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Experimental analysis of multiple factors on hydraulic fracturing in coalbed methane reservoirs

机译:煤层气储层水力压裂多因素试验分析

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摘要

Hydraulic fracturing can improve the permeability of coalbed methane (CBM) reservoirs effectively, which is of great significance to the commercial production of CBM. However, the efficiency of hydraulic fracturing is affected by multiple factors. The mechanism of fracture initiation, morphology and propagation in CBM reservoirs is not clear and need to be further explored. Hydraulic fracturing experiment is an accurate tool to explore these mechanisms. The quantity of experimental coal rock is large and processing method is complex, so specimen made of similar materials was applied to replace coal rock. The true triaxial hydraulic fracturing experimental apparatus, 3D scanning device for coal rock section were applied to carry out hydraulic fracturing experiment. The results show that the initiation pressure is inversely proportional to the horizontal stress difference (Δσ) and positively related to fracturing fluid injection rate. When vertical stress (σv) is constant, the initiation pressure and fracture width decrease with the increasing of Δσ. Natural fractures can be connected by main fracture when propagates perpendicular to the direction of minimum horizontal stress (σh), then secondary fractures and fracture network form in CBM reservoirs. When two stresses of crustal stress are close and far different from the third one, the fracture morphology and propagation become complex. Influenced by perforations and filtration of fracturing fluid in specimen, fracturing fluid flows to downward easily after comparing horizontal well fracturing with vertical well fracturing. Fracture width increases with the decreasing of elastic modulus, the intensity of fracture is positively related with the elastic modulus of coal rock. The research results can provide theoretical basis and technical support for the efficient development of CBM.
机译:水力压裂可有效提高煤层气储层的渗透率,对煤层气的商业化生产具有重要意义。但是,水力压裂的效率受多种因素影响。煤层气储层的裂缝起裂,形态和扩散机理尚不清楚,需要进一步探讨。水力压裂实验是探索这些机理的准确工具。实验用煤岩数量多,加工方法复杂,因此采用类似材料制成的试样代替煤岩。运用真三轴水力压裂实验装置,煤岩断面三维扫描仪进行水力压裂实验。结果表明,起始压力与水平应力差(Δσ)成反比,与压裂液注入速率成正比。当垂直应力(σv)恒定时,起始压力和断裂宽度随Δσ的增加而减小。当垂直于最小水平应力(σh)方向传播时,天然裂缝可以由主裂缝连接,然后在煤层气储层中形成次生裂缝和裂缝网络。当两个地壳应力与第三个应力相差甚远时,裂缝的形态和扩展变得复杂。在水平井压裂与垂直井压裂进行比较之后,受样品中压裂液的穿孔和过滤的影响,压裂液容易向下流动。断裂宽度随着弹性模量的减小而增加,断裂强度与煤岩弹性模量成正相关。研究成果可为煤层气的有效开发提供理论依据和技术支持。

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