Abstract
The lack of data such as nutrient release rate and denitrification rate in enclosed bays sometimes makes it difficult to grasp the structure of the nutrient budget that is essential to solve the problemsin estuaries such as red tides, anoxic events etc. We conducted field observation of the nutrient release rate and denitrification rate in the head of Ariake bay using the nitrogen isotope pairing, for the purpose of figuring out the changes and distributions of those fluxes, and also analyzed the sediment such as carbon stable isotope, quinone profile, carbon content so as to find out the mechanism and the key factor of those nutrient fluxes.
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