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Variation of soil organic matter depends on light-fraction organic matter under long-term monocropping of different crops

Author

Listed:
  • Futao Zhang

    (National Observation Station of Hailun Agroecology System, Key Laboratory of Mollisols Agroecology, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Harbin, P.R. China
    University of Chinese Academy of Sciences, Beijing, P.R. China
    National Engineering Laboratory for Improving Quality of Arable Land, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing, P.R. China)

  • Yunfa Qiao

    (Nanjing University of Information Science and Technology, Nanjing, P.R. China)

  • Xiaozeng Han

    (National Observation Station of Hailun Agroecology System, Key Laboratory of Mollisols Agroecology, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Harbin, P.R. China)

  • Bin Zhang

    (National Observation Station of Hailun Agroecology System, Key Laboratory of Mollisols Agroecology, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Harbin, P.R. China
    University of Chinese Academy of Sciences, Beijing, P.R. China
    National Engineering Laboratory for Improving Quality of Arable Land, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing, P.R. China)

Abstract

Cultivating crops influences soil organic matter (SOM), but the effect of different crops remains unclear, particularly under long-term monocropping. The objective of this study was to identify how different crops influence the content and chemical structures of SOM under long-term monocropping. Here, soils were sampled (0-20 cm) under 27-year soybean and maize monocropping and separated into different physical fractions. The content and chemical structures of SOM in all fractions were determined. SOM contents were higher under soybean than maize in bulk soil and macroaggregates and their light-fractions instead of microaggregates and silt and clay. The difference in SOM chemical structure was observed in aggregates and density fractions rather than bulk soils and supported by the result of principal component analysis. The proportion of O-alkyl C in macro- and microaggregates and all free light fractions and that of aromatic C in mineral-associated fractions were higher, while that of carbonyl C was lower under maize than soybean. These results demonstrated that different crops monocropping influences the content and chemical structures of SOM, and the variations were mainly in the light-fraction SOM and highlight a higher sensitivity of physical fractions than bulk soil to different crops.

Suggested Citation

  • Futao Zhang & Yunfa Qiao & Xiaozeng Han & Bin Zhang, 2021. "Variation of soil organic matter depends on light-fraction organic matter under long-term monocropping of different crops," Plant, Soil and Environment, Czech Academy of Agricultural Sciences, vol. 67(10), pages 588-599.
    • Handle: RePEc:caa:jnlpse:v:67:y:2021:i:10:id:350-2021-pse
    DOI: 10.17221/350/2021-PSE
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    References listed on IDEAS

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    1. X.B. Liu & X.Y. Zhang & Y.X. Wang & Y.Y. Sui & S.L. Zhang & S.J. Herbert & G. Ding, 2010. "Soil degradation: a problem threatening the sustainable development of agriculture in Northeast China," Plant, Soil and Environment, Czech Academy of Agricultural Sciences, vol. 56(2), pages 87-97.
    2. Margaret S. Torn & Susan E. Trumbore & Oliver A. Chadwick & Peter M. Vitousek & David M. Hendricks, 1997. "Mineral control of soil organic carbon storage and turnover," Nature, Nature, vol. 389(6647), pages 170-173, September.
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