4.7 Article

Linking chemical structure of dissolved organic carbon and microbial community composition with submergence-induced soil organic carbon mineralization

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 692, Issue -, Pages 930-939

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2019.07.286

Keywords

Cropland soils; Submergence-induced SOC mineralization; Concentration and chemical structure of soil; DOC; Soil microbial metabolic potential and community composition; Solution-state H-1 NMR

Funding

  1. National Natural Science Foundation of China [31700452, 41877099]
  2. Natural Science Foundation of Anhui Province [1808085MD97]
  3. Science and Technology Major Project of Anhui Province [18030701188]
  4. State Key Research and Development Program of China [2016YFD0200107]
  5. Project of the Introduction of the Leading Talent Team in Colleges and Universities of Anhui Province of China [gxljtdzd201607]

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Much research has been devoted to investigating how water-extractable organic carbon (DOC) concentration and microbial activity regulate soil organic carbon (SOC) mineralization when soils are saturated with water. However, the relationships of DOC chemical structure and microbial community composition with SOC mineralization, as well as the relative contributions of microbial decomposers and their substrates on the mineralization rate have rarely been examined. In a laboratory experiment, we incubated two typical cropland soils (an Entisol and a Mollisol) of China for 360 days under submerged and non-submerged conditions, and we evaluated the concentration and chemical structure of soil DOC, soil microbial metabolic potential and community composition by using total C/N analysis, solution-state H-1 NMR, Biolog EcoPlates, and 16S rRNA amplicon sequencing, respectively. The results showed that submergence significantly increased DOC concentration (P< 0.01) and microbial activity (P < 0.001) and changed DOC chemical structure in the Entisol (P < 0.01). In the Mollisol, it significantly increased the rate (P<0.01) and cumulative extent (P< 0.001) of SOC mineralization and DOC concentration (P< 0.01) as well as altering the composition of the microbial community (P< 0.001). Moreover, the SOC mineralization rate was better explained by microbial community composition (Entisol: SPC = -0.71, P < 0.001; Mollisol: SPC = 0.92, P < 0.001) than by DOC concentration (Entisol: SPC = 0.21, P> 0.05; Mollisol: SPC = 0.30, P< 0.05) or DOC chemical structure (Entisol: SPC = 0.12, P> 0.05; Mollisol: SPC = -0.45, P <, 0.001). Our study revealed that the bacterial community composition had a close relationship to the rate of submergence-induced SOC mineralization in both soils, but only DOC concentration and chemical structure were effective predictors of mineralization rate in the low-pH Mollisol. (C) 2019 Elsevier B.V. All rights reserved.

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