后套平原浅层高氟地下水分布及成因

陈占强; 马腾; 陈柳竹; 武显仓; 巨凡凡; 刘文辉

doi:10.3799/dqkx.2021.237

Volume 48 Issue 10

Oct. 2023

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Article Navigation > Earth Science > 2023 > 48(10): 3856-3865

Chen Zhanqiang, Ma Teng, Chen Liuzhu, Wu Xiancang, Ju Fanfan, Liu Wenhui, 2023. Distribution and Formation of Shallow Groundwater with High Fluoride in Houtao Plain. Earth Science, 48(10): 3856-3865. doi: 10.3799/dqkx.2021.237

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Chen Zhanqiang, Ma Teng, Chen Liuzhu, Wu Xiancang, Ju Fanfan, Liu Wenhui, 2023. Distribution and Formation of Shallow Groundwater with High Fluoride in Houtao Plain. Earth Science, 48(10): 3856-3865. doi: 10.3799/dqkx.2021.237

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Distribution and Formation of Shallow Groundwater with High Fluoride in Houtao Plain

doi: 10.3799/dqkx.2021.237

Chen Zhanqiang^{1
,
,},
Ma Teng^{1, 2
,
,},
Chen Liuzhu¹,
Wu Xiancang¹,
Ju Fanfan¹,
Liu Wenhui¹

1.
School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
2.
College of Resource and Environmental Engineering, Wuhan University of Science and Technology, Wuhan 430081, China

Received Date: 2021-09-25
Available Online: 2023-10-31
Publish Date: 2023-10-25

Abstract

Abstract

In order to investigate the distribution and formation of shallow groundwater with high fluoride in Houtao plain, Inner Mongolia, 64 group hydrochemistry data of shallow groundwater were analyzed using correlation, Gibbs diagram, mineral saturation index, ion intensity and chlor-alkali index. The results show that 53.1% of the shallow groundwater samples have a F^- concentration exceeding the limit value of drinking water standard of China (1.0 mg/L). The shallow groundwater samples with high fluorine mainly distribute in the Yellow River flood plain, eastern Houtao plain, and most of them were Cl-Na type water with high TDS value and weak alkalinity. Fluoride in shallow groundwater mainly came from fluorine-containing minerals such as fluorite in the surrounding rock of Yin Mountain and water-bearing media in the plain. Limited by the topography, climate and irrigation activities, the formation of high fluoride groundwater in Houtao plain was mainly controlled by the evaporation process, which also affected the precipitation-dissolution process. These two processes promoted the release of F^- in the water-bearing media. The effect of cation exchange on the formation of high fluoride groundwater is small because of high ionic strength.
- Houtao plain,
- fluoride,
- groundwater,
- water chemistry,
- hydrogeology

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References(45)

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Distribution and Formation of Shallow Groundwater with High Fluoride in Houtao Plain

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