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首页> 外文期刊>Geoderma: An International Journal of Soil Science >C-13 NMR and FTIR spectroscopy characterization of humic acids in spodosols under tropical rain forest in southeastern Brazil
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C-13 NMR and FTIR spectroscopy characterization of humic acids in spodosols under tropical rain forest in southeastern Brazil

机译:巴西东南部热带雨林下藤茎溶胶中腐殖酸的C-13 NMR和FTIR光谱表征

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The aim of the present study was to characterize the humic acids (HAs) in spodosols developed on quartzitic, sandy, nutrient-poor parent materials under restinga forest. C-13 NMR and FTIR spectroscopy were used to obtain information about the mechanism of podzolization in tropical climates in three sandy coastal podzols (Histic Alaquod, Typic Alorthod and Arenic Alorthod) from Cardoso Island (Sao Paulo-Brazil). HAs were extracted from all horizons and C-13 NMR and FTIR measurements were performed on all HA samples. Similarities between the surface horizon A from a Typic Alorthod (C14) and the Ho horizon from a Histic Alaquod (H13) were observed. Below the E horizon, the spectra of profile H13 closely resembled the spectra of C14. The increase in alkyl carbon and decrease in acetal carbon, aromatic C and phenolic C with increasing depth suggests enrichment of methylene structures by the microbial biomass. This idea was further supported by an increase in the decomposition of polysaccharides and lignin throughout the profiles. The similarity of the composition may be evidence of vertical translocation throughout the profile, with no incorporation of organic matter (OM) components from other sources such as roots or their residues. The chemical structure of profile Arenic Alorthod (H9) differed from that of the other profiles. The increase in methoxylic, aromatic and phenolic groups as depth increased probably indicates an increase in tannin-like compounds with depth. The higher content of tannins in this soil indicates the presence of more fresh litter and/or a less intense decomposition process than in Histic Alaquod and Typic Alorthod soils. In the latter soil the large amounts of aliphatics and small amounts of lignin-derived products reflect strong aerobic decay. The presence of significant methylene absorption in the FTIR spectra indicates that this alkyl material was dominated by the mobile lignin-derived products, in accordance with the NMR results, which revealed that the HAs have greater aliphatic than aromatic character. (C) 2008 Elsevier B.V. All rights reserved.
机译:本研究的目的是表征在resta森林下在石英质,沙质,营养缺乏的母体材料上形成的spodosol中的腐殖酸(HAs)。使用C-13 NMR和FTIR光谱来获得有关热带气候中来自卡多索岛(圣保罗-巴西)的三个沙质沿海小动物(Histic Alaquod,Typic Alorthod和Arenic Alorthod)中动物足动物化机理的信息。从所有视野中提取HA,并对所有HA样品进行C-13 NMR和FTIR测量。观察到典型Tyor Alorthod(C14)的表面层A与Histic Alaquod(H13)的Ho层之间的相似性。在E地平线以下,剖面H13的光谱与C14的光谱非常相似。随着深度的增加,烷基碳的增加和乙缩醛碳,芳族碳和酚类碳的减少表明微生物生物质对亚甲基结构的富集。整个剖面中多糖和木质素分解的增加进一步支持了这一想法。组成的相似性可能是整个剖面中垂直易位的证据,而没有掺入其他来源(例如根或残留物)的有机物(OM)成分。轮廓Arenic Alorthod(H9)的化学结构不同于其他轮廓。随着深度的增加,甲氧基,芳族和酚基的增加可能表明单宁类化合物随深度的增加而增加。与Histic Alaquod和Typic Alorthod土壤相比,该土壤中单宁含量较高表明存在更多的新鲜凋落物和/或分解强度较低的过程。在后一种土壤中,大量的脂肪族物质和少量的木质素衍生产品反映出强烈的需氧能力。根据NMR结果,在FTIR光谱中存在大量的亚甲基吸收表明该烷基材料主要由可移动的木质素衍生产物控制,这表明HA具有更高的脂族特性而不是芳族特性。 (C)2008 Elsevier B.V.保留所有权利。

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