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Benthic nutrient recycling in shallow coastal waters of the Bohai Sea
作者姓名:刘素美  张经  陈洪涛  T.Raabe
作者单位:[1]CollegeofChemistryandChemicalEngineering,OceanUniversityofQingdao,Qingdao266003,China [2]CollegeofChemistryandChemicalEngineering,OceanUniversityofQingdao,Qingdao266003,China [3]StateKeyLaboratoryofEstuarineandCoastalResearch,EastChinaNormalUniversity,Shanghai200062,China [4]InstituteofBiogeochemistryandMarineChemistry,Universi~'ofHamburg,Martin-Luther-King-Platz6,20146Hamburg,Germany
基金项目:This study was funded by NSFC (Nos. 40036010 and 40206017),and the Special Funds from National Key Basic Research Program of P. R. China (No. 2001CB409703).
摘    要:Sediment-water fluxes of N and P species in the Bohai Sea were investigated in September-October 1998 and April-May 1999. The benthic fluxes of nutrient species were determined by incubating sediment core samples with bottom seawater bubbled with air or nitrogen. NO^-2,NH4, dissolved organic nitrogen (DON) and phosphorus (DOP), total dissolved nitrogen (TDN) and phosphorus (TDP), and PO4^3- showed a net exchange flux from seawater to sediment, while NO^-3, dissolved inorganic nitrogen (DIN) and SiO3^2- were released from sediment to seawater in the Bohai Sea. Sediment-water nutrient exchange increases DIN and reduces the phosphorus load in the Bohai Sea. The release of silicate from sediment to overlying seawater reduces potential silicate limitation of primary production resulted from decrease of riverine discharge.The exchange flux of nutrients showed no obvious seasonal variation. The present study showed that the concentrations and composition of nutrients in the water column were affected by suspended sediment, and that not all the exchangeable phosphate in sediment could be released via sediment resuspension.

关 键 词:沉积水层交换  营养元素  渤海  生态吸附
收稿时间:18 June 2003
修稿时间:12 December 2003

Benthic nutrient recycling in shallow coastal waters of the Bohai Sea
Liu?Sumei,Zhang?Jing,Chen?Hongtao,T.?Raabe.Benthic nutrient recycling in shallow coastal waters of the Bohai Sea[J].Chinese Journal of Oceanology and Limnology,2004,22(4):365-372.
Authors:Liu Sumei  Zhang Jing  Chen Hongtao  T Raabe
Institution:(1) College of Chemistry and Chemical Engineering, Ocean University of Qingdao, 266003 Qingdao, China;(2) State Key Laboratory of Estuarine and Coastal Research, East China Normal University, 200062 Shanghai, China;(3) Institute of Biogeochemistry and Marine Chemistry, University of Hamburg, Martin-Luther-King-Platz 6, 20146 Hamburg, Germany
Abstract:Sediment-water fluxes of N and P species in the Bohai Sea were investigated in Septem-ber-October 1998 and April-May 1999. The benthic fluxes of nutrient species were determined by incubating sediment core samples with bottom seawater bubbled with air or nitrogen. -2NO,+4NH, dissolved organic nitrogen (DON) and phosphorus (DOP), total dissolved nitrogen (TDN) and phosphorus (TDP), and -34PO showed a net exchange flux from seawater to sediment, while -3NO, dissolved inorganic nitrogen (DIN) and -23SiO were released from sediment to seawater in the Bohai Sea. Sediment-water nutrient exchange increases DIN and reduces the phosphorus load in the Bohai Sea. The release of silicate from sediment to overlying seawater reduces potential silicate limitation of primary production resulted from decrease of riverine discharge. The exchange flux of nutrients showed no obvious seasonal variation. The present study showed that the concentrations and composition of nutrients in the water column were affected by suspended sediment, and that not all the exchangeable phosphate in sediment could be released via sediment resuspension.
Keywords:sediment-water exchange  nutrient elements  adsorption  release  Bohai Sea  
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