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Experimental Investigation on the Basic Law of Hydraulic Fracturing After Water Pressure Control Blasting

机译:水压控制爆破后水力压裂基本规律的实验研究

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Because of the advantages of integrating water pressure blasting and hydraulic fracturing, the use of hydraulic fracturing after water pressure control blasting is a method that is used to fully transform the structure of a coal-rock mass by increasing the number and range of hydraulic cracks. An experiment to study hydraulic frac-turing after water pressure blasting on cement mortar samples (300 x 300 x 300 mm~3) was conducted using a large-sized true triaxial hydraulic fracturing experimental system. A traditional hydraulic fracturing experiment was also performed for comparison. The experimental results show that water pressure blasting produces many blasting cracks, and follow-up hydraulic fracturing forces blasting cracks to propagate further and to form numerous multidirectional hydraulic cracks. Four macroscopic main hydraulic cracks in total were noted along the borehole axial and radial directions on the sample surfaces. Axial and radial main failure planes induced by macroscopic main hydraulic cracks split the sample into three big parts. Meanwhile, numerous local hydraulic cracks were formed on the main failure planes, in different directions and of different types. Local hydraulic cracks are mainly of three types: local hydraulic crack bands, local branched hydraulic cracks, and axial layered cracks. Because local hydraulic cracks produce multiple local layered failure planes and lamellar ruptures inside the sample, the integrity of the sample decreases greatly. The formation and prop-agation process of many multidirectional hydraulic cracks is affected by a combination of water pressure blasting, water pressure of fracturing, and the stress field of the surrounding rock. To a certain degree, the stress field of surrounding rock guides the formation and propagation process of the blasting crack and the follow-up hydraulic crack. Following hydraulic fracturing that has been conducted after water pressure blasting, the integrity of the sample is found to be far lower than after traditional hydraulic fracturing; moreover, both the water injection volume and water injection pressure for hydraulic fracturing after water pressure blasting are much higher than they are for traditional hydraulic fracturing.
机译:由于将水压爆破与水力压裂相结合的优势,水压控制爆破后水力压裂的使用是一种通过增加水力裂缝的数量和范围来完全改变煤岩体结构的方法。利用大型真三轴水力压裂实验系统,对水泥砂浆样品(300 x 300 x 300 mm〜3)进行水压喷射后的水力压裂试验。为了比较,还进行了传统的水力压裂实验。实验结果表明,水压爆破产生许多爆破裂缝,后续的水力压裂力使爆破裂缝进一步传播并形成众多的多向水力裂缝。沿钻孔轴向和径向在样品表面总共记录了四个宏观的主要水力裂缝。宏观的主要水力裂缝引起的轴向和径向主要破坏面将样品分成三大部分。同时,在主破坏平面上,沿不同方向和不同类型形成了大量局部水力裂缝。局部水力裂缝主要有三种类型:局部水力裂缝带,局部分支水力裂缝和轴向分层裂缝。由于局部水力裂纹会在样品内部产生多个局部分层的破坏平面和层状破裂,因此样品的完整性会大大降低。水压爆破,压裂水压和围岩应力场共同影响着许多多向水力裂缝的形成和传播过程。围岩的应力场在一定程度上指导了爆破裂纹和后续水力裂纹的形成和传播过程。在水压喷射之后进行水力压裂后,发现样品的完整性远低于传统水力压裂后的完整性。而且,水压爆破后水力压裂的注水量和注水压力均远高于传统水力压裂。

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