煤细层状低渗透煤层气藏水力压裂治理

Xi Zhang, Bisheng Wu, L. Connell, Yanhui Han, R. Jeffrey
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摘要

本文建立了层状低渗透岩石裂缝发育的裂缝力学模型,并将其应用于煤层气储层水力压裂改造。该模型采用传统的伪三维处理方法,将垂直平面裂缝沿水平方向划分为多个单元。对于每个单元,断裂变形由二维平面应变断裂表示。为了保证数值的稳定性,该模型采用了基于每个单元流体体积增量的优化方法,并且在使用多CPU内核的计算机时,可以并行获得每个单元的解。通过与已有解的比较,验证了该方法的有效性,通过并行计算可以显著提高计算速度。数值算例说明了由于较软的薄煤层与相邻较硬的岩石之间的材料性质差异而导致裂隙几何复杂性的情况。基于与层无关的均匀水平应变假设,计算了各层的局部水平应力。给出了覆盖层应力。当煤受到较小的应力时,煤中的裂缝长度和开口可以比其他层大。这将促进裂缝平面的增长,包括在井筒中没有接受注入流体的煤层。煤的围应力增大会阻碍煤中发育良好的裂隙。在煤层下方存在的低应力岩层中,压裂产生了宽的支撑通道。这些导电通道允许气体和水流入井筒。考虑了应力不确定性,有趣的是,注入压力趋势对局部应力的变化不敏感。在所有情况下,都有一个有利于软煤层生长的过程,这导致注入压力轻微而渐进地增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydraulic Fracturing Treatment of Low-Permeability Coal Seam Gas Reservoirs with Finely Layered Coals
In this paper, a fracture mechanics model that deals with fracture growth in layered low-permeability rocks is presented and applied to hydraulic fracturing stimulation of coal seam gas reservoirs. The model uses the conventional pseudo-3D treatment by which the vertically planar fracture is divided into cells along the horizontal direction. For each cell, the fracture deformation is represented by a 2D plane-strain fracture. To ensure numerical stability, the model uses an optimization method based on the fluid volume increase of each cell and the solutions for each cell can be obtained in parallel when using a computer with multiple CPU cores. The method was verified based on the comparisons with existing solutions and the computational speed can be significantly increased by using parallel computing. Numerical examples are presented to illustrate cases that result in fracture geometrical complexities caused by material properties contrasts between the thin softer coal seams and the adjacent stiffer rocks. The local horizontal stresses in each layer are calculated based on the layer-independent uniform horizontal strain assumption. The overburden stress is given. The fracture length and opening in the coal can be larger than other layers if the coal is subject to a smaller stress. This will promote growth of the fracture plane to include coal seams that do not receive injected fluid at the wellbore. The well developed fracture opening in the coal can be impeded by an increase in the confining stress of the coal. The fracturing produces wide propped channels below the coal seam in the low stress rock that exists there. These conductive channels allow flow of gas and water to the wellbore. The stress uncertainty is considered and interestingly the injection pressure trends are insensitive to the variation of local stresses. There is a process that favors growth in the softer coal seams for all cases, which yields a slight and progressive increase in the injection pressure.
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