潞安矿区中部煤矿充水水源水化学特征及水源识别意义

杜金龙. 2022. 潞安矿区中部煤矿充水水源水化学特征及水源识别意义. 西北地质, 55(1): 208-215. doi: 10.19751/j.cnki.61-1149/p.2022.01.017
引用本文: 杜金龙. 2022. 潞安矿区中部煤矿充水水源水化学特征及水源识别意义. 西北地质, 55(1): 208-215. doi: 10.19751/j.cnki.61-1149/p.2022.01.017
DU Jinlong. 2022. Hydrochemical Characteristics of Water Filling Source in Central Lu'an Mining Area and Water Source Identification Significance. Northwestern Geology, 55(1): 208-215. doi: 10.19751/j.cnki.61-1149/p.2022.01.017
Citation: DU Jinlong. 2022. Hydrochemical Characteristics of Water Filling Source in Central Lu'an Mining Area and Water Source Identification Significance. Northwestern Geology, 55(1): 208-215. doi: 10.19751/j.cnki.61-1149/p.2022.01.017

潞安矿区中部煤矿充水水源水化学特征及水源识别意义

  • 基金项目:

    国家重点研发计划资助项目“矿井突水水源快速判识与水灾防控关键技术研究”(2017YFC0804104)。

详细信息
    作者简介: 杜金龙(1980-),男,湖北枝江人,高级工程师,博士,从事煤炭绿色勘查、煤矿防治水、矿山环境修复方面研究。E-mail:19084548@qq.com。
  • 中图分类号: P641.4+61

Hydrochemical Characteristics of Water Filling Source in Central Lu'an Mining Area and Water Source Identification Significance

  • 采集了潞安矿区中部煤矿5类80份已知水源水样,利用PIPER三线图对不同来源水样水文地球化学特征进行了分析;利用聚类分析方法(Ward法)对三线图上存在重叠的砂岩水、太灰水与奥灰水进行分类,显示奥灰水与太灰水明显聚类,局部存在两者混合,砂岩水则与上述两者难以区分;最后利用Bayes模型建立了不同水源判别函数(自我检验准确率达91.5%),对采集的19个矿井涌水水样进行了识别,识别出顶板砂岩水样12个,地表水、孔隙水样4个,太灰水样3个;对于后验概率不高的水样(低于80%)存在水源混合的可能性。
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出版历程
收稿日期:  2021-01-11
修回日期:  2021-05-23

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