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首页> 外文期刊>iForest: Biogeosciences and Forestry >The manipulation of aboveground litter input affects soil CO2 efflux in a subtropical liquidambar forest in China
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The manipulation of aboveground litter input affects soil CO2 efflux in a subtropical liquidambar forest in China

机译:地上凋落物输入的操作影响中国亚热带枫香林的土壤CO2排放

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Litters on the forest floor represent an important organic carbon (C) sources from aboveground plants to the soil, which therefore have a significant influence on belowground processes such as soil respiration. In this study, dynamic property of soil respiration was investigated under aboveground litter manipulation treatments in a liquidambar forest in subtropical China. The purpose of this study was to examine the impacts of changing aboveground litter inputs on soil CO2 emission in forests. The litter manipulation included litter addition (LA), litter removal (LR) and litter control (LC) treatments. Each litter treatment had six replications. Soil respiration rates were measured using an infrared gas analyzer system (LI-COR 8100) with soil chambers. The results showed that mean soil respiration rates increased significantly in LA plots (mean ?± SE: 2.21 ?± 0.44 ??mol m-2 s-1; P0.05) and decreased slightly in LR plots (1.17 ?± 0.16 ??mol m-2 s-1) when compared to control plots (1.42 ?± 0.20 ??mol m-2 s-1). On average, LA treatment significantly increased annual soil respiration by about 56% (837.5 ?± 165 gC m-2 year-1), while LR treatment decreased soil respiration by approximately 17% (443.1 ?± 61.7 gC m-2 year-1) compared with the control (535.5 ?± 75.7 gC m-2 year-1). The a??priming effecta?? was a primary contributor to the increase of soil respiration in LA treatments and the reduction of soil CO2 efflux was mainly ascribed to the elimination of organic C sources in LR treatments. Soil temperature was the main factor affecting seasonal variation in soil respiration. Up to the 90% to 95% seasonal variation in soil respiration is explained by soil temperature within each of the litter treatments. Our study indicated that changes in litter inputs due to climate change and human practices would significantly affected soil CO2 emission and would subsequently affect C balance in subtropical forests.
机译:森林地面上的凋落物是从地上植物到土壤的重要有机碳(C)来源,因此对地下过程(例如土壤呼吸)具有重要影响。本文研究了亚热带枫香林地上凋落物处理条件下土壤呼吸的动态特性。这项研究的目的是研究改变地上凋落物投入对森林土壤CO2排放的影响。垃圾处理包括添加垃圾(LA),清除垃圾(LR)和控制垃圾(LC)。每个垫料处理重复六次。使用带有土壤室的红外气体分析仪系统(LI-COR 8100)测量土壤呼吸速率。结果表明,LA样地的平均土壤呼吸速率显着提高(平均Δ±SE:2.21Δ±0.44 mol m-2 s-1; P <0.05),而在LR样地(1.17Ω±0.16Ω)。 mol m-2 s-1)与对照图(1.42Ω±0.20Ω·mol m-2 s-1)相比。平均而言,LA处理显着增加了每年土壤呼吸约56%(837.5?±165 gC m-2 year-1),而LR处理则使土壤呼吸减少了约17%(443.1?±61.7 gC m-2 year-1) )与对照组(535.5±75.7 gC m-2 year-1)进行比较。引发作用这是造成LA处理土壤呼吸增加的主要原因,而土壤CO2外排的减少主要归因于LR处理中有机碳源的消除。土壤温度是影响土壤呼吸季节变化的主要因素。每种垫料处理中的土壤温度可以解释多达90%至95%的土壤呼吸季节变化。我们的研究表明,由于气候变化和人类行为造成的垫料输入量变化将显着影响土壤CO2排放,并随后影响亚热带森林中的碳平衡。

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