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Influence of particle size on seepage of water and sediment in fractured rock

机译:粒径对裂缝岩中水和沉积物渗漏的影响

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Coal excavations performed in areas of shallow, thick sand can overburden the strata layers of the excavation site, resulting in fractures in the strata layers. Surface water, groundwater and sand layers can flow into mine goaf through the fractured rock and thus often lead to inrush of water and collapsing of sand. It is important to study the mechanical properties of water and sand in excavations sites under different conditions and the influencing factors of the water and sand seepage system. The viscosity of water-sand mixtures of various particle sizes were tested based on the relationship between the shear strain rate and the surface viscosity. A seepage system test was designed to analyze the permeability of water and sand in fractured rock. According to the seepage test, effective fluidity is in 10~(-8)~10~(-5)m~(n+2)·s~(2-n)/kg, while the non-Darcy coefficient ranges from 10~5 to 10~8 m~(-1) with the change of particle size of sand. Effective fluidity decreased as the particle size of sand increased. The non-Darcy coefficient ranged from 10~5 to 10~8 m~(-1) depending on particle size and showed contrary results.
机译:在浅层厚的砂区域中进行的煤炭挖掘可以覆盖挖掘部位的地层层,导致地层层中的骨折。地表水,地下水和砂层可以通过骨折岩石流入矿井,因此通常导致水和砂坍塌。在不同条件下研究挖掘部位的水和沙子的机械性能以及水和沙子渗流系统的影响因素非常重要。基于剪切应变速率和表面粘度之间的关系来测试各种颗粒尺寸的水砂混合物的粘度。渗透系统测试旨在分析水和沙子在裂缝岩中的渗透性。根据渗流测试,有效的流动性在10〜(-8)〜10〜(-5)m〜(n + 2)·s〜(2-n)/ kg,而非达到系数范围为10 〜5至10〜8 m〜(-1)随着粒度的粒度的变化。随着砂的粒度增加,有效的流动性降低。根据粒径,非达到的系数范围为10〜5至10〜8 m〜(-1),并显示出相反的结果。

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