三峡水库水体几种主要阴离子变化特征 |
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引用本文: | 黄礼昕 孙荣国 王永敏 马明 王定勇. 三峡水库水体几种主要阴离子变化特征[J]. 中国农学通报, 2014, 30(23): 184-189. DOI: 10.11924/j.issn.1000-6850.2013-3249 |
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作者姓名: | 黄礼昕 孙荣国 王永敏 马明 王定勇 |
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作者单位: | 1. 土壤多尺度界面过程与调控重庆市重点实验室/西南大学资源环境学院2. 西南大学资源环境学院/三峡库区生态环境教育部重点实验室3. 土壤多尺度界面过程与调控重庆市重点实验室/西南大学资源环境学院;重庆市三峡库区农业面源污染控制工程技术研究中心;重庆市农业资源与环境研究重点实验室4. 西南大学 |
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基金项目: | 公益性行业(农业)科研专项 |
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摘 要: | 为了了解三峡水库典型阴离子(Cl-、NO3-、SO42-)随时间、水位的变化特征,选取三峡水库重庆段长江干流涪陵珍溪、忠县石宝寨和开县长江支流汉丰湖为调查点,每2个月1次,连续1年在调查点设置断面分层采集水样,利用离子色谱仪分析水样中典型阴离子Cl-、NO3-、SO42-浓度随时间、水位的变化特征,并初步分析了变化原因。结果表明:全年研究区SO42-浓度为14.67±1.71 mg/L,Cl-浓度为10.66±4.88 mg/L,NO3-浓度为1.89±0.15 mg/L,随季节变化差异均较为显著(CV>43%),且库区水位变化对干流阴离子含量影响较大;涪陵、忠县和开县各不同采样点之间阴离子浓度变化差异也均较为明显(CV>40%)。春季总离子浓度(平均为13.02 mg/L)普遍高于其他3季。
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关 键 词: | 启动子 启动子 |
收稿时间: | 2013-12-12 |
修稿时间: | 2014-01-22 |
Variation Characteristics of Main Anions in Water Bodies of the Three Gorges Reservoir Area |
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Affiliation: | Huang Lixin1, Sun Rongguo1, Wang Yongmin1, Ma Ming1 2 3, Wang Dingyong1 2 3 (1Chongqing Key Laboratory of Soil Multi-scale Interfacial Process/ College of Resources and Environment, Southwest University, Chongqing 400715; 2Chongqing Engineering Research Center for Agricultural Non-point Source Pollution Control in the Three Gorges Reservoir Area, Chongqing 400716; 3Chongqing Key Laboratory of Agricultural Resources and Environment, Chongqing 4O0716) |
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Abstract: | In order to investigate the changing characteristics of concentrations for typical anions (CI-, NOr, and SO42-) along with the variation of time and water level in water bodies of the Three Gorges Reservoir, Fuling, Shibaozhai in Zhongxian, which are located in the main stream of Yangtze River, and Hanfeng Lake, which is located in the Branch of Yangtze River, were selected as study sites. During the whole year, sections were set in investigate spots for stratified water sampling, and CI-, NO3- and SO42- in water samples were continuously monitored by an Ion chromatography once every two months, with the causes of there change being preliminary analyzed. The results showed that the whole year in research area, ion concentration of SO42-, CI- and NO3- were 14.67_+ 1.71 mg/L, 10.66+4.88 mg/L and 1.89_+0.15 mg/L respectively, and they all displayed significant variations along with seasonal change, with a coefficient variation larger than 43%. Meanwhile, the change of water levels at the dam' s reservoir had great influence on the content of anions in main stream. Variations of anion concentration in different sampling different, with a coefficient variation larger than 40%. sites between Fuling, Zhongxian and Kaixian were quite The total ionic concentration of reservoir area in spring,an average of 13.02 mg/L, was much higher than that in other seasons. |
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Keywords: | temporal and spatial variation |
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