砂岩-煤互层近井裂缝起裂机理数值模拟与实验研究

Liming Wan, Mian Chen, Fengshou Zhang, Li Wang, Wangang Chen
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引用次数: 1

摘要

随着非常规油气资源的开发,煤系混采技术的研究日益深入,这就要求我们对多层井筒附近裂缝有更深入的认识。以往的研究主要集中在单层裂缝形态上,缺乏微裂缝扩展的三维演化作用,因此本文对煤层多层裂缝几何形态及近井微裂缝起裂进行了研究。本研究基于XSite模拟器,采用三维点阵模型模拟多层煤井筒附近三维动态水力裂缝形态,重点研究螺旋射孔位置。为了验证数值模拟的正确性,采用真三轴试验体系对煤、砂岩和灰岩露头组合进行了压裂模拟实验。改变射孔位置,分析井筒附近的裂缝形态。此外,利用三维扫描技术和压裂曲线对裂缝特征进行了研究。研究了不同射孔位置井筒附近的裂缝形态。数值模拟结果表明,螺旋射孔微裂缝演化过程可分为3个阶段:(a)第一阶段:垂直微裂缝带沿射孔发育;(b)阶段2:井筒周围形成微环空裂缝;(c)阶段3:裂缝沿垂直于最小地应力的射孔突破。煤层射孔时裂隙起裂形态主要由理缝和天然裂缝决定。次生分支裂缝和阶梯式裂缝是煤的主要特征。砂岩是煤层在压裂过程中良好的阻隔层,煤中的裂隙容易冲破灰岩层。煤层起裂时,井筒附近裂缝复杂,次生裂缝较多,裂缝表面粗糙,连续性差;在砂岩层和煤层同时起裂时,主裂缝在煤层中发育较快,井筒附近形成光滑的裂缝面。室内实验结果与数值模拟结果吻合较好。近井微裂缝的三维演化作用有助于深入了解煤近井区裂缝的复杂性。实验考虑了实际地层组合,多层压裂的结果对煤系地层混叠时的现场射孔优化具有很好的指导作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Numerical Simulation and Experimental Study of Near-Wellbore Fracture Initiation Mechanism on Sandstone Coal Interbedding
With the development of unconventional oil and gas resources, the technology of commingling production in coal measure has been studied, which requires us to have a better understanding of the fracture near the wellbore in multi-layers. Previous studies mainly focused on the fracture morphology in a single layer and lack of 3D evolution role of microfracture propagation, so the fracture geometry in multi-layers of the coal seam and microfracture initiation near wellbore were studied in this paper. In this study, the 3D-lattice model was used to simulate the 3D dynamic hydraulic fracture morphology near the wellbore in multi-layered coal based on XSite simulator, and the spiral perforation position was mainly studied. To verify the numerical simulation, the true tri-axial test system was implied for fracturing simulation experiments on the combination of coal, sandstone and limestone outcrops. The perforation position was changed to analyze the fracture morphology near the wellbore. Besides, the 3D scanning technology and the fracturing curve were used to study the fracture characters. As a result, the fracture morphologies near the wellbore in different perforation positions were studied. The numerical simulation results showed that the microfracture evolution process in spiral perforation can be divided into three stages, (a) Stage 1: the vertical microfracture bands develop along the perforation hole; (b) stage 2: micro-annulus fracture forms around the wellbore; (c) stage 3: fractures break through along the perforation holes perpendicular to the minimum in-situ stress. The cleats and the natural fractures dominated the fracture initiation geometry when perforating in coal. The secondary branch fractures and the stepped fractures were the main characters in coal. Sandstone was a good barrier layer for the coal seam in fracturing, and the fracture in coal was easy to break through the limestone layer. When fracture initiated in coal layer, the fracture near the wellbore was complex with many secondary fractures, and the fracture surface was rough with poor continuity; when initiated in both sandstone and coal layers simultaneously, the main fracture developed quickly in coal and the smooth fracture surface formed near the wellbore. The results of laboratory experiments were in good agreement with numerical simulation. The 3D evolution role of microfracture near wellbore could give a deep understanding of fracture complexity in near-wellbore area in coal. The experiments considered the actual formation combination, and the results of multi-layer fracturing could give a good guidance for field perforation optimization in the commingling of coal measure strata.
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