方解石
文石
结晶学
单斜晶系
八面体
晶体结构
亚稳态
衍射
材料科学
粉末衍射
矿物学
地质学
化学
物理
光学
有机化学
作者
Joseph R. Smyth,Thomas J. Ahrens
摘要
The crystal structure of calcite III has been deduced from existing high pressure powder X‐ray diffraction patterns, based on the assumption that it is a displacive modification of the calcite I structure. The structure is monoclinic with space group C2 and a Z of 6. There are two Ca and two C positions, and five O positions, and atom coordinates have been refined by distance‐least‐squares methods to give reasonable octahedral coordination for Ca and parallel, planar CO 3 groups. Unit cell parameters refined from a published powder diffraction pattern at 4.1 GPa are: a = 8.746(8)Å; b = 4.685(5)Å; c = 8.275(8)Å; and β= 94.4°. The structure has a calculated density of 2.949 Mg/m³ at 4.1 GPa which is less than that of aragonite at this pressure and consistent with early piston cylinder studies. This implies that calcite III is indeed a metastable intermediary between calcite I and aragonite.
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