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High pressure elasticity and phase transformation in brucite, Mg(OH)2
Authors:K P Jayachandran  Lin-gun Liu
Institution:(1) Institute of Earth Sciences, Academia Sinica, Nankang, Taipei, 11529, Taiwan, ROC;(2) Present address: Centro de Projecto Mecanico, IDMEC–Instituto de Engenharia Mecanica, Pólo IST, Av. RoviscoPais, 1, 1049-001 Lisbon, Portugal
Abstract:The first pressure derivatives of the second-order elastic constants $${\rm d}C^{\prime}_{IJ}/{\rm d}p$$ have been calculated for brucite, Mg(OH)2 from the second- and third-order elastic constants. The deformation theory and finite strain elasticity theory have been used to obtain the second- and third-order elastic constants of Mg(OH)2 from the strain energy of the lattice. The strain energy ϕ is calculated by taking into account the interactions up to third nearest neighbors in the Mg(OH)2 lattice. ϕ is then compared with the strain dependent lattice energy from continuum model approximation to obtain the expressions of elastic constants. The complete set of six second-order elastic constants C IJ of brucite exhibits large anisotropy. Since C 33 (= 21.6 GPa), which corresponds to the strength of the material along the c-axis direction, is less than the longitudinal mode C 11 (= 156.7 GPa), the interlayer binding forces are weaker than the binding forces along the basal plane of Mg(OH)2. The 14 nonvanishing components of the third-order elastic constants, C IJK , of brucite have been obtained. All the C IJK of brucite are negative except the values of C 114 (= 230.36 GPa), C 124 (= 75.45 GPa) and C 134 (= 36.98 GPa). The absolute values of the C IJK are, in general, one order of magnitude greater than the C IJ ’s in the Mg(OH)2 system as usually expected for a crystalline material. To our knowledge, no previous data are available to compare the pressure derivatives of brucite. The pressure derivatives of the two components viz., C 14 and C 33 become negative $$({\rm d}C^{\prime}_{14}/dp = -1.51{\rm and}{\rm d}C^{\prime}_{33}/{\rm d}p= -1.41)$$ indicating an elastic instability in brucite while under pressure. This may be related to the phase transition of brucite largely involving rearrangements of H atoms revealed in the Raman spectroscopic, powder neutron diffraction and synchrotron X-ray diffraction studies.
Keywords:Brucite  Elastic properties  Phase transition  High pressure
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