Abstract
Regeneration of silicate in the Japan Sea, an example of semi-closed sea, was studied. In the Japan Sea Proper Water the apparent regenerative ratio of the nutrients was determined to be:ΔO ∶ΔC ∶ΔN ∶ΔP ∶ΔSi=−289 ∶(116)∶14.3∶1∶81.
It was assumed that the dissolved silicate present in sea water is grouped into three fractions; 1)preformed silicate of conservative nature, 2)oxidative silicate which dissolves in oxidation process of organisms with consumption of oxygen, and 3)non-oxidative silicate which dissolves without oxygen consumption. The dissolution rate ofnon-oxidative silicate in the Japan Sea Proper Water was estimated to be 0.07μg-at. Si/l/yr from the data ofΔAOU values and assumed rates of oxygen consumption. This dissolution rate ofnon-oxidative silicate agreed with that obtained in the deep Pacific by the vertical advection diffusion model byKido andNishimura (1972).
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Kido, K., Nishimura, M. Regeneration of silicate in the ocean. Journal of the Oceanographical Society of Japan 29, 185–192 (1973). https://doi.org/10.1007/BF02108525
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DOI: https://doi.org/10.1007/BF02108525