Abstract
In May 2011, a Water Quality Monitor (WQM) hydrological station was maintained in the hypoxia area of Amur Bay one meter above the bottom, at the depth of 19 m. The temperature, electric conductivity, pressure, and content of dissolved oxygen were registered every four hours for more than three months. On the basis of these data, it was found that the period of hypoxia at the observation point lasted 93 days and a model of calculation of the rate of biochemical oxygen demand and the velocity of ventilation of the bottom waters is suggested.
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Original Russian Text © P.P. Tishchenko, P.Ya. Tishchenko, V.I. Zvalinskii, P.Yu. Semkin, 2014, published in Doklady Akademii Nauk, 2014, Vol. 459, No. 6, pp. 750–754.
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Tishchenko, P.P., Tishchenko, P.Y., Zvalinskii, V.I. et al. Rate of Biochemical oxygen demand during formation of hypoxia in Amur Bay, Sea of Japan. Dokl. Earth Sc. 459, 1627–1630 (2014). https://doi.org/10.1134/S1028334X14120320
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DOI: https://doi.org/10.1134/S1028334X14120320