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

机译:长期氮沉降对北方森林地上凋落物数量和质量的影响较小

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摘要

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.
机译:有证据表明,人为氮(N)的沉积增强了北方土壤中的碳(C)隔离。但是,解释这种增加的关键基础机制尚未解决。两种潜在的重要机制是地上凋落物产量增加,或者凋落物质量响应氮富集而变化。因此,我们的目的是量化模拟的慢性氮沉降是否引起了北方森林凋落物产量或质量的变化。我们进行了一个长期(17年)的林分规模(0.1公顷)森林试验,该试验由三个氮素添加水平(0、12.5和50 kg N ha -1 yr - 1 )在瑞典北部,那里的背景N沉积速率非常低。我们测量了8种不同垃圾类型的年产垃圾量,以及它们的C,N,磷(P),木质素,纤维素和半纤维素的浓度。我们的结果表明,苔藓是唯一的主要凋落物成分,显示出对氮的添加有明显的数量和质量变化,表明它们能够拦截大部分氮。但是,这些影响被其他垃圾分数所抵消,当我们将所有垃圾类别相加时,我们发现总垃圾通量或单个化学成分没有变化。这项研究表明,目前每年的凋落物通量不能解释我们的研究系统中模拟的长期施氮对土壤碳增加的影响。这些结果表明,其他机制也可能解释了我们观察到的土壤碳积累速率的增加,例如土壤微生物活性的变化,或我们研究时不再存在的地上垃圾的潜在瞬时变化。

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