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Influence of global climate change on stability of gas hydrate in permafrost of Qinghai-Tibet Plateau

机译:全球气候变化对青藏高原多年冻土天然气水合物稳定性的影响

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摘要

The Qinghai-Tibet Plateau has the largest distribution of permafrost region in China. The Meso-Cenozoic marine strata and marine and terrestrial basins are well developed, which provides good conditions for the formation and accumulations of the natural gas hydrate on the plateau. The article forecasts the stability of the Qinghai-Tibet Plateau permafrost hydrate based on a 0.04 ℃/a temperature increasing according to the character of Qinghai-Tibet Plateau permafrost morbid leucorrhoea hydrate and the global warming situation. The results demonstrate that the greenhouse effect causes the temperature to change and the change of the permafrost layer section plane pressure condition will affect the distribution and the stability of the hydrate directly, thus it has a severe influence on the global environment.
机译:青藏高原是中国多年冻土地区分布最大的地区。中新生代海相地层,海相和陆相盆地发育良好,为高原天然气水合物的形成和聚集提供了良好条件。根据青藏高原多年冻土病态白带水合物的特征和温度升高0.04℃/ a的温度,预测青藏高原多年冻土水合物的稳定性。结果表明,温室效应导致温度变化,多年冻土层断面压力条件的变化将直接影响水合物的分布和稳定性,从而对全球环境产生严重影响。

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