H2O: another ice phase and its melting curve

H2O: another ice phase and its melting curve
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H2O:另一种冰相及其融化曲线

DOI:
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发表时间:
2008
期刊:
影响因子:
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通讯作者:
R. Boehler
R. Boehler
中科院分区:
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文献类型:
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作者:
B. Schwager;R. Boehler

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先前测量的H2O在20gpa以上的熔化曲线的巨大差异可以用激光加热的金刚石细胞中的新测量来解释,揭示了从冰VII到新的固相的转变。这种转变很可能在以前的熔化实验中被解释为由于观察到的拉曼或x射线信号的损失而熔化。因此,这个新阶段的结构将难以确定。
The large disagreement in the previously measured melting curves of H2O above 20 GPa may be explained by new measurements in the laser-heated diamond cell, revealing a transition from ice VII to a new solid phase. This transition was most likely interpreted as melting in previous melting experiments due to the observed loss of Raman or X-ray signals. The structure of this new phase will therefore be difficult to indentify.