多孔地层含水合物区域热冲击下天然气水合物分解过程的数值研究

IF 0.1 Q4 MATHEMATICS, APPLIED
N. Musakaev, D. S. Belskikh
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引用次数: 1

摘要

提出了一个二维近似描述热影响(储层上界温度升高)对初始状态下含甲烷及其水合物的多孔介质区域的数学模型。该区域的边界对天然气水合物(气和水)的分解产物是不渗透的。考虑了多孔介质中气体的实际情况以及气体和水在多孔介质中运动时的非等温效应。假定甲烷水合物的分解处于平衡状态。考虑甲烷水合物在多孔介质中的解离,对非等温过滤流动进行了数值研究。结果表明,在热冲击作用下,相变呈现出正面模式。随着地层上边界温度和初始渗透率的升高,水合物饱和度的降低,含天然气水合物分解产物的区域也随之增大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Numerical Study of the Process of Gas Hydrate Decomposition under the Thermal Impact on the Hydrate-Containing Region of a Porous Formation
A mathematical model that describes, in a two-dimensional approximation, the thermal impact (a temperature increase at the upper boundary of the reservoir) on the region of the porous medium containing methane and its hydrate in the initial state is proposed. The boundaries of the region are impermeable to decomposition products of the gas hydrate (gas and wa-ter). The gas reality and the non-isothermal effects during the movement of gas and water in the porous medium are considered. The methane hydrate decomposition is assumed to be in equilibrium. A numerical study of non-isothermal filtration flow is performed considering the dissociation of methane gas hydrate in the porous medium. The obtained results show that a frontal mode of phase transitions is observed under the thermal impact. The region containing the products of gas hydrate decomposition grows along with the increase in the values of temperature at the upper boundary of the formation and its initial permeability, as well as with the decrease in the hydrate saturation.
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来源期刊
CiteScore
0.60
自引率
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审稿时长
17 weeks
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