ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    吴君毅, 刘洪, 欧阳渊, 李樋, 张景华, 张腾蛟, 黄勇, 段声义. 螺髻山北麓地下水化学特征与水质评价[J]. 西北地质,2023,56(5): 151-164.
    引用本文: 吴君毅, 刘洪, 欧阳渊, 李樋, 张景华, 张腾蛟, 黄勇, 段声义. 螺髻山北麓地下水化学特征与水质评价[J]. 西北地质,2023,56(5): 151-164.
    WU Junyi, LIU Hong, OUYANG Yuan, LI Tong, ZHANG Jinghua, ZHANG Tengjiao, HUANG Yong, DUAN Shengyi. Hydrochemical Characteristics and Water Quality Assessment of Groundwater in Northern Foothill of Luoji Mountains[J]. Northwestern Geology,2023,56(5): 151-164.
    Citation: WU Junyi, LIU Hong, OUYANG Yuan, LI Tong, ZHANG Jinghua, ZHANG Tengjiao, HUANG Yong, DUAN Shengyi. Hydrochemical Characteristics and Water Quality Assessment of Groundwater in Northern Foothill of Luoji Mountains[J]. Northwestern Geology,2023,56(5): 151-164.

    螺髻山北麓地下水化学特征与水质评价

    Hydrochemical Characteristics and Water Quality Assessment of Groundwater in Northern Foothill of Luoji Mountains

    • 摘要: 为研究川西大凉山区螺髻山北麓地下水化学特征、演化机制以及评价地下水质现状,笔者系统采集研究区不同地段的15组地下水样品为研究对象。利用Gibbs图解法、离子比例系数法和基于RMSprop算法的BP神经网络评价法,探讨该地区地下水化学特征演化机制,评价地下水质现状,支持服务帮助当地合理开发和安全利用水资源。结果表明研究区水化学类型以Mg2+·Ca2+−HCO3为主,其水化学离子的形成主要以岩土风化溶滤作用为主,由硅酸盐矿物与碳酸盐矿物共同控制,硅酸盐矿物控制更显著。结合地质背景,认为硅酸盐矿物主要来自火山碎屑岩类、花岗岩类、砂岩类和泥质岩类等岩石。利用BP神经网络对5000组地下水样本学习训练,对研究区样本进行评价,模型训练图像表明BP神经网络能很好拟合地下水样本训练集并且对测试集进行客观准确的判断。研究区地下水评价结果显示:Ⅰ类水质点占13.3%,Ⅱ类水质点占40%,Ⅲ类水质点占46.6%,整体水质较好,建议Ⅲ类水质地区普格县特尔果乡甲甲沟村、普格县特补乡白庙子需要加强地下水污染源调查以及水质保护。

       

      Abstract: To investigate the hydrochemical characteristics, evolution, and assessment of water quality in the northern foot of the Luoyang Mountains in the western Sichuan Daliang Mountains, 15 sets of local groundwater chemistry samples from different sections of the study area were collected as research objects. Analysis and study of hydrochemical characteristics and evolution in this area use Gibbs’ diagram and ion proportion coefficient method. Furthermore, assessing groundwater quality BP neural network classification method with RMSprop algorithm, supporting services to help local communities develop and use water resources wisely and safely. The results show that the water chemistry of the study area is dominated by Mg2+·Ca2+−HCO3. The hydrochemical evolution of groundwater in this area are mainly derived from rock weathering-dissolution. It is controlled by rocks of silicate and carbonate, with silicate playing a more significant role. Considering the geological background of this area, silicate mainly comes from volcanic, clastic, granitic, sandstone and mud stone. The BP neural network was used to train 5000 groups of groundwater samples, and the samples in the study area were evaluated. The training image of the model showed that the BP neural network could well fit the training set of groundwater samples and accurately judge the test set. The result of groundwater quality in this area indicates that Class I water quality points accounted for 13.3%, Class II water quality points accounted for 40%, Class III water quality points accounted for 46.6%. Its overall water quality is good, and the Class III water quality area needs to strengthen groundwater pollution source investigation as well as water quality protection.

       

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