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Study on the regularity of fault water inrush in Yuzhou mine area

机译:禹州矿区断层突水规律研究。

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Fault is one of the important reasons causing floor water invasion of coal seam.It shows that the water irruption quantity of fault is large,the water bursting source is the limestone water of the cambrian mainly,and the types of fault water inrush is diversity through the characteristic analysis of all previous fault water inrush in Yuzhou mine area.It also can be found that water inrush quantities of faults present positive correlation with the water inrush channel area of faults,the porosity of fault zones and the water pressure value of aquifer by the water inrush quantity calculated of main influence faults.The fault type,water inrush quantity,cutting the cambrain limestone aquifer or not and the water pressure value of aquifer are chosen as discrimination factors,through which the risk of fault water inrush can be divided into four kinds.With this method,four strips of main influence faults in Yuzhou mine area are classified,where the number of the first risk fault is four and other faults can be distinguished as the lower grades.
机译:断层是引起煤层底板水入侵的重要原因之一。表明断层的突水量大,突水源主要是寒武纪的石灰岩水,断层突水的类型通过通过对禹州矿区以前所有断层突水的特征分析,发现断层突水量与断层突水通道面积,断层孔隙度和含水层水压值呈正相关。选择故障类型,突水量,是否切割坎布林石灰岩含水层以及含水层的水压值作为判别因素,由此可将断裂突水的风险分为四种方法。用这种方法,将禹州矿区的四个主要影响断层划分为四个,其中第一个危险断层的数目为四个她的缺点可以被认为是低年级。

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