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Eutrophication modeling, management and decision making: The Kis-Balaton case

机译:富营养化建模,管理和决策:Kis-Balaton案例

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Main shortcomings of eutrophication models are related to the uncertain cause-effect relations of mostly shallow, hypertrophic, blue-green algae and large internal load dominated systems. Additional difficulties emerge when these tools are used to tackle complex decision making problems, of which eutrophication may be only one element. The Kis-Balaton Reservoir (in Hungary) is characterized by both features. The system, consisting of an Upper and Lower Reservoir was designed to reduce the phosphorus load bf agricultural nonpoint source origin to control the eutrophication of Lake Balaton. The original assumption in the late seventies was that macrophytes would play the decisive role in nutrient removal. Operational experiences and the ongoing unique monitoring program demonstrated that this assumption was not met: the Upper Reservoir quickly developed into a hypertrophic phytoplankton system. The P retention of the inundated reed area of the Lower Reservoir is not satisfactory and the large, intact reed stand of high nature conservation value started to die off due to the water level increase and algal-rich inflow. Thus, the need for revision of the original design (more than half of which was implemented) became evident. The paper summarizes the approach adopted, the project alternatives and criteria of evaluation used, details of phosphorus cycle models applied for the Upper Reservoir, and their transfer to the lower one to derive estimates for the future P retention. We also discuss dilemmas related to the estimation of the sorption isotherm of the soil/sediment system which appear in the models and which are crucial to 'extrapolate the future'. Finally, we outline the multi-criteria evaluation, the recommendations prepared for modifying the original design of the Lower Reservoir and the outcome of decision making. (C) 1998 IAWQ. Published by Elsevier Science Ltd. [References: 16]
机译:富营养化模型的主要缺点与不确定的因果关系有关,这些因果关系主要是浅水,肥大,蓝绿色藻类和大型内部负载为主的系统。这些工具用于解决复杂的决策问题时,还会出现其他困难,富营养化可能只是其中的一个因素。 Kis-Balaton水库(在匈牙利)具有两个特征。该系统由上,下水库组成,旨在减少农业面源来源的磷负荷,以控制巴拉顿湖的富营养化。七十年代末期最初的假设是,大型植物将在营养去除中起决定性作用。运行经验和正在进行的独特监测程序表明,这一假设没有得到满足:上层水库迅速发展为肥厚性浮游植物系统。下水库淹没的芦苇区的磷保持能力不令人满意,并且由于水位增加和藻类丰富的流入,具有高自然保护价值的大型完整芦苇林开始消失。因此,很明显需要修改原始设计(实施了一半以上)。本文总结了所采用的方法,所采用的项目替代方案和所采用的评估标准,在上部水库中应用的磷循环模型的详细信息,以及将其转移至下部模型以得出对未来磷保持量的估算。我们还将讨论与模型中出现的土壤/泥沙系统吸附等温线估计有关的难题,这对于“推算未来”至关重要。最后,我们概述了多标准评估,为修改下层水库的原始设计而准备的建议以及决策的结果。 (C)1998 IAWQ。由Elsevier Science Ltd.发布[参考文献:16]

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