National Marine Fisheries Research Institute, ul. Kołłątaja 1, 81-332, Gdynia, Poland.
Chair of Environmental Chemistry and Bioanalytics, Faculty of Chemistry, Nicolaus Copernicus University, ul. Gagarina 7, Toruń, Poland.
Environ Sci Pollut Res Int. 2018 Oct;25(29):29734-29751. doi: 10.1007/s11356-018-2945-7. Epub 2018 Aug 25.
Modeling (MONERIS) studies allowed calculation of nitrogen (N) and phosphorus (P) emission into the Vistula and Oder basins (Poland), and facilitated estimation of N and P retention in these catchments in 1995-2015. In the discussion of results, data of other authors were used in order to get an insight into N (1880-2015) and P emission (1955-2015) into the Oder basin. Population growth and agricultural intensification were responsible for respective 5.3-fold and 3.5-fold increase in N and P emission into the Oder basin, with the maximum (135,000 tons N year; 14,000 tons P year) observed at the turn of the 1980s/1990s. Pro-ecological activities during the economic transition period (since 1989) covered various sectors of the economy including agriculture, environmental protection related to, e.g., construction of a large number of waste water treatment plants (WWTPs). Consequently, in 1985-2015, the emission into the Oder basin decreased from the abovementioned maxima to 94,000 tons N year and to 5000 tons P year, whereas in 1995-2015, the emission into the Vistula basin decreased from 170,000 to 140,000 tons N year and from 14,200 to 10,600 tons P year. In 1995-2015, groundwater, tile drainage, and WWTPs played a key role in N emission, while erosion, overland flow, WWTPs, and urban areas played a predominant role in P emission. The relative shares of nutrient emission pathways in overall N and P emission were considerably changing over time. Extreme weather conditions have a great impact on increased (floods) or decreased (droughts) nutrient emission; particularly, N emission is susceptible to variable weather conditions. In total, approximately 91,000 tons of N and 7600 tons of P were retained annually in the river basins.
建模 (MONERIS) 研究允许计算进入维斯瓦河和奥得河盆地(波兰)的氮 (N) 和磷 (P) 排放量,并有助于估计 1995-2015 年这些集水区中 N 和 P 的保留量。在讨论结果时,使用了其他作者的数据,以便深入了解奥得河盆地的 N(1880-2015 年)和 P 排放(1955-2015 年)。人口增长和农业集约化分别导致奥得河盆地 N 和 P 排放量增加了 5.3 倍和 3.5 倍,最大排放量(135000 吨 N 年;14000 吨 P 年)出现在 20 世纪 80 年代末/90 年代初之交。经济转型期(自 1989 年以来)的亲生态活动涵盖了农业等经济各个部门,以及与建设大量废水处理厂(WWTP)相关的环境保护。因此,1985-2015 年,奥得河盆地的排放量从上述最大值降至 94000 吨 N 年和 5000 吨 P 年,而 1995-2015 年,维斯瓦河盆地的排放量从 170000 吨降至 140000 吨 N 年和 14200 吨降至 10600 吨 P 年。1995-2015 年,地下水、排水渠和 WWTP 在 N 排放中发挥了关键作用,而侵蚀、地表径流、WWTP 和城市地区在 P 排放中发挥了主要作用。营养物质排放途径在总 N 和 P 排放中的相对份额随时间发生了很大变化。极端天气条件对增加(洪水)或减少(干旱)养分排放有很大影响;特别是,N 排放易受天气条件变化的影响。总的来说,每年大约有 91000 吨 N 和 7600 吨 P 在流域中得到保留。