ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
江苏平原地区(淮河流域)潜水碘含量控制因素探讨
  
关键词:iodine  groundwater  soil  groundwater flow conditions  organic matter
基金项目:中国地质调查局地质大调查项目“江苏平原地区地下水污染调查评价(淮河流域)”(编号: 1212010634504);江苏国土资源厅科技计划项目“淮河污染与江苏沿淮地区饮用水安全关系研究”(编号: 苏国土资发[2011]453文, 序号为201101)
作者单位E-mail
陆徐荣 江苏省地质调查研究院
国土资源部地裂缝地质灾害重点实验室 
lxr1027@126.com 
杨磊 江苏省地质调查研究院
国土资源部地裂缝地质灾害重点实验室 
 
陆华 江苏省地质调查研究院
国土资源部地裂缝地质灾害重点实验室 
 
谷小溪 江苏省地质调查研究院
国土资源部地裂缝地质灾害重点实验室 
 
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摘要:
A Tentative Discussion on the Control Factors of Iodine Content in Phreatic Water in Huaihe River Plains of Jiangsu Province
      Based on an analysis of the distribution of iodine content in phreatic water, soil and hydrogeological conditions and land form, the authors have a new understanding on the control factors of iodine content in groundwater: The previous researchers hold that the iodine content in groundwater is proportional to the organic matter, whereas the authors consider that there is no fixed relationship between the iodine content and organic matter content in groundwater, but the organic matter contributes to the increase of water-soluble iodine content, and they are directly proportional in some areas. Groundwater flow conditions impact significantly the iodine content. The iodine content is often low and in compliance with drinking water standards in hilly land where the runoff conditions are better, whereas the iodine content often exceeds drinking water standards in low-lying areas of poor runoff conditions; The iodine content in groundwater is directly proportional to the content in soil under the same hydrogeological conditions. Another important feature of the iodine concentration in groundwater is that it is very stable and changes very little with time and mining activity.
LU Xu-rong,YANG Lei,LU Hua,GU Xiao-xi.2014.A Tentative Discussion on the Control Factors of Iodine Content in Phreatic Water in Huaihe River Plains of Jiangsu Province[J].Acta Geoscientica Sinica,35(2):211-216.
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