首页> 外文期刊>Arabian journal of geosciences >A GIS-based method of risk assessment on no. 11 coal-floor water inrush from Ordovician limestone in Hancheng mining area, China
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A GIS-based method of risk assessment on no. 11 coal-floor water inrush from Ordovician limestone in Hancheng mining area, China

机译:基于GIS的风险评估方法没有。 11中国汉城矿区奥陶涅迪师石灰石煤层水涌入

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摘要

The no. 11 coal seam in the deep area of Hancheng mining area is mining in recent years, which is threatened by the water inrush from the Ordovician limestone aquifer. Coal-floor water inrush is governed by the water abundance of coal-floor aquifer, the water-resisting performance of coal-floor aquitard, and the pathway connecting the water source and the working face. To make an accuracy risk assessment of water inrush from the no. 11 coal seam floor, a GIS-based vulnerability index method (VIM) is adopted for its superior comprehensive consideration of more controlling factors, powerful spatial analysis, and intuitively display functions. This study firstly established an index system including the water pressure of the coal-floor aquifer, the unit water inflow, the thickness, the core recovery percentage, the thickness ratio of brittle rocks to ductile rocks, the thickness of effective aquitard, and the accumulated length of faults and folds, of which the former six indexes governed the water abundance of the coal-floor aquifer which was combined with the last two factors to determine the risk of coal-floor water inrush. Secondly, the thematic map of each controlling factor is established by GIS using the geological prospecting data, and the weight of each factor is determined by the analytic hierarchy process (AHP) after consulting the expert review panel. At last, a vulnerability index is obtained and used to assess the risk of coal-floor water inrush of the no. 11 coal seam. The risk of water inrush of the no. 11 coal seam of the study area was ranked to three zones: the southeastern shallow area in red color is the dangerous zone, the wide northwestern area in green color is the safe zone, and the transition area in yellow color is the moderate-risk zone. Compared with the actual water-inrush incidents, the risk assessment result was verified to achieve an accuracy of 82.35%, which is proved to be a dependable reference for the prevention and controlling of c
机译:否。 11河城矿区深面积的煤层近年来正在采矿,这受到奥陶省石灰石含水层的水中涌入的威胁。煤层水涌入由煤层含水层的水丰富,煤楼水上耐水性能,以及连接水源和工作面的途径。从NO中提出对水中涌入的准确性风险评估。 11煤层地板,采用了GIS的漏洞指标方法(VIM),以卓越的全面考虑更多控制因素,强大的空间分析,直观显示功能。本研究首先建立了一个指数系统,包括煤层含水层的水压,单位水流入,厚度,核心回收率,脆性岩石厚度比韧性岩石,厚度有效的水,和积累的厚度故障和折叠的长度,其中六个指数控制了与最后两个因素相结合的煤层含水层的水丰度,以确定煤层涌出的风险。其次,通过GIS使用地质勘探数据建立了每个控制因子的主题地图,并且在咨询专家审查小组后,每个因素的重量由分析层次处理(AHP)确定。最后,获得了漏洞指数,并用于评估煤层涌入的风险。 11煤层。禁止侵入的风险。 11煤层的研究区被排名为三个区域:红颜色的东南浅面积是危险区,绿色宽阔的西北地区是安全区,黄色的过渡区是中等风险区。与实际的水涌入事故相比,核实风险评估结果达到了82.35%的准确性,这被证明是预防和控制C的可靠参考

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