Aso-Kai is a brackish lagoon separated by sand bar of Amanohashidate, one of the three noted views of Japan, from Miyazu Bay, having an area of 5 km
2 and an average depth of 8.4m. COD data of the surface water have often exceeded 3 mg·
l-1 and transparencies have been less than 2m, following the progress of water pollution since about 1970. Investigation of standing mass of COD, nitrogen and phosphorus and the factors determining them is quite important in explaining the mechanism of Aso-Kai's water pollution.
In this research, the authors studied the tidal exchange ratio of Aso-Kai's water with the open-sea water of Miyazu Bay through two channels which is considered one of the factors controlling them.
The results are as follows :
1) According to the survey in October, 1980, the tidal exchange ratios at flood tide and ebb tide were about 0.84 and 0.55 respectively, and the tidal exchange ratio (
rG) that Aso-Kai's water exchange directly with Miyazu Bay's in one tidal cycle was about 0.49;
2) It was estimated that
rG changed seasonally and it was generally high from winter to spring and low from summer to autumn. The median of estimated
rG of each month varied between 0.29 and 0.61.
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