The oxygen consumption by bottom sediment containing organic matter was examined. The oxygen consumption by suspended sediment particles showed two stages. One of them due to chemical consumption continued for about 3 hours, another one due to biological consumption for 3 days. The rate constant of oxygen consumption was calculated. Its dependence on ignition loss, water temperature and so on was examined.
The experiment of oxygen consumption by sediment was carried out using an experimental flume. According to the multiple regression analysis the oxygen transfer coefficient showed positive relationships with following
(1) shear velocity acting on water sediment interface, (2) water content of sediment, (3) rate constant of oxygen consumption of sediment particles, and negative relationships with size of sediment particle.
A model which estimates the oxygen transfer coefficient by shear velocity, water content, sediment particle size and rate constant of oxygen consumption by sediment particles was presented. The oxygen transfer coefficient obtained by this model showed a close agreement with the experimental results.
In this study, the method of giving a general and quantitative estimation of oxygen consumption by bottom sediment was presented.
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