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Modelling stream and soil water nitrate dynamics during experimentally increased nitrogen deposition in a coniferous forest catchment at Gardsjoen, Sweden

机译:模拟瑞典Gardsjoen针叶林流域实验性增加氮沉积过程中的水流和土壤水硝酸盐动态

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Increased atmospheric deposition of inorganic nitrogen (N) may lead to increased leaching of nitrate (NO_3~-) to surface waters. The mechanisms responsible for, and controls on, this leaching are matters of debate. An experimental N addition has been conducted at Gardsjon, Sweden to determine the magnitude' and identify the mechanisms of N leaching from forested catchments within the EU funded project NITREX. The ability of INCA-N, a simple process-based model of catchment N dynamics, to simulate catchment-scale inorganic N dynamics in soil and stream water during the course of the experimental addition is evaluated. Simulations were performed for 1990-2002. Experimental N addition began in 1991. INCA-N was able to successfully reproduce stream and soil water dynamics before and during the experiment. While INCA-N did not correctly simulate the lag between the start of N addition and NO_3~- breakthrough, the model was able to simulate the state change resulting from increased N deposition. Sensitivity analysis showed that model behaviour was controlled primarily by parameters related to hydrology and vegetation dynamics and secondarily by in-soil processes.
机译:大气中无机氮(N)的增加沉积可能导致硝酸盐(NO_3--)向地表水中的浸出增加。负责和控制这种浸出的机制尚有争议。在瑞典加兹洪进行了一项试验性的氮添加实验,以确定欧盟资助的NITREX项目中森林集水区氮淋失的幅度并确定其机理。评估了INCA-N(一个简单的基于过程的集水区N动力学模型)在实验添加过程中模拟土壤和溪流中集水规模无机N动力学的能力。对1990-2002年进行了模拟。 1991年开始添加实验性N。INCA-N能够在实验之前和过程中成功重现溪流和土壤水动力学。虽然INCA-N不能正确模拟开始添加N和突破NO_3〜-之间的滞后时间,但该模型仍可以模拟由于增加N沉积而导致的状态变化。敏感性分析表明,模型行为主要由与水文和植被动力学相关的参数控制,其次由土壤过程控制。

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