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Thermosolutal transport in reservoirs generated by release and leaching of salinity and nutrients from anaerobic bed

Thermosolutal transport in reservoirs generated by release and leaching of salinity and nutrients from anaerobic bed
厌氧床释放和淋滤盐度和营养物而产生的水库热溶质输送
批准号:
10650505
负责人:
MICHIOKU Kohji
金额:
$2.56万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (C)
财政年份:
1998
资助国家:
日本
项目状态:
已结题
起止时间:
1998 至 1999

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中文摘要
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英文摘要
In eutrophic reservoirs, high concentration of nutrients and ionic matters are released from the bed under badly anaerobic condition. Since the leaching process produces high salinity or heavy water mass on the bed, it gravitationally generates an inclined plume on the sloping bed and transport heat and mass to the bottom layer. This process may bring serious eutrophication of bottom water.In order to predict heat and mass flux due to the thermosolutal transport and device a countermeasure against this, the following were examined. (1)Focusing on heat and salinity balance in the anaerobic bottom water, a water quality measurement was performed in a eutrophic reservoir. (2)Release flux of salinity from the bed was examined in an experimental model in which the bed materials sampled from the reservoir were installed in a tank and filled with anaerobic water. (3)Using a micro-bubble aerator system, an in-situ experiment of water purification was carried out. (4)A model experiment and an a … More nalysis on the inclined plume were performed in order to investigate buoyancy and flow fields.The main findings are as follows. The thermosolutal convection is the main reason of making the reservoir bottom water to be extraordinary heavy and salty. Because of its very stable salinity stratification, the impounded water has never been overturned in the last many years. It makes the bottom water to be more seriously eutrophicated. It is the plume convection of warm water from the shallow layer to the bottom layer that is responsible for producing an inverse temperature stratification in the bottom layer. The heat and mass flux can be computed by the plume theory which was verified with the experimental data. The flux law was successfully applied for computing heat and salinity balance observed in the field survey. The micro-bubble aeration system was found to be very useful for promoting vertical mixing and aerating the bottom layer. After starting the aeration, the heavy and anaerobic bottom water mass was completely disappeared and the reservoir was fully overturned.The next step we should take is to develop a prediction tool of water quality by considering the thermosolutal convection process. We should also continue the water purification experiment for improving the system to be of user-convenience. Less
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会议论文
大成博文: "マイクロバブル発生技術と水環境蘇生"日本高専学会誌. 3-4. 12-20 (1998)
Hirofumi Taisei:“微气泡发生技术和水环境复苏”日本工业学院学报3-4(1998)。
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通讯作者:
Michioku,K.: "Nutrient transport due to heat-salt convection in a eutrophic reservoir"Proc.28th Conf.IAHR. 28(SD-ROM). (1999)
Michioku,K.:“富营养化水库中热盐对流引起的养分输送”Proc.28th Conf.IAHR。
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通讯作者:
道奥康治: "マイクロバブル・エアレータによる貯水池の水質浄化実験"水工学論文集. 44(印刷中). (1999)
Yasuharu Michio:“使用微泡曝气器的水库净化实验”水利工程杂志 44(出版中)。
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神田徹: "貯水池での水温計測に基づく内部波・自然対流の抽出" 水工学論文集. 43. 1049-1054 (1999)
Toru Kanda:“基于水库水温测量的内波和自然对流提取”《水利工程学报》43. 1049-1054 (1999)。
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