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The effect of eutrophication on greenhouse gas emissions in three reservoirs of the Middle Tiete River, southeastern Brazil

机译:富营养化对巴西东南三河水库温室气体排放的影响

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Classic organic pollution, eutrophication, and hypolimnetic anoxia are some of the common water quality problems in reservoirs (STRASKRABA & TUNDISI 1999). In Brazil these problems are related mainly to the loading of untreated sewage to the water bodies; most of the sewage produced has no treatment. In addition to the known consequences, such as hygienic problems, formation of potentially toxic cyanobacterial blooms, and fish mortalities, these impacts may also contribute to greenhouse gas production in the reservoirs and emission to the atmosphere. Untreated sewage loading promotes high dissolved carbon, phosphorus, and nitrogen input, which results in increased autochtonous biomass in the water column; however, the sinking of the organic particles (dead organisms, fecal pellets) results in increased accumulation of organic matter in the sediments. Precipitation also makes an important contribution to the input of allochtonous dissolved and particulate organic matter from the watershed to the reservoirs. As the accumulated organic matter in the sediments is decomposed by microorganisms, increased gas production in the sediments and in the anoxic hypolimnion might occur. This study was designed to evaluate the sediment CH_4, CO_2 and N_2O concentrations of 3 tropical reservoirs in Brazil, as well as to determine the diffusive fluxes of these gases across the water-air interface. The trophic conditions for these reservoirs were also evaluated to determine the relationships between sediment gas accumulation, diffusive fluxes across the water-air interface, and changing conditions in the trophic status of these water bodies.
机译:经典的有机污染,富营养化和低估缺氧是水库中的一些常见水质问题(Straskraba&Tundisi 1999)。在巴西,这些问题主要是为了将未经处理的污水装载到水体;生产的大部分污水都没有治疗。除了已知的后果,例如卫生问题,潜在有毒的蓝藻绽放和鱼类死亡的形成,这些影响也可能导致水库中的温室气体生产和大气排放。未经治疗的污水负荷促进了高溶解的碳,磷和氮气输入,这导致水柱中的自同组织生物质增加;然而,有机颗粒(死亡生物,粪便颗粒)的下沉导致沉积物中有机物质的积累增加。沉淀还对从流域的分散溶解和微粒有机物的输入进行了重要贡献。随着沉积物中累积的有机物质被微生物分解,可能发生沉积物和缺氧缺氧中的增加的天然气生产。本研究旨在评估巴西的3个热带储层的沉积物CH_4,CO_2和N_2O浓度,以及在水 - 空气界面上确定这些气体的扩散势倍。还评估了这些储存器的营养条件,以确定沉积物气体积聚,跨空中界面的扩散助焊剂之间的关系,以及这些水体的营养状况的变化条件。

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