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高氟湖库底泥中氟的存在形态分析——以洋沙泡水库为例
引用本文:梁秀娟,方樟,季超,王雪芹,李钦伟.高氟湖库底泥中氟的存在形态分析——以洋沙泡水库为例[J].吉林大学学报(地球科学版),2010,40(3):651-656.
作者姓名:梁秀娟  方樟  季超  王雪芹  李钦伟
作者单位:1.吉林大学 环境与资源学院,长春 130026; 2.吉林省水利水电勘测设计研究院,长春 130021; 3.郑州工业贸易学校,郑州 450007; 4.吉林省电力勘测设计院,长春 130022
基金项目:吉林省科技攻关项目,高等学校博士学科点专项科研基金,"十一·五"国家科技支撑项目 
摘    要:论述了底泥中氟的存在形态及其浸提方法。通过洋沙泡水库底泥氟各种形态的分析实验,发现底泥氟形态的含量分布为残余态水溶态>有机态>铁锰结合态>可交换态;底泥各形态氟含量呈对数分布;水溶性氟质量分数为26.77~112.39 mg/kg,占总氟的2.699%~19.114%。底泥全氟含量、氟的来源、气候因素的影响、区域理化环境以及湖泊曾数度干涸是造成水溶性氟含量高的主要原因。

关 键 词:底泥    存在形态  影响因素  
收稿时间:2009-06-10

Analysis on the Existing Forms of Fluorine in the Bottom Mud of High Fluorine Lakes and Reservoirs-A Case Study of Yangshapao Reservior
LIANG Xiu-juan,FANG Zhang,JI Chao,WANG Xue-qin,LI Qin-wei.Analysis on the Existing Forms of Fluorine in the Bottom Mud of High Fluorine Lakes and Reservoirs-A Case Study of Yangshapao Reservior[J].Journal of Jilin Unviersity:Earth Science Edition,2010,40(3):651-656.
Authors:LIANG Xiu-juan  FANG Zhang  JI Chao  WANG Xue-qin  LI Qin-wei
Institution:1.College of Environment and Resources, Jilin University|Changchun 130026, China;
2. Jilin Province Water Resources and Hydropower Consulting Company, Changchun 130021, China;
3. Zhengzhou Industry and Trade School, Zhengzhou 450007, China;
4. Jilin Provincial Electric Power Survey and Design Institute, Changchun 130022, China
Abstract:The existing state and extracting method of fluorine in bottom mud are discussed. Based on the experimental analysis of different fluoride forms in the bottom mud of Yangshapao reservoir, the distribution of various fluoride forms in the bottom mud is clear. The content of residual state fluorine is much more than that of water soluble fluorine, more than that of the organic-bound state fluorine, more than that of iron and manganese bound state fluorine, and more than that of exchangeable state fluorine. The fluorine content of different forms in the bottom mud is in logarithmic distribution character. The content of water soluble fluorine is 26.77-112.39 mg/kg,which accounts 2.699%-19.114% of the total fluorine content. The content of the total fluorine in the bottom mud, source of fluorine, the climate factor, the regional physical and chemical environment, and several time dry-out of the lake are considered to be the main factors of the high content of water soluble fluorine depositing into the bottom mud.
Keywords:bottom mud  fluorine  existing forms  influence factors  
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