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Effect of matrix shrinkage on permeability of coalbed methane reservoirs.

机译:基质收缩对煤层气储层渗透率的影响。

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The dynamic nature of coalbed methane reservoir permeability makes the continuous modeling of the flow process difficult. Knowledge of conventional reservoir modeling is of little value because the gas storage and flow mechanisms in coal are remarkably different. Field observations suggest that the gas productivity does not decline with time as expected. An increasing permeability is a possible explanation. This laboratory study is aimed at measuring the volumetric changes in coal matrix resulting from gas desorption, its impact on coal porosity and permeability, and an estimate of the stage when the effect is significant.; Results using cylindrical samples of coal suggest that coal matrix shrinks with desorption of gas. The shrinkage is linearly proportional to the quantity of gas desorbed. Using the measured changes in matrix volume, variations in total and cleat porosity were estimated and found to increase significantly with desorption. These changes should, therefore, be used as input when simulating long-term gas production.
机译:煤层气储层渗透率的动态性质使得难以对流动过程进行连续建模。常规储层建模的知识意义不大,因为煤中的气体存储和流动机制存在显着差异。现场观察表明,天然气生产率不会随着时间的推移而下降。渗透率增加是可能的解释。该实验室研究旨在测量气体脱附引起的煤基质体积变化,其对煤孔隙度和渗透率的影响以及对影响显着性阶段的估计。使用圆柱状煤样品的结果表明,煤基质随着气体的解吸而收缩。收缩率与脱附的气体量成线性比例关系。使用测得的基质体积变化,可以估算出总孔隙孔隙度和割理孔隙度的变化,发现它们随着解吸而显着增加。因此,这些变化应在模拟长期天然气生产时用作输入。

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