Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/26100
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dc.contributor.authorSubke, Jens-Arneen_UK
dc.contributor.authorMoody, Catherine Sen_UK
dc.contributor.authorHill, Timothy Cen_UK
dc.contributor.authorVoke, Naomien_UK
dc.contributor.authorToet, Sylviaen_UK
dc.contributor.authorIneson, Philipen_UK
dc.contributor.authorTeh, Yit Arnen_UK
dc.date.accessioned2018-01-27T04:33:49Z-
dc.date.available2018-01-27T04:33:49Z-
dc.date.issued2018-01en_UK
dc.identifier.urihttp://hdl.handle.net/1893/26100-
dc.description.abstractAerated soils represent an important sink for atmospheric methane (CH4), due to the effect of methanotrophic bacteria, thus mitigating current atmospheric CH4increases. Whilst rates of CH4oxidation have been linked to types of vegetation cover, there has been no systematic investigation of the interaction between plants and soil in relation to the strength of the soil CH4sink. We used quasi-continuous automated chamber measurements of soil CH4and CO2flux from soil collar treatments that selectively include root and ectomycorrhizal (ECM) mycelium to investigate the role of rhizosphere activity as well as the effects of other environmental drivers on CH4uptake in a temperate coniferous forest soil. We also assessed the potential impact of measurement bias from sporadic chamber measurements in altering estimates of soil CO2efflux and CH4uptake. Results show a clear effect of the presence of live roots and ECM mycelium on soil CO2efflux and CH4uptake. The presence of ECM hyphae alone (without plant roots) showed intermediate fluxes of both CO2and CH4relative to soils that either contained roots and ECM mycelium, or soil lacking root- and ECM mycelium. Regression analysis confirmed a significant influence of soil moisture as well as temperature on flux dynamics of both CH4and CO2flux. We further found a surprising increase in soil CH4uptake during the night, and discuss diurnal fluctuations in atmospheric CH4(with higher concentrations during stable atmospheric conditions at night) as a potential driver of CH4oxidation rates. Using the high temporal resolution of our data set, we show that low-frequency sampling results in systematic bias of up-scaled flux estimates, resulting in under-estimates of up to 20% at our study site, due to fluctuations in flux dynamics on diurnal as well as longer time scales.en_UK
dc.language.isoenen_UK
dc.publisherElsevieren_UK
dc.relationSubke J, Moody CS, Hill TC, Voke N, Toet S, Ineson P & Teh YA (2018) Rhizosphere activity and atmospheric methane concentrations drive variations of methane fluxes in a temperate forest soil. Soil Biology and Biochemistry, 116, pp. 323-332. https://doi.org/10.1016/j.soilbio.2017.10.037en_UK
dc.rightsThis article is available under the terms of the Creative Commons Attribution License (CC BY). You may copy and distribute the article, create extracts, abstracts and new works from the article, alter and revise the article, text or data mine the article and otherwise reuse the article commercially (including reuse and/or resale of the article) without permission from Elsevier. You must give appropriate credit to the original work, together with a link to the formal publication through the relevant DOI and a link to the Creative Commons user license above. You must indicate if any changes are made but not in any way that suggests the licensor endorses you or your use of the work.en_UK
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/en_UK
dc.titleRhizosphere activity and atmospheric methane concentrations drive variations of methane fluxes in a temperate forest soilen_UK
dc.typeJournal Articleen_UK
dc.identifier.doi10.1016/j.soilbio.2017.10.037en_UK
dc.citation.jtitleSoil Biology and Biochemistryen_UK
dc.citation.issn0038-0717en_UK
dc.citation.volume116en_UK
dc.citation.spage323en_UK
dc.citation.epage332en_UK
dc.citation.publicationstatusPublisheden_UK
dc.citation.peerreviewedRefereeden_UK
dc.type.statusAM - Accepted Manuscripten_UK
dc.contributor.funderNatural Environment Research Councilen_UK
dc.citation.date06/11/2017en_UK
dc.contributor.affiliationBiological and Environmental Sciencesen_UK
dc.contributor.affiliationUniversity of Leedsen_UK
dc.contributor.affiliationUniversity of Exeteren_UK
dc.contributor.affiliationUniversity of Yorken_UK
dc.contributor.affiliationUniversity of Yorken_UK
dc.contributor.affiliationUniversity of Yorken_UK
dc.contributor.affiliationUniversity of Aberdeenen_UK
dc.identifier.isiWOS:000419417900035en_UK
dc.identifier.scopusid2-s2.0-85032909147en_UK
dc.identifier.wtid512892en_UK
dc.contributor.orcid0000-0001-9244-639Xen_UK
dc.date.accepted2017-10-30en_UK
dcterms.dateAccepted2017-10-30en_UK
dc.date.filedepositdate2017-11-06en_UK
rioxxterms.apcnot requireden_UK
rioxxterms.typeJournal Article/Reviewen_UK
rioxxterms.versionAMen_UK
local.rioxx.authorSubke, Jens-Arne|0000-0001-9244-639Xen_UK
local.rioxx.authorMoody, Catherine S|en_UK
local.rioxx.authorHill, Timothy C|en_UK
local.rioxx.authorVoke, Naomi|en_UK
local.rioxx.authorToet, Sylvia|en_UK
local.rioxx.authorIneson, Philip|en_UK
local.rioxx.authorTeh, Yit Arn|en_UK
local.rioxx.projectInternal Project|University of Stirling|https://isni.org/isni/0000000122484331en_UK
local.rioxx.freetoreaddate2017-11-08en_UK
local.rioxx.licencehttp://www.rioxx.net/licenses/under-embargo-all-rights-reserved||2017-11-06en_UK
local.rioxx.licencehttp://creativecommons.org/licenses/by-nc-nd/4.0/|2017-11-08|en_UK
local.rioxx.filenameSubke et al Manuscript_2nd_revision_.pdfen_UK
local.rioxx.filecount1en_UK
local.rioxx.source0038-0717en_UK
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