院报 ›› 2020, Vol. 37 ›› Issue (4): 30-36.DOI: 10.11988/ckyyb.20181319

• 水资源与环境 • 上一篇    下一篇

焦作地区地下水水化学特征分析及水质评价

钱声源1, 张乾坤2, 陈从建1, 杨国平3   

  1. 1.江苏开放大学 建筑工程学院,南京 210019;
    2.郑州市市政工程勘测设计研究院,郑州 450000;
    3.南京城市职业学院,南京 211200
  • 收稿日期:2018-12-13 出版日期:2020-04-01 发布日期:2020-05-21
  • 作者简介:钱声源(1980-),男,江苏南京人,副教授,硕士,主要从事水文地质及地下水保护研究。E-mail:64820173@qq.com
  • 基金资助:
    中国地质调查局水文地质环境地质调查中心调查项目(20170601)

Groundwater Hydrochemical Characteristics and Water Quality Assessment in Jiaozuo

QIAN Sheng-yuan1, ZHANG Qian-kun2, CHEN Cong-jian1, YANG Guo-ping3   

  1. 1.School of Civil Engineering and Architecture, Jiangsu Open University, Nanjing 210019, China;
    2.Zhengzhou City Municipal Engineering Design & Research Institute,Zhengzhou 450000, China;
    3.Nanjing City Vocational College, Nanjing 211200, China
  • Received:2018-12-13 Online:2020-04-01 Published:2020-05-21

摘要: 2017年对焦作地区42个地下水样品进行了采集和测试,综合运用数理统计、Piper三线图和相关性分析等方法分析了该区地下水水化学特征,并运用单因子评价和基于主成分分析的模糊综合评价法对研究区地下水水质进行了评价。研究结果表明:地下水中Ca2+、Mg2+、SO2-4和HCO3-占主要优势,浅层地下水水化学类型按地下水径流方向由HCO3-Ca型逐渐演变为HCO3·SO4-Ca·Mg型和HCO3·SO4·Cl-Ca ·Mg型,深层地下水水化学类型主要为HCO3·SO4-Ca·Mg型,局部为HCO3·SO4-Ca·Mg型;水体离子组分变化主要受碳酸盐、硫酸盐和岩盐等风化溶滤作用影响;单因子评价结果显示TH、Mg2+、TDS、SO2-4等组分的超标是影响地下水质量的主要因素;模糊综合评价结果显示研究区浅层及深层地下水质满足Ⅲ类水及以上标准的采样点,分别占总采样点的61%和75%。研究成果可为该地区水质评价和水资源合理开发利用提供依据。

关键词: 地下水, 水化学特征, 水质评价, 主成分分析, 模糊综合评价, 焦作地区

Abstract: The hydrochemical characteristics of groundwater samples collected from Jiaozuo in 2017 were analyzed using mathematical statistics, Piper'plot, and correlation of components. The groundwater quality in the study area were also assessed using the method of single-factor evaluation and fuzzy comprehensive evaluation method based on principal component analysis. Results unveiled that Ca2+, Mg2+, SO2-4 and HCO3- were dominant in the groundwater of Jiaozuo. In shallow groundwater, the hydrochemical type evolved from HCO3-Ca to HCO3·SO4-Ca·Mg and HCO3·SO4·Cl- Ca·Mg along the direction of groundwater runoff. In deep groundwater, the hydrochemical type was mainly HCO3·SO4-Ca·Mg, with some local HCO3·SO4-Ca·Mg. The change of ion content in groundwater was mainly affected by weathering and leaching of carbonate, sulfate and rock salt. Single factor evaluation result showed that the excessive TH, Mg2+, TDS, SO2-4 and other components were major factors that affect the quality of groundwater. Fuzzy comprehensive evaluation results revealed that 61% and 75% of the shallow and deep groundwater quality in the study area met the Ⅲ-level water standard and above. The research findings offer basis for the water quality assessment and reasonable utilization of water resources in Jiaozuo.

Key words: groundwater, hydrochemical characteristics, water quality assessment, principal component analysis, fuzzy comprehensive evaluation, Jiaozuo

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