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滇池流域宝象河暴雨径流初始冲刷效应
引用本文:郭怀成,向男,周丰,王永华,李发荣,朱翔,毛国柱,于书霞,李娜,盛虎,杨永辉,何成杰,王翠榆.滇池流域宝象河暴雨径流初始冲刷效应[J].环境科学,2013,34(4):1298-1307.
作者姓名:郭怀成  向男  周丰  王永华  李发荣  朱翔  毛国柱  于书霞  李娜  盛虎  杨永辉  何成杰  王翠榆
作者单位:1. 北京大学环境科学与工程学院,水沙科学教育部重点实验室,北京100871
2. 北京大学城市与环境学院,地表过程分析与模拟教育部重点实验室,北京 100871
3. 昆明市环境监测中心,昆明,650028
4. 云南省环境科学研究院,昆明,650034
5. 天津大学环境科学与工程学院,天津,300072
6. 华中农业大学资源与环境学院,武汉,430070
基金项目:国家水体污染控制与治理科技重大专项(2008ZX07102-006, 2013ZX07102-06);国家自然科学基金项目(41201077)
摘    要:为了有效理解滇池非点源入湖过程,选择滇池流域宝象河开展暴雨径流初始冲刷效应的初步研究.2009年雨季,在其干流沿程上、中、下游设置3个断面进行了初期3场暴雨及河道水量、水质同步观测,并提出降雨净冲刷量、负荷净冲刷量以及净冲刷径流平均浓度EMCn的定义与计算方法.结果表明,宝象河TSS、TN、TP、高锰酸盐指数的EMCn、累积曲线M(V)随着河道沿程不透水地面比例和人口规模的增加而提高,TSS、TP负荷贡献率及其M(V)与降雨强度的变化趋势一致,而TN和高锰酸盐指数负荷贡献率则与降雨量表现正相关,其中TN中NO3--N所占比例随着降雨事件次数增加而逐渐降低;此外,提出的EMCn也被证实能有效消除各点位的基流及其负荷影响,相对冲刷径流平均浓度,更为真实反映且能放大沿程断面间、不同降雨事件间的暴雨初始冲刷效应的差异.

关 键 词:河流暴雨径流  冲刷径流平均浓度  富营养化  非点源污染  滇池
收稿时间:2012/6/14 0:00:00
修稿时间:2012/9/27 0:00:00

First Flush Effects of Storm Events of Baoxiang River in Lake Dianchi Watershed
GUO Huai-cheng,XIANG Nan,ZHOU Feng,WANG Yong-hu,LI Fa-rong,ZHU Xiang,MAO Guo-zhu,YU Shu-xi,LI N,SHENG Hu,YANG Yong-hui,HE Cheng-jie and WANG Cui-yu.First Flush Effects of Storm Events of Baoxiang River in Lake Dianchi Watershed[J].Chinese Journal of Environmental Science,2013,34(4):1298-1307.
Authors:GUO Huai-cheng  XIANG Nan  ZHOU Feng  WANG Yong-hu  LI Fa-rong  ZHU Xiang  MAO Guo-zhu  YU Shu-xi  LI N  SHENG Hu  YANG Yong-hui  HE Cheng-jie and WANG Cui-yu
Institution:Laboratory of Water and Sediment Sciences, Ministry of Education, College of Environmental Sciences and Engineering, Peking University, Beijing 100871,China;Laboratory of Water and Sediment Sciences, Ministry of Education, College of Environmental Sciences and Engineering, Peking University, Beijing 100871,China;Laboratory for Earth Surface Process, Ministry of Education, College of Urban and Environmental Sciences, Peking University, Beijing 100871,China;Laboratory for Earth Surface Process, Ministry of Education, College of Urban and Environmental Sciences, Peking University, Beijing 100871,China;Kunming Environmental Monitoring Center, Kunming 650028,China;Yunnan Institute of Environmental Science, Kunming 650034,China;School of Environmental Science and Engineering, Tianjin University,Tianjin 300072,China;College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070,China;Laboratory of Water and Sediment Sciences, Ministry of Education, College of Environmental Sciences and Engineering, Peking University, Beijing 100871,China;Laboratory of Water and Sediment Sciences, Ministry of Education, College of Environmental Sciences and Engineering, Peking University, Beijing 100871,China;Laboratory of Water and Sediment Sciences, Ministry of Education, College of Environmental Sciences and Engineering, Peking University, Beijing 100871,China;Laboratory of Water and Sediment Sciences, Ministry of Education, College of Environmental Sciences and Engineering, Peking University, Beijing 100871,China;Laboratory of Water and Sediment Sciences, Ministry of Education, College of Environmental Sciences and Engineering, Peking University, Beijing 100871,China
Abstract:
Keywords:riverine storm runoff  event mean concentration  eutrophication  non-point source  Lake Dianchi
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