海水
覆盖层
渗透(HVAC)
座舱增压
水合物
沉积物
笼状水合物
海床
地质学
孔隙水压力
环境科学
岩土工程
化学
海洋学
地貌学
材料科学
有机化学
复合材料
作者
Yingrui Ma,Shuaishuai Nie,Xiuping Zhong,Xitong Li,Kunyan Liu,Chen Chen,Zhenhui Zhao
标识
DOI:10.1080/10916466.2023.2231026
摘要
The overburden of marine hydrate sediment is usually a permeable cover, and the presence of permeable overburden directly affects the depressurization effect. However, previous studies have mainly focused on the effect of the permeable overburden without considering seawater infiltration, and the influence of seawater infiltration on the production of hydrate cannot be ignored. In this article, a new numerical model considering seawater infiltration is developed and this study is completed by numerical simulation. The results show that seawater infiltration significantly reduces hydrate dissociation, and the presence of seawater substantially reduces cumulative gas production and increases water production compared to non-permeable overburden, with higher permeability resulting in lower gas production and higher water production. It is an effective means to extract hydrates through lower bottom-hole pressure by increasing the gas–water ratio. It is of great significance to further understand the production characteristics of hydrate reservoirs.
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