Structure and thermal expansion of natural gas clathrate hydrates

被引:87
|
作者
Takeya, S
Kida, M
Minami, H
Sakagami, H
Hachikubo, A
Takahashi, N
Shoji, H
Soloviev, V
Wallmann, K
Biebow, N
Obzhirov, A
Salomatin, A
Poort, J
机构
[1] Natl Inst Adv Ind Sci & Technol, AIST, Tsukuba, Ibaraki 3058565, Japan
[2] Kitami Inst Technol, Kitami, Hokkaido 0908507, Japan
[3] All Russian Res Inst Geol & Mineral Resources Oce, St Petersburg 190121, Russia
[4] IFM, GEOMAR, Leibniz Inst Marine Sci, D-24148 Kiel, Germany
[5] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany
[6] Russian Acad Sci, Far Eastern Branch, VI Ilichev Pacific Oceanol Inst, Vladivostok 690041, Russia
[7] Univ Ghent, Renard Ctr Marine Geol, B-9000 Ghent, Belgium
基金
俄罗斯基础研究基金会;
关键词
energy; gases; chemical analysis; clathrate hydrate; thermal expansion;
D O I
10.1016/j.ces.2005.11.049
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
We report on the structural properties of natural gas hydrate crystals from the Sea of Okhotsk. Using powder X-ray diffraction (PXRD), it was determined that sediments from four locations contained type I gas hydrate, which encage mostly methane (96-98%) and a small amount of carbon dioxide. For all hydrates, the lattice constant was estimated to be 11.85 angstrom at 113 K, which approximately equals that of pure methane hydrate. The result is in good agreement with the structure of artificially synthesized methane + carbon dioxide mixed-gas hydrates. These results suggest that the lattice constant of the natural gas hydrate does not change due to a change of CO2 gas content. In addition, the thermal expansion of the sampled hydrate was measured for the temperature range of 83-173 K, and the resulting density of the hydrate crystal at 273 K was estimated to be 0.92 g/cm(3). These results are essential for applying natural gas hydrates as an alternative natural fuel resources. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2670 / 2674
页数:5
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