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首页> 外文期刊>International Journal of Rock Mechanics and Mining Sciences >The distinct element analysis for hydraulic fracturing in hard rock considering fluid viscosity and particle size distribution
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The distinct element analysis for hydraulic fracturing in hard rock considering fluid viscosity and particle size distribution

机译:考虑流体黏度和粒径分布的硬岩水力压裂独特元素分析

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A series of simulations for hydraulic fracturing in competent rock was performed by using the flow-coupled DEM code to discuss the influence of the fluid viscosity and the particle size distribution. The simulation results show good agreement with experimental results that contain the AE measurement data. The following observations can be made. When a low viscosity fluid is used, the fluid infiltrates into the fracture immediately. On the other hand, when a high viscosity fluid is used, the fluid infiltrates slowly into the crack after the fracture first elongates. Although tensile cracks are dominantly generated in the simulation, the energy released from a tensile crack becomes small because the tensile strength of rock is obviously small compared with the compressive strength. Such a small AE is easily buried in a noise and difficult to be measured in an experiment Therefore, in AE measurement experiment shear type AE with large energy is dominantly observed, as many previous researches have indicated.
机译:通过使用流动耦合的DEM代码进行了一系列的模拟实验,证明了压裂岩石中水力压裂对流体粘度和粒径分布的影响。仿真结果与包含AE测量数据的实验结果吻合良好。可以进行以下观察。当使用低粘度流体时,流体会立即渗入裂缝。另一方面,当使用高粘度流体时,在裂缝首先拉长之后,流体会缓慢渗透到裂缝中。尽管在模拟中主要产生拉伸裂纹,但从拉伸裂纹释放的能量变小,因为岩石的拉伸强度明显比抗压强度小。如此小的AE容易被噪声掩盖,并且在实验中难以测量。因此,如许多先前的研究表明,在AE测量实验中,主要观察到具有大能量的剪切型AE。

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