朱洲洋,肖长来,梁秀娟,杨伟飞,贾璐

• 1:吉林大学地下水资源与环境教育部重点实验室
• 2:吉林大学油页岩地下水原位转化与钻采技术国家地方联合工程实验室
• 3:吉林大学新能源与环境学院

摘要(Abstract)：

针对长白山玄武岩区矿泉水资源开发利用程度不断增加的现状,为进一步保护及合理开发安图县矿泉水资源,根据野外实际调查数据,利用数理统计方法及水化学模拟等多种方法开展对安图县矿泉水形成机理的研究。首先绘制Piper三线图和离子浓度箱型图分析安图县矿泉水水化学特征;然后利用SPSS软件对特征组分偏硅酸展开相关性分析;运用离子比值分析法初步判定离子主要来源;再利用Phreeqc软件反向模拟研究区地下水三条路径的水岩交互作用;最后根据模拟结果综合分析安图县玄武岩区矿泉水的形成机理。结果显示,安图县玄武岩区天然矿泉水属弱碱性偏硅酸型矿泉水,偏硅酸含量介于28.8～62.4 mg/L之间,水化学类型以HCO_3-Na型和HCO_3-Na·Ca型为主。地下水发生了溶滤作用和Ca-Na离子交换作用。偏硅酸主要来源于长石和辉石的溶解,且偏硅酸含量沿径流途径增大。K~+、Na~+主要来源于硅酸盐矿物(钾长石、钠长石)和岩盐,Ca~(2+)、Mg~(2+)主要来源于碳酸盐矿物(方解石和白云石)。

关键词(KeyWords)： 玄武岩区;矿泉水;水化学特征;反向地球化学模拟;形成机理;地下水;水环境;水质

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(41572216);; 中国地质调查局项目(DD20190340);; 吉林省地质勘查基金项目(2018-13);; 省校共建计划专项(SXGJQY2017-6);; 陕西省重点研发计划(2017ZDCXL-SF-03-01-01)

作者(Author): 朱洲洋,肖长来,梁秀娟,杨伟飞,贾璐

DOI: 10.13928/j.cnki.wrahe.2021.10.014

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