TY - JOUR
T1 - Inventory of nutrient compounds in the Yellow Sea
AU - Liu, S. M.
AU - Zhang, J.
AU - Chen, S. Z.
AU - Chen, H. T.
AU - Hong, G. H.
AU - Wei, H.
AU - Wu, Q. M.
PY - 2003
Y1 - 2003
N2 - Nutrient species were analyzed from samples collected in the Yellow Sea in May 1998, including NO3-, NO2-, NH4+, PO43-, SiO3 2-, dissolved organic nitrogen (DON), particulate nitrogen, dissolved organic phosphorus (DOP), particulate phosphorus, etc. The exchange fluxes of nutrients across the sediment/water interface were determined by incubation of sediment on board the ship. The concentrations of N, P and Si compounds were high in coastal areas of the Yellow Sea, reflecting the effects of the Changjiang effluent plume, surface runoff in the west and east coasts and the circulation in the Yellow Sea. The high proportions of DON and DOP should be considered in models of nutrients cycling, which could help to explain observations of nutrient limitation in ecosystems of the Yellow Sea. The vertical distribution of N, P and Si compounds in the water column showed stratification feature. Simple box model was used to estimate the water-mass balance and nutrient budgets for the Yellow Sea. The data suggested that water turn-over time is about 2.2 years. Nutrient budgets demonstrated that net sink of NO3-, NH4+ and SiO 32- can be mainly from water column into bottom sediments and/or transform to other forms of nitrogen (e.g. particulate pool and gas species). A net source of PO43- is estimated to be 75% of inputs from external sources in the Yellow Sea.
AB - Nutrient species were analyzed from samples collected in the Yellow Sea in May 1998, including NO3-, NO2-, NH4+, PO43-, SiO3 2-, dissolved organic nitrogen (DON), particulate nitrogen, dissolved organic phosphorus (DOP), particulate phosphorus, etc. The exchange fluxes of nutrients across the sediment/water interface were determined by incubation of sediment on board the ship. The concentrations of N, P and Si compounds were high in coastal areas of the Yellow Sea, reflecting the effects of the Changjiang effluent plume, surface runoff in the west and east coasts and the circulation in the Yellow Sea. The high proportions of DON and DOP should be considered in models of nutrients cycling, which could help to explain observations of nutrient limitation in ecosystems of the Yellow Sea. The vertical distribution of N, P and Si compounds in the water column showed stratification feature. Simple box model was used to estimate the water-mass balance and nutrient budgets for the Yellow Sea. The data suggested that water turn-over time is about 2.2 years. Nutrient budgets demonstrated that net sink of NO3-, NH4+ and SiO 32- can be mainly from water column into bottom sediments and/or transform to other forms of nitrogen (e.g. particulate pool and gas species). A net source of PO43- is estimated to be 75% of inputs from external sources in the Yellow Sea.
KW - Atmospheric deposition
KW - Budget
KW - Nutrients
KW - Riverine input
KW - Sediment-water exchange
KW - Yellow Sea
UR - https://www.scopus.com/pages/publications/0242660851
U2 - 10.1016/S0278-4343(03)00089-X
DO - 10.1016/S0278-4343(03)00089-X
M3 - 文章
AN - SCOPUS:0242660851
SN - 0278-4343
VL - 23
SP - 1161
EP - 1174
JO - Continental Shelf Research
JF - Continental Shelf Research
IS - 11-13
ER -