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慢性氮沉降对北方森林地上凋落物的数量和质量影响较小。

Chronic Nitrogen Deposition Has a Minor Effect on the Quantity and Quality of Aboveground Litter in a Boreal Forest.

作者信息

Maaroufi Nadia I, Nordin Annika, Palmqvist Kristin, Gundale Michael J

机构信息

Department of Forest Ecology and Management, Swedish University of Agricultural Sciences (SLU), Umeå, Sweden.

Umeå Plant Science Center (UPSC), Department of Forest Genetics and Plant Physiology, Swedish University of Agricultural Sciences, Umeå, Sweden.

出版信息

PLoS One. 2016 Aug 31;11(8):e0162086. doi: 10.1371/journal.pone.0162086. eCollection 2016.

Abstract

There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C) sequestration in boreal soils. However, key underlying mechanisms explaining this increase have not been resolved. Two potentially important mechanisms are that aboveground litter production increases, or that litter quality changes in response to N enrichment. As such, our aim was to quantify whether simulated chronic N deposition caused changes in aboveground litter production or quality in a boreal forest. We conducted a long-term (17 years) stand-scale (0.1 ha) forest experiment, consisting of three N addition levels (0, 12.5, and 50 kg N ha-1 yr-1) in northern Sweden, where background N deposition rates are very low. We measured the annual quantity of litter produced for 8 different litter categories, as well as their concentrations of C, N, phosphorus (P), lignin, cellulose and hemi-cellulose. Our results indicate that mosses were the only major litter component showing significant quantitative and qualitative alterations in response to the N additions, indicative of their ability to intercept a substantial portion of the N added. These effects were, however, offset by the other litter fractions where we found no changes in the total litter fluxes, or individual chemical constituents when all litter categories were summed. This study indicates that the current annual litter fluxes cannot explain the increase in soil C that has occurred in our study system in response to simulated chronic N application. These results suggest that other mechanisms are likely to explain the increased soil C accumulation rate we have observed, such as changes in soil microbial activity, or potentially transient changes in aboveground litter inputs that were no longer present at the time of our study.

摘要

有证据表明,人为氮(N)沉降会增强北方土壤中的碳(C)固存。然而,解释这种增加的关键潜在机制尚未得到解决。两个潜在的重要机制是地上凋落物产量增加,或者凋落物质量因氮富集而发生变化。因此,我们的目标是量化模拟慢性氮沉降是否会导致北方森林地上凋落物产量或质量的变化。我们在瑞典北部进行了一项长期(17年)的林分尺度(0.1公顷)森林实验,该地区背景氮沉降率非常低,实验包括三个氮添加水平(0、12.5和50千克氮 公顷⁻¹ 年⁻¹)。我们测量了8种不同凋落物类别的年凋落物产量,以及它们的碳、氮、磷(P)、木质素、纤维素和半纤维素浓度。我们的结果表明,苔藓是唯一对氮添加表现出显著数量和质量变化的主要凋落物成分,这表明它们能够截留相当一部分添加的氮。然而,其他凋落物部分抵消了这些影响,当我们将所有凋落物类别相加时,我们发现总凋落物流通量或单个化学成分没有变化。这项研究表明,当前的年凋落物流通量无法解释我们研究系统中因模拟慢性氮应用而发生的土壤碳增加。这些结果表明,其他机制可能解释了我们观察到的土壤碳积累速率增加,例如土壤微生物活动的变化,或者可能是我们研究时已不存在的地上凋落物输入的短暂变化。

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