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首页> 外文期刊>Global change biology >Estimating the contribution of leaf litter decomposition to soil CO2 efflux in a beech forest using C-13-depleted litter
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Estimating the contribution of leaf litter decomposition to soil CO2 efflux in a beech forest using C-13-depleted litter

机译:使用贫C-1​​3凋落物估算山毛榉林中凋落物分解对土壤CO2外流的贡献

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摘要

The contribution of leaf litter decomposition to total soil CO2 efflux (F-L/F) was evaluated in a beech (Fagus sylvatica L.) forest in eastern France. The Keeling-plot approach was applied to estimate the isotopic composition of respired soil CO2 from soil covered with either control (-30.32 parts per thousand) or C-13-depleted leaf litter (-49.96 parts per thousand). The delta(13)C of respired soil CO2 ranged from -25.50 parts per thousand to -22.60 parts per thousand and from -24.95 parts per thousand to -20.77 parts per thousand, respectively, with depleted or control litter above the soil. The F-L/F ratio was calculated by a single isotope linear mixing model based on mass conservation equations. It showed seasonal variations, increasing from 2.8% in early spring to about 11.4% in mid summer, and decreasing to 4.2% just after leaf fall. Between December 2001 and December 2002, cumulated F and F-L reached 0.98 and 0.08 kg(C) m(-2), respectively. On an annual basis, decomposition of fresh leaf litter accounted for 8% of soil respiration and 80% of total C loss from fresh leaf litter. The other fraction of carbon loss during leaf litter decomposition that is assumed to have entered the soil organic matter pool (i.e. 20%) represents only 0.02 kg(C) m(-2).
机译:在法国东部的山毛榉(Fagus sylvatica L.)森林中评估了凋落物分解对土壤总CO2外流的贡献(F-L / F)。应用Keeling-plot方法估算覆盖有对照(-30.32份/千)或C-13枯竭的枯枝落叶(-49.96份/千)的土壤中呼吸的土壤CO2的同位素组成。呼吸土壤CO2的δ(13)C范围分别为每千分之-25.50至-22.60,以及每千分之-24.95至-20.77,土壤上已枯竭或控制凋落。基于质量守恒方程,通过单个同位素线性混合模型计算F-L / F比。它显示出季节变化,从早春的2.8%增加到夏中的大约11.4%,并在叶子落下后下降到4.2%。在2001年12月至2002年12月之间,累积的F和F-L分别达到0.98和0.08 kg(C)m(-2)。每年,新鲜凋落物的分解占土壤呼吸的8%,占新鲜凋落物总C损失的80%。假定已进入土壤有机质库的叶子凋落物分解过程中的碳损失的其他部分(即20%)仅代表0.02 kg(C)m(-2)。

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