A soil circulation occurs in the south of Cheju Island in the spring. Nutrients and its influence on chloro-phyll a （Chla） around the circulations were studied from April 9 to May 6, 2007. Spring bloom with elevated...A soil circulation occurs in the south of Cheju Island in the spring. Nutrients and its influence on chloro-phyll a （Chla） around the circulations were studied from April 9 to May 6, 2007. Spring bloom with elevated concentrations of Chla was observed during the investigation. High concentrations of phosphate, nitrate and silicate at 0.6, 12, and 8 mmol/m3, respectively, were detected. A low water temperature prevented the growth of phytoplankton. Chla concentrations in the study area might be strongly associated with the high silicate concentration.展开更多
基金The National Marine Important Charity Special Foundation of China under contract No.201305019the National Natural Science Foundation of China under contract No.41340049+4 种基金Guangdong Planning of Philosophy and Social Science Funding Projectsunder contract No.GD12YGL04Foundation for Distinguished Yong Talents in Higher Education of Guangdong under contract No.2012WYM_0077the Post-Doctoral Starting Fund of Zhejiang under contract No.BSH1301015Second Institute of Oceanography,State Oceanic Administration Post-Doctoral Starting Fund of china under contract Nos JG1208 and JG1319Guangdong Ocean University Doctor Starting Fund of China under contract Nos E11332,E11097 and E12248
文摘A soil circulation occurs in the south of Cheju Island in the spring. Nutrients and its influence on chloro-phyll a （Chla） around the circulations were studied from April 9 to May 6, 2007. Spring bloom with elevated concentrations of Chla was observed during the investigation. High concentrations of phosphate, nitrate and silicate at 0.6, 12, and 8 mmol/m3, respectively, were detected. A low water temperature prevented the growth of phytoplankton. Chla concentrations in the study area might be strongly associated with the high silicate concentration.
