Fracture permeability and relative permeability of coal and their dependence on stress conditions

Dennis Arun Alexis , Zuleima T. Karpyn , Turgay Ertekin , Dustin Crandall
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引用次数: 29

Abstract

Determination of petro-physical properties of coal bed methane (CBM) reservoirs is essential in evaluating a potential prospect for commercial exploitation. In particular, permeability of coal and relative permeability of coal to gas and water directly impact the amount of hydrocarbons that can be ultimately recovered. Due to the complex and heterogeneous nature of coal seams, proper relative permeability relationships are needed to accurately describe the transport characteristics of coal for reservoir modeling and production forecasting. In this work, absolute and relative permeability of different coal samples were determined experimentally under steady-state flowing conditions. Multiphase flow tests were conducted using brine, helium and carbon dioxide as the flowing phases under different magnitudes of confining and pore pressures. Results indicate that effective stress (confining pressure – average pore pressure) has a significant effect on both absolute and relative permeability of coal. With increases in effective stresses, the absolute permeability decreases. Effective permeability and relative permeability, as well as the cross over point and the width of the mobile two-phase region decrease as the effective stress increases. In addition, the mobile range of gas and water in the coal samples investigated corresponds with water saturations above 50%, irrespective of the base absolute permeability of the sample. In brine–carbon dioxide two-phase flow experiments, the effect of carbon dioxide adsorption was observed as effective permeabilities decreased in comparison to the helium–brine permeabilities at the same flowing ratios. As a result, relative permeability characteristics of CBM systems were found to be insufficiently represented as sole functions of fluid saturation. Field scale simulations of primary recovery from CBM systems using variable, stress-dependent relative permeabilities, showed a significant decrease in cumulative gas recovered. A multi-dimensional correlation between relative permeability, fluid saturation and specific surface area of the cleat network is proposed as a continuation from this work in order to account for stress-related changes in cleat network connectivity.

煤的裂隙渗透率和相对渗透率及其对应力条件的依赖性
确定煤层气储层的岩石物性是评价潜在商业开发前景的关键。特别是煤的渗透率以及煤对气和水的相对渗透率直接影响到最终可采出的碳氢化合物的数量。由于煤层的复杂性和非均质性,在储层建模和产量预测中需要适当的相对渗透率关系来准确描述煤的输运特征。在稳态流动条件下,实验测定了不同煤样的绝对渗透率和相对渗透率。在不同围压和孔隙压力下,以盐水、氦气和二氧化碳为流动相进行了多相流动试验。结果表明,有效应力(围压-平均孔隙压力)对煤的绝对渗透率和相对渗透率均有显著影响。随着有效应力的增大,绝对渗透率减小。随着有效应力的增大,有效渗透率和相对渗透率以及可动两相区的交叉点和宽度均减小。此外,无论样品的基本绝对渗透率如何,所研究的煤样中气体和水的移动范围对应于50%以上的水饱和度。在盐水-二氧化碳两相流实验中,与相同流动比下的氦-盐水渗透率相比,二氧化碳吸附的效果是有效渗透率降低。因此,煤层气系统的相对渗透率特征不能充分表征为流体饱和度的唯一函数。利用可变的、与压力相关的相对渗透率,对煤层气系统进行了一次采收率的现场规模模拟,结果显示,累计采收率显著降低。作为这项工作的延续,研究人员提出了相对渗透率、流体饱和度和净网比表面积之间的多维相关性,以解释净网连通性中与应力相关的变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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