on a thorough investigation of the H-bond network of clathrate hydrates, including the three dominant and two relative rare crystals (Type HS-I23,24 and TS-I25, their counterparts in FK are Z and Sigma phases), we propose an alternative way to understand these intricate 3D networks. In addition to unveiling the intrinsic relations and pathways linking these crystals, we further illustrate the richness in structural possibilities of clathrate hydrates. Importantly, given the topological dual relations discussed above, our findings of H-bonded networks of clathrate hydrates can be directly extended to other apparently unrelated materials and kinetic processes in different physical scales.
Results
Basic building blocks
Conventionally, the crystalline clathrate hydrates structures are described by the combination of elementary cages as listed in Supplementary Table S1, mindful that numerical descriptions cannot express the steric connectivities. Through careful deconstruction of the H-bond network of clathrate hydrates, we replaced the well-established elementary cages description to define one common building block that is identified in all crystal structures discussed in this work: 512 cage with two hexagonal rings. As shown in Fig. 2a, the two hexagonal rings lie in the same plane and each share an edge with the 512 cage. The line connecting the center of the hexagonal rings passes through the center of the 512 cage, and it will be called centerline. We summarize three primitive connectivities of this basic building block (BBB) in crystalline clathrate hydrates, as shown in Fig 2c: (PC1) two BBBs are connected via a node in the hexagonal rings (a water molecule) and their centerline are perpendicular; (PC2) BBBs are connected by sharing hexagonal rings, meanwhile their 512 cages merge through pentagonal faces, which leads to an equilateral triangle building block; (PC3) the arrangement of the 512 cage is the same as in PC2, while their centerlines are parallel. Following these three primitive connectivities, other more complex building blocks can be derived to assemble diverse crystalline H-bonded networks. The network extends exclusively following the PC1 forming a cube building block (CBD, Fig. 2d). The 2D tiling of the equilateral triangle building block has six-fold symmetry, which is represented by a rhombic block (R-A, Fig. 2f); similarly, PC3 derives another type of rhombic block (R-B, Fig. 2g). Moreover, the PC2 interlaced in 3D forms a pyramid building block (Fig. 2e)—a detail structure is shown in Supplementary Fig. 4.
All the other elementary cages can be generated via symmetry operations of these building blocks (Supplementary Fig. 5), which means the crystalline network of H-bonded water molecules can be generated from this proposed basic building block. In other words, the diverse crystal structures of clathrate hydrates are geometrically different stacking patterns of one common building block. This interesting fact and the building blocks lead us to discover pathways among different crystals and further unveil other structural complexities. It is noteworthy that “pathways” in this work mean different structures that connect seamlessly in the solid state, not the transformation among structures through local rearrangement of atoms.
Pathways and structure complexity among Type I, HS-I, and TS-I
Type I clathrate hydrates are the most abundant in the Earth’s natural environments1,24,26, and its FK counterpart, the A15 phase, also widely occurs in alloys and soft matter9,27. A unit cell of Type I is composed of two 512 cages and six 51262 cages with cubic \(Pm\overline{3}n\) space group. From the viewpoint of the building blocks, the Type I network can be depicted by the CBD (Fig. 2d). Focusing on the hexagonal rings present on the corner of the CBD, it is clear that their centers are equivalent points that can be generated via three independent translational movements (see Supplementary Fig. 6), thus the CBD satisfies the definition of 3D lattice (unit cell) in space group. As the duplication of CBD unit cells can generate the Type I structure, one may take for granted that this primitive cubic lattice falls into the \(Pm\overline{3}n\) space group, but it is not the case. The CBD cell is an alternative unit cell (AUC) of the Type I structure, and can be obtained by shifting the periodic box of the conventional unit cell (CUC) by half unit cell, that is, scan 0.5–1.5 of the CUC (see Fig. 3a, b and Supplementary Fig. 7). Consequently the three-fold symmetry axes (more exactly, the \(\overline{3}\) axis) along the body diagonals of the CUC, is not along the body diagonals of the AUC, as also shown by the arrangement of the 512 cages (Supplementary Fig. 6e). This renders the symmetry of nodes in the AUC different from that of the CUC, even though the unit cell remains cubic and the unit cell content is unchanged (Supplementary Fig. 7 and Supplementary Table 3). We identify the symmetry of the CBD as tetragonal P42/mmc, a lower symmetry version of the \(Pm\overline{3}n\). Normally, there is no reason to describe Type I (and A15) structure as P42/mmc. However, the 42 screw symmetry explicitly expressed by the CBD cell, together with its cell geometry (arrangement of nodes), opens up pathways for linking different crystals, an insight central but not appreciated prior to this work.
Type HS-I (Z phase) structure is a hexagonal crystal with P6/mmm space group, which unit cell can be established by the stacking of 2D hexagonal lattice (represented by R-A building block). Beside the conventional rhombic cell, the 2D hexagonal lattice can be treated as centered rectangular cell28. This equivalent conversion leads to the orthorhombic AUC of Type HS-I with Cmmm space group (Supplementary Fig. 8 and Supplementary Table 4). The Cmmm returns to the orthogonal coordinate system and it has the same surface with P42/mmc (the face orthogonal to the ac plane, see Fig. 3b, d). Figure 3 illustrates two distinct lattices merged through their AUCs, where the six-fold rotation axes implicit in Cmmm lattice coincides with the 42 screw axes of the P42/mmc lattice. On one side it retains the 42 screw symmetry, while in the opposite side, the axes switch to the six-fold rotation symmetry, and as such, the structural change smoothly occurs without changing the phase. Moreover, considering the FK phases counterparts, A15 and Z phases, this result indicates that despite the structural change that occurs, the TCP identity is still continuous, even at the joints. The coincidence of six-fold and 42 screw axis does not create new symmetry, so the pathway between Types I and HS-I structures cannot be assigned a space group, while it is structurally compatible. In principle, the differences between Types I and HS-I are relatively minor, as they both can be generated through one common building block with just a different type of rotation axis: the six-fold rotation axis builds Type HS-I network while the 42 screw axis sets up the Type I network (Supplementary Fig. 9). Both rotation operations result in a column of 51262 and create a common cross-section, which is the fundamental reason for the structural compatibility between Types I and HS-I.
Type TS-I (P42/mnm, Sigma phase) can be interpreted as another manifestation of the compatibility between Types I and HS-I. As shown in Fig. 4, Type TS-I structure can be tiled with Types I and HS-I. Two different appearances of rhombic prism cells are essentially equivalent, and they can be mutually converted by translating half unit cell along the c direction. The collective shift happens along the rotation axis, so nothing changes in terms of symmetry, just a matter of the choice of the basal plane. The 42 symmetry of P42/mmc clearly illustrates the complex connectivity among these three building blocks, that is, two adjacent surfaces (intersected along the 42 axis) differ by \(\frac{1}{2}\) unit cell along the 42 axis direction. However, following this connectivity, the obtained structure does not just point to Type TS-I, as some combinations may lead to other unexpected ordered structures – quasicrystals, which will be discussed later.
Given that Type TS-I can be understood as a specific mixture of Type I and HS-I, thus, predictably, these three crystals can together build one phase. Including but not limited to the so-called polycrystals, that each crystal has its domain and concatenate together. Figure 5 shows an example captured from our molecular dynamics (MD) simulations to further present the structural complexity that the mixture of Type I, HS-I, and TS-I could manifest. Through different partitions of the local region, traces of the three aforementioned crystals can be recognized in Fig. 5a, and Supplementary Movie 1 shows its nucleation process. Obviously there is no translational symmetry in this cluster, nevertheless, it is improper to classify it as amorphous solid without further analysis. Leaving aside complete unit cells, the Fig. 5a cluster can be considered as the random tessellation of squares and equilateral triangles, which are the 2D substitutions for P42/mmc and half cell of P6/mmm (Fig. 5b, c), respectively. Analogous patterns are found in dodecagonal quasicrystals of alloys29 and soft matter7,10. We further conducted the fast Fourier transform (FFT) along the high-symmetry direction of the captured cluster, which clearly shows 12-fold symmetry and confirms the quasiperiodicity (Fig. 5d). Thus, there is a strong possibility that H-bonded water molecules formed under certain conditions and with certain guest molecules can manifest quasi-periodic order, which is an original concept for clathrate hydrates, the cluster captured in our simulations is the first identified evidence of this possibility. The P42/mmc and half unit cell of P6/mmm as building blocks clearly shows 2D tilings stretching to 3D, and the connectivities among building blocks shown in Fig. 4 are helpful for describing the complex structure in relatively simple terms.
Pathways and structure complexity among Types II, HS-I, and H
The network of Type II structure (\(Fd\overline{3}m\), C15 phase) can be set up exclusively by the pyramid building blocks, connected by sharing one node (a 512 cage), resulting in a cubic crystal symmetry, as shown in Supplementary Figs. 10a,b. The inverted connected pyramid building blocks automatically generates a series of layers of R-A building blocks with p6 symmetry. Interestingly, the inverted connected pyramids means that the six-fold symmetry axes of the upper p6 monolayer coincide with the three-fold symmetry axes of the lower p6 monolayer (see Supplementary Fig. 10). Only the three-fold symmetry survives in this case, and this special offset stacking of 2D hexagonal lattice indicates the cubic Type II can be converted to a trigonal lattice28. We conduct the coordinate system conversion based on the original cubic lattice to obtain the trigonal alternative unit cell with \(R\overline{3}m\) space group. It has two versions, one prismatic cell and one rhombohedral cell: they are equivalent, just different expressions of the three-fold symmetry (Supplementary Fig. 10 and Supplementary Table 5).
The lattice produced by the duplication of the AUC is identical to the one produced by the CUC. Just as one always can find different ways to describe a lattice, it is the nature of symmetry, the difference is the degree of symmetry among these descriptions. It should be noted that the space group and unit cell are just tools for understanding infinite crystal lattices rather than a template or instructions for crystal growth. In reality, crystals are finite and they neither have to build complete unit cells nor have to show the highest symmetry during growth. Indeed, the \(R\overline{3}m\) cannot compare with \(Fd\overline{3}m\) in terms of symmetry, but it clarifies the layered characteristic of the Type II clathrate hydrate network. The immediate implication of this interpretation is that unexpected morphology may be observed during nucleation and crystal growth. In the process of clathrate hydrate growth, typically cubic crystals (Type II) are expected but it is not uncommon to observe hexagonal or trigonal patterns, as a recent experimental work probably captured this phenomenon30.
For a better illustration of structure complexity, we choose the two offset p6 monolayers versions of the unit cell to represent the layered Type II. Types HS-I and H can be constructed by the stacking of the p6 monolayer represented by R-A building blocks as well, so the difference among these three (II, HS-I, H) crystals is the interlayer structures (Fig. 6a–g). Through the same monolayer, these three crystals can alternatively grow in any order. Of course, certain stacking combinations can be crystalline as long as the three-fold or six-fold symmetry is retained. A more intractable scenario is that the layers are stacked in random order or each crystal domain grows random layers. No symmetry would exist in this case and the crystal would not be defined by a lattice constant (d-spacing), that is, no clear diffraction pattern.
Besides the stacking order, the offset orientation also matters. Figure 6h, i illustrates the subtle structural difference when a change in the offset orientation occurs. The p6 monolayer can work as a mirror plane in between two continuous layers, as captured in a cluster from our MD simulation as evidence for such structural complexity (Fig. 6j). This fact reminds us that despite the cubic Type II can be interpreted as a layered structure, only when the offset orientation is consistent across layers, the formed phase possesses the conventional cubic \(Fd\overline{3}m\) symmetry. The possibility of changing offset orientation highlights the layered inter-growth structure complexity into another level, and it also indicates the twinned Type II crystals (p6 monolayer as mirror surface), which expands the possible morphologies one could observe macroscopically31.
Focusing on the 512 cages and hexagonal rings, one can notice a common pattern in the interlayer of Types II and HS-I (gray lines in Fig. 6e, f), which indicates another pathway linking these two structures. A simple geometrical calculation also gives further evidence to this possibility: 9.988 Å/\(\sin 54.{7}^{\circ }\) = 12.2 Å, which is consistent with the d-spacing in Type HS-I, 12.1 Å. Figure 6k illustrates how the Types II and HS-I fuse together through the same arrangement of the interlayer structure, and Fig. 6l,m shows an example captured from our MD simulations. As described in the previous section, a complex H-bond network can be generated by considering the building blocks, this special pathway can be derived from the combination of pyramid building blocks and PC3 building blocks (see detail structure in Supplementary Movie 2). In addition, as discussed in the former section, Type HS-I can transit to Type I. Viewing from the Fig. 6m, its right surface can smoothly transit to AUC of Type I (Supplementary Fig. 11). Type HS-I is a bridge whereby the Types I and II can be linked, which is the rationale for the 51263 cages found in the interface between Types I and II clathrate hydrates in previous studies32,33, however, there is no evidence in the literature that anyone has realized this pathway is made possible via the Type HS-I.
Except for Type H, all the other crystals discussed in this work have counterparts as FK phases. Considering close-packed mode, the topological dual of Type H network corresponds to the CaCu5 prototype in the intermetallic structure, which is considered quasi-FK phases22. Natarajan and Van der Ven34 demonstrated the hexagonal close-packed (HCP) can easily transform to the CaCu5 prototype via one layer’s atoms slight collective displacement. From the viewpoint of topological duals, the pathways from Type H to other clathrate hydrates networks described in this work provide further diverse pathways from HCP to TCP, which is useful for a deeper understanding the structural transition in continuous solid phase of other materials.
Discussion
We report an alternative way to understand clathrate hydrates, that is, diverse crystalline H-bonded networks can be generated through assembling of one common building block. Based on the building blocks proposed in this work, we unveil hidden symmetries contained in clathrate hydrates crystals and intrinsic relations among them. The alternative interpretations of structures not only clarify the richness of pathways linking different crystals, but further derive some unexpected structure complexities, supported by evidence from MD simulations. Results also suggest a continuous nucleation and crystal growth mechanism, that is, one ordered structure could be a seed for another structure to consecutively grow without forming a structurally incompatible interface. Except for the Type H, the H-bonded network of clathrate hydrates discussed in this work are the topological duals of FK phases, including three of their cornerstone structures (A15, C15, Z). In the light of this dual relation, the assembly of building blocks described in this work automatically provides a description of the space-filling of TCP networks. Thus, our results from clathrate hydrates can be directly extrapolated to other TCP ordered materials and detail a rational phase transition mechanisms in the solid state. These results demonstrate the structural richness of clathrate hydrates, which being connected to the Frank–Kasper phases, offer opportunity to apply these same ideas to other order materials. For clathrate hydrates in particular, this opens venues to explore structures that may have never been considered before, providing further diverse options for energy/gas storage. Finally, we argue that the significance of clathrate hydrates research is more than just in the energy areas. Based on the simple and common patterns observed, this class of natural substances contains clues for a deeper understanding of other apparently unrelated materials across different physical scales.
Methods
MD simulation method
Our MD simulations were performed using open-source GROMACS 202035,36. All the simulations started from completely disordered two phases separated configurations with the guest molecules (methane and propane molecules described by OPLS-UA model37) in a nano-bubble surrounded by water molecules (described by TIP4P/ice model38). The system contained 3672 water molecules, 432 methane molecules, and 54 propane molecules. The simulation box considered was a cubic box 5 nm in length. The initial configuration were obtained by melting 3 × 3 × 3 Type II crystal. We performed 20 repeat NPT simulations at 250 K and 1000 bar to capture the nucleation, each 3000 ns long. Briefly, this set of conditions was obtained by performing successive simulations, if nucleation was not observed at a given set of conditions, then the pressure was increased in the following set of simulations; more details of this procedure and simulation parameters can be found in our previous paper39. All of the captured ordered clusters in this work formed spontaneously without any constraints. In total, all simulations conducted during this study required about 4000 h (using 72 CPUs in parallel per simulation) on the High Performance Computing cluster at the Colorado School of Mines.
Analysis
Hydrogen bonds and water cages were analyzed via custom-developed codes in Python. The ordered cluster are captured semi-automatically by looking at trajectory frame by frame and pick up cages manually. The fast Fourier transform is conducted by GIXStapose, an open source Python package, it can be download at, https://github.com/cmelab/GIXStapose. The 2D-FFT image was obtained by projecting the ordered cluster along high-symmetry axes and then applying a fast Fourier transform.
Data availability
The data that support the findings of this study are available from the corresponding author upon request.
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Acknowledgements
Y.C. performed part of this work during his time at the Colorado School of Mines as a visiting scholar. Computational portion of this work was made possible by HPC resources allocations at Mines.
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Y.C. designed the research, performed the simulations and analysis, prepared all visual material, wrote the paper. A.K.S. designed and guided the research, guided the discussions and analysis, wrote the paper. S.T. contributed to the discussions and interpretation, revised paper. All authors reviewed and contributed to the final paper.
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Chen, Y., Takeya, S. & Sum, A.K. Topological dual and extended relations between networks of clathrate hydrates and Frank-Kasper phases. Nat Commun 14, 596 (2023). https://doi.org/10.1038/s41467-023-36242-4
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DOI: https://doi.org/10.1038/s41467-023-36242-4
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