Contribution of Particulate and Mineral-Associated Organic Matter to Potential Denitrification of Agricultural Soils

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dc.identifier.uri http://dx.doi.org/10.15488/14604
dc.identifier.uri https://www.repo.uni-hannover.de/handle/123456789/14722
dc.contributor.author Surey, Ronny
dc.contributor.author Kaiser, Klaus
dc.contributor.author Schimpf, Corinna M.
dc.contributor.author Mueller, Carsten W.
dc.contributor.author Böttcher, Jürgen
dc.contributor.author Mikutta, Robert
dc.date.accessioned 2023-09-01T04:26:53Z
dc.date.available 2023-09-01T04:26:53Z
dc.date.issued 2021
dc.identifier.citation Surey, R.; Kaiser, K.; Schimpf, C.M.; Mueller, C.W.; Böttcher, J. et al.: Contribution of Particulate and Mineral-Associated Organic Matter to Potential Denitrification of Agricultural Soils. In: Frontiers in Environmental Science 9 (2021), 640534. DOI: https://doi.org/10.3389/fenvs.2021.640534
dc.description.abstract Water-extractable organic carbon (WEOC) is considered as the most important carbon (C) source for denitrifying organisms, but the contribution of individual organic matter (OM) fractions (i.e., particulate (POM) and mineral-associated (MOM)) to its release and, thus, to denitrification remains unresolved. Here we tested short-time effects of POM and MOM on potential denitrification and estimated the contribution of POM- and MOM-derived WEOC to denitrification and CO2 production of three agricultural topsoils. Suspensions of bulk soils with and without addition of soil-derived POM or MOM were incubated for 24 h under anoxic conditions. Acetylene inhibition was used to determine the potential denitrification and respective product ratio at constant nitrate supply. Normalized to added OC, effects of POM on CO2 production, total denitrification, and its product ratios were much stronger than those of MOM. While the addition of OM generally increased the (N2O + N2)-N/CO2-C ratio, the N2O/(N2O + N2) ratio changed differently depending on the soil. Gas emissions and the respective shares of initial WEOC were then used to estimate the contribution of POM and MOM-derived WEOC to total CO2, N2O, and N2O + N2 production. Water-extractable OC derived from POM accounted for 53–85% of total denitrification and WEOC released from MOM accounted for 15–47%. Total gas emissions from bulk soils were partly over- or underestimated, mainly due to nonproportional responses of denitrification to the addition of individual OM fractions. Our findings show that MOM plays a role in providing organic substrates during denitrification but is generally less dominant than POM. We conclude that the denitrification potential of soils is not predictable based on the C distribution over POM and MOM alone. Instead, the source strength of POM and MOM for WEOC plus the WEOC’s quality turned out as the most decisive determinants of potential denitrification. eng
dc.language.iso eng
dc.publisher Lausanne : Frontiers Media
dc.relation.ispartofseries Frontiers in Environmental Science 9 (2021)
dc.rights CC BY 4.0 Unported
dc.rights.uri https://creativecommons.org/licenses/by/4.0
dc.subject agricultural soils eng
dc.subject carbon dioxide eng
dc.subject denitrification potential eng
dc.subject mineral-associated OM eng
dc.subject nitrous oxide eng
dc.subject organic matter fractions eng
dc.subject particulate OM eng
dc.subject water-extractable OM eng
dc.subject.ddc 333,7 | Natürliche Ressourcen, Energie und Umwelt
dc.title Contribution of Particulate and Mineral-Associated Organic Matter to Potential Denitrification of Agricultural Soils eng
dc.type Article
dc.type Text
dc.relation.essn 2296-665X
dc.relation.doi https://doi.org/10.3389/fenvs.2021.640534
dc.bibliographicCitation.volume 9
dc.bibliographicCitation.firstPage 640534
dc.description.version publishedVersion
tib.accessRights frei zug�nglich


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