塔里木盆地南缘浅层高碘地下水的分布及成因：以新疆民丰县平原区为例

孙英; 周金龙; 梁杏; 周殷竹; 曾妍妍; 林丽

doi:10.3799/dqkx.2020.260

Volume 46 Issue 8

Aug. 2021

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Sun Ying, Zhou Jinlong, Liang Xing, Zhou Yinzhu, Zeng Yanyan, Lin Li, 2021. Distribution and Genesis of Shallow High-Iodine Groundwater in Southern Margin of Tarim Basin: A Case Study of Plain Area in Minfeng County, Xinjiang. Earth Science, 46(8): 2999-3011. doi: 10.3799/dqkx.2020.260

Citation:

Sun Ying, Zhou Jinlong, Liang Xing, Zhou Yinzhu, Zeng Yanyan, Lin Li, 2021. Distribution and Genesis of Shallow High-Iodine Groundwater in Southern Margin of Tarim Basin: A Case Study of Plain Area in Minfeng County, Xinjiang. Earth Science, 46(8): 2999-3011. doi: 10.3799/dqkx.2020.260

Citation:

Sun Ying, Zhou Jinlong, Liang Xing, Zhou Yinzhu, Zeng Yanyan, Lin Li, 2021. Distribution and Genesis of Shallow High-Iodine Groundwater in Southern Margin of Tarim Basin: A Case Study of Plain Area in Minfeng County, Xinjiang. Earth Science, 46(8): 2999-3011. doi: 10.3799/dqkx.2020.260

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Distribution and Genesis of Shallow High-Iodine Groundwater in Southern Margin of Tarim Basin: A Case Study of Plain Area in Minfeng County, Xinjiang

doi: 10.3799/dqkx.2020.260

Sun Ying^{1, 2
,
,},
Zhou Jinlong^{1, 2
,
,
,},
Liang Xing³,
Zhou Yinzhu⁴,
Zeng Yanyan^{1, 2},
Lin Li^{1, 2}

1.
College of Water Conservancy and Civil Engineering, Xinjiang Agricultural University, Urumqi 830052, China
2.
Xinjiang Hydrology and Water Resources Engineering Research Center, Urumqi 830052, China
3.
School of Environmental Studies, China University of Geosciences, Wuhan 430078, China
4.
Center for Hydrogeology and Environmental Geology, China Geological Survey, Baoding 071051, China

Received Date: 2020-05-25
Available Online: 2021-09-14
Publish Date: 2021-08-15

Abstract

Abstract

Tarim Basin is located in the hinterland of Eurasia, far away from the sea. Groundwater is an important source of water supply in the southern margin of Tarim Basin. Based on the 44 groups of shallow groundwater samples from the plain area of Minfeng County in the southern margin of Tarim Basin, Xinjiang Uygur Autonomous Region, the hydrochemical characteristics of unconfined groundwater and shallow confined groundwater, the spatial distribution of iodine and the causes of the high-iodine groundwater were analyzed by using the hydrochemical graphic method, mathematical statistics method and geographic information system (GIS) techniques. The results show that iodine enrichment and iodine deficiency coexist in groundwater in plain area of Minfeng County. The I^- contents in unconfined groundwater and shallow confined groundwater were ≤ 730 μg/L and ≤ 183 μg/L respectively. The proportions of iodine deficient water, suitable iodine water, high iodine water and ultra-high iodine water in unconfined groundwater samples were 19.4%, 69.4%, 5.6% and 5.6%, respectively. The proportions of iodine deficient groundwater, suitable iodine water and high iodine water in shallow confined groundwater samples were 12.5%, 75.0% and 12.5%, respectively. From the sloping plain in front of the mountain to the plain in the fine earth, the I^- content in the groundwater increased obviously. The main hydrochemical types of high iodine groundwater and ultra-high iodine groundwater are Cl·SO₄-Na and Cl-Na. In addition to the hydrogeological conditions and alkaline groundwater environment, iodine content in unconfined groundwater is mainly affected by strong evaporation and concentration, Quaternary Holocene swamp deposits and mineral dissolution precipitation, and the shallow confined groundwater is mainly affected by mineral dissolution precipitation and reduction environment.
- high iodine,
- shallow groundwater,
- factor analysis,
- cluster analysis,
- southern margin of Tarim Basin,
- Minfeng County,
- hydrogeology

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References(61)

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Distribution and Genesis of Shallow High-Iodine Groundwater in Southern Margin of Tarim Basin: A Case Study of Plain Area in Minfeng County, Xinjiang

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