Department of Hydraulic Engineering, Faculty of Civil and Environmental Engineering, Warsaw University of Life Sciences - SGGW, ul. Nowoursynowska 159, 02-776 Warsaw, Poland.
Department of Hydraulic Engineering, Faculty of Civil and Environmental Engineering, Warsaw University of Life Sciences - SGGW, ul. Nowoursynowska 159, 02-776 Warsaw, Poland.
J Environ Manage. 2015 Apr 1;152:230-40. doi: 10.1016/j.jenvman.2015.01.049. Epub 2015 Feb 11.
A multi-model-based study was performed in order to unravel valuable fen meadow habitats' possible exposure to eutrophication, which is expected to occur as a result of the re-saturation of degraded peat soils. The framework was tested in a 3000-ha fen-drain system to be restored in the Middle Biebrza Basin (northeast Poland), where the datasets and related models were used to delineate prospective eutrophication hotspots and nutrient transport. A 1-d hydrodynamic model and a 3-d groundwater flow model were applied to constitute the hydrological response of the fen-drain system to the prospective construction and function of weirs and spillways, which are expected to induce the increase of groundwater levels in degraded fens. A groundwater particle-tracking postprocessor was applied to delineate flow pathways and discharge zones and to determine water residence time in modelled layers. Soil and habitat maps, a high-resolution digital elevation model and historic groundwater level observations were applied to the model performance, calibration and spatial analysis of prospective eutrophication hotspots where increased eutrophication of groundwater can be expected due to the re-saturation of degraded peat soils. The study revealed that the large-scale fen rewetting that occurred as a result of surface water bodies' damming can potentially result in groundwater-driven nutrient dispersion along with an enhanced nutrient transport from a fen to the adjacent water bodies. Spatial analyses showed that, although the rewetting-driven eutrophication of Molinia fen meadows located in the study area is not likely, one can expect increased nutrient discharges to adjacent drains, inducing the contamination of ox-bow lakes located along the rivers. We propose the presented methodology to be applied ex-ante to fen-rewetting projects in strategic environmental assessments of restoration projects in order to manage the potentially negative environmental consequences of fen and river eutrophication with special regard to nutrient hotspots that are likely to occur within the rewetted fens.
进行了一项基于多模型的研究,以揭示有价值的草本沼泽栖息地可能面临富营养化的风险,这种情况预计是由于退化泥炭土壤的再饱和而导致的。该框架在一个 3000 公顷的草本沼泽排水系统中进行了测试,该系统位于波兰东北部的比亚韦斯托克盆地中部,在那里使用数据集和相关模型来划定潜在的富营养化热点和养分传输。应用了一个一维水动力模型和一个三维地下水流动模型来构建草本沼泽排水系统对拟议的堰和溢洪道的建设和功能的水文响应,预计这将导致退化草本沼泽地下水水位的增加。应用地下水粒子跟踪后处理器来划定水流路径和排放区,并确定模型化层中的水停留时间。土壤和栖息地图、高分辨率数字高程模型和历史地下水水位观测值被应用于模型性能、校准和潜在富营养化热点的空间分析,在这些热点中,由于退化泥炭土壤的再饱和,地下水可能会出现富营养化增加的情况。研究表明,由于地表水坝的拦蓄,大规模的草本沼泽重新湿润可能导致地下水驱动的养分扩散,以及从草本沼泽向相邻水体增强的养分输送。空间分析表明,尽管研究区域内的草本沼泽湿地由于再湿润而导致富营养化的可能性不大,但可以预计到相邻排水渠的养分排放量会增加,从而导致沿河流的牛轭湖受到污染。我们建议在战略环境评估中,将提出的方法应用于草本沼泽的重新湿润项目,以管理草本沼泽和河流富营养化的潜在负面环境影响,特别关注可能在重新湿润的草本沼泽中出现的养分热点。