长江科学院院报 ›› 2020, Vol. 37 ›› Issue (9): 18-23.DOI: 10.11988/ckyyb.20190476

• 水资源与环境 • 上一篇    下一篇

山东淄博大武水源地地下水水化学特征及水质评价

冯建国1, 季德帅1, 高宗军1, 杨丽芝2, 朱恒华2, 刘治政2   

  1. 1.山东科技大学 地球科学与工程学院, 山东 青岛 266590;
    2.山东省地质调查院,济南 250013
  • 收稿日期:2019-04-25 修回日期:2019-06-18 出版日期:2020-09-01 发布日期:2020-09-25
  • 通讯作者: 高宗军(1964-),男,山东泰安人,教授,博士,博士生导师,从事水工环地质方面的教学与研究工作。E-mail:gaozongjun@126.com
  • 作者简介:冯建国(1976-),男,河北卢龙人,讲师,博士,从事水文地质环境地质教学与研究工作。E-mail:fengjianguo20316@sohu.com
  • 基金资助:
    山东省地质调查院研究基金项目(SDLR-2017-138)

Hydrochemical Characteristics and Water Quality Evaluation of Groundwater in Zibo Dawu Water Source, Shandong Province

FENG Jian-guo1, JI De-shuai1, GAO Zong-jun1, YANG Li-zhi2, ZHU Heng-hua2, LIU Zhi-zheng2   

  1. 1. College of Earth Science and Engineering, Shandong University of Science and Technology,Qingdao 266590,China;
    2. Shandong Provincial Institute of Geological Survey,Jinan 250013,China
  • Received:2019-04-25 Revised:2019-06-18 Online:2020-09-01 Published:2020-09-25

摘要: 为了解大武水源地地下水水化学特征及水质现状,选取2017年12月采集的57件水样,综合运用数理统计、相关性分析、Piper三线图、Gibbs模型和离子比法,分析了大武水源地的主要离子特征及其成因,并运用综合评价法对水源地水质进行评价。结果表明:大武水源地地下水主要阳离子为Ca2+和Na+,约占阳离子总量的82.8%;主要阴离子为HCO3-、SO42-、Cl-,约占阴离子总量的91.9%;水化学类型以HCO3·SO4-Ca·Mg(Ca)型、HCO3·SO4·Cl-Ca·Mg(Ca)型、HCO3·Cl-Ca·Mg(Ca)型为主;水化学组分主要受碳酸盐岩风化溶解控制;地下水水质都在Ⅲ类水以上,Ⅲ类水占据总水样的47.4%,Ⅳ类和Ⅴ类水占据了52.6%。研究成果对了解大武水源地水环境现状具有重要意义。

关键词: 地下水, 水化学特征, 水质评价, 大武水源地, 相关性分析

Abstract: The hydrochemical characteristics and water quality status of karst confined water in Dawu water source of Shandong Province were investigated using mathematical statistics, correlation analysis, Piper's plot, Gibbs model and ion ratio method by analyzing 57 groundwater samples taken in 2017. The major ion characteristics and causes were examined, and the water quality was assessed by comprehensive evaluation method. Results reveal that Ca2+ and Na+ are the major cations of groundwater, accounting for 82.8% of the total cations; HCO3-, SO42-, and Cl- are the main anions, accounting for 91.9% of the total anions. HCO3·SO4-Ca· Mg(Ca), HCO3·SO4·Cl-Ca·Mg(Ca), and HCO3·Cl-Ca·Mg(Ca) are dominant hydrochemical patterns. The hydrochemical components are mainly controlled by weathering and dissolution of carbonate rock. The groundwater quality is above class Ⅲ, which accounts for 47.4% of the total water samples, while Ⅳ and Ⅴ classes occupy 52.6% of the total water samples.

Key words: groundwater, hydrochemical characteristics, water quality evaluation, Dawu water source, correlation analysis

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