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首页> 外文期刊>Global change biology >Fate of airborne nitrogen in heathland ecosystems: a 15N tracer study.
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Fate of airborne nitrogen in heathland ecosystems: a 15N tracer study.

机译:荒地生态系统中空气中氮的命运: 15 N示踪剂研究。

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In the present study, we analyze the fate of airborne nitrogen in heathland ecosystems (NW Germany) by means of a 15N tracer experiment. Our objective was to quantify N sequestration and N allocation patterns in an ecosystem that is naturally limited by N, but that has been exposed to airborne N inputs exceeding critical loads for more than 3 decades. We hypothesized that the system has a tendency towards N saturation, which should be indicated by low N sequestration and high N leaching. We analyzed 15N partitioning (aboveground biomass and soil horizons) and investigated 15N leaching over 2 years following a 15N tracer pulse addition. 15N tracer recovery was 90% and 76% in the first and second year, respectively. Contrary to our expectations, more than 99% of the tracer recovered was sequestered in the biomass and soil, while leaching losses were <0.05% after 2 years. Mosses were the most important short-term sink for 15N (64% recovery in the first year), followed by the organic layer. In the second year, the moss layer developed from a sink to a source (23% losses), and soil compartments were the most important sink (gains of 11.2% in the second year). Low 15N recovery in the current year's shoots of Calluna vulgaris (<2%) indicated minor availability of 15N tracer sequestered in the organic layer. N partitioning patterns showed that the investigated heaths still have conservative N cycling, even after several decades of high N loads. This finding is mainly attributable to the high immobilization capacities for N of podzols in soil compartments. In the long term, the podzol A- and B-horizons in particular may immobilize considerable amounts of incoming N. Since N compounds of these horizons are not readily bio-available, podzols have a high potential to withdraw airborne N from the system's N cycle.Digital Object Identifier http://dx.doi.org/10.1111/j.1365-2486.2010.02322.x
机译:在本研究中,我们通过 15 N示踪剂实验分析了荒地生态系统(德国西北部)中空气中氮的结局。我们的目标是量化自然受N限制但暴露于超过临界负荷的机载N输入超过3十年的生态系统中的N固存和N分配模式。我们假设系统具有趋于N饱和的趋势,这应通过低N固存和高N浸出来表明。我们分析了 15 N的分配(地上生物量和土壤层),并研究了添加 15 N示踪脉冲后2年内 15 N的淋溶。在第一年和第二年, 15 N示踪剂回收率分别为90%和76%。与我们的预期相反,回收的示踪剂中有99%以上被隔离在生物量和土壤中,而2年后的浸出损失<0.05%。苔藓是 15 N最重要的短期下沉(第一年恢复64%),其次是有机层。在第二年,苔藓层从一个汇变成了一个汇源(损失了23%),而土壤室是最重要的汇(第二年收益为11.2%)。当年寻常菜Calluna 的芽中 15 N回收率低(<2%),表明有机层中隔离的 15 N示踪剂的利用率较低。 N的划分模式表明,即使经过数十年的高N负荷,所研究的荒地仍具有保守的N循环。这一发现主要归因于土壤隔室中N唑烷的高固定能力。从长远来看,尤其是podzol A和B地平线可能会固定大量进入的N。由于这些视野中的N化合物不易生物利用,因此Podzoll具有从系统N循环中撤出空气中N的高潜力。数字对象标识符http://dx.doi.org/10.1111/j.1365-2486.2010.02322.x

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