4.7 Article

Sub-micron level investigation reveals the inaccessibility of stabilized carbon in soil microaggregates

Journal

SCIENTIFIC REPORTS
Volume 8, Issue -, Pages -

Publisher

NATURE RESEARCH
DOI: 10.1038/s41598-018-34981-9

Keywords

-

Funding

  1. National Science Foundation [NSF EPS 0903806, KCUR NSF73698]
  2. Department of Agronomy, Kansas State University
  3. Canada Foundation for Innovation
  4. Natural Sciences and Engineering Research Council of Canada
  5. University of Saskatchewan
  6. Government of Saskatchewan
  7. Western Economic Diversification Canada
  8. National Research Council Canada
  9. Canadian Institutes of Health Research
  10. DOE Office of Science User Facility [DE-AC02-05CH11231]
  11. Kansas State University

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Direct evidence-based approaches are vital to evaluating newly proposed theories on the persistence of soil organic carbon and establishing the contributions of abiotic and biotic controls. Our primary goal was to directly identify the mechanisms of organic carbon stabilization in native-state, free soil microaggregates without disrupting the aggregate microstructure using scanning transmission x-ray microscopy coupled with near edge x-ray absorption fine structure spectroscopy (STXM-NEXAFS). The influence of soil management practices on microaggregate associated-carbon was also assessed. Free, stable soil microaggregates were collected from a tropical agro-ecosystem in Cruz Alta, Brazil. The long-term experimental plots (>25 years) comparing two tillage systems: no-till and till with a complex crop rotation. Based on simultaneously collected multi-elemental associations and speciation, STXM-NEXAFS successfully provided submicron level information on organo-mineral associations. Simple organic carbon sources were found preserved within microaggregates; some still possessing original morphology, suggesting that their stabilization was not entirely governed by the substrate chemistry. Bulk analysis showed higher and younger organic carbon in microaggregates from no-till systems than tilled systems. These results provide direct submicron level evidence that the surrounding environment is involved in stabilizing organic carbon, thus favoring newly proposed concepts on the persistence of soil organic carbon.

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