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Ise Bay and Mikawa Bay are typical semi-enclosed bays. For this reason in both bays oxygen-deficient water mass is generated mainly during summer and has caused heavy damage to the sea area environment. It is important to reduce the generation of the oxygen deficient water mass to improve the sea area environment of both bays. In this research, a field investigation was conducted to find out the behavior of the oxygendeficient water mass in Ise Bay and Mikawa Bay. As a result, it was confirmed that a physical process that forms isolated water mass at the bottom layer in the central part of the bay has caused the oxygen -deficient water mass in Ise Bay. On the other hand, it was found out that the stratification developed by the inflow of fresh water on the eastern side of the bay has generated the oxygen-deficient water mass in Mikawa Bay.

THE BEHAVIOR OF OXYGEN-DEFICIENT WATER MASS IN ISE BAY AND MIKAWA BAY