Hydrogen bonding and structural complexity of the Cu3(AsO4)(OH)3 polymorphs (clinoclase, gilmarite): a theoretical study

被引:13
|
作者
Krivovichev, Sergey V. [1 ]
机构
[1] St Petersburg State Univ, Inst Earth Sci, Dept Crystallog, Univ Emb 7-9, St Petersburg 199034, Russia
基金
俄罗斯科学基金会;
关键词
hydrogen bonding; clinoclase; gilmarite; density functional theory; structural complexity; metastability; ARSENATE MINERALS OLIVENITE; TOLBACHIK VOLCANO; CRYSTAL-STRUCTURES; KAMCHATKA; FUMAROLE; CORNWALLITE; CORNUBITE; JACHYMOV;
D O I
10.3190/jgeosci.231
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Density functional theory (DFT) is used to determine positions of H atoms and to investigate hydrogen bonding in the crystal structures of two polymorphs of Cu-3(AsO4)(OH)(3) : clinoclase and gilmarite. Hydrogen bonds in clinoclase involve interactions between hydroxyl groups and O atoms of arsenate tetrahedra, whereas the crystal structure of gilmarite features OH. OH bonding, which is rather uncommon in copper hydroxy-oxysalts. Information-based parameters of structural complexity for clinoclase and gilmarite show that the former is more complex (I-G,I-total = 213.212 bits/cell) than the latter (I-G,I-total = 53.303 bits/cell), which indirectly points out that gilmarite is metastable. This suggestion is supported by the lower density of gilmarite (4.264 g/cm(3)) compared to that of clinoclase (4.397 g/cm(3)). The hypothesis of metastable character of gilmarite is in agreement with the Goldsmith's simplexity principle and the Ostwald-Volmer rule.
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页码:79 / 85
页数:7
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