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Phenomenon of methane driven caused by hydraulic fracturing in methane-bearing coal seams

机译:含瓦斯煤层水力压裂引起的瓦斯驱动现象

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The methane concentration of the return current will always be enhanced to a certain degree when hydraulic fracturing with bedding drilling is implemented to a gassy coal seam in an underground coal mine. The methane in coal seam is driven out by hydraulic fracturing. Thus, the phenomenon is named as methane driven effect of hydraulic fracturing. After deep-hole hydraulic fracturing at the tunneling face of the gassy coal seam, the coal methane content exhibits a ‘‘low-high-low' distribution along excavation direction in the following advancing process, verifying the existence of methane driven caused by hydraulic fracturing in methane-bearing coal seam. Hydraulic fracturing causes the change of pore-water and methane pressure in surrounding coal. The uneven distribution of the pore pressure forms a pore pressure gradient. The free methane migrates from the position of high pore(methane) pressure to the position of low pore(methane) pressure. The methane pressure gradient is the fundamental driving force for methane-driven coal seam hydraulic fracturing. The uneven hydraulic crack propagation and the effect of time(as some processes need time to complete and are not completed instantaneously) will result in uneven methane driven. Therefore, an even hydraulic fracturing technique should be used to avoid the negative effects of methane driven; on the other hand, by taking fully advantage of methane driven, two technologies are presented.
机译:当在地下煤矿的瓦斯煤层中进行带层钻的水力压裂时,返回电流的甲烷浓度将始终提高到一定程度。水力压裂驱除煤层中的甲烷。因此,该现象被称为水力压裂的甲烷驱动效应。在瓦斯煤层掘进面进行深孔水力压裂后,煤层气在随后的推进过程中沿开挖方向呈“低-高-低”分布,验证了水力压裂引起的甲烷驱替存在。在含甲烷的煤层中。水力压裂导致周围煤中孔隙水和甲烷压力的变化。孔隙压力的不均匀分布形成孔隙压力梯度。游离甲烷从高孔隙(甲烷)压力的位置迁移到低孔隙(甲烷)压力的位置。甲烷压力梯度是甲烷驱动煤层水力压裂的基本动力。水力裂纹的不均匀扩展和时间的影响(由于某些过程需要时间才能完成,而并非立即完成),将导致甲烷驱散不均。因此,应采用均匀的水力压裂技术,以避免甲烷驱替的负面影响。另一方面,通过充分利用甲烷驱动,提出了两种技术。

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