首页> 外文OA文献 >We conducted experiments using a Solar-Sea-Oasis (SSO) and a microbubble generator (MB) toimprove hypoxic condition at mooring place in Tokyo University of Marine Science and Technology. We looked intoeffects of these apparatuses by computational fluid dynamics (CFD). When we operated SSO, the effect of dissolvedoxygen (DO) supply was only confirmed near the water outlet. This was suggested by computational fluid dynamicsthat water that came out from water outlet rising upward without staying in the bottom was the causes. Then, weconducted experiments using a MB to aerate bottom of the sea more directly. Vertical distributions of DO showedoxygen was supplied horizontally, but DO concentration increased about 0.24 mg L-1 that was lower than SSOexperiment. This was suggested by CFD that water came out from MB generator spread horizontally without stayingnear the MB generator was the cause. Therefore, it is necessary to improve of making the MB water staying morenear the MB generator.
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We conducted experiments using a Solar-Sea-Oasis (SSO) and a microbubble generator (MB) toimprove hypoxic condition at mooring place in Tokyo University of Marine Science and Technology. We looked intoeffects of these apparatuses by computational fluid dynamics (CFD). When we operated SSO, the effect of dissolvedoxygen (DO) supply was only confirmed near the water outlet. This was suggested by computational fluid dynamicsthat water that came out from water outlet rising upward without staying in the bottom was the causes. Then, weconducted experiments using a MB to aerate bottom of the sea more directly. Vertical distributions of DO showedoxygen was supplied horizontally, but DO concentration increased about 0.24 mg L-1 that was lower than SSOexperiment. This was suggested by CFD that water came out from MB generator spread horizontally without stayingnear the MB generator was the cause. Therefore, it is necessary to improve of making the MB water staying morenear the MB generator.

机译:我们使用solar-sea-Oasis(ssO)和微泡发生器(mB)进行了实验,以改善东京海洋科技大学系泊处的低氧条件。我们通过计算流体动力学研究了这些能力的影响( CFD)。当我们操作ssO时,溶解无氧(DO)供应的影响仅在出水口附近得到证实。这是通过计算流体动力学提出的,从出水口出来的水不会停留在底部是然后,我们利用mB进行实验,更直接地对海底进行曝气.DO的垂直分布显示水平供给无氧,但DO浓度增加约0.24 mg L-1,低于ssO nexperiment。这是CFD建议的,水从mB发生器中流出,水平传播而不停留在mB发生器的原因。 mB发电机。

摘要

東京海洋大学品川キャンパス係船場にてソーラーシーオアシス (SSO) 並びに,マイクロバブル発生装置による貧酸素水塊改善実験を行い,流体シミュレーションにより効果を検証した。現場観測からSSO の効果が放出部付近でのみ確認されたことは,流体シミュレーションにより放出部から出た水が海底付近に留まらずに鉛直上向きに上昇してしまうことが原因だと示唆された。そこで,より直接海底付近に酸素を供給するためにマイクロバブル発生装置を用いた実験を行った。現場観測では水平方向に酸素が供給されている分布を示したが,DO 増加量が0.24 mg L-1 とSSO よりも低い値となった。これは放出した水が,その場に滞留することはなく水平方向に広がっていることが原因と流体シミュレーションによりわかった。このため今後はより海底付近に滞留させる方法を考える必要がある。
机译:我们在东京海洋科学技术大学品川校区使用微气泡发生器进行了太阳绿洲(SSO)和缺氧水质改善实验,并通过流体模拟验证了该效果。现场观察证实了SSO的作用仅在排放部分附近,表明从排放部分排放的水垂直向上上升,而不是停留在海床附近。因此,我们进行了一个实验,使用微气泡发生器将氧气更直接地供应到海底。原位观察表明氧水平分布,但溶解氧增加为0.24 mg L-1,低于SSO。通过流体模拟发现,这是由于释放的水在水平方向上扩散而没有停留在那里的事实所致。因此,有必要考虑将来留在海床附近的方法。

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