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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Assessment of lignin and (poly-)phenol transformations in oak (Quercus robur) dominated soils by 13C-TMAH thermochemolysis
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Assessment of lignin and (poly-)phenol transformations in oak (Quercus robur) dominated soils by 13C-TMAH thermochemolysis

机译:通过13C-TMAH热化学分析评估橡树(栎木)为主的土壤中木质素和(多)酚的转化

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Two sandy soil profiles under oak forest were examined for their phenolic composition using 13C labelled tetramethylammonium hydroxide (TMAH) thermochemolysis, the first application of this method to soils. Lignin, demethylated lignin, hydrolysable tannin, and other phenolic acids could be distinguished, and as such indications of the relative distribution of these sources among the soil horizons was determined. Some compounds extracted from soils using TMAH thermochemolysis, all of which are permethylated phenols, can have multiple structural and botanical sources, such as 3,4-dimethoxybenzoic acid methyl ester from vanillic acid or demethylated vanillic acid derived from lignin, or protocatechuic acid as the initial compound. Correcting the common lignin proxies for contributions of non-lignin phenols and altered lignin, it was found that Λ (yield of monomers upon thermochemolysis), F/P (ferulic acid/p-coumaric acid), Ac/Al (acid/aldehyde) ratios, and Γ (indicator of side chain shortening) were severely influenced by non-lignin phenols. By contrast, the S/G (syringyl/guaiacyl) and C/G (cinnamyl/guaiacyl) ratios remained rather similar. The proxies that changed the most were those that affect interpretations of lignin patterns in terms of source, alteration and preservation. From L to Ah horizons, a progressive lignin alteration was found for both soils, but the differences in litter input among plant materials (leaves, bark, branches, roots) also potentially affected the lignin patterns within and between both profiles. Therefore, important insights into the rapid changes in lignin chemistry between organic and mineral horizons were provided as this method permitted enhanced distinction between fresh source input and decomposition. Even with the corrections to lignin proxies, the soil lignin and polyphenol chemistry remained complex and highlights the limitations of using a few or only one lignin proxy in assessing soil organic matter dynamics.
机译:使用13C标记的四甲基氢氧化铵(TMAH)热化学分解法研究了橡树林下的两个沙质土壤剖面的酚类组成,这是该方法的首次应用。可以区分木质素,脱甲基木质素,可水解单宁和其他酚酸,因此可以确定这些来源在土壤层中的相对分布。使用TMAH热化学法从土壤中提取的某些化合物都是全甲基化酚,它们可能具有多种结构和植物来源,例如来自香草酸的3,4-二甲氧基苯甲酸甲酯或来自木质素的去甲基化香草酸或原儿茶酸。初始化合物。校正常见的木质素代理对非木质素酚和改变的木质素的贡献,发现Λ(热化学分解时的单体产率),F / P(阿魏酸/对香豆酸),Ac / Al(酸/醛)比率和Γ(侧链缩短的指标)受到非木质素酚的严重影响。相比之下,S / G(丁香基/愈创木基)和C / G(肉桂基/愈创木基)的比率仍然相当相似。变化最大的代理是那些在来源,变更和保存方面影响木质素模式解释的代理。从L到Ah地平线,两种土壤都发现了木质素的逐步变化,但是植物材料(叶子,树皮,树枝,根)之间的凋落物输入差异也可能影响两种剖面内和之间的木质素模式。因此,提供了有关有机层和矿物层之间木质素化学快速变化的重要见解,因为这种方法可以增强区分新鲜源输入和分解的能力。即使对木质素代理进行了校正,土壤木质素和多酚化学仍然复杂,并突出了使用少量或仅一种木质素替代物评估土壤有机质动态的局限性。

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