Nitrogen fertilization modifies organic transformations and coatings on soil biogeochemical interfaces through microbial polysaccharides synthesis

Research output: Contribution to journalArticleResearchpeer review

Authors

  • Xizhi Huang
  • Georg Guggenberger
  • Yakov Kuzyakov
  • Olga Shibistova
  • Tida Ge
  • Yiwei Li
  • Bifeng Liu
  • Jinshui Wu

External Research Organisations

  • Huazhong University of Science and Technology
  • Chinese Academy of Sciences (CAS)
  • University of Göttingen
  • Kazan Volga Region Federal University
  • Peoples' Friendship University of Russia (RUDN)
  • V.N. Sukachev Institute of Forest SB RAS
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Details

Original languageEnglish
Article number18684
JournalScientific reports
Volume9
Issue number1
Publication statusPublished - 10 Dec 2019

Abstract

The soil-water interfaces (SWI) in soil pores are hotspots for organic matter (OM) transformation. However, due to the heterogeneous and opaque nature of soil microenvironment, direct and continuous tracing of interfacial reactions, such as OM transformations and formation of organo-mineral associations, are rare. To investigate these processes, a new soil microarray technology (SoilChips) was developed and used. Homogeneous 800-μm-diameter SoilChips were constructed by depositing a dispersed Oxisol A horizon suspension on a patterned glass. Dissolved organic matter from the original soil was added on the SoilChips to mimic SWI processes. The effects of ammonium fertilization (90 mg N kg−1 soil) on chemical composition of SWIs were evaluated via X-ray photoelectron spectroscopy. Over 21 days, ammonium addition increased OM coatings at SWIs and modified the OM chemical structure with more alcoholic- and carboxylic-C compared to the unfertilized control. Molecular modeling of OM composition at SWIs showed that N fertilization mainly facilitated the microbial production of glucans. We demonstrated that N availability modifies the specific OM molecular processing and its immobilization on SWIs, thereby providing a direct insight into biogeochemical transformation of OM at micro-scale.

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Cite this

Nitrogen fertilization modifies organic transformations and coatings on soil biogeochemical interfaces through microbial polysaccharides synthesis. / Huang, Xizhi; Guggenberger, Georg; Kuzyakov, Yakov et al.
In: Scientific reports, Vol. 9, No. 1, 18684, 10.12.2019.

Research output: Contribution to journalArticleResearchpeer review

Huang X, Guggenberger G, Kuzyakov Y, Shibistova O, Ge T, Li Y et al. Nitrogen fertilization modifies organic transformations and coatings on soil biogeochemical interfaces through microbial polysaccharides synthesis. Scientific reports. 2019 Dec 10;9(1):18684. doi: 10.1038/s41598-019-55174-y, 10.15488/10477
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title = "Nitrogen fertilization modifies organic transformations and coatings on soil biogeochemical interfaces through microbial polysaccharides synthesis",
abstract = "The soil-water interfaces (SWI) in soil pores are hotspots for organic matter (OM) transformation. However, due to the heterogeneous and opaque nature of soil microenvironment, direct and continuous tracing of interfacial reactions, such as OM transformations and formation of organo-mineral associations, are rare. To investigate these processes, a new soil microarray technology (SoilChips) was developed and used. Homogeneous 800-μm-diameter SoilChips were constructed by depositing a dispersed Oxisol A horizon suspension on a patterned glass. Dissolved organic matter from the original soil was added on the SoilChips to mimic SWI processes. The effects of ammonium fertilization (90 mg N kg−1 soil) on chemical composition of SWIs were evaluated via X-ray photoelectron spectroscopy. Over 21 days, ammonium addition increased OM coatings at SWIs and modified the OM chemical structure with more alcoholic- and carboxylic-C compared to the unfertilized control. Molecular modeling of OM composition at SWIs showed that N fertilization mainly facilitated the microbial production of glucans. We demonstrated that N availability modifies the specific OM molecular processing and its immobilization on SWIs, thereby providing a direct insight into biogeochemical transformation of OM at micro-scale.",
author = "Xizhi Huang and Georg Guggenberger and Yakov Kuzyakov and Olga Shibistova and Tida Ge and Yiwei Li and Bifeng Liu and Jinshui Wu",
note = "Funding information: The authors gratefully acknowledge financial support from the National Natural Science Foundation of China (No. 41090283; No. 41430860; No. 41807051) as well as and National Science Foundation of China and Russian Foundation of Basic Research joint project (N 19-54-53026) granted to T.G. and O.S. The publication was supported by the Russian Government Program of Competitive Growth of Kazan Federal University and with the support of the “RUDN University program 5–100”. Contribution of YK was supported by the Russian Science Foundation (project No. 19-77-30012).",
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AU - Ge, Tida

AU - Li, Yiwei

AU - Liu, Bifeng

AU - Wu, Jinshui

N1 - Funding information: The authors gratefully acknowledge financial support from the National Natural Science Foundation of China (No. 41090283; No. 41430860; No. 41807051) as well as and National Science Foundation of China and Russian Foundation of Basic Research joint project (N 19-54-53026) granted to T.G. and O.S. The publication was supported by the Russian Government Program of Competitive Growth of Kazan Federal University and with the support of the “RUDN University program 5–100”. Contribution of YK was supported by the Russian Science Foundation (project No. 19-77-30012).

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N2 - The soil-water interfaces (SWI) in soil pores are hotspots for organic matter (OM) transformation. However, due to the heterogeneous and opaque nature of soil microenvironment, direct and continuous tracing of interfacial reactions, such as OM transformations and formation of organo-mineral associations, are rare. To investigate these processes, a new soil microarray technology (SoilChips) was developed and used. Homogeneous 800-μm-diameter SoilChips were constructed by depositing a dispersed Oxisol A horizon suspension on a patterned glass. Dissolved organic matter from the original soil was added on the SoilChips to mimic SWI processes. The effects of ammonium fertilization (90 mg N kg−1 soil) on chemical composition of SWIs were evaluated via X-ray photoelectron spectroscopy. Over 21 days, ammonium addition increased OM coatings at SWIs and modified the OM chemical structure with more alcoholic- and carboxylic-C compared to the unfertilized control. Molecular modeling of OM composition at SWIs showed that N fertilization mainly facilitated the microbial production of glucans. We demonstrated that N availability modifies the specific OM molecular processing and its immobilization on SWIs, thereby providing a direct insight into biogeochemical transformation of OM at micro-scale.

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