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Gas slippage and matrix shrinkage effects on permeability of coal.

机译:瓦斯滑移和基体收缩对煤渗透性的影响。

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摘要

The permeability of coal is one of the most important basic parameters in the simulation of gas transport in coalbeds and in the evaluation of the commercial feasibility of coalbed gas reservoirs. However, the permeability of coal and its variation as gas is produced are still not well understood. Unlike that in conventional gas reservoirs, the gas permeability of a coalbed is influenced during gas production, not only by the simultaneous changes in effective stress and gas slippage, but also by the matrix shrinkage associated with gas desorption. The objective of this work was to investigate experimentally the matrix shrinkage and gas slippage effects on the permeability of coal. Since these effects occur simultaneously during gas production, a theory to separate these effects was first developed. This dissertation presents a technique to conduct laboratory experiments to estimate their individual contribution, along with the results obtained for quantitative relationships of the gas slippage and matrix shrinkage effects with gas pressure. The results show that the total permeability of the coal sample increased dramatically due to gas slippage and matrix shrinkage effects with decrease in pressure. When the gas pressure is above 250 psi, the effect of matrix shrinkage dominates. As gas pressure falls below 250 psi, both the gas slippage and matrix shrinkage effects play important role in influencing the permeability. Finally, the change in permeability of coal sample resulting from gas slippage was found to be proportional to the reciprocal of the gas pressure. The change in permeability due to matrix shrinkage was found to be linearly proportional to the volumetric strain associated with desorption. Since the latter is linearly proportional to the amount of gas desorbed, the change in permeability is a linear function of the amount of desorbing gas.
机译:煤的渗透率是煤层气运移模拟和煤层气储层商业可行性评估中最重要的基本参数之一。但是,对煤的渗透性及其随产生的气体的变化仍知之甚少。与常规气藏不同,煤层气的渗透率不仅受有效应力和瓦斯滑移的同时变化影响,而且受与气体脱附有关的基质收缩的影响。这项工作的目的是通过实验研究基质收缩和瓦斯滑移对煤渗透性的影响。由于这些效应在气体生产过程中同时发生,因此首先提出了分离这些效应的理论。本文提出了一种进行实验室实验以估计其个体贡献的技术,以及获得的瓦斯滑移和基体收缩效应与瓦斯压力之间定量关系的结果。结果表明,由于压力降低,瓦斯滑移和基体收缩效应,煤样的总渗透率急剧增加。当气压高于250 psi时,基体收缩的影响占主导。当气体压力降至250 psi以下时,气体滑移和基体收缩效应都在影响渗透率方面起着重要作用。最后,发现由瓦斯滑脱引起的煤样品渗透率的变化与瓦斯压力的倒数成正比。发现由于基质收缩引起的渗透率变化与与解吸有关的体积应变成线性比例关系。由于后者与脱附的气体量成线性比例关系,因此渗透率的变化与脱附的气体量成线性关系。

著录项

  • 作者

    Chen, Guoliang.;

  • 作者单位

    The University of Arizona.;

  • 授予单位 The University of Arizona.;
  • 学科 Mining engineering.;Civil engineering.;Geology.
  • 学位 Ph.D.
  • 年度 1994
  • 页码 153 p.
  • 总页数 153
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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