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作 者:赵宝峰[1,2,3]
机构地区:[1]中煤科工集团西安研究院有限公司,陕西西安710054 [2]陕西省煤矿水害防治技术重点实验室,陕西西安710177 [3]中国地质大学(武汉)环境学院,湖北武汉430074
出 处:《煤矿安全》2015年第7期189-192,共4页Safety in Coal Mines
基 金:国家科技支撑计划资助项目(2012BAC10B03);中煤科工集团西安研究院面上资助项目(2014MS010);中煤科工集团青年基金资助项目(2014QN004)
摘 要:为了准确判别复合含水层条件下封闭不良钻孔的突水水源,在分析矿井水文地质条件和地下水化学特征的基础上,排除了不可能为突水水源的第四系和延安组含水层,对于可能为突水水源的直罗组及其下段含水层,由于两者富水性和水化学条件较为相似,因此,采用了模糊聚类分析法,将突水点和直罗组及其下段含水层中的K++Na+、Ca2+、Mg2+、Cl-、SO2-4、HCO-3作为评价指标,并利用Matlab平台进行计算,将待判别水样划分为2类,其中突水点与直罗组下段含水层为一类。在确定了突水水源后,在井下对直罗组下段含水层进行注浆封孔,对突水点成功进行了封堵。对于水文地质和水化学条件相似的含水层,可以采用模糊聚类分析对突水水源进行有效判别。In order to identify water- inrush source of poor sealed borehole under the compound aquifer,based on the analysis of hydrogeology and hydrochemistry conditions in coal mining,Quaternary and Yan'an formation which were not water- inrush source were excluded. Zhiluo formation and its lower segment aquifer may be water- inrush resource. Because of the similarity of Zhiluo formation and its lower segment aquifer's water yield property and hydrochemistry conditions,fuzzy clustering analysis was adopted. K++ Na+、Ca2 +、Mg2 +、Cl-、SO2-4、HCO-3in water- inrush point,Zhiluo formation and its lower segment aquifer were selected as evaluation index. Matlab was used to calculate and the water samples were divided into two types; the water sample of water- inrush point was the same as Zhiluo formation lower segment aquifer. After determination of water- inrush source,the poor sealed borehole was sealed. For similar hydrogeology and hydrochemistry conditions of aquifer,fuzzy clustering analysis is effective method to identify the water- inrush resource.
关 键 词:模糊聚类 复合含水层 封闭不良钻孔 矿井突水 突水水源
分 类 号:TD745[矿业工程—矿井通风与安全]
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