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Nitrogen surface water retention in the Baltic Sea drainage basin

机译:波罗的海流域的氮表面持水量

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摘要

In this paper, we estimate the surface water retention of nitrogen (N) in all the 117 drainage basins to the Baltic Sea with the use of a statistical model (MESAW) for source apportionment of riverine loads of pollutants. Our results show that the MESAW model was able to estimate the N load at the river mouth of 88 Baltic Sea rivers, for which we had observed data, with a sufficient degree of precision and accuracy. The estimated retention parameters were also statistically significant. Our results show that around 380 000 t of N are annually retained in surface waters draining to the Baltic Sea. The total annual riverine load from the 117 basins to the Baltic Sea was estimated at 570 000 t of N, giving a total surface water N retention of around 40 %. In terms of absolute retention values, three major river basins account for 50% of the total retention in the 117 basins; i.e. around 104 000 t of N are retained in Neva, 55 000 t in Vistula and 32 000 t in Oder. The largest retention was found in river basins with a high percentage of lakes as indicated by a strong relationship between N retention (%) and share of lake area in the river drainage areas. For example in Gota alv, we estimated a total N retention of 72 %, whereof 67% of the retention occurred in the lakes of that drainage area (Lake Vanern primarily). The obtained results will hopefully enable the Helsinki Commission (HELCOM) to refine the nutrient load targets in the Baltic Sea Action Plan (BSAP), as well as to better identify cost-efficient measures to reduce nutrient loadings to the Baltic Sea.
机译:在本文中,我们使用统计模型(MESAW)估算了河流污染物的源头,估算了波罗的海的所有117个流域中氮(N)的地表持水量。我们的结果表明,MESAW模型能够以足够的精确度和精确度估算出我们观察到的88条波罗的海河流的河口处的氮负荷。估计的保留参数也具有统计学意义。我们的结果表明,每年排放到波罗的海的地表水中保留着约38万吨氮。从117个盆地到波罗的海的河流总年负荷估计为570千吨N,总地表水N保留量约为40%。就绝对保留值而言,三个主要流域占117个流域总保留量的50%;也就是说,内娃(Neva)保留了约104万吨的氮,维斯瓦(Vistula)保留了5.5万吨,奥得河(Oder)保留了3.2万吨。 N保留率(%)与河流流域中湖区份额之间的密切关系表明,在湖泊比例较高的流域发现了最大的保留。例如,在Gota alv地区,我们估计总氮保留率为72%,其中67%的氮保留发生在该流域的湖泊中(主要是Vanern湖)。获得的结果有望使赫尔辛基委员会(HELCOM)完善波罗的海行动计划(BSAP)中的养分负荷目标,并更好地确定降低波罗的海养分负荷的经济有效措施。

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