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Fluxes of greenhouse gases from incubated soils using different lid-closure times

dc.contributor.authorDang, Duy (Minh)
dc.contributor.authorMacdonald, Ben
dc.contributor.authorWarneke, Sören
dc.contributor.authorWhite, Ian
dc.date.accessioned2022-12-07T23:02:41Z
dc.date.issued2018
dc.date.updated2021-11-28T07:32:32Z
dc.description.abstractLaboratory incubations and field measurements have provided valuable information on the production of green-house gases. However, information about the effects of pre-incubation and closure time on soil-induced gas emissions is currently limited. Our findings showed that different closure times and pre-incubation times altered gas emissions from incubated soils. A standardised procedure to investigate gas fluxes is needed for application to other studied soils.Different sampling times for greenhouse gas measurements have been proposed in many incubation studies. Little is known about effects of closure time on denitrification and nitrification rates from incubation experiments. The objectives of this study were to analyse greenhouse gas (carbon dioxide, methane and nitrous oxide) production from different soils with different times of lid closure and to assess effects of different activation times (defined as additional pre-incubation periods before incubation experiments) on gas emissions from soils. Forty grams of air-dried soil samples (depth 0–10 cm) were incubated in 125-mL jars at 258C with the addition of glucose and nitrate. The first experiment measured greenhouse gas fluxes at different lid-closure times (40, 80, 120 and 1440 min). The second experiment assessed the effects of different durations of soil activation (0.7, 1.3, 2 and 24 h) on gas emissions. Both were conducted with a completely randomised design, with three replicates per treatment. Our findings showed closure time <1 h or >2 h may cause an underestimate of greenhouse gas emissions. Lengthening activation times resulted in different emission rates consistent with soil characteristics. To measure gas fluxes based on linear regression would require four or five sampling points and sampling at a 20-min interval over a maximum period of 80 min for estimating gas fluxes from soil. Because pre-incubation time is critical and a driving factor in the measurement of soil-induced gas emissions, a standardised procedure to quantify gas fluxes is needed for application to other soils.en_AU
dc.format.mimetypeapplication/pdfen_AU
dc.identifier.issn1838-675Xen_AU
dc.identifier.urihttp://hdl.handle.net/1885/281631
dc.language.isoen_AUen_AU
dc.publisherCSIRO Publishingen_AU
dc.rightsJournal compilation © CSIRO 2018en_AU
dc.sourceSoil Researchen_AU
dc.subjectamendmenten_AU
dc.subjectgreenhouse gas emissionsen_AU
dc.subjectincubationen_AU
dc.subjectnitrogen cycleen_AU
dc.subjectsoil activationen_AU
dc.titleFluxes of greenhouse gases from incubated soils using different lid-closure timesen_AU
dc.typeJournal articleen_AU
local.bibliographicCitation.issue1en_AU
local.bibliographicCitation.lastpage48en_AU
local.bibliographicCitation.startpage39en_AU
local.contributor.affiliationDang, Duy (Minh), College of Science, ANUen_AU
local.contributor.affiliationMacdonald, Ben, CSIRO Agriculture Flagshipen_AU
local.contributor.affiliationWarneke, Sören, CSIROen_AU
local.contributor.affiliationWhite, Ian, College of Science, ANUen_AU
local.contributor.authoruidDang, Duy (Minh), u5225331en_AU
local.contributor.authoruidWhite, Ian, u9609393en_AU
local.description.embargo2099-12-31
local.description.notesImported from ARIESen_AU
local.identifier.absfor000000 - Internal ANU use onlyen_AU
local.identifier.ariespublicationu4485658xPUB2539en_AU
local.identifier.citationvolume56en_AU
local.identifier.doi10.1071/SR17050en_AU
local.identifier.scopusID2-s2.0-85040178608
local.identifier.thomsonID000419096100004
local.publisher.urlhttps://www.publish.csiro.au/en_AU
local.type.statusPublished Versionen_AU

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