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Crystal structure of potassium chloride monohydrate: water intercalation into the B1 structure of KCl under high pressure

A new hydrate form of potassium chloride, KCl·H(2)O, is identified for the first time by in situ single-crystal X-ray diffraction under high pressure. It has a monoclinic structure with lattice parameters of a = 5.687 (7), b = 6.3969 (3), c = 8.447 (3) Å and β = 107.08 (8)° at 2.23 (4) GPa and 295 K...

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Detalles Bibliográficos
Autores principales: Yamashita, Keishiro, Komatsu, Kazuki, Kagi, Hiroyuki
Formato: Online Artículo Texto
Lenguaje:English
Publicado: International Union of Crystallography 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9720884/
https://www.ncbi.nlm.nih.gov/pubmed/36468558
http://dx.doi.org/10.1107/S2053229622011135
Descripción
Sumario:A new hydrate form of potassium chloride, KCl·H(2)O, is identified for the first time by in situ single-crystal X-ray diffraction under high pressure. It has a monoclinic structure with lattice parameters of a = 5.687 (7), b = 6.3969 (3), c = 8.447 (3) Å and β = 107.08 (8)° at 2.23 (4) GPa and 295 K. The structure of this hydrate has K—Cl alignments similar to the B1 phase of anhydrous KCl, while water molecules intercalate among the ionic species. The coordination structures of the K and Cl atoms can be regarded as the intermediate states between the B1 and B2 phases of KCl. This finding provides a perspective on the structural interpretation of multicomponent materials and an additional candidate for bound water in salt–water systems under high pressure, such as inside of icy bodies.