{"title":"Impact of runoff prediction on grey water footprint in a small agricultural catchment","authors":"L. Hejduk, A. Hejduk","doi":"10.26491/MHWM/95137","DOIUrl":null,"url":null,"abstract":"According to Hoekstra et al. (2011) the water footprint within a geographic area is defined as the total freshwater consumption and pollution within the boundaries of the area. The grey part of the water footprint refers to pollution and is an indicator of the water volume needed to assimilate a pollutant load that reaches a water body. It is possible then, based on the grey water footprint to estimate if the water available in a river at a particular crosssection will be sufficient to maintain a water pollution level (WPL) below 100%. The crossing of 100% indicates that the waste assimilation capacity has been fully consumed in this particular catchment. In this paper, the grey water footprint from nonpoint source pollution has been calculated based on long-term hydrometrological data for the upper part of a small agricultural catchment (area of 23.4 km) (Zagożdżonka River) in central Poland. Based on land use and the amount of fertilizers applied in the catchment, together with information about the natural concentration of nitrogen and phosphorus in the river, as well as maximum acceptable concentration, the water pollution level has been calculated for actual conditions. The estimation of future runoff decreases for the considered catchment (Banasik, Hejduk 2012) has been applied in order to estimate potential future water pollution levels. The calculation shows that, even when the management practices in this catchment remain as they are, including the current extensive crop production, the WPL of 100% will be exceeded in the year 2033 (for phosphorus) and 2043 (for nitrogen) due only to the decreasing availability of water.","PeriodicalId":42852,"journal":{"name":"Meteorology Hydrology and Water Management-Research and Operational Applications","volume":"14 1","pages":""},"PeriodicalIF":0.8000,"publicationDate":"2019-01-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Meteorology Hydrology and Water Management-Research and Operational Applications","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.26491/MHWM/95137","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"WATER RESOURCES","Score":null,"Total":0}
引用次数: 3
Abstract
According to Hoekstra et al. (2011) the water footprint within a geographic area is defined as the total freshwater consumption and pollution within the boundaries of the area. The grey part of the water footprint refers to pollution and is an indicator of the water volume needed to assimilate a pollutant load that reaches a water body. It is possible then, based on the grey water footprint to estimate if the water available in a river at a particular crosssection will be sufficient to maintain a water pollution level (WPL) below 100%. The crossing of 100% indicates that the waste assimilation capacity has been fully consumed in this particular catchment. In this paper, the grey water footprint from nonpoint source pollution has been calculated based on long-term hydrometrological data for the upper part of a small agricultural catchment (area of 23.4 km) (Zagożdżonka River) in central Poland. Based on land use and the amount of fertilizers applied in the catchment, together with information about the natural concentration of nitrogen and phosphorus in the river, as well as maximum acceptable concentration, the water pollution level has been calculated for actual conditions. The estimation of future runoff decreases for the considered catchment (Banasik, Hejduk 2012) has been applied in order to estimate potential future water pollution levels. The calculation shows that, even when the management practices in this catchment remain as they are, including the current extensive crop production, the WPL of 100% will be exceeded in the year 2033 (for phosphorus) and 2043 (for nitrogen) due only to the decreasing availability of water.
Hoekstra et al.(2011)将地理区域内的水足迹定义为该区域边界内的淡水消耗和污染总量。水足迹的灰色部分是指污染,是同化到达水体的污染物负荷所需的水量的指标。然后,根据灰水足迹来估计某一特定断面的河流中可用的水是否足以维持在100%以下的水污染水平(WPL)是可能的。超过100%表明该特定集水区的废物同化能力已完全消耗。本文基于波兰中部一个小型农业集水区(面积23.4公里)(Zagożdżonka河)上部的长期水文气象数据,计算了非点源污染的灰水足迹。根据流域土地利用情况和化肥施用量,结合河流中氮、磷的自然浓度和最大可接受浓度等信息,根据实际情况计算出了流域的水污染水平。对所考虑的集水区未来径流减少的估计(Banasik, Hejduk 2012)已用于估计未来潜在的水污染水平。计算表明,即使在该流域的管理实践保持不变的情况下,包括目前的广泛作物生产,由于水的可用性减少,2033年(磷)和2043年(氮)的WPL将超过100%。