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Linking litter production, quality and decomposition to vegetation succession following agricultural abandonment.

机译:农业弃耕后将枯枝落叶的生产,质量和分解与植被演替联系起来。

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Agricultural land abandonment has been increasing worldwide for environmental and socio-economic reasons, and knowledge of its key ecological processes (e.g., carbon (C) and nitrogen (N) input and accumulation) in relation to vegetation succession can provide important information for ecosystem management and greenhouse gas emissions mitigation. In order to better understand the above- and belowground litter dynamics following agricultural abandonment, we simultaneously studied the litter and fine root production, quality, decomposition, C and N input in ecosystems along a secondary successional gradient (i.e., grassland, shrub-grass land, young secondary forest, and mature secondary forest) following agricultural abandonment in China's Qinling Mountains. Results showed that the significant increase of aboveground woody plant litter and decrease of grass litter during vegetation succession led little changes in total litter production and annual total C and N input in different succession stages, while the fine root production, fine root biomass, C input from fine root production increased significantly with stand age. The initial litter C concentration and fine root carbon: phosphorous ratio (C:P) were the main factors in explaining the variations of decomposition rates of litter and fine root, respectively. The increasing C concentration in litter and the increasing C:P ratio in fine root during vegetation succession had potentially driven the decreases in litter and fine root decomposition rate respectively. The accumulation of litter standing crop during vegetation succession could be attributed to the decreases in litter decomposition rate partly caused by changes in litter quality, rather than the increases in litter production. Our results imply that the changes in vegetation type have a much smaller role in the annual total litter production and the total litter C and N input than previously assumed, while the changes in quality and decomposition rate may have largely influenced C accumulation in stand floor and soil during secondary succession following agricultural abandonment.Digital Object Identifier http://dx.doi.org/10.1016/j.soilbio.2012.08.005
机译:由于环境和社会经济原因,世界范围内的农业用地弃置量在不断增加,有关其与植被演替有关的关键生态过程(例如碳(C)和氮(N)的输入和积累)的知识可以为生态系统管理提供重要信息和减少温室气体排放。为了更好地了解农业废弃后地上和地下凋落物的动态,我们同时研究了次生演替梯度(即草地,灌木草地)上生态系统中凋落物和细根的产量,质量,分解,碳和氮的输入秦岭山区放弃农业后,又形成了幼小的次生林和成熟的次生林)。结果表明,植被演替期间地上木本植物凋落物的显着增加和草凋落物的减少,导致不同演替阶段的凋落物总产量和年度总C,N输入变化不大,而细根产量,细根生物量,C输入细根产量的增加随着林龄的增加而显着增加。凋落物C的初始浓度和细根碳:磷比(C:P)分别是解释凋落物和细根分解速率变化的主要因素。植被演替过程中凋落物中碳含量的增加和细根中C:P比率的增加可能分别导致凋落物和细根分解速率的降低。植被演替过程中凋落物站立作物的积累可能归因于凋落物分解速率的降低,部分原因是凋落物质量的变化,而不是凋落物产量的增加。我们的结果表明,植被类型的变化在年度总凋落物产量以及总凋落物碳和氮输入中的作用要比以前假定的要小得多,而质量和分解速率的变化可能在很大程度上影响了立地和地下土壤中碳的积累。农业废弃后二次演替期间的土壤。数字对象标识符http://dx.doi.org/10.1016/j.soilbio.2012.08.005

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