five

Kaolinite edge surfaces

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Mendeley Data2026-04-09 收录
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Kaolinite is one of the most common minerals found in various soils and sedimentary rocks. Its three-dimensional structure includes a grid of SiO4 tetrahedrons linked to a sheet of AlO4(OH)2 octahedrons. The data presented include structures of the most frequently occurring stable surfaces of kaolinite: (001), (00 -1), (010), (110). Models of these surfaces can be used to study comparative adsorption activity and stability of kaolinite particle edges.
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Rostov State University for Railway Transportation; Novosibirsk State University Faculty of Natural Sciences
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