华北平原地下水碘形态及其对碘富集的潜在影响

Junxia Li, Kun Qian, Yijun Yang, Xianjun Xie
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引用次数: 6

摘要

为了揭示华北平原地下水中碘的空间分布规律,沿区域地下水流道共采集了136份地下水样品。结果表明,地下水碘含量在1.51 ~ 1106μg/L之间,其中31.4%的样品碘浓度高于150μg/L。高碘地下水样品主要分布在渤海沿岸地区,井深大于350 m。碘形态分析结果表明,地下水碘、碘酸盐和有机碘的分布范围分别为0.025 ~ 854μg/L、0.035 ~ 293μg/L和10 ~ 296μg/L,表明碘化物是NCP地下水碘的优势形态。碘酸盐仅在Eh值大于0mV的地下水中存在,说明地下水氧化还原条件是控制碘形态形成的主要因素。广泛的亚还原/还原条件和低亲和力是促使地下水中碘富集的两个主要因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Iodine Speciation and its Potential Influence on Iodine Enrichment in Groundwater from North China Plain

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 1106μg/L, and 31.4% of the samples have iodine concentrations higher than 150μg/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∼854μg/L, <0.035∼293μg/L and <10∼296μg/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 0mV, 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.

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