Vis enkel innførsel

dc.contributor.authorInagaki, Thiago Massao
dc.contributor.authorPossinger, Angela R.
dc.contributor.authorSchweizer, Steffen A.
dc.contributor.authorMueller, Carsten W.
dc.contributor.authorHoeschen, Carmen
dc.contributor.authorZachman, Michael J.
dc.contributor.authorKourkoutis, Lena F.
dc.contributor.authorKögel-Knabner, Ingrid
dc.contributor.authorLehmann, Johannes
dc.date.accessioned2023-07-18T08:48:24Z
dc.date.available2023-07-18T08:48:24Z
dc.date.created2023-03-01T10:16:29Z
dc.date.issued2023-01-10
dc.identifier.issn0038-0717
dc.identifier.urihttps://hdl.handle.net/11250/3079681
dc.description.abstractThe spatial distribution of organic substrates and microscale soil heterogeneity significantly influence organic matter (OM) persistence as constraints on OM accessibility to microorganisms. However, it is unclear how changes in OM spatial heterogeneity driven by factors such as soil depth affect the relative importance of substrate spatial distribution on OM persistence. This work evaluated the decomposition and persistence of 13C and 15N labeled water-extractable OM inputs over 50 days as either hotspot (i.e., pelleted in 1 – 2 mm-size pieces) or distributed (i.e., added as OM < 0.07 µm suspended in water) forms in topsoil (0-0.2 m) and subsoil (0.8-0.9 m) samples of an Andisol. We observed greater persistence of added C in the subsoil with distributed OM inputs relative to hotspot OM, indicated by a 17% reduction in cumulative mineralization of the added C and a 10% higher conversion to mineral-associated OM. A lower substrate availability potentially reduced mineralization due to OM dispersion throughout the soil. NanoSIMS (nanoscale secondary ion mass spectrometry) analysis identified organo-mineral associations on cross-sectioned aggregate interiors in the subsoil. On the other hand, in the topsoil, we did not observe significant differences in the persistence of OM, suggesting that the large amounts of particulate OM already present in the soil outweighed the influence of added OM spatial distribution. Here, we demonstrated under laboratory conditions that the spatial distribution of fresh OM input alone significantly affected the decomposition and persistence of OM inputs in the subsoil. On the other hand, spatial distribution seems to play a lower role in topsoils rich in particulate OM. The divergence in the influence of OM spatial distribution between the top and subsoil is likely driven by differences in soil mineralogy and OM composition.en_US
dc.description.abstractMicroscale spatial distribution and soil organic matter persistence in top and subsoilen_US
dc.language.isoengen_US
dc.publisherElsevier Ltd.en_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.subjectJordkvaliteten_US
dc.subjectSoil qualityen_US
dc.titleMicroscale spatial distribution and soil organic matter persistence in top and subsoilen_US
dc.title.alternativeMicroscale spatial distribution and soil organic matter persistence in top and subsoilen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© 2022 The Authorsen_US
dc.subject.nsiVDP::Matematikk og naturvitenskap: 400en_US
dc.subject.nsiVDP::Mathematics and natural scienses: 400en_US
dc.subject.nsiVDP::Matematikk og naturvitenskap: 400en_US
dc.subject.nsiVDP::Mathematics and natural scienses: 400en_US
dc.source.volume178en_US
dc.source.journalSoil Biology and Biochemistryen_US
dc.identifier.doi10.1016/j.soilbio.2022.108921
dc.identifier.cristin2130377
dc.relation.projectKavli Foundation: DE-SC0001086en_US
dc.source.articlenumber108921en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


Tilhørende fil(er)

Thumbnail

Denne innførselen finnes i følgende samling(er)

Vis enkel innførsel

Navngivelse 4.0 Internasjonal
Med mindre annet er angitt, så er denne innførselen lisensiert som Navngivelse 4.0 Internasjonal