4.7 Article

High-pressure phase transformation of carbonate malachite Cu2(CO3)(OH)2 driven by [CuO6] regularization and [CO3] rotation

Journal

GEOSCIENCE FRONTIERS
Volume 12, Issue 2, Pages 965-973

Publisher

CHINA UNIV GEOSCIENCES, BEIJING
DOI: 10.1016/j.gsf.2020.07.006

Keywords

X-ray diffraction; Infrared spectroscopy; Hydrogen bond; Carbonates; Phase transformation

Funding

  1. National Key Research and Development Program of China [2018YFA 0702601]
  2. U.S. National Science Foundation [EAR-1555388, EAR-1565708, EAR-1829273]
  3. National Natural Science Foundation of China [41902035, 41490614, 41822202]
  4. China Postdoctoral Science Foundation [2018M640179, 2019T120132]
  5. Department of Energy [DEAC98-06CH10886]
  6. COMPRES under NSF [EAR 11-57758]
  7. CDAC [DE-FC03-03N00144]

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High-pressure synchrotron X-ray diffraction and infrared absorption spectroscopy were used to study the crystal chemistry and phase transitions in [OH]-bearing carbonate malachite Cu-2(CO3)(OH)(2). It was found that malachite is stabilized by a high degree of [CuO6]-octahedron distortion, and external pressure promotes compression and regularization of the octahedron, leading to a phase transformation into rosasite above 6 GPa. The mechanism of phase transformation from malachite to rosasite is different from other carbonates, with the former being driven by compression and rotation/translation under pressure.
High-pressure synchrotron X-ray diffraction and infrared absorption spectroscopy have been employed to study the crystal chemistry and phase transitions in an [OH]-bearing carbonate, malachite Cu-2(CO3)(OH)(2), to determine the effect of [OH] on the stability of carbonate. We found that the crystal structure of malachite is stabilized by a high degree of [CuO6]-octahedron distortion, as is manifested by large variations in Cu-O bond lengths resulting from oxygen atoms that connect to hydrogen at crystallographically different sites. External pressure offsets the effect of hydrogen bond, promotes [CuO6] compression and regularization and accordingly [CO3] rotation. Rotation of [CO3]-triangles, in turn, assists in a conversion in the crystal orientation of the [CuO6] structural unit. During compression to above similar to 6 GPa, malachite begins to turn into the rosasite lattice, accompanied with a jump in density of 3.3%. Rosasite is characterized with a hardened lattice and preserves to the maximum pressure (18.2 GPa) of the present study. Phase transformation mechanism of malachite to rosasite is different from that of carbonates, with the latter being driven by an almost uniform compression of [MO6]-octahedron (M = Ca, Cd, Mn, Fe, Zn, Mg, etc.) and rotation/translation of [CO3]-triangle under pressure.

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