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首页> 外文期刊>Biogeosciences >Effects of belowground litter addition, increased precipitation and clipping on soil carbon and nitrogen mineralization in a temperate steppe
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Effects of belowground litter addition, increased precipitation and clipping on soil carbon and nitrogen mineralization in a temperate steppe

机译:温带草原地下凋落物添加,降水增加和截断对土壤碳和氮矿化的影响

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摘要

Soil carbon (C) and nitrogen (N) cycling are sensitive to changes in environmental factors and play critical roles in the responses of terrestrial ecosystems to natural and anthropogenic perturbations. This study was conducted to quantify the effects of belowground particulate litter (BPL) addition, increased precipitation and their interactions on soil C and N mineralization in two adjacent sites where belowground photosynthate allocation was manipulated through vegetation clipping in a temperate steppe of northeastern China from 2010 to 2011. The results show that BPL addition significantly increase soil C mineralization rate (CMR) and net N mineralization rate (NMR). Although increased precipitation-induced enhancement of soil CMR essentially ceased after the first year, stimulation of soil NMR and net nitrification rate continued into the second year. Clipping only marginally decreased soil CMR and NMR during the two years. There were significant synergistic interactions between BPL addition (and increased precipitation) and clipping on soil CMR and NMR, likely to reflect shifts in soil microbial community structure and a decrease in arbuscular mycorrhizal fungi biomass due to the reduction of belowground photosynthate allocation. These results highlight the importance of plants in mediating the responses of soil C and N mineralization to potentially increased BPL and precipitation by controlling belowground photosynthate allocation in the temperate steppe.
机译:土壤碳(C)和氮(N)的循环对环境因素的变化敏感,并在陆地生态系统对自然和人为干扰的响应中起关键作用。这项研究的目的是量化从2010年开始在中国东北温带草原上通过植被截留操纵地下光合产物分配的两个相邻地点的地下微粒凋落物(BPL)添加,降水增加及其相互作用对土壤C和N矿化的影响。到2011年。结果表明,添加BPL显着提高了土壤C矿化率(CMR)和净N矿化率(NMR)。尽管在第一年之后基本上停止了增加降水引起的土壤CMR的增强,但是土壤核磁共振和净硝化率的刺激一直持续到第二年。在这两年中,修剪仅使土壤CMR和NMR略有降低。 BPL的添加(和增加的降水)与土壤CMR和NMR的剪切之间存在显着的协同相互作用,这可能反映了土壤微生物群落结构的变化和丛枝菌根真菌生物量的减少,这归因于地下光合产物分配的减少。这些结果凸显了植物在控制温带草原地下光合产物分配中介导土壤C和N矿化对潜在增加的BPL和降水的响应中的重要性。

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