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Tannins and nutrient dynamics in forest soils: Plant-litter-soil interactions.

机译:森林土壤中的单宁和养分动态:植物-凋落物-土壤的相互作用。

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Tannins affect ecosystem processes such as organic matter degradation, nitrogen cycling, soil formation and successional dynamics. In woody species, foliar tannin levels commonly range from 10 to 25% dry weight. Through litter leaching and deposition forest soils receive appreciable tannin inputs. Tannins in litter and soil may affect nutrient cycling by hindering decomposition, complexing proteins, inhibiting enzyme activities and inducing toxicity to microbial populations. Research presented in this thesis addressed the following questions: (1) What is known about the influence of tannins on nutrient dynamics? (2) How does tannin structure influence tannin reactivity? (3) How do soil conditions influence plant tannin production? and (4) How do tannins with different structures affect soil C and N mineralization? Standard assays used to quantify tannins were found to be affected by tannin structural characteristics. Particularly important was the distinction between condensed and hydrolyzable tannins, the hydroxylation pattern of the condensed tannin B-ring and the stereochemistry at the C2–C3 position. In greenhouse studies using soil and sand culture, fertility and pH effects on foliar and fine root growth and chemical composition were found. While lower nutrient levels were clearly related to higher concentrations of total phenols and tannins, acidity effects were less consistent. Results derived from laboratory C and N mineralization studies in the presence of different purified tannins support a hypothesis that ascribes reduced N availability in the presence of tannins to sequestration of organic N, as well as to immobilization associated with the addition of a labile C source. Differences in reactivity among tannins have important implications both for tannin quantification and their effects on ecological processes. The chemical structure of individual tannins can most likely explain differences in the type and magnitude of effects observed among tannin sources. Because plant species, as well as foliar and root materials, do not respond uniformly to changing soil fertility and pH it is difficult to generalize about how site conditions influence phytochemistry. Studies on tannins should recognize that tannins with varying structures may have different chemical reactivities and thus are expected to have distinct fates and effects on biogeochemical processes and ecosystem function.
机译:单宁会影响生态系统过程,例如有机物降解,氮循环,土壤形成和演替动力学。在木本物种中,叶面单宁含量通常为干重的10%至25%。通过垃圾的淋洗和沉积,森林土壤获得了大量的单宁投入。凋落物和土壤中的单宁酸可能通过阻碍分解,复合蛋白质,抑制酶活性以及对微生物种群产生毒性而影响养分循环。本文提出的研究解决了以下问题:(1)关于单宁对营养动力学的影响了解多少? (2)单宁结构如何影响单宁反应性? (3)土壤条件如何影响植物单宁的产量? (4)不同结构的单宁如何影响土壤碳和氮的矿化作用?发现用于定量单宁的标准测定法受单宁结构特征的影响。尤其重要的是缩合单宁和可水解单宁的区别,缩合单宁B环的羟基化方式以及C2-C3位置的立体化学。在使用土壤和沙土栽培的温室研究中,发现了肥力和pH对叶面和细根生长以及化学成分的影响。虽然较低的养分水平显然与总酚和单宁含量较高有关,但酸度影响却不太一致。在不同的纯化单宁存在下从实验室C和N矿化研究得出的结果支持这样一个假说,即单宁存在下氮的有效性降低是由于螯合有机N以及与添加不稳定C源相关的固定化。单宁之间反应性的差异对于单宁定量及其对生态过程的影响都具有重要意义。单宁的化学结构很可能可以解释单宁来源中观察到的作用类型和程度的差异。由于植物物种以及叶面和根部材料对变化的土壤肥力和pH值的响应不一致,因此很难概括一下场地条件如何影响植物化学。有关单宁的研究应认识到,结构不同的单宁可能具有不同的化学反应性,因此有望对生物地球化学过程和生态系统功能产生不同的命运和影响。

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