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N fluxes in two nitrogen saturated forested catchments in Germany: dynamics and modelling with INCA

机译:德国两个氮饱和森林流域的N通量:INCA的动力学和建模

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The N cycle in forests ofthe temperate zone in Europe has been changed substantially by the impact ofatmospheric N deposition. Here, the fluxes and concentrations of mineral N inthroughfall, soil solution and runoff in two German catchments, receiving high Ninputs are investigated to test the applicability of an Integrated NitrogenModel for European Catchments (INCA) to small forested catchments. TheLehstenbach catchment (419 ha) is located in the German Fichtelgebirge (NOBavaria, 690-871 m asl.) and is stocked with Norway spruce (Picea abies (L.) Karst.) of different ages. The Steinkreuzcatchment (55 ha) with European beech (Fagus sylvatica L.) as thedominant tree species is located in the Steigerwald (NW Bavaria, 400-460 m asl.).The mean annual N fluxes with throughfall were slightly higher at theLehstenbach (24.6 kg N ha-1) than at the Steinkreuz (20.4 kg N ha-1).In both catchments the N fluxes in the soil are dominated by NO3. AtLehstenbach, the N output with seepage at 90 cm soil depth was similar to the Nflux with throughfall. At Steinkreuz more than 50 % of the N deposited wasretained in the upper soil horizons. In both catchments, the NO3fluxes with runoff were lower than those with seepage. The average annual NO3concentrations in runoff in both catchments were between 0.7 to 1.4 mg NO3-N L-1 and no temporal trend was observed. The N budgets at the catchment scale indicated similar amounts of N retention (Lehstenbach: 19 kg N ha-1yr-1 ; Steinkreuz: 17 kg N ha-1yr-1). The parameter settings of the INCA model were simplified to reduce the modelcomplexity. In both catchments, the NO3 concentrations and fluxes inrunoff were matched well by the model. The seasonal patterns with lower NO3runoff concentrations in summer at the Lehstenbach catchment were replicated.INCA underestimated the increased N3 concentrations during shortperiods of rewetting in late autumn at the Steinkreuz catchment. The model willbe a helpful tool for the calculation of “critical loads?? for the Ndeposition in Central European forests including different hydrological regimes. style="line-height: 20px;">Keywords: forest ecosystem, modelling, N budgets, N saturation, NO3 leaching, water quality, INCA
机译:欧洲温带地区森林中的氮循环由于大气氮沉降的影响而发生了很大变化。在这里,研究了接受高氮输入的两个德国集水区的矿物质氮渗透,土壤溶液和径流的通量和浓度,以测试欧洲集水区综合氮模型对小型森林集水区的适用性。 The Lehstenbach集水区(419公顷)位于德国Fichtelgebirge(NOBavaria,690-871 m asl。),并存有不同年龄的挪威云杉(Picea abies(L。)喀斯特)。以欧洲山毛榉(Fagus sylvatica L.)为主要树种的Steinkreuz集水区(55公顷)位于Steigerwald(巴伐利亚州西北部,400-460 m asl。)。在Lehstenbach(24.6 kg N ha -1 )比Steinkreuz(20.4 kg N ha -1 )略高。在两个流域,土壤中的N通量均为由NO 3 主导。在Lehstenbach,土壤深度为90 cm时,渗漏的氮输出与穿透的Nflux相似。在Steinkreuz,上部土壤层中保留了超过50%的氮。在两个流域,径流的NO 3 通量均低于渗流的通量。两个流域的径流中NO 3 年平均浓度在0.7至1.4 mg NO 3 -NL -1 之间,未观察到时间趋势。 。流域规模上的N预算显示了相似的N保留量(Lehstenbach:19 kg N ha -1 yr -1 ; Steinkreuz:17 kg N ha - 1 yr -1 )。 INCA模型的参数设置得到简化,以降低模型的复杂性。在两个流域,NO 3 的浓度和通量径流均与模型很好地匹配。复制了夏季Lehstenbach流域NO 3 径流浓度较低的季节模式.INCA低估了Steinkreuz流域在深秋短时重湿期间N 3 浓度增加的趋势。该模型将成为计算“临界载荷”的有用工具。 style =“ line-height:20px;”> 关键字:森林生态系统,模型,N个预算,N个饱和度,NO 3 浸出,水质,INCA

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