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新疆玛纳斯河流域地下水砷氟分布及共富集成因

  • 康文辉 ,
  • 周殷竹 ,
  • 孙英 ,
  • 周金龙 ,
  • 曹月婷 ,
  • 鲁涵 ,
  • 涂治
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  • 1.新疆农业大学水利与土木工程学院,新疆 乌鲁木齐 830052
    2.新疆水文水资源工程技术研究中心,新疆 乌鲁木齐 830052
    3.新疆水利工程安全与水灾害防治重点实验室,新疆 乌鲁木齐 830052
    4.中国地质调查局水文地质环境地质调查中心,河北 保定 071051
康文辉(1998-),男,硕士研究生,主要研究方向为水文地球化学及地下水保护. E-mail: 1754243549@qq.com

收稿日期: 2023-03-27

  修回日期: 2023-06-15

  网络出版日期: 2023-09-28

基金资助

国家自然科学基金项目(42007161)

Distribution and coenrichment of arsenic and fluorine in the groundwater of the Manas River Basin in Xinjiang

  • Wenhui KANG ,
  • Yinzhu ZHOU ,
  • Ying SUN ,
  • Jinlong ZHOU ,
  • Yueting CAO ,
  • Han LU ,
  • Zhi TU
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  • 1. College of Hydraulic and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, Xinjiang, China
    2. Xinjiang Hydrology and Water Resources Engineering Research Center, Urumqi 830052, Xinjiang, China
    3. Xinjiang Key Laboratory of Hydraulic Engineering Security and Water Disasters Prevention, Urumqi 830052, Xinjiang, China
    4. Center for Hydrogeology and Environmental Geology Survey, China Geological Survey, Baoding 071051, Hebei, China

Received date: 2023-03-27

  Revised date: 2023-06-15

  Online published: 2023-09-28

摘要

砷(As)、氟(F)污染水体及其共存问题是环境领域的热点问题,长期暴露其中对公众的身体健康存在巨大威胁。以新疆玛纳斯河流域为研究区,分析高As、高F地下水的水化学及空间分布特征,结合地质条件、赋存环境和人类活动的影响进一步阐明地下水As和F的来源、迁移与富集的水文地球化学过程。结果表明:研究区地下水整体为弱碱性、还原环境的淡水,地下水As、F质量浓度变化范围分别为1.13~41.35 μg·L-1、0.06~8.02 mg·L-1,高As、高F地下水水样占总水样的62.9%、45.7%,砷氟共富集占总水样的37.1%。砷氟共富集地下水主要分布在平原区北部靠近沙漠边缘,水化学类型主要为HCO3·Cl型和HCO3·SO4·Cl型。研究区南部山区高As、高F岩层是地下水As、F的原生来源,区域地质构造与水文地质条件是影响地下水砷氟富集的重要因素。玛纳斯河流域高As地下水具有高pH值、低γSO42-/γCl-比、低Eh等特征,说明弱碱性的还原环境有利于地下水中As富集;高F地下水具有高pH值、高HCO3-、高Na+和低Ca2+等特征,说明高Na+和低Ca2+的碱性环境有利于地下水中F富集。

本文引用格式

康文辉 , 周殷竹 , 孙英 , 周金龙 , 曹月婷 , 鲁涵 , 涂治 . 新疆玛纳斯河流域地下水砷氟分布及共富集成因[J]. 干旱区研究, 2023 , 40(9) : 1425 -1437 . DOI: 10.13866/j.azr.2023.09.06

Abstract

Arsenic (As) and fluoride (F) pollution in water bodies, along with their coexistence, are critical environmental concerns, with long-term exposure posing a significant threat to public health. This study focuses on the Manas River Basin as the research area, analyzing the hydrochemical, and spatial distribution characteristics of groundwater with high As and F content. Furthermore, the study aims to elucidate the hydrogeochemical processes related to the origin, migration, and enrichment of As, and F in groundwater, considering geological conditions, occurrence environments, and the influence of human activities. The results show that the groundwater in the study area exhibits an alkaline-reducing environment. The mass concentrations of As and F in groundwater range from 1.13 to 41.35 μg·L-1 and from 0.06 to 8.02 mg·L-1, respectively. Groundwater samples with high As and F content constituted 62.9% and 45.7% of the total samples, respectively, while samples with a coenrichment of As and F accounted for 37.1% of the total samples. As-F coenriched groundwater is mainly distributed in the northern plain region, near the edge of the desert, with the dominant hydrochemical types being HCO3·Cl and HCO3·SO4·Cl. The primary sources of As and F in groundwater are high-content rock strata found in the southern mountainous area of the Manas River Basin. The high pH value, low SO42-/Cl- molar ratio, and low Eh of the high-As-content groundwater in the Manas River Basin indicate that a weak alkaline-reducing environment facilitates As enrichment in groundwater. Conversely, groundwater with high F content is characterized by high pH, HCO3-, and Na+ levels, as well as low Ca2+, indicating that an alkaline environment with high Na+ and low Ca2+ content favors F enrichment in groundwater.

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