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Dynamics of de Novo Formation of Amino Sugars in Soil via CSSIA

机译:通过CSSIA的土壤中氨基糖的De Novo形成动态

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Amino sugars are the building blocks of microbial cell walls and have been used widely to assess microbial residues. To have a better insight in the formation dynamics of amino sugars in soil, uniformly carbon-13 (~(13)Cs)-labelled wheat residue of different quality (grain, leaf and root) was amended to two soils under distinct tillage managements. The isotopic composition of individual amino sugars was measured using liquid chromatography — isotope ratio mass spectrometry (LC-IRMS). Maximum formationwas reached within a few days after residue addition. Glucosamine and galactosamine followed dissimilar formation kinetics. The maxima of incorporation of residue C into the amino sugar pools ranged from 1.0 percent for galactosamine to 10.6 percent forglucosamine. Formation rate constants of residue-derived amino sugars ranged from 0.11 to 0.48/d for galactosamine and glucosamine, respectively. In general, larger amounts of amino sugars were formed at a higher rate with increasing plant residue quality. The microbial community of the no-till soil was better adapted to assimilate low quality plant residues (i.e. leaf and root). All together, the formation dynamics of microbial cell wall components was component-specific and determined by residue quality and the soil microbial community.
机译:氨基糖是微生物细胞壁的构建块,并且已广泛用于评估微生物残留物。为了更好地了解土壤中氨基糖的形成动态,均匀的碳-13(〜(13)Cs)不同质量(谷物,叶子和根)的标记小麦残留物在不同的耕作管理下进行两种土壤。使用液相色谱 - 同位素比质谱法(LC-IRMS)测量单个氨基糖的同位素组成。在残留物添加后几天内达到的最大形成。氨基葡萄糖和半乳糖胺跟随不同的形成动力学。将残余物C掺入氨基糖池中的最大值范围为半乳糖胺的1.0%至10.6%的Forglucosamine。残留衍生的氨基糖的形成速率常数分别为半乳糖胺和葡糖胺的0.11至0.48 / d。通常,随着植物残留物质的增加,以更高的速率形成较大量的氨基糖。 No-Till土壤的微生物群落更好地适应吸收低质量的植物残留物(即叶子和根)。全部,微生物细胞壁组分的形成动态是特异性的,由残留质量和土壤微生物群落确定。

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