沈虎地区含水合物沉积物减压产气数值模拟:负荷渗透率的影响

Jiaxin Sun , Fulong Ning , Shi Li , Ke Zhang , Tianle Liu , Ling Zhang , Guosheng Jiang , Nengyou Wu
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引用次数: 72

摘要

自20世纪90年代以来,人们一直在研究天然气水合物作为一种潜在的商业生产天然气资源。基于南海神虎海域的最新资料,通过选择有利于井眼稳定性和产气的射孔段,建立了一个实用的二维模型,研究了交替地层的产气潜力和不同物性的分布。重点讨论了上覆岩和下覆岩渗透率对产气的影响。模拟结果表明,初始水合物解离主要发生在上部高渗透率含水合物沉积物中,后期主要分布在下部低渗透率含水合物沉积物中。此外,在中间储层可以观察到明显的水合物再生成,并且底部低渗透储层的稀释效应强于上部高渗透储层。对比研究表明,神虎地区只有一种可渗透岩层(上覆或下覆)的GHBS并不是最有希望的降压目标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Numerical simulation of gas production from hydrate-bearing sediments in the Shenhu area by depressurising: The effect of burden permeability

Natural gas hydrates have been investigated as a potential resource for commercially producing gas since the 1990s. Based on the latest available data for the Shenhu area of the South China Sea (SH7), a practical two-dimensional model has been constructed to investigate the gas production potential and the distributions of different physical properties in alternating formations by selecting a proper perforated interval favouring borehole stability and gas production. The effects of overburden and underburden permeability on gas production are intensively discussed. The simulation results indicate that the initial hydrate dissociation mainly occurs among the upper gas hydrate bearing-sediments (GHBS) with a high permeability but that in the later period, it is mainly distributed among the bottom low permeability GHBS. In addition, an obvious hydrate re-formation can be observed in the middle GHBS, and the dilution effect in the bottom low permeability GHBS is stronger than that in the upper space with high permeability. A comparative study showed that the GHBS in the Shenhu area with only one permeable burden (overburden or underburden) is not the most promising target for depressurisation.

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