Iodine speciation and its potential influence on iodine enrichment in groundwater from North China Plain

被引:9
|
作者
Li, Junxia [1 ,2 ]
Qian, Kun [1 ,2 ]
Yang, Yijun [1 ,2 ]
Xie, Xianjun [1 ,2 ]
机构
[1] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China
[2] China Univ Geosci, Sch Environm Studies, Wuhan 430074, Peoples R China
基金
中国国家自然科学基金;
关键词
Iodine; Speciation; North China Plain; Groundwater; SEDIMENTS; SORPTION; IODATE;
D O I
10.1016/j.proeps.2016.12.069
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In order to reveal the pattern of spatial distribution of iodine in groundwater at North China Plain (NCP), a total of 136 groundwater samples were collected along the regional groundwater flow paths. The results showed that groundwater iodine ranged from 1.51 to 1106 mu g/L, and 31.4% of the samples have iodine concentrations higher than 150 mu g/L. High iodine groundwater samples are mainly observed in the coastal area of Bohai sea, and well depths greater than 350 m. The results of iodine speciation analysis showed that groundwater iodide, iodate and organic iodine had the ranges of < 0.025 similar to 854 mu g/L, < 0.035 similar to 293 mu g/L and < 10 similar to 296 mu g/L, respectively, indicating that iodide is the dominant species of iodine in groundwater at NCP. Iodate is only observed in groundwater with Eh values higher than 0 mV, suggesting that groundwater redox condition is the main factor controlling iodine speciation. The widespread sub-reducing/reducing condition and low affinity of iodide are the two main factors promoting the iodine enrichment in groundwater. (C) 2017 The Authors. Published by Elsevier B.V.
引用
收藏
页码:312 / 315
页数:4
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