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Effectiveness of Best Management Practices to Reduce Phosphorus Loading to a Highly Eutrophic Lake

机译:最佳管理措施的有效性以减少磷向富营养化湖泊的负荷

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摘要

Reducing nonpoint source pollution is an ongoing challenge in watersheds throughout the world. Implementation of best management practices, both structural and nonstructural, is the usual response to this challenge, with the presumption that they are effective. However, monitoring of their efficacy is not a standard practice. In this study, we evaluate the effectiveness of two wetland restoration projects, designed to handle runoff during high flow events and serve as flow-through retention basins before returning flow further downstream. The Macatawa Watershed is located in west Michigan, is heavily agricultural, and drains into Lake Macatawa, a hypereutrophic lake with total phosphorus concentrations usually exceeding 100 µg/L. We measured turbidity, total phosphorus, and soluble reactive phosphorus both upstream and downstream of these wetland complexes during base flow and storm events. While both turbidity and phosphorus increased significantly during storm events compared to baseflow, we found no significant difference in upstream vs. downstream water quality two years following BMP construction. We also measured water quality in Lake Macatawa, and found the lake remained highly impaired. Possible reasons for the lack of improved water quality: (1) The restored wetlands are too young to function optimally in sediment and phosphorus retention; (2) the scale of these BMPs is too small given the overall loads; (3) the locations of these BMPs are not optimal in terms of pollutant reduction; and (4) the years following postconstruction were relatively dry so the wetlands had limited opportunity to retain pollutants. These possibilities are evaluated.
机译:减少非点源污染是世界各地流域面临的持续挑战。对结构性和非结构性最佳管理实践的实施是对这一挑战的通常应对,并假定它们是有效的。但是,监测其功效不是标准做法。在这项研究中,我们评估了两个湿地恢复项目的有效性,这些项目旨在处理高流量事件期间的径流,并在将流量返回下游之前充当流通保留盆地。 Macatawa流域位于密歇根州西部,农业资源丰富,流向Macatawa湖,这是一种富营养化的湖泊,总磷浓度通常超过100 µg / L。我们在基流和暴风雨期间测量了这些湿地复合体上游和下游的浊度,总磷和可溶性反应性磷。尽管与基流相比,暴风雨期间的浊度和磷均显着增加,但在BMP施工两年后,我们发现上游和下游水质没有显着差异。我们还测量了马卡塔瓦湖的水质,发现该湖仍然严重受损。缺乏改善的水质的可能原因:(1)恢复的湿地太年轻,无法在沉积物和磷的保持方面发挥最佳作用; (2)考虑到总体负荷,这些BMP的规模太小; (3)这些BMP的位置在减少污染物方面不是最佳的; (4)施工后的几年相对干燥,因此湿地保留污染物的机会有限。对这些可能性进行了评估。

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