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Influence of hypersaturated dissolved oxygenated water on the elution of hydrogen sulfide and methane from sediment in the dredged area in polyhaline Lake Nakaumi

机译:多饱和盐中湖疏poly区过饱和溶解氧水对沉积物中硫化氢和甲烷洗脱的影响

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摘要

Equipment for supplying hypersaturated dissolved oxygen (DO) into water without vertical mixing was installed at a depth of 13.8 m (1 m above the bottom) in the dredged area of polyhaline Lake Nakaumi. The vertical profile of dissolved sulfides, including H2S and HS- (I H2S) pound, and the CH4 concentrations in the water column and interstitial water of bottom sediment were investigated monthly during a period when hypersaturated DO water was delivered at a depth of 13.8 m. The area near the bottom was identified as oxic. H2S is easily and rapidly oxidized in an oxic environment through a chemical reaction with DO. Although the concentration of CH4 in the experimental area was 95 % lower than that in the control area, CH4 was detected, even though 20-220 % DO was observed near the bottom, where no H2S was detected. We can therefore confirm that supplying hypersaturated DO can improve the water quality, as well as the ecosystem, by preventing the evolution of H2S.
机译:在多盐湖中海疏the区的深度为13.8 m(底部上方1 m)处安装了用于在不垂直混合的情况下向水中供应过饱和溶解氧(DO)的设备。在13.8 m深度输送过饱和溶解氧水期间,每月对溶解的硫化物(包括H2S和HS-(I H2S)磅)的垂直剖面以及水柱和底部沉积物的间隙水中的CH4浓度进行每月调查。 。底部附近的区域被确定为有氧的。 H2S通过与DO的化学反应在有氧环境中容易而迅速地被氧化。尽管实验区中的CH4浓度比对照区中的CH4浓度低95%,但即使在底部未发现H2S的底部观察到20-220%DO,仍检测到CH4。因此,我们可以确定,通过防止H2S的释放,提供过饱和的DO可以改善水质以及生态系统。

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