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通过碳-13交叉极化和魔角旋转核磁共振对腐殖质中高单宁组分进行表征。

Characterization of high-tannin fractions from humus by carbon-13 cross-polarization and magic-angle spinning nuclear magnetic resonance.

作者信息

Lorenz Klaus, Preston Caroline M

机构信息

Institute of Soil Science, University of Hohenheim, Stuttgart, Germany.

出版信息

J Environ Qual. 2002 Mar-Apr;31(2):431-6.

Abstract

Condensed tannins can be found in various parts of many plants. Unlike lignin there has been little study of their fate as they enter the soil organic matter pool and their influence on nutrient cycling, especially through their protein-binding properties. We extracted and characterized tannin-rich fractions from humus collected in 1998 from a black spruce [Picea mariana (Mill.) Britton et al.] forest in Canada where a previous study (1995) showed high levels (3.8% by weight) of condensed tannins. A reference tannin purified from black spruce needles was characterized by solution 13C nuclear magnetic resonance (NMR) as a pure procyanidin with mainly cis stereochemistry and an average chain length of four to five units. The colorimetric proanthocyanidin (PA) assay, standardized against the black spruce tannin, showed that both extracted humus fractions had higher tannin contents than the original humus (2.84% and 11.17% vs. 0.08%), and accounted for 32% of humus tannin content. Consistent with the results from the chemical assay, the aqueous fraction showed higher tannin signals in the 13C cross-polarization and magic-angle spinning (CPMAS) NMR spectrum than the emulsified one. As both tannin-rich humus fractions were depleted in N and high in structures derived from lignin and cutin, they did not have properties consistent with recaldtrant tannin-protein complexes proposed as a mechanism for N sequestration in humus. Further studies are needed to establish if tannin-protein structures in humus can be detected or isolated, or if tannins contribute to forest management problems observed in these ecosystems by binding to and slowing down the activity of soil enzymes.

摘要

缩合单宁存在于许多植物的不同部位。与木质素不同,对于它们进入土壤有机质库后的归宿及其对养分循环的影响,尤其是通过其蛋白质结合特性产生的影响,研究较少。我们从1998年在加拿大黑云杉[Picea mariana (Mill.) Britton et al.]林中收集的腐殖质中提取并表征了富含单宁的组分,此前一项研究(1995年)表明该林分中缩合单宁含量很高(重量比为3.8%)。从黑云杉针叶中纯化得到的一种参考单宁,通过溶液13C核磁共振(NMR)表征为一种主要具有顺式立体化学结构、平均链长为四到五个单元的纯原花青素。以黑云杉单宁为标准的比色原花青素(PA)分析表明,两个提取的腐殖质组分的单宁含量均高于原始腐殖质(分别为2.84%和11.17%,而原始腐殖质为0.08%),占腐殖质单宁含量的32%。与化学分析结果一致,水相组分在13C交叉极化和魔角旋转(CPMAS)NMR谱中的单宁信号比乳化相的更高。由于两个富含单宁的腐殖质组分的氮含量较低,且木质素和角质衍生结构含量较高,它们不具有与被认为是腐殖质中氮固存机制的难降解单宁 - 蛋白质复合物一致的特性。需要进一步研究以确定腐殖质中的单宁 - 蛋白质结构是否能够被检测或分离出来,或者单宁是否通过与土壤酶结合并减缓其活性而导致这些生态系统中观察到的森林管理问题。

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