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太湖藻源性"湖泛"形成机制的气象因素分析
引用本文:王成林,张咏,张宁红,钱新,孔繁翔. 太湖藻源性"湖泛"形成机制的气象因素分析[J]. 环境科学, 2011, 32(2): 401-408
作者姓名:王成林  张咏  张宁红  钱新  孔繁翔
作者单位:1. 解放军理工大学气象学院,南京,211101
2. 江苏省环境监测中心,南京,210036
3. 南京大学环境学院,污染控制与资源化研究国家重点实验室,南京,210093
4. 中国科学院南京地理与湖泊研究所湖泊与环境国家重点实验室,南京,210008
基金项目:解放军理工大学基础理论研究基金项目(2008009);江苏省环保厅重点科研项目(2008010);江苏省环境监测科研基金项目(0919);国家重点基础研究发展规划(973)项目(2008CB418003);国家自然科学基金项目(40805046/D0508)
摘    要:将蓝藻水华引发的太湖水域黑臭水团现象称为藻源性"湖泛",并将其形成过程分为藻源形成、厌氧反应产物"泛"起、黑臭水团聚积3个阶段.针对2007年5月和2008年5月2次藻源性"湖泛"形成过程中气象要素演变的共同特征,结合水动力模型研究发现,适宜的气象条件提供了必要的热力与动力环境,是诱发"湖泛"形成的必要因素之一.第1阶...

关 键 词:"  湖泛"    太湖  蓝藻水华  热力与动力机制  气象因素
收稿时间:2010-03-23
修稿时间:2010-08-10

Analysis of Meteorological Factors of Forming Feculent and Anaerobic Water Aggregation Induced by Algal Bloom in Taihu Lake
WANG Cheng-lin,ZHANG Yong,ZHANG Ning-hong,QIAN Xin and KONG Fan-xiang. Analysis of Meteorological Factors of Forming Feculent and Anaerobic Water Aggregation Induced by Algal Bloom in Taihu Lake[J]. Chinese Journal of Environmental Science, 2011, 32(2): 401-408
Authors:WANG Cheng-lin  ZHANG Yong  ZHANG Ning-hong  QIAN Xin  KONG Fan-xiang
Affiliation:Institute of Meteorology, People's Liberation Army University of Science and Technology, Nanjing 211101, China. chenglinwang@126.com
Abstract:The water quality pollution problem about feculent and anaerobic water aggregation (FAWA) induced by algal bloom in Taihu Lake, which is often called 'hufan' in Chinese, was studied. Its forming process is divided into 3 phases, i. e., material elements forming of FAWA, anaerobic products to be brought to the water surface and the maintaining of FAWA in the water surface. The conventional observational data from Wuxi meteorological station was analyzed. The result shows that there are similar meteorological characteristics of two FAWA phenomena in Taihu Lake in May, 2007 and May, 2008. A numerical simulation was performed to prove the analysis results. It indicates that propitious meteorological condition is one of the necessary forming factors of FAWA, which provides thermal and dynamical environment for FAWA. During the first phase, the weather conditions, such as high air temperature, gentle breeze and nearly invariable wind direction, maintain for more than 3 days and cause algal bloom to aggregate, then die, sink and anaerobic decay near lake bank. All these provide the precondition for FAWA. During the second phase, when the cold air mass passes across the Taihu basin, almost counter-direction wind, which maintains for more than 1 day with higher speed and lower air temperature, makes anaerobic products to be brought to the water surface by uplifted current. This is the trigger mechanism of FAWA. During the last phase, continual high air temperature and gentle breeze is favorable for FAWA in the water surface. Because meteorological factors are predictable, this research provides a way and basis for the further study of warning and controlling approaches of FAWA.
Keywords:feculent and anaerobic water aggregation (FAWA)   Taihu Lake   algal bloom   thermal and dynamical mechanism   meteorological factors
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