地应力和瓦斯压力作用下煤岩组合裂隙渗透率演化机理的试验研究

IF 1.827 Q2 Earth and Planetary Sciences
Yulin Li, YiXin Zhao
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引用次数: 0

摘要

针对 L 型水平井水力压裂工程和煤层气开发过程中的气体流动问题,进行了单层压裂煤岩组合渗透应力试验。分析了压裂煤岩组合在轴向压缩、约束压缩和瓦斯压力作用下的渗透率演化规律。轴向压缩对断裂煤岩组合的渗透率影响不大,渗透率无明显变化。以 0.25 MPa 瓦斯压力为例,N1 样本的渗透率在 0.004 至 0.005 mD 之间波动,N2 和 N3 样本的渗透率在 0.002 至 0.0035 mD 之间波动。随着约束压缩率的增加,渗透率也随之降低。以 N4 样品为例,当气体压力为 0.50 MPa 时,N4 的渗透率从 0.351 mD 迅速下降到 0.0025 mD。渗透率下降了 99.3%。随着瓦斯压力的增加,压裂煤岩组合的渗透率和应力敏感性逐渐降低。在瓦斯压力加载过程中,由于低压阶段存在瓦斯滑移效应,透气性大大降低。当瓦斯压力超过 1 MPa 时,在滑移效应和速度敏感效应的共同作用下,渗透率几乎没有变化。以 N4 样品为例,当轴向压力和约束压力为 6 MPa 时,渗透率从 1.298 mD 衰减到 0.382 mD,衰减比为 70.6%。最后,原位应力和瓦斯压力下单断裂煤岩组合的渗透率计算模型能够很好地与实验数据相匹配,并明确了各渗透率对整体渗透率的影响。渗透率模型表明,整体渗透率取决于渗透率较小的部分,渗透率较高的部分仅使整体渗透率略有增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Experimental study on the permeability evolution mechanism of fractured coal-rock combination under ground stress and gas pressure

In view of the gas flow problem in the hydraulic fracturing engineering of L-type horizontal well and in the process of gas production in coalbed methane development, the permeability stress test of single fracture coal-rock combination was carried out. The permeability evolution law of fractured coal-rock combination under axial compression, confining compression, and gas pressure is analyzed. The axial compression has little effect on the permeability of coal-rock combination with fractures, and the permeability has no obvious change. Taking 0.25 MPa gas pressure as an example, the permeability of N1 fluctuates between 0.004 and 0.005 mD, and the permeability of N2 and N3 samples fluctuates between 0.002 and 0.0035 mD. With the increase of confining compression, the permeability decreases with the increase of confining compression. Taking the N4 sample as an example, when the gas pressure is 0.50 MPa, the permeability of N4 rapidly decreases from 0.351 to 0.0025 mD. The permeability has decreased by 99.3%. With the increase of gas pressure, the permeability and stress sensitivity of fractured coal-rock combination decrease gradually. In the process of gas pressure loading, the permeability decreases greatly due to the existence of gas slippage effect in the low-pressure stage. When the gas pressure exceeds 1 MPa, the joint action of slip effect and velocity-sensitive effect makes the permeability almost unchanged. Taking the N4 sample as an example, when the axial and confining pressures are 6 MPa, the permeability decays from 1.298 to 0.382 mD, with a decay ratio of 70.6%. Finally, the permeability calculation model of single fracture coal-rock combination under in situ stress and gas pressure can well match the experimental data and clarify the influence of each permeability on the overall permeability. The permeability model shows that the overall permeability depends on the part of the smaller permeability, and the higher permeability only makes the overall permeability increase slightly.

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来源期刊
Arabian Journal of Geosciences
Arabian Journal of Geosciences GEOSCIENCES, MULTIDISCIPLINARY-
自引率
0.00%
发文量
1587
审稿时长
6.7 months
期刊介绍: The Arabian Journal of Geosciences is the official journal of the Saudi Society for Geosciences and publishes peer-reviewed original and review articles on the entire range of Earth Science themes, focused on, but not limited to, those that have regional significance to the Middle East and the Euro-Mediterranean Zone. Key topics therefore include; geology, hydrogeology, earth system science, petroleum sciences, geophysics, seismology and crustal structures, tectonics, sedimentology, palaeontology, metamorphic and igneous petrology, natural hazards, environmental sciences and sustainable development, geoarchaeology, geomorphology, paleo-environment studies, oceanography, atmospheric sciences, GIS and remote sensing, geodesy, mineralogy, volcanology, geochemistry and metallogenesis.
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