ABSTRACT: It is said that the tidal current in the Ariake Sea has changed since the construction of the Isahaya Dyke. The change may bring on the environmental deterioration in the Ariake Sea. Especially in the Isahaya Bay, the emergence of oxygen-deficient water has been prominent. In this study, firstly, we simulated the emergence of oxygen-deficient water by incorporating an ecosystem model into an ocean current model and elucidated the mechanism of such a phenomenon both from physical and biological viewpoints. Secondly, we proposed a local engineering solution, i.e. a seawater-quality enhancer, which mixes bottom and surface waters and discharges the mixture at the depth of euphotic layer, and numerically simulated its effects on the ecosystems. It was shown that 16% of the oxygen-deficient water in the Isahaya Bay is reduced by the apparatus with the flow rate of 1-million-ton water per day and 52 % in the 10-million-ton case 8 weeks after the start of operation. In the future, it is necessary that the reliability of the present model is improved by conducting more accurate simulations with incorporating a benthic model, which is deeply concerned with oxygen-deficient water, and by comparing the computational results with measurements more precisely.
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