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Influence of Litter Diversity on Dissolved Organic Matter Release and Soil Carbon Formation in a Mixed Beech Forest

机译:凋落物多样性对山毛榉混交林中可溶性有机物释放和土壤碳形成的影响

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摘要

We investigated the effect of leaf litter on below ground carbon export and soil carbon formation in order to understand how litter diversity affects carbon cycling in forest ecosystems. 13C labeled and unlabeled leaf litter of beech (Fagus sylvatica) and ash (Fraxinus excelsior), characterized by low and high decomposability, were used in a litter exchange experiment in the Hainich National Park (Thuringia, Germany). Litter was added in pure and mixed treatments with either beech or ash labeled with 13C. We collected soil water in 5 cm mineral soil depth below each treatment biweekly and determined dissolved organic carbon (DOC), δ13C values and anion contents. In addition, we measured carbon concentrations and δ13C values in the organic and mineral soil (collected in 1 cm increments) up to 5 cm soil depth at the end of the experiment. Litter-derived C contributes less than 1% to dissolved organic matter (DOM) collected in 5 cm mineral soil depth. Better decomposable ash litter released significantly more (0.50±0.17%) litter carbon than beech litter (0.17±0.07%). All soil layers held in total around 30% of litter-derived carbon, indicating the large retention potential of litter-derived C in the top soil. Interestingly, in mixed (ash and beech litter) treatments we did not find a higher contribution of better decomposable ash-derived carbon in DOM, O horizon or mineral soil. This suggest that the known selective decomposition of better decomposable litter by soil fauna has no or only minor effects on the release and formation of litter-derived DOM and soil organic matter. Overall our experiment showed that 1) litter-derived carbon is of low importance for dissolved organic carbon release and 2) litter of higher decomposability is faster decomposed, but litter diversity does not influence the carbon flow.
机译:我们调查了树叶凋落物对地下碳出口和土壤碳形成的影响,以了解凋落物多样性如何影响森林生态系统中的碳循环。在海尼希国家公园(德国图林根州)的凋落物交换实验中使用了 13 C标记和未标记的山毛榉(Fagus sylvatica)和灰烬(Fraxinus excelsior)具有低可分解性和高分解性的叶子。 )。在纯净和混合处理中添加了标记为山毛榉或灰分 13 C的垃圾。我们每两周收集一次低于每次处理的5 cm矿物土壤深度的土壤水,并确定溶解有机碳(DOC),δ 13 C值和阴离子含量。另外,在实验结束时,我们测量了土壤和土壤中碳的浓度和δ 13 C值(以1 cm的增量收集)直至5 cm的土壤深度。源自垃圾的碳对5 cm矿物土壤深度中收集的溶解有机物(DOM)的贡献不足1%。更好的可分解灰渣释放的碳比山毛榉垃圾(0.17±0.07%)的更多(0.50±0.17%)。所有土壤层中总共含有约30%的凋落物碳,表明凋落物C在顶部土壤中具有很大的保留潜力。有趣的是,在混合处理(灰烬和山毛榉凋落物)中,我们发现在DOM,O层或矿物土壤中,更好的可分解灰分衍生的碳的贡献更大。这表明已知的土壤动物更好分解的垃圾的选择性分解对垃圾衍生的DOM和土壤有机质的释放和形成没有或只有很小的影响。总体而言,我们的实验表明,1)源自垃圾的碳对于溶解性有机碳释放的重要性不高,并且2)具有较高可分解性的垃圾分解速度更快,但垃圾的多样性不会影响碳流量。

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  • 作者

    Andrea Scheibe; Gerd Gleixner;

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  • 年(卷),期 -1(9),12
  • 年度 -1
  • 页码 e114040
  • 总页数 21
  • 原文格式 PDF
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