辛置煤矿复杂灰岩含水层的模糊综合判别法
Fuzzy comprehensive discriminant method for complex limestone aquifers in Xinzhi coal mine
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摘要: 本文通过对辛置煤矿52个矿井水水质的系统研究,总结了辛置煤矿3个复杂灰岩含水层的水化学特征,并利用改进的模糊综合判别法对辛置煤矿3个灰岩含水层的水样进行了判别研究。研究结果表明:辛置煤矿石炭系太原组K;灰岩含水层水化学特征明显,其判别依据为SO4-Na型,且水样的yca/Yso4,比值均小于0.5;由于地质构造复杂、地层岩性不均一和地下水径流条件多变,造成石炭系太原组K,灰岩含水层和奥陶系峰峰组O,f灰岩含水层的水质参数相互重叠,无法通过常规水化学方法进行有效判别。本研究采用常量离子当量浓度百分比、YcaYa和YMgYa作为模糊综合判别模型中的判别因子,取代传统判别法中利用常量离子质量浓度作为判别因子,将水化学机理与模糊数学原理有机融合,使模糊综合判别法的准确度由原来的75%提高至96.2%。Abstract: This paper summarized the water chemistry characteristics of three complex limestone aquifers in Xinzhi coal mine by systematically studying the water quality of 52 water samples.The improved fuzzy comprehensive discriminant method was used to discriminate the water samples of three limeston&aquifers in Xinzhi coal mine.The water chemistry characteristics of the K,limestone aquifer in the Taiyuan Formation of the Carboniferous in Xinzhi coal mine are obvious. The discriminating basis of K, limestone aquifer are SO,-Na type and the ratio of yca/Yso, of the water sample less than 0.5.Due to the complicalted geological structure , the uneven lithology of the stratum and the variable groundwater runoff conditions , the water quality parameters of the K,limestone aquifer of the Carboniferous Taiyuan Formation and the O,f limestone aquifer of the Ordovician Fengfeng Formation overlap each other and cannot be effectively identified by conventional hydrochemical methods.In this study , the percentage of constantion equivalent concentration , ratio coefficients of Yca/Yaand YuYc were used as the identification factors in the fuzzy comprehensive discriminant model , which organically integrated the water chemical mechanism with the fuzzy mathematical principle.The constantion mass concentration is used as the identification factor in the traditional fuzzy comprehensive identification method.Through these improvements , the accuracy of the fuzzy comprehensive identification method has been improved from 75% to 96.2%.