In order to clarify the biochemical and the physical processes of the suspended organic matter derived from phytoplankton detritus and inorganic soil, the sedimentation characteristics are investigated using sediment traps and turbidity sensors in the Hiroshima Bay.
The mineralization rate of the suspended organic matter is estimated using the results of analyses of variations in characteristics of the suspended organic matter, and the incubational experiments on the sediment. It is suggested that the mineralization rate could be roughly determined by the C/N ratio.
Based on the estimations above, a model is presented, which can express the process of the decreasing of the mineralization rate with the sedimentary years increasing. Furthermore, the settling velocity of the suspended organic matter could also be determined using the equations presented in this paper, which focuses on the changes of the density and particle diameter of the suspended organic matter during particle settling, estimated using the model above.
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