Lake surveys and in-situ experiments were conducted to study the dissolved oxygen budget in natural lake and artificial lake. Differences of dissolved oxygen budget in each stage of summer stratification were studied on Lake Yunoko (surface area = 0.33 km
2, maximum depth = 12.5m, mean depth = 7.4m). Lake Kamafusa is a artificial lake (surface area = 2.66kni, maximum depth = 33m at elevation of 148m), which was surved to compair the difference of dissolved oxygen budget from Lake Yunoko. A mathematical model, in which the production of oxygen by photosynthesis of phytoplankton, the consumption by respiration of microorganisms, sediment oxygen demand, and oxygen transfer by the eddy diffusion and reaeration at the surface of water were taken into consideration, was developed to estimate the dissolved oxygen budget in the lake. The results of this research are as follows.
(1) In a first stage of stratification in summer, that the sediment oxygen demand (SOD) played significant role on largest deficit in DO at the bottom layer.
(2) After the hypolimnion becomes a low level in dissolved oxygen in such lakes, water column oxygen dmand was dominating facters rather than the others facters.
(3) Significant oxygen depletion in the hypolimnion was not observed in the presence of small oxygen demand in sediment and/or large amount of oxygen transferred from upper layer to deeper layer.
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