在饱和甲烷和水的多孔介质中注入液态二氧化硫时二氧化硫氢氧化物的形成

M. Khasanov, S. R. Kildibaeva
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引用次数: 1

摘要

建立了液体二氧化硫注入饱和水-甲烷多孔介质并在锋面形成SO2气体水合物的数学模型。探讨了二氧化硫水合物形成锋的温度和坐标与注入压力和地层初始压力的关系。在足够高的注入压力值和层初温度以及较低的层初压力下,二氧化硫天然气水合物形成边界上的多孔介质温度可能高于二氧化硫天然气水合物分解平衡温度。这相当于在饱和了水、二氧化硫及其气体水合物的混合物的多孔介质中出现一个处于相平衡状态的区域。建立了液体二氧化硫注入饱和水-甲烷多孔介质并在锋面形成SO2气体水合物的数学模型。探讨了二氧化硫水合物形成锋的温度和坐标与注入压力和地层初始压力的关系。在足够高的注入压力值和层初温度以及较低的层初压力下,二氧化硫天然气水合物形成边界上的多孔介质温度可能高于二氧化硫天然气水合物分解平衡温度。这相当于在饱和了水、二氧化硫及其气体水合物的混合物的多孔介质中出现一个处于相平衡状态的区域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Formation of gas hydroxide of sulfur dioxide at liquid sulfur dioxide injection in a porous medium saturated with methane and water
A mathematical model of injection of liquid sulfur dioxide into a porous medium saturated with water and methane, accompanied by the formation of SO2 gas hydrate on the frontal surface is presented. The dependences of the temperature and the coordinates for the formation front of sulfur dioxide gas hydrate on the pressure of the injection and the initial pressure of the layer are explored. It is established that at sufficiently high injection pressure values and the initial temperature of the layer, as well as the low values of the layer’s initial pressure, the temperature of the porous medium on the boundary of gas hydrate formation of sulfur dioxide may rise above the decomposition’s equilibrium temperature of the gas hydrate of sulfur dioxide. This corresponds to the appearance of a zone in a porous medium saturated with a mixture of water, sulfur dioxide and its gas hydrate, being in a state of phase equilibrium.A mathematical model of injection of liquid sulfur dioxide into a porous medium saturated with water and methane, accompanied by the formation of SO2 gas hydrate on the frontal surface is presented. The dependences of the temperature and the coordinates for the formation front of sulfur dioxide gas hydrate on the pressure of the injection and the initial pressure of the layer are explored. It is established that at sufficiently high injection pressure values and the initial temperature of the layer, as well as the low values of the layer’s initial pressure, the temperature of the porous medium on the boundary of gas hydrate formation of sulfur dioxide may rise above the decomposition’s equilibrium temperature of the gas hydrate of sulfur dioxide. This corresponds to the appearance of a zone in a porous medium saturated with a mixture of water, sulfur dioxide and its gas hydrate, being in a state of phase equilibrium.
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