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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Effect of N content and soil texture on the decomposition of organic matter in forest soils as revealed by solid-state CPMAS NMR spectroscopy
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Effect of N content and soil texture on the decomposition of organic matter in forest soils as revealed by solid-state CPMAS NMR spectroscopy

机译:固态CPMAS NMR光谱显示氮含量和土壤质地对森林土壤中有机物分解的影响

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摘要

N has a controlling effect on litter biodegradation in the forest floor, while stabilization of organic matter in the mineral soil may be influenced by physical parameters related to soil texture. In this study, in order to understand the processes involved in soil organic matter (SOM) formation, the chemical composition of SOM was followed and evaluated with regards to N contents and soil texture. Samples were taken on sites covered with Norway spruce and displaying contrasting values of C/N ratios in the forest floor. The chemical structure of OM was characterized using solid-state CPMAS C-13 and N-15 nuclear magnetic resonance (NMR) spectroscopy, along with Proton Spin Relaxation Editing (PSRE) sequences. Four groups of sampling sites were defined based on the NMR spectra of Oh and A horizons. In each group displaying similar NMR characteristics, N content and soil texture could be highly different among sites. Some Oh horizons with similar NMR spectra had very different N contents. Highly humified OM in Oh horizons were observed mainly on sites with low N contents. Some A horizons with different soil texture displayed similar OM chemical structure. High contents of O-alkyl C in some A horizons could originate from higher fresh root material input. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 24]
机译:氮对林地凋落物的生物降解具有控制作用,而矿质土壤中有机物的稳定可能受到与土壤质地有关的物理参数的影响。在这项研究中,为了了解涉及土壤有机质(SOM)形成的过程,遵循了SOM的化学成分并就N含量和土壤质地进行了评估。在挪威云杉覆盖的地点取样,并在林地中显示出对比的C / N比值。 OM的化学结构使用固态CPMAS C-13和N-15核磁共振(NMR)光谱以及质子自旋弛豫编辑(PSRE)序列进行表征。根据Oh和A层的NMR光谱定义了四组采样点。在显示相似的NMR特征的每个组中,站点之间的N含量和土壤质地可能存在很大差异。一些具有相似NMR光谱的Oh层具有非常不同的N含量。在Oh层中高度腐殖化的OM主要观察到低N含量的部位。不同土壤质地的一些A层显示出相似的OM化学结构。在某些A层中,高含量的O-烷基C可能源于较高的新鲜根料输入。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:24]

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