SPATIAL VARIATION OF WITHIN-DAY AND BETWEEN-DAY CHLOROPHYLL A DYNAMICS DURING SUMMER IN GUANTING RESERVOIR, BEIJING, CHINA

被引:4
作者
Jiang, W. W. [1 ]
Yu, J. S. [1 ]
Li, Z. J. [1 ]
Nakamura, T. [2 ]
Yu, F. Q. [1 ]
Zhang, J. Y. [3 ]
机构
[1] Beijing Normal Univ, Key Lab Urban Hydrol Cycle & Sponge City Technol, Digital Watershed Lab, Coll Water Sci, Beijing 100875, Peoples R China
[2] Tokyo Inst Technol, Dept Global Engn Dev Environm & Soc, Yokohama, Kanagawa 2268502, Japan
[3] Shijiazhuang Hydrol & Water Resources Survey Bur, Shijiazhuang 050051, Hebei, Peoples R China
来源
APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH | 2019年 / 17卷 / 03期
基金
中国国家自然科学基金;
关键词
eutrophication; reservoir stratification; phytoplankton occurrence; meteorological factors; short-term distribution; PHYTOPLANKTON DISTRIBUTION; MICROCYSTIS-AERUGINOSA; VERTICAL-DISTRIBUTION; LAKE; LIGHT; WIND; CYANOBACTERIA; TEMPERATURE; COMMUNITY; BLOOMS;
D O I
10.15666/aeer/1703_57655780
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Recognizing intra- and inter-daily dynamics of chlorophyll a (Chl-a) and its related environmental variables on consecutive days is essential to assessing and managing water quality and eutrophication. In this study, the Chl-a concentration, nutrients, water temperature and meteorological factors in Guanting Reservoir in Beijing were collected at six sampling times during summer. The Chl-a concentration generally decreased from May to September. At both test times, thermal stratification and mixing in the water column controlled temporal and vertical variations in the maximum Chl-a concentration layer. The position of the maximum Chl-a concentration layer between days generally followed that of the thermocline. Daily stratifications were temporary and downwelling variations in the maximum Chl-a concentration layer were wind driven; therefore, the vertical distribution of Chl-a was homogenized at night. Surface Chl-a concentrations increased at night and decreased during the day, except on rainy days. Principal component analysis and Pearson's correlations indicated that daily average and raw surface Chl-a concentrations generally changed as a negative function of air temperature, solar radiation, wind speed and water temperature. However, when a 5-hour time lag was considered, the relationship between surface Chl-a concentration, all meteorological factors and water temperature became significantly positive.
引用
收藏
页码:5765 / 5780
页数:16
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