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New evaluation and prediction method to determine the risk of water inrush from mining coal seam floor

机译:新的评价与预测方法,以确定采煤煤层焊缝涌入潮流风险的研究

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摘要

The aim of this study is to remedy the existing problems in the prediction methods of water inrush from the mining coal seam floor. This paper analyzes a large number of water inrush cases and proposes that there are four main factors, namely water pressure and water abundance of the confined karst aquifer in the mine floor, the lithological thickness and characteristics of different structures of aquiclude in the mine floor, the geotectonic characteristics of the aquifer and aquiclude, and mining ground pressure, which affect water inrush from the mining coal seam floor. Based on structural and damage mechanics, a mechanical model of homogeneously fractured weak rock stratum is established for the water-impermeable layer of the floor, 354 points of water inrush are used to investigate and analyze, critical curve equation of P vs. M of mine floor is determined and the primary factor that affects water inrush from the mine floor is obtained. Combined with the geological structure characteristics, the three-grade evaluation and prediction model is established for water inrush from mining coal seam floor. The results can be used toward a new evaluation and prediction method of water inrush from the mine floor.
机译:本研究的目的是纠正来自采矿煤层地板的水中涌入预测方法的现有问题。本文分析了大量的水中侵入案例,并提出有四种主要因素,即雷区狭窄的喀斯特含水层的水压和水丰富,矿山地板中水上水平不同结构的岩性厚度和特征,含水层和水平的地理位置特征,以及采矿地面压力,影响采矿煤层焊缝的涌入水涌。基于结构和损坏力学,建立了均匀断裂弱岩层的机械模型,为水域不透水层建立了354点的水涌,用于研究和分析,临界曲线等于矿井的临界曲线方程确定地板,获得影响来自矿地板的水涌出的主要因素。结合地质结构特征,建立了三级评价和预测模型,采用矿泉煤层涌出水涌。结果可用于矿山涌出的新评价和预测方法。

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