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Phosphorus fertilization alters complexity of paddy soil dissolved organic matter

机译:磷肥改变水稻土溶解有机质的复杂性

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摘要

The structural complexity of soil dissolved organic matter(DOM)may reflect soil biogeochemical processes due to its spectral characteristics.However,the features of DOM structural complexity in paddy soil amended with long-term chemical P fertilization are still unclear,which may limit understanding of nutrient-related soil C cycle.We collected soil samples from field experiments receiving application of 0,30,60,and 90 kg P ha–1 yr–1 to assess the effect of exogenous P on the complexity of soil DOM structure.Three-dimensional excitation-emission matrix fluorescence analysis and enzymatic activity assay were used to determine the features of soil DOM molecular structure and the associated microbial reactions.The results showed that P input increased the biodegradability of DOM,indicating by the increased lower molecular weight components and decreased humic degree in the DOM.P input also reduced the structural complexity of DOM with blue shifts of fluorescent signals.The fluorescence index andβ/αindex of DOM increased with increasing P application by 4–5%and 3–11%,respectively,while humification index decreased by 8–13%.The P input increased the abundance of bacteria and fungi by 34–167%and 159–964%,respectively,while 29–54%increments were found for theβ-1,4-glucosidase activities.These results implicated that P fertilization accelerated the soil DOM cycle,although the structural complexity of DOM declined,which potentially benefits soil C sequestration in paddy fields and may be a C sequestration mechanism in the P-dependent paddy.
机译:土壤溶解性有机质(DOM)的光谱复杂性可能反映了土壤生物地球化学过程。但是,长期施用化学磷肥后,水稻土壤中DOM复杂性的特征仍不清楚,这可能限制了对土壤有机质的认识。与养分有关的土壤碳循环。我们从野外试验中收集了土壤样品,分别接受了0、30、60和90 kg P ha-1 yr-1的施用,以评估外源P对土壤DOM结构复杂性的影响。三利用三维激发-发射矩阵荧光分析和酶活性测定方法确定了土壤DOM的分子结构特征和相关的微生物反应。结果表明,P输入增加了DOM的生物降解性,表明低分子量成分增加而降低。 DOM.P输入中的腐烂度还通过荧光信号的蓝移降低了DOM的结构复杂性。 DOM的dex和β/α指数随施磷量的增加分别增加4–5%和3–11%,而腐殖化指数则降低8–13%。磷的输入使细菌和真菌的丰度增加34–167%, β-1,4-葡萄糖苷酶的活性分别增加了159–964%,而增加了29–54%。这些结果表明,尽管施肥使土壤DOM循环加快,但DOM的结构复杂性有所降低,这可能有利于土壤C在稻田中的螯合,可能是依赖P的稻田中的C螯合机制。

著录项

  • 来源
    《农业科学学报:英文版》 |2020年第009期|P.2301-2312|共12页
  • 作者单位

    College of Environmental and Resource Science Zhejiang University Hangzhou 310058 P.R.ChinaChina Academy of West Region Development Zhejiang University Hangzhou 310058 P.R.China;

    College of Environmental and Resource Science Zhejiang University Hangzhou 310058 P.R.China;

    College of Environmental and Resource Science Zhejiang University Hangzhou 310058 P.R.China;

    Hangzhou Gusheng Agricultural Technology Company Limited Hangzhou 311108 P.R.China;

    College of Environmental and Resource Science Zhejiang University Hangzhou 310058 P.R.China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 土壤学;
  • 关键词

    soil carbon; fertilization; fluorescence; humification; agroecosystem;

    机译:土壤碳;施肥;荧光;增湿;农业生态系统;
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