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Altered humin compositions under organic and inorganic fertilization on an intensively cultivated sandy loam soil

机译:集约耕作的沙壤土上有机和无机施肥下腐殖质组成的变化

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Humin is the most recalcitrant fraction of soil organic matter (SOM). However, little is known about quantitative structural information on humin and the roles of soil mircoorganisms involved in the humin formation. We applied advanced solid-state ~(13)C nuclear magnetic resonance (NMR) spectroscopy to provide deep insights into humin structural changes in response to long-term balanced fertilization on a Calcaric Fluvisol in the North China plain. The relationships between humin structure and microbiological properties such as microbial bio-mass, microbial quotient (q_(mic)) and metabolic quotient (qCO_2) were also studied. The humins had a considerable (35-44%) proportion of aromatic C being nonprotonated and the vast majority of O-alkyl and anomeric C being protonated. Alkyl (24-27% of all C), aromatic C (17-28%) and O-alkyl (13-20%) predominated in humins. Long-term fertilization promoted the aliphatic nature of humins, causing increases in O-alkyl, anomeric and NCH functional groups and decreases in aromatic C and aromatic C-O groups. All these changes were more prominent for treatments of organic fertilizer (OF) and combined mineral NPK fertilizer with OF (NPKOF) relative to the Control and NPK treatments. Fertilization also decreased the alkyl/O-alkyl ratio, aromaticity and hydrophobic characteristics of humins, suggesting a more decomposed and humified state of humin in the Control soil. Moreover, the soil microbiological properties had strong correlations with functional groups of humins. Particularly, microbial biomass C was a relatively sensitive indicator, having positive correlations with oxygen-containing functional groups, i.e., COO/N-C=O and protonated O-alkyl C, and negative correlations with nonprotonated aromatic C. The q_(mic) and qCO_2 were also significantly positively correlated with NCH and aromatic C-O, respectively. Our results deepen our understanding of how long-term fertilization impacts the structure of humin, and highlight a linkage between microbiological properties and recalcitrant fraction of SOM besides labile fraction.
机译:腐殖质是土壤有机质(SOM)中最顽固的部分。但是,关于腐殖质的定量结构信息以及参与腐殖质形成的土壤微生物的作用知之甚少。我们应用先进的固态〜(13)C核磁共振(NMR)光谱技术,深入了解了华北平原钙碳氟维素上长期平衡施肥引起的人类结构变化。还研究了人体结构与微生物特性如微生物生物量,微生物商(q_(mic))和代谢商(qCO_2)之间的关系。腐殖质具有相当比例(35-44%)的芳族碳未被质子化,并且绝大多数的O-烷基和异头C被质子化。腐殖质中,烷基(占所有C的24-27%),芳族C(占17-28%)和O-烷基(占13-20%)占主导地位。长期施肥促进了腐殖质的脂族性质,导致O-烷基,端基和NCH官能团增加,芳族C和芳族C-O减少。与对照和NPK处理相比,所有这些变化在有机肥(OF)以及将矿物NPK肥料与OF(NPKOF)组合处理中均更为突出。施肥还降低了腐殖质的烷基/ O-烷基比率,芳香性和疏水性,这表明对照土壤中的腐殖质更加腐化和腐殖化。此外,土壤微生物学特性与腐殖质的功能基团有很强的相关性。特别地,微生物生物质C是一个相对敏感的指标,与含氧官能团(COO / NC = O和质子化的O-烷基C)呈正相关,与非质子化的芳族C呈负相关。q_(mic)和qCO_2它们也分别与NCH和芳族CO呈显着正相关。我们的研究结果加深了我们对长期施肥如何影响腐殖质结构的理解,并突出了微生物特性和SOM除难降解成分以外的顽固成分之间的联系。

著录项

  • 来源
    《The Science of the Total Environment》 |2017年第1期|356-364|共9页
  • 作者单位

    State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China,University of Chinese Academy of Science, Beijing 100049, China;

    State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China;

    Department of Chemistry and Biochemistry, Old Dominion University, Norfolk, VA 23529, United States;

    Department of Chemistry and Biochemistry, Old Dominion University, Norfolk, VA 23529, United States;

    USDA-ARS, National Laboratory for Agriculture and the Environment, Ames, IA 50011, USA;

    State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China;

    State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Soil organic matter; MultiCP/MAS NMR; Organic fertilizer; Microbial biomass; Microbial quotient; Metabolic quotient;

    机译:土壤有机质;MultiCP / MAS NMR;有机肥料;微生物生物量;微生物商;代谢商;

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