Distribution and Hydrogeochemical Characteristic of High Iodine Groundwater in Oasis Zone in the Tarim Basin in Xinjiang,China  

作　　者：Ying Sun Yinzhu Zhou Jinlong Zhou Yanyan Zeng Yuanyuan Ji Mi Lei 

机构地区：[1]College of Hydraulic and Civil Engineering,Xinjiang Agricultural University,Urumqi 830052,China [2]Xinjiang Hydrology and Water Resources Engineering Research Center,Urumqi 830052,China [3]Xinjiang Key Laboratory of Hydraulic Engineering Security and Water Disasters Prevention,Urumqi 830052,China [4]Center for Hydrogeology and Environmental Geology,China Geological Survey,Tianjin 300304,China [5]Xinjiang Agricultural Professional Technological College,Changji 831100,China

出　　处：《Journal of Earth Science》2025年第1期173-183,共11页地球科学学刊(英文版)

基　　金：financially supported by the National Natural Science Foundation of China(Nos.42067035 and 42007161);Water Conservancy Engineering Key Discipline Project of Xinjiang Agricultural University(No.SLXK2019-10);the Opening Project of Xinjiang Key Laboratory of Hydraulic Engineering Security and Water Disasters Prevention in 2021(No.ZDSYS-JS-2021-10)。

摘　　要：Groundwater is the main water supply source in the Tarim Basin in China.Endemic disease caused by high iodine(I)groundwater in the Tarim Basin was reported previously.Therefore,it is crucial to systematically identify the distribution and genesis of groundwater I.Based on hydrochemical analysis of 717 groundwater samples collected in 2015–2018,spatial distribution and hydrogeochemistry characteristic of high I groundwater in different aquifers were analyzed.Results showed that groundwater I ranged between<10.00 and 4000.00μg/L(mean of 53.71μg/L).High I groundwater(I>100.00μg/L)accounted for 7.25%of the total samples.Horizontally,groundwater I significantly increased from recharge zone(RZ)to transition zone(TZ)and to evaporation zone(EZ).Vertically,groundwater in shallow confined aquifer(SCA)had the greatest I concentration,followed by single-structure phreatic aquifer(SSPA),phreatic aquifer in confined groundwater area(PACGA),while groundwater in deep confined aquifer(DCA)generally had low I concentration.Groundwater I enrichment in SSPA was mainly affected by organic matter(OM)decomposition and that in SCA was mainly affected by evaporite mineral dissolution,OM decomposition under alkaline environment.While I enrichment in groundwater of PACGA was restrained under neutral environment.Lacustrine sedimentary environment was crucial for I enrichment in groundwater.Besides,fine-grained lithology of aquifer,smooth topographic slope,shallow buried depth of groundwater,weak alkaline and reducing environment,reductive dissolution of iron oxide/hydroxide minerals and OM decomposition were advantageous to I enrichment in groundwater.

关 键 词：high iodine GROUNDWATER hydrogeochemical processes depositional environment hydrogeological condition Tarim Basin 

分 类 号：P641.3[天文地球—地质矿产勘探]