华北平原原生富碘地下水系统中碘的迁移富集规律:以石家庄-衡水-沧州剖面为例

薛肖斌; 李俊霞; 钱坤; 谢先军

doi:10.3799/dqkx.2017.564

Volume 43 Issue 3

Mar. 2018

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Xue Xiaobin, Li Junxia, Qian Kun, Xie Xianjun, 2018. Spatial Distribution and Mobilization of Iodine in Groundwater System of North China Plain: Taking Hydrogeological Section from Shijiazhuang, Hengshui to Cangzhou as an Example. Earth Science, 43(3): 910-921. doi: 10.3799/dqkx.2017.564

Citation:

Xue Xiaobin, Li Junxia, Qian Kun, Xie Xianjun, 2018. Spatial Distribution and Mobilization of Iodine in Groundwater System of North China Plain: Taking Hydrogeological Section from Shijiazhuang, Hengshui to Cangzhou as an Example. Earth Science, 43(3): 910-921. doi: 10.3799/dqkx.2017.564

Citation:

Xue Xiaobin, Li Junxia, Qian Kun, Xie Xianjun, 2018. Spatial Distribution and Mobilization of Iodine in Groundwater System of North China Plain: Taking Hydrogeological Section from Shijiazhuang, Hengshui to Cangzhou as an Example. Earth Science, 43(3): 910-921. doi: 10.3799/dqkx.2017.564

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Spatial Distribution and Mobilization of Iodine in Groundwater System of North China Plain: Taking Hydrogeological Section from Shijiazhuang, Hengshui to Cangzhou as an Example

doi: 10.3799/dqkx.2017.564

Xue Xiaobin^{1,2
,},
Li Junxia^{1,2,3
,
,},
Qian Kun^1,2,
Xie Xianjun^1,2,3

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

Received Date: 2017-12-03
Publish Date: 2018-03-15

Abstract

Abstract

High iodine groundwater is another global drinking water safety problem in addition to after high arsenic and high fluorine groundwater. However, the research on the existing forms of iodine and the mechanisms of migration and enrichment of iodine in groundwater system is still insufficient research on the existing forms of iodine and the mechanisms of migration and enrichment of iodine in groundwater system. To understand spatial distribution and mobilization of iodine in groundwater system of North China plain(NCP), a hydrochemical study was conducted. The results show that iodine concentration in groundwater from NCP rangesd from 3.35 to 1 106 μg/L, and 41.86% of groundwater samples has iodine concentration exceeding drinking water level (150 μg/L) recommended by Chinese government. High iodine groundwater (>150 μg/L) is mainly distributed in deep aquifers of Bohai bay area. The main species of groundwater iodine include mainly diodide and iodate, the distribution of which is controlled by redox environment of groundwater, and iodate mainly occurs in oxidizing condition. Along the groundwater flow path from Shijiazhuang, Hengshui to Cangzhou, hydrochemical evolution and inverse modeling were performed to understand the groundwater environment favoring iodine enrichment in groundwater. The results of hydrochemical evolution showed that at Bohai bay area, the weak-alkalinity and (sub)reducing environment influenced by seawater intrusion favor the iodine release and enrichment in groundwater.The adsorption equilibration of iodine among metal oxyhydroxides under various environments is the primary hydrogeochemical process controlling iodine mobilization in the groundwater system of the North China plain.
- iodine,
- mobilization,
- groundwater,
- North China Plain

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References(58)

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Spatial Distribution and Mobilization of Iodine in Groundwater System of North China Plain: Taking Hydrogeological Section from Shijiazhuang, Hengshui to Cangzhou as an Example

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