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Experimental study of mechanism of non-Darcy flow in broken rocks

机译:破碎岩石非达西渗流机理的实验研究

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This paper used MTS815.02 Electro-Hydraulic Servocontrolled Rock Mechanics Testing System to conduct seepage experiments in broken sandstones which had different porosity and different particle sizes. It studied the effect of porosity and particle size of broken sandstones on non-Darcy flow in broken sandstones. Experimental results showed that the broken sandstones with smaller porosity had more obvious non-Darcy property than the broken sandstones with the same particle size. Based on the experimental data obtained, this paper got the relationships that how permeability K and non-Darcy flow factor β varied with porosity and particle size and the equations that porosity and particle size had a combination effect on permeability K and non-Darcy flow factor β by using 1stOpt software. Finally, through the analysis of experimental results, the cause of non-Darcy flow in broken rocks was discussed.
机译:本文采用MTS815.02电液伺服岩石力学测试系统,对孔隙度,粒径不同的破碎砂岩进行渗流试验。研究了破碎砂岩的孔隙度和粒径对破碎砂岩中非达西渗流的影响。实验结果表明,孔隙度较小的破碎砂岩比相同粒径的破碎砂岩具有更明显的非达西性质。根据获得的实验数据,得出渗透率K和非达西流动因子β如何随孔隙度和粒径变化的关系,以及孔隙度和粒径对渗透率K和非达西流动因子具有联合作用的方程式使用1stOpt软件的β。最后,通过对实验结果的分析,探讨了破碎岩石非达西渗流的成因。

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