邯郸地区典型剖面浅层地下水碘分布特征及成因初探  

The Iodine Distribution Characteristics and Causes of Groundwater in Typical Section in Handan

作　　者：张宝匀 简明[2] 张媛静[3] 李亚松[3] 

机构地区：[1]中国地质大学(北京)地下水资源与环境学院,北京100083 [2]河北省地矿局第四水文工程地质大队,河北沧州061000 [3]中国地质科学院水文地质环境地质研究所,石家庄050061

出　　处：《湖北农业科学》2015年第20期5004-5007,共4页Hubei Agricultural Sciences

基　　金：全国地下水基础环境状况调查评估项目(2110302);国家自然科学基金项目(41402235)

摘　　要：邯郸地区大多数居民以地下水作为主要或者惟一的供水水源,地下水碘含量以及食用碘盐的情况成为了影响居民健康的重要因素。在邯郸地区选择典型剖面开展了地下水碘分布及配碘情况调查,共采集了17组地下水样品进行碘化物含量分析,基本掌握了该剖面地下水碘化物浓度分布状况。分析发现地下水碘分布受地质条件、水文地质条件等内在因素,以及气候条件等外在因素的控制,并结合配碘调查结果提出了合理配碘建议。In Handan area, most of the residents take groundwater as the main or the only source of water supply, groundwater and the situation of the consumption of iodized salt iodine content became important factors which influencing the residents＇ health. Basic on the selection of typical section in Handan area groundwater distribution of iodine and iodine investigation, collected a total of 17 pairs of groundwater samples collected iodide content analysis, basically mastered the profile iodide concentration distribution of groundwater. Also, found that groundwater iodine distribution was affected by some internal factors like geological condition, hydrogeological condition, and other external factors like the climate condition. Combining with iodine results,reasonable iodine suggestions were put forward.

关 键 词：邯郸地区 地下水 碘 成因 

分 类 号：P641.69[天文地球—地质矿产勘探]