Transformations in methane hydrates

被引:170
作者
Chou, IM [1 ]
Sharma, A
Burruss, RC
Shu, JF
Mao, HK
Hemley, RJ
Goncharov, AF
Stern, LA
Kirby, SH
机构
[1] US Geol Survey, Natl Ctr 954, Reston, VA 20192 USA
[2] US Geol Survey, Natl Ctr 956, Reston, VA 20192 USA
[3] Carnegie Inst Washington, Geophys Lab, Washington, DC 20015 USA
[4] Carnegie Inst Washington, Ctr High Pressure Res, Washington, DC 20015 USA
[5] US Geol Survey, Menlo Park, CA 94025 USA
关键词
D O I
10.1073/pnas.250466497
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Detailed study of pure methane hydrate in a diamond cell with in situ optical, Raman, and x-ray microprobe techniques reveals two previously unknown structures, structure II and structure H, at high pressures. The structure Il methane hydrate at 250 MPa has a cubic unit cell of a = 17.158(2) Angstrom and volume V = 5051.3(13) Angstrom (3); structure H at 600 MPa has a hexagonal unit cell of a = 11.980(2) A, c = 9.992(3) Angstrom, and V = 1241.9(5) Angstrom (3). The compositions of these two investigated phases are still not known. With the effects of pressure and the presence of other gases in the structure, the structure Ii phase is likely to dominate over the known structure I methane hydrate within deep hydrate-bearing sediments underlying continental margins.
引用
收藏
页码:13484 / 13487
页数:4
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