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Divisions based on groundwater chemical characteristics and discrimination of water inrush sources in the Pingdingshan coalfield

机译:平顶山煤田地下水化学特征划分与突水水源判别。

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Within the Pingdingshan coalfield, the spatial distribution characteristics of key groundwater chemical components were studied in four aquifers that influence coal-mining operations. Thirty-six water samples were collected from the four aquifers, which were divided into smaller units. Discriminant models of mine-water inrush sources were developed for the three divisions I, III, and IIII, and engineering verification was conducted. The results showed that the main indices influencing groundwater chemical characteristics were Na+ + K+, Ca2+, Mg2+, Cl-, SO42-, and HCO3- in the Pingdingshan coalfield with regional variations according to faults and synclines. The Guodishan fault was the primary groundwater chemical division structure, which divides the Pingdingshan coalfield into two primary groundwater chemically characteristic units, divisions I and II. The Likou syncline was the secondary groundwater chemically characteristic structure, which divides division II into two secondary groundwater chemically characteristic units: divisions III and IIII. Discriminant models of water inrush sources in divisions I, III, and IIII (12 discriminant functions) were developed, and engineering verification showed that discrimination accuracy for 16 groundwater samples in four aquifers of three divisions was 93.75 %.
机译:在平顶山煤田内,研究了影响采矿作业的四个含水层中关键地下水化学成分的空间分布特征。从四个含水层中收集了36个水样,将它们分成较小的单元。为I,III和IIII三个部门开发了判别水雷涌源的模型,并进行了工程验证。结果表明,平顶山煤田影响地下水化学特征的主要指标为Na + + K +,Ca2 +,Mg2 +,Cl-,SO42-和HCO3-,并根据断层和向斜方向发生区域性变化。郭帝山断层是主要的地下水化学分区结构,它将平顶山煤田划分为两个主要的地下水化学特征单元,分别为I区和II区。荔口向斜线是次要地下水的化学特征结构,将II类划分为两个次要地下水的化学特征单元:III类和IIII类。建立了I,III和IIII分区(12个判别函数)的判别模型,工程验证表明,三个分区的四个含水层中的16个地下水样品的判别准确度为93.75%。

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