Stability of methane hydrate at high-pressure and high-temperature of up to 40 GPa and 573 K

被引:1
|
作者
Kadobayashi, Hirokazu [1 ,2 ]
Ohfuji, Hiroaki [2 ]
Hirai, Hisako [3 ]
Ohtake, Michika [4 ]
Yamamoto, Yoshitaka [4 ]
机构
[1] Natl Inst Mat Sci, Tsukuba, Ibaraki, Japan
[2] Ehime Univ, Geodynam Res Ctr, Matsuyama, Ehime, Japan
[3] Rissho Univ, Dept Environm Syst, Kumagaya, Saitama, Japan
[4] Natl Inst Adv Ind Sci & Technol, Tsukuba, Ibaraki, Japan
关键词
DISSOCIATION;
D O I
10.1088/1742-6596/1609/1/012007
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
High-pressure and high-temperature experiments were performed to investigate the stability of methane hydrate under 6-40 GPa and 298-573 K using synchrotron X-ray powder diffraction in combination with a diamond anvil cell. The results thus obtained revealed that methane hydrate decomposes into solid methane and ice VII at temperatures considerably lower than the melting curves of solid methane and ice VII in the pressure range of 6-40 GPa.
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页数:5
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