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Long-term modelling of nitrogen turnover and critical loads in a forested catchment using the INCA model

机译:使用INCA模型对森林集水区的氮周转和临界负荷进行长期建模

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Many forest ecosystems in Central Europe have reached thestatus of N saturation due to chronically high N deposition. In consequence, theNO3 leaching into ground- and surface waters is often substantial.Critical loads have been defined to abate the negative consequences of the NO3leaching such as soil acidification and nutrient losses. The steady state massbalance method is normally used to calculate critical loads for N deposition inforest ecosystems. However, the steady state mass balance approach is limitedbecause it does not take into account hydrology and the time until the steadystate is reached. The aim of this study was to test the suitability of anotherapproach: the dynamic model INCA (Integrated Nitrogen Model for EuropeanCatchments). Long-term effects of changing N deposition and critical loads for Nwere simulated using INCA for the Lehstenbach spruce catchment (Fichtelgebirge,NE Bavaria, Germany) under different hydrological conditions. Long-termscenarios of either increasing or decreasing N deposition indicated that, inthis catchment, the response of nitrate concentrations in runoff to changing Ndeposition is buffered by a large groundwater reservoir. The critical loadsimulated by the INCA model with respect to a nitrate concentration of 0.4 mg N l–1 as threshold value in runoff was 9.7 kg N ha–1yr–1compared to 10 kg ha–1yr–1 for the steady statemodel. Under conditions of lower precipitation (520 mm) the resulting criticalload was 7.7 kg N ha–1yr–1 , suggesting the necessityto account for different hydrological conditions when calculating criticalloads. The INCA model seems to be suitable to calculate critical loads for N inforested catchments under varying hydrological conditions e.g. as a consequenceof climate change. style="line-height: 20px;">Keywords: forest ecosystem, N saturation, critical load, modelling, long-term scenario, nitrate leaching, critical loads reduction, INCA
机译:中长期以来,由于中长期存在大量氮沉降,中欧许多森林生态系统已达到氮饱和状态。因此,NO 3 向地下水和地表水中的浸出通常是大量的。确定了临界负荷以减轻NO 3 浸出的负面影响,例如土壤酸化和营养损失。通常使用稳态质量平衡法来计算森林生态系统中氮沉降的临界负荷。但是,稳态质量平衡方法是有限的,因为它没有考虑水文学和达到稳态的时间。这项研究的目的是测试另一种方法的适用性:动态模型INCA(欧洲汇水区的集成氮模型)。在不同的水文条件下,使用INCA模拟了Lesstenbach云杉流域(Fichtelgebirge,NE Bavaria,德国)的变化的N沉降和N的临界负荷的长期影响。 长期增加或减少氮沉降的情况表明,在该流域,径流中硝酸盐浓度对变化的N沉积的响应受到大型地下水库的缓冲。 INCA模型模拟的硝酸盐浓度为0.4 mg N l –1 作为径流阈值的临界载荷为9.7 kg N ha -1 yr –1 相比稳态模型为10 kg ha –1 yr –1 。在较低降水量(520毫米)的条件下,产生的临界负荷为7.7 kg N ha –1 yr –1 ,这表明计算临界负荷时有必要考虑不同的水文条件。 INCA模型似乎适合计算变化的水文条件下N个森林集水区的临界负荷。 style =“ line-height:20px;”> 关键字:森林生态系统,氮饱和度,临界负荷,模型,长期情景,硝酸盐淋失,关键负载减少,INCA

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