新疆和田地区平原区地下水硬度空间分布及影响因素分析

杨锐, 周金龙, 张杰, 魏兴, 陈劲松. 新疆和田地区平原区地下水硬度空间分布及影响因素分析[J]. 环境化学, 2020, (11): 3255-3263. doi: 10.7524/j.issn.0254-6108.2020051803
引用本文: 杨锐, 周金龙, 张杰, 魏兴, 陈劲松. 新疆和田地区平原区地下水硬度空间分布及影响因素分析[J]. 环境化学, 2020, (11): 3255-3263. doi: 10.7524/j.issn.0254-6108.2020051803
YANG Rui, ZHOU Jinlong, ZHANG Jie, WEI Xing, CHEN Jinsong. Analysis on spatial distribution and influencing factors of groundwater hardness in the plain area of Hetian Prefecture, Xinjiang[J]. Environmental Chemistry, 2020, (11): 3255-3263. doi: 10.7524/j.issn.0254-6108.2020051803
Citation: YANG Rui, ZHOU Jinlong, ZHANG Jie, WEI Xing, CHEN Jinsong. Analysis on spatial distribution and influencing factors of groundwater hardness in the plain area of Hetian Prefecture, Xinjiang[J]. Environmental Chemistry, 2020, (11): 3255-3263. doi: 10.7524/j.issn.0254-6108.2020051803

新疆和田地区平原区地下水硬度空间分布及影响因素分析

    通讯作者: 周金龙, E-mail: zjzhoujl@163.com
  • 基金项目:

    国家自然科学基金(41662016)资助.

Analysis on spatial distribution and influencing factors of groundwater hardness in the plain area of Hetian Prefecture, Xinjiang

    Corresponding author: ZHOU Jinlong, zjzhoujl@163.com
  • Fund Project: Supported by the National Natural Science Foundation of China (41662016).
  • 摘要: 以2017年新疆和田地区平原区240组地下水水质检测数据为基础,综合运用离子比、Gibbs模型和氯碱指数等方法对其地下水硬度空间分布特征及影响因素进行分析.结果表明,水平方向上,高硬度地下水主要分布在研究区中北部靠近沙漠一带呈面状分布,总体呈现自南向北逐渐递增的趋势;垂直方向上,单一结构潜水总硬度随着埋深增加而降低,多层结构潜水-承压水总硬度均值排序为深层承压水(859.9 mg·L-1)、潜水(628.7 mg·L-1)、浅层承压水(471.8 mg·L-1);研究区地下水总硬度空间分布格局主要受水文地球化学作用和水化学环境因素共同影响,其中水文地球化学作用占主导因素.离子来源分析表明,该区地下水总硬度中Ca2+和Mg2+来源于蒸发盐岩与碳酸盐岩的风化溶解和阳离子交替吸附作用.
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  • 收稿日期:  2020-05-18

新疆和田地区平原区地下水硬度空间分布及影响因素分析

    通讯作者: 周金龙, E-mail: zjzhoujl@163.com
  • 1. 新疆农业大学水利与土木工程学院, 乌鲁木齐, 830052;
  • 2. 新疆水文水资源工程技术研究中心, 乌鲁木齐, 830052;
  • 3. 新疆水利工程安全与灾害防治重点实验室, 乌鲁木齐, 830052
基金项目:

国家自然科学基金(41662016)资助.

摘要: 以2017年新疆和田地区平原区240组地下水水质检测数据为基础,综合运用离子比、Gibbs模型和氯碱指数等方法对其地下水硬度空间分布特征及影响因素进行分析.结果表明,水平方向上,高硬度地下水主要分布在研究区中北部靠近沙漠一带呈面状分布,总体呈现自南向北逐渐递增的趋势;垂直方向上,单一结构潜水总硬度随着埋深增加而降低,多层结构潜水-承压水总硬度均值排序为深层承压水(859.9 mg·L-1)、潜水(628.7 mg·L-1)、浅层承压水(471.8 mg·L-1);研究区地下水总硬度空间分布格局主要受水文地球化学作用和水化学环境因素共同影响,其中水文地球化学作用占主导因素.离子来源分析表明,该区地下水总硬度中Ca2+和Mg2+来源于蒸发盐岩与碳酸盐岩的风化溶解和阳离子交替吸附作用.

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