CO2 clathrate formation and its properties in a simulated deep ocean
CO2 clathrate formation and its properties in a simulated deep ocean
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模拟深海中 CO2 包合物的形成及其特性
DOI：
10.1016/0196-8904(93)90057-h
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发表时间：
1993
影响因子：
10.4
通讯作者：
M. Morishita
中科院分区：
文献类型：
--
作者：
H. Kimuro;Fumihiko Yamaguchi;Kiyohito Ohtsubo;T. Kusayanagi;M. Morishita
研究了以下两个课题：（1）假设日本附近海洋的相应深度-温度剖面，在700米和1，000米的海洋深处形成CO[sub 2]笼形水合物的条件是否有利。(2)液态CO[sub 2]对周围海水中3，000 m深处海洋环境的影响。测试结果得出以下结论：在对马海流和Oashio区域，在700 m和1,000 m深处容易形成CO[sub 2]笼形水合物，而在黑潮区域，由于水温略高，形成困难;在3,000 m深处，溶解到海水中的CO[sub 2]量与其注入速度成正比;澄清了形成CO[sub 2]笼形水合物所需的条件。参考文献3篇，图3，3个标签。
The following two topics were examined: (1) The conduciveness of conditions for the formation of CO[sub 2] clathrate hydrate at ocean depths of 700 m and 1,000 m with assumption of corresponding depth-temperature profile of the ocean near Japan. (2) The effect of liquid CO[sub 2] on an ocean environment at a depth of 3,000 m in ambient sea water. Test results concluded that: while the CO[sub 2] clathrate hydrate would form easily at the depths of 700 m and 1,000 m in the Tsushima ocean current and Oashio region, it would be difficult in the Kuroshio region due to a slightly higher water temperature; the amount of CO[sub 2] dissolved into sea water at a depth of 3,000 m is proportional to its velocity of injection; the conditions required for the formation of CO[sub 2] clathrate hydrate were clarified. 3 refs., 3 figs., 3 tabs.