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Matrix Heterogeneity Effects on Gas Transport and Adsorption in Coalbed and Shale Gas Reservoirs

机译:基质非均质性对煤层气和页岩气储层中气体运移和吸附的影响

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In coalbeds and shales, gas transport and storage are important for accurate prediction of production rates and for the consideration of subsurface greenhouse gas sequestration. They involve coupled fluid phenomena in porous medium including viscous flow, diffusive transport, and adsorption. Standard approach to describe gas-matrix interactions is deterministic and neglects the effects of local spatial heterogeneities in porosity and material content of the matrix. In this study, adopting weak-noise and mean-field approximations and using a statistical approach in spectral domain, matrix heterogeneity effects are investigated in the presence of non-equilibrium adsorption with random partition coefficient. It is found that the local heterogeneities can generate non-trivial transport and kinetic effects which retard gas release from the matrix and influence the ultimate gas recovery adversely. Macro-transport shows 1/ [1 + N_(Pe)/(1 + N_(Pe))] dependence on the Peclet number, and persists at the diffusive ultra-low permeability limit. Macro-kinetics is directly related to Thiele modulus by the following expression: N_(Th)/(1 +2N_(Pe)). It leads to trapping of gas in the adsorbed phase during its release from the matrix, and to an adsorption threshold during the gas uptake by the matrix. Both effects are proportional to the initially available adsorbed gas amount and becomes more pronounced with the increasing variance of the porosity field. Consequently, a new upscaled deterministic gas mass balance is proposed for practical purposes. Numerical results are presented showing free and adsorbed gas distributions and fractional gas sorp-tion curves for unipore coal matrix exhibiting Gaussian porosity distribution. This study is a unique approach for our further understanding of the coalbeds and gas shales, and it is important for the development of sound numerical gas production and sequestration models.
机译:在煤层和页岩中,气体的运输和存储对于准确预测生产率以及考虑地下温室气体的固存至关重要。它们涉及多孔介质中的耦合流体现象,包括粘性流,扩散传输和吸附。描述气体-基质相互作用的标准方法是确定性的,并且忽略了局部空间异质性对孔隙率和基质材料含量的影响。在这项研究中,采用弱噪声和均值逼近,并在频谱域中使用统计方法,研究了在存在具有随机分配系数的非平衡吸附的情况下基质异质性的影响。发现局部异质性可产生非平凡的传输和动力学效应,这会延迟气体从基质中的释放并不利地影响最终的气体采收率。宏观传输显示出对Peclet数的1 / [1 + N_(Pe)/(1 + N_(Pe))]依赖性,并在扩散超低磁导率极限处持续存在。宏观动力学通过以下表达式与Thiele模量直接相关:N_(Th)/(1 + 2N_(Pe))。它导致气体从基质中释放时被吸附相中的气体捕获,并导致基质吸收气体时的吸附阈值。两种影响都与初始可用的吸附气体量成正比,并且随着孔隙率变化的增加而变得更加明显。因此,出于实用目的,提出了一种新的按比例确定的气体质量平衡。给出了数值结果,显示了具有高斯孔隙率分布的单孔煤基质的自由气体和吸附气体分布以及分数气体吸附曲线。这项研究是我们进一步了解煤层气和页岩气的独特方法,对于开发合理的数值天然气生产和固存模型非常重要。

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