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Patterns of dissolved organic carbon and nitrogen fluxes in deciduous and coniferous forests under historic high nitrogen deposition

机译:历史高氮沉积下落叶林和针叶林溶解有机碳和氮通量的变化规律

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摘要

Numerous recent studies have indicated that dissolved organic carbon (DOC) and nitrogen (DON) play an important role in C and N cycling in natural ecosystems, and have shown that N deposition alters the concentrations and fluxes of dissolved organic substances and may increase leaching losses from forests. Our study was set up to accurately quantify concentrations and flux patterns of DOC, DON and dissolved inorganic nitrogen (DIN) in deciduous and coniferous forest in Flanders, Belgium, under historical high nitrogen deposition. We measured DOC, DON and DIN concentrations at two weekly intervals in a silver birch (SB) stand, a corsican pine (CP) stand and a pine stand with higher N deposition (CPN), and used the SWAP model (calibrated with PEST) for generating accurate water and matter fluxes. The input with precipitation was an important source of DON, but not for DOC. Release of DOC from the forest floor was minimally affected by forest type, but higher N deposition (CPN stand) caused an 82% increase of DOC release from the forest floor. Adsorption to mineral soil material rich in iron and/or aluminum oxyhydroxides was suggested to be the most important process removing DOC from the soil solution, responsible for substantial retention (67–84%) of DOC entering the mineral soil profile with forest floor leachate. Generally, DON was less reactive (i.e. less removal from the soil solution) than DOC, resulting in decreasing DOC/DON ratios with soil depth. We found increased DOC retention in the mineral soil as a result of higher N deposition (84 kg ha−1 yr−1 additional DOC retention in CPN compared to CP). Overall DON leaching losses were 2.2, 3.3 and 5.0 kg N yr−1 for SB, CP and CPN, respectively, contributing between 9–28% to total dissolved N (TDN) leaching. The relative contribution to TDN leaching from DON loss from SB and CP was mainly determined by (large) differences in DIN leaching. The large TDN leaching losses are alarming, especially in the CPN stand that was N saturated.
机译:最近的大量研究表明,溶解的有机碳(DOC)和氮(DON)在自然生态系统中的碳和氮循环中起着重要作用,并表明氮的沉积会改变溶解的有机物质的浓度和通量,并可能增加浸出损失来自森林。我们的研究旨在准确定量比利时富兰德州落叶和针叶林在高氮沉积条件下的DOC,DON和溶解性无机氮(DIN)的浓度和通量模式。我们在白桦林(SB)林分,科西嘉松树(CP)林分和N沉积较高(CPN)的松树林中每两周测量一次DOC,DON和DIN的浓度,并使用SWAP模型(通过PEST进行了校准)用于产生精确的水和物质通量。降水的输入是DON的重要来源,但对于DOC却不是。森林类型对DOC的释放影响最小,但是较高的N沉积量(CPN林分)导致森林底层的DOC释放量增加了82%。吸附到富含铁和/或氢氧化铝的矿质土壤材料被认为是从土壤溶液中去除DOC的最重要过程,这导致大量的DOC(67-84%)DOC被森林地层渗滤液保留在矿质土壤中。通常,DON比DOC的反应性小(即从土壤溶液中去除的少),导致DOC / DON比随土壤深度而降低。我们发现由于较高的N沉积(与CP相比CPN中的DOC保留量增加了84 kg ha-1 yr-1),矿物土壤中的DOC保留量增加了。 SB,CP和CPN的总DON淋失损失分别为2.2、3.3和5.0 kg N yr-1,占总溶解氮(TDN)淋失的9–28%。 SB和CP的DON损失对TDN浸出的相对贡献主要取决于DIN浸出的(较大)差异。巨大的TDN浸出损失令人震惊,尤其是在N饱和的CPN林中。

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