压缩性
环境压力
化学
静水压力
体积模量
各向异性
衍射
氢键
高压
压缩(物理)
氢
结晶学
热力学
材料科学
复合材料
物理
分子
有机化学
光学
量子力学
作者
Asami Sano–Furukawa,Hiroyuki Kagi,Takaya Nagai,Satoshi Nakano,Satoshi Fukura,Daichi Ushijima,Riko Iizuka,Eiji Ohtani,T. Yagi
出处
期刊:American Mineralogist
[Mineralogical Society of America]
日期:2009-08-01
卷期号:94 (8-9): 1255-1261
被引量:82
摘要
The compression behaviors of δ-AlOOH and δ-AlOOD were investigated under quasi-hydrostatic conditions at pressures up to 63.5 and 34.9 GPa, respectively, using results from synchrotron X-ray diffraction experiments conducted at ambient temperature. Because of the geometric isotope effect, at ambient pressure, the a and b axes of δ-AlOOD, which define the plane in which the hydrogen bond lies, are longer than those of δ-AOOH. Under increasing pressure, the a and b axes of δ-AlOOH stiffen at 10 GPa, although the c axis shows no marked change. Identical behavior was found in δ-AlOOD, but the change in compressibility was observed at a slightly higher pressure of 12 GPa. Axial ratios a/c and b/c first decrease rapidly with increasing pressure, then begin to increase at pressures >10 GPa in δ-AlOOH and >12 GPa in δ-AlOOD. At these pressures, the pressure dependence of a/b also changes from increasing to decreasing. The unit-cell volumes of δ-AlOOH and δ-AlOOD become slightly less compressible at high pressures. Assuming K0′ = 4, the calculated bulk moduli of δ-AlOOH below and above 10 GPa are 152(2) and 219(3) GPa, respectively. Those of δ-AlOOD below and above 12 GPa are 151(1) and 207(2) GPa, respectively.
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