不同温度下煤层气多尺度动态渗透率的内外膨胀机制

Zhiqiang Li, Xiaoqiang Hao, Yanwei Liu, Lin Li
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引用次数: 1

摘要

煤中多尺度的微米-纳米孔隙会导致煤的超低渗透性,从而限制了瓦斯提取的效率。传统的防渗措施很难影响煤基质中的纳米孔隙。热刺激可以深入煤基质中的微米-纳米孔隙,以提高渗透率。因此,研究多尺度微纳孔在不同温度下的扩散率和渗透率具有重要意义。在本研究中,用GRI(气体研究所)和稳态方法测量了圆柱形煤在不同温度和压力下的扩散渗流实验。实验结果表明,圆柱形煤的表观扩散系数不是恒定的,而是动态变化的;经典的扩散模型不能准确地描述气体流动的全时过程。在此基础上,提出了一种能够准确描述全时渗流过程的多尺度动态表观扩散渗流模型。观察到,在没有应力加载的情况下,表观渗透率随时间动态衰减,初始表观渗透率和衰减系数随温度升高单调增加。在应力约束下,稳态渗透率随着温度的升高在降低后增加,呈现“U”型模式。在没有应力约束的情况下,温度的升高导致外部多尺度孔隙不同程度地向外膨胀,从而增加渗透率,而内部微纳孔隙则表现出三种向内和向外膨胀的机制。在应力约束下,在低温和高有效应力下,温度的升高导致孔隙向内膨胀,渗透率相应降低。当温度继续升高时,由于有效应力被热应力抵消,煤向外膨胀,导致渗透率增加。本研究对热采气工程具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

The mechanism of inward and outward expansion of multiscale dynamic permeability of coalbed methane at different temperatures

The mechanism of inward and outward expansion of multiscale dynamic permeability of coalbed methane at different temperatures

The multiscale micro-nano pores in coal can result in the ultra-low permeability of coal, which restricts the efficiency of gas extraction. It is difficult for the conventional seepage-enhancement measures to affect the nanoscale pores within the coal matrix. Thermal stimulation can reach deep into the micro-nano pores within coal matrix to improve the permeability. Therefore, it is important to study the diffusivity and permeability of the multiscale micro-nano pores at different temperatures. In this study, the experiments of diffusion-seepage measured by the methods of GRI (Gas Research Institution) and steady-state were conducted using a cylindrical coal at different temperatures and pressures. The experimental results show that the apparent diffusion coefficient of cylindrical coal is not constant but variable dynamically; and the classical diffusion model fails to describe the full-time process of gas flow accurately. On this basis, a model of multiscale dynamic apparent diffusion-seepage that can accurately describe the full-time flow process was proposed. As is observed, the apparent permeability attenuates dynamically with time without stress loading, and the initial apparent permeability and the attenuation coefficient increase monotonically with the rise of temperature. Under the stress constraint, the steady-state permeability increases after a decrease as the temperature rises, displaying a “U-shaped” pattern. Without stress constraint, the increasing temperature causes the exterior multiscale pores to expand outward by different degrees so as to increase permeability, while the interior micro-nano pores show three inward and outward expansion mechanisms. Under stress constraint, at low temperature and high effective stress, the increasing temperature causes pores to expand inward and the permeability decreases accordingly. When temperature continues to increase, coal expands outward because the effective stress is counteracted by the thermal stress, leading to an increase in permeability. This study is of significance for thermal gas extraction engineering.

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