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Soil carbon and nitrogen stocks in forests along an altitudinal gradient in the eastern Himalayas and a meta-analysis of global data

机译:喜马拉雅山脉东部沿海拔梯度森林土壤碳氮储量及全球数据的荟萃分析

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High-altitude soils potentially store a large pool of carbon (C) and nitrogen (N). The assessment of total C and N stocks in soils is vital to understanding the C and N dynamics in terrestrial ecosystems. In this study, we examined effects of altitude and forest composition on soil C and N along a transect from 317 to 3300 m a.s.l. in the eastern Himalayas. We used meta-analysis to establish the context for our results on the effects of altitude on soil C, including variation with depth. Total C and N contents of soils significantly increased with altitude, but decreased with soil depth. Carbon and N were similarly correlated with altitude and temperature, and temperature was seemingly the main driver of soil C along the altitudinal gradient. Altitude accounted for 73% of the variation in C and 47% of the variation in N stocks. Soil pH and cation exchange capacity were correlated with both soil C and N stocks. Increases in soil C and N stocks were related to forest composition, forest basal area as well as quantity of leaf litter that were in turn influenced by altitude and temperature. Concentrations of C in foliage increased by 2.1% for every 1000 m rise in altitude, while that in leaf litter increased by 2.3%.
机译:高海拔土壤可能会储存大量的碳(C)和氮(N)。评估土壤中碳和氮的总量对于了解陆地生态系统中的碳和氮动态至关重要。在这项研究中,我们研究了海拔和森林组成对沿317至3300 m a.s.l的样带土壤C和N的影响。在喜马拉雅山脉东部。我们使用荟萃分析为研究结果对海拔高度对土壤C(包括深度变化)的影响建立了背景。土壤总碳和氮含量随海拔高度显着增加,但随土壤深度降低。碳和氮也与海拔高度和温度相关,温度似乎是土壤碳沿海拔梯度的主要驱动力。海拔占C变化的73%和N种群变化的47%。土壤的pH值和阳离子交换能力与土壤碳氮储量相关。土壤碳和氮储量的增加与森林组成,森林基础面积以及枯枝落叶的数量有关,而后者又受海拔和温度的影响。海拔每增加1000 m,叶子中的C浓度增加2.1%,而凋落物中的C浓度增加2.3%。

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