Microbial carbon use efficiency of litter with distinct C/N ratios in soil at different temperatures, including microbial necromass as growth component

dc.date.accessioned2022-10-12T12:50:19Z
dc.date.available2022-10-12T12:50:19Z
dc.date.issued2022-08-10
dc.description.sponsorshipGefördert im Rahmen des Projekts DEALger
dc.identifierdoi:10.17170/kobra-202209226891
dc.identifier.urihttp://hdl.handle.net/123456789/14186
dc.language.isoengeng
dc.relation.doidoi:10.1007/s00374-022-01656-7
dc.rightsNamensnennung 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subjectmicrobial biomasseng
dc.subject¹⁵ N/¹⁴ N ratioeng
dc.subject¹³C/¹²C ratioeng
dc.subjectCO₂ mineralizationeng
dc.subjectparticulate organic mattereng
dc.subjectmicrobial necromasseng
dc.subject.ddc570
dc.subject.swdBiomasseger
dc.subject.swdBodenchemieger
dc.subject.swdKohlenstoffger
dc.subject.swdMineralisationger
dc.subject.swdPartikulärer organischer Stoffger
dc.subject.swdStreuger
dc.titleMicrobial carbon use efficiency of litter with distinct C/N ratios in soil at different temperatures, including microbial necromass as growth componenteng
dc.typeAufsatz
dc.type.versionpublishedVersion
dcterms.abstractAn incubation study was carried out to investigate the effects of litter quality, i.e. ¹⁵ N-labelled maize (C/N of 25.5) and Rhodes grass (C/N of 57.8) leaf litter on microbial carbon use efficiency (CUE) and priming effects in a moderate alkaline soil at two different temperatures (15 and 25 °C). CUE values were calculated from the isotopic composition of the particulate organic matter (POM) recovered as an index for the amount of non-decomposed litter. This approach allows the inclusion of microbial necromass growth components in the calculation of CUE values. Additionally, the soil was incubated for 10, 20, and 30 days to determine the optimum incubation period. Soil microbial CUE values of maize and Rhodes grass leaf litter, including microbial necromass C in the calculation of CUE, varied around 0.61, regardless of litter type, temperature, and incubation period. However, the optimum incubation time is between 20 and 30 days, depending on temperature. The strong priming effect on autochthonous soil organic carbon (SOC) mineralization was apparently not caused by N mining, as it was similar for both litter qualities. It most likely resulted from SOC being used by microbial co-metabolism. The litter-induced true priming effect was accompanied by a significant increase in autochthonous POM. The current approach, including microbial necromass as growth component, has been shown to be a strong tool for investigating CUE values and priming effects after application of litter and harvest residues to soil, probably under all environmental conditions.eng
dcterms.accessRightsopen access
dcterms.creatorBörger, Marie
dcterms.creatorBublitz, Tabata
dcterms.creatorDyckmans, Jens
dcterms.creatorWachendorf, Christine
dcterms.creatorJörgensen, Rainer Georg
dcterms.source.identifiereissn:1432-0789
dcterms.source.issueIssue 7
dcterms.source.journalBiology and Fertility of Soilseng
dcterms.source.pageinfo761-770
dcterms.source.volumeVolume 58
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