华北平原与大同盆地原生高碘地下水赋存主控因素的异同

王雨婷; 李俊霞; 薛肖斌; 田小伟; 迟秀成

doi:10.3799/dqkx.2019.261

Volume 46 Issue 1

Jan. 2021

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Wang Yuting, Li Junxia, Xue Xiaobin, Tian Xiaowei, Chi Xiucheng, 2021. Similarities and Differences of Main Controlling Factors of Natural High Iodine Groundwater between North China Plain and Datong Basin. Earth Science, 46(1): 308-320. doi: 10.3799/dqkx.2019.261

Citation:

Wang Yuting, Li Junxia, Xue Xiaobin, Tian Xiaowei, Chi Xiucheng, 2021. Similarities and Differences of Main Controlling Factors of Natural High Iodine Groundwater between North China Plain and Datong Basin. Earth Science, 46(1): 308-320. doi: 10.3799/dqkx.2019.261

Citation:

Wang Yuting, Li Junxia, Xue Xiaobin, Tian Xiaowei, Chi Xiucheng, 2021. Similarities and Differences of Main Controlling Factors of Natural High Iodine Groundwater between North China Plain and Datong Basin. Earth Science, 46(1): 308-320. doi: 10.3799/dqkx.2019.261

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Similarities and Differences of Main Controlling Factors of Natural High Iodine Groundwater between North China Plain and Datong Basin

doi: 10.3799/dqkx.2019.261

Wang Yuting^{1
,
,},
Li Junxia^{1, 2, 3
,
,
,},
Xue Xiaobin^{1, 2},
Tian Xiaowei⁴,
Chi Xiucheng⁴

1.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
3.
Laboratory of Basin Hydrology and Wetland Eco-Restoration, China University of Geosciences, Wuhan 430074, China
4.
The Fourth Team of Hydrogeological and Engineering Geology, Hebei Bureau of Geo-Exploration, Cangzhou 061000, China

Received Date: 2019-10-22
Publish Date: 2021-01-15

Abstract

Abstract

Natural high iodine groundwater is widely distributed in China. In order to find out the similarities and differences of mechanism of iodine occurrence in groundwater,the Datong basin and the North China Plain (NCP) were selected as representative areas in this study.Groundwater sampling and the analysis of hydrochemistry and iodine species were performed to understand the groundwater environment and hydrochemical evolution.The results showed that total iodine concentration in groundwater from Datong basin was 2.86-1 286 μg/L,and that in NCP was 2.40-1 106 μg/L. Approximately 50.0% and 49.5% of groundwater iodine from Datong basin and North China Plain exceed the national standard of 100 μg/L(GB19380- 2016),respectively. At the Datong basin,the groundwater environment was characterized by organic matter-rich,alkaline,weak reducing and Na-HCO₃ type water,which was formed by Quaternary fluvial and lacustrine deposits. Under this environment,the sediment iodine was prone to be released into groundwater in the form of iodide and further enrich in the discharge area along the groundwater flow direction.At the NCP,the six transgressions in the Quaternary leads to the alluvial-lacustrine and marine loose sediments rich in Na,Cl and I. At the coastal area,the alkaline and weak reducing conditions in combination with low hydraulic gradient were favorable for iodine release from aquifer matrix to groundwater.The main species of iodine in groundwater was also iodide.The differences between two areas was that high iodine groundwater at Datong basin was mainly influenced by enriched organic matter in groundwater system,while that at NCP was mainly controlled by iodine-rich marine sediments.
- iodine,
- Datong basin,
- North China Plain,
- groundwater,
- controlling factors,
- environmental geology

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References(55)

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Similarities and Differences of Main Controlling Factors of Natural High Iodine Groundwater between North China Plain and Datong Basin

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