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Long-Term Simulated Atmospheric Nitrogen Deposition Alters Leaf and Fine Root Decomposition

机译:长期模拟大气氮沉积改变叶和细根分解

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摘要

Atmospheric nitrogen deposition increases forest carbon sequestration across broad parts of the Northern Hemisphere. Slower organic matter decomposition and greater soil carbon accumulation could contribute to this increase in carbon sequestration. We investigated the effects of chronic simulated nitrogen deposition on leaf litter and fine root decomposition at four sugar maple (Acer saccharum)-dominated northern hardwood forests. At these sites, we previously observed that nitrogen additions increased soil organic carbon and altered litter chemistry. We conducted a 3-year decomposition study with litter bags. Litter production of leaves and fine roots were combined with decomposition dynamics to estimate how fine roots and leaf litter contribute to soil organic carbon. We found that nitrogen additions marginally stimulated early-stage decomposition of leaf litter, an effect associated with previously documented changes in litter chemistry. In contrast, nitrogen additions inhibited the later stages of fine root decomposition, which is consistent with observed decreases in lignin-degrading enzyme activities with nitrogen additions at these sites. At the ecosystem scale, slower fine root decomposition led to additional root mass retention (g m(-2)), and this greater retention of root residues was estimated to explain 5-51% of previously documented carbon accumulation in the surface soil due to nitrogen additions. Our results demonstrated that simulated nitrogen deposition created contrasting effects on the decomposition of leaf litter and fine roots. Although previous nitrogen deposition studies have focused on leaf litter, this work suggests that slower fine root decomposition is a major driver of soil organic carbon accumulation under elevated nitrogen deposition.
机译:大气氮沉积增加了北半球宽部位的森林碳封存。较慢的有机物分解和更大的土壤碳积累可能导致碳封存的这种增加。我们研究了慢性模拟氮沉积对叶片凋落物和细根分解的影响,在四个糖枫(Acer Saccharum) - 德国北硬木林中。在这些位点,我们以前观察到氮气增加的土壤有机碳和改变的垃圾化学。我们用垃圾袋进行了3年的分解研究。叶片和细根的垃圾产生与分解动力学结合,以估计源根和叶片凋落物如何促成土壤有机碳。我们发现氮气添加了薄片凋落物的初步刺激的早期分解,一种与先前记录的垃圾化学变化相关的效果。相反,氮添加抑制了细根分解的后期阶段,这与在这些位点的氮气添加中观察到的木质素降解酶活性的降低一致。在生态系统规模,细根分解较慢导致额外的根质量保留(GM(-2)),估计根残留物的更大保留以解释由于氮导致的表面土壤中先前记录的碳积累的5-51%添加。我们的结果表明,模拟氮沉积对叶子凋落物和细根的分解产生了对比作用。尽管以前的氮沉积研究集中于叶子垃圾中,但这项工作表明,细根分解较慢,是在氮沉积下的土壤有机碳积累的主要驱动器。

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