Effects of soil water content at freezing, thaw temperature, and snowmelt infiltration on N2O emissions and the abundance and gene expression of denitrifier communities during a single freeze-thaw event

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creativework.keywords - en
water
pore space
soil microcosms
nitrous oxide
denitrifier abundance
denitrifier
transcription, genetic
temperature
creativework.keywords - fr
dénitrificateur
abondance des dénitrifiants
oxyde de diazote
éspace interstitiel
microcosmes du sol
température
transcription génétique
eau
dc.contributor.author
Sennett, Louise B.
Brin, Lyndsay D.
Goyer, Claudia
Zebarth, Bernie J.
Burton, David L.
dc.date.accepted
2024-03-19
dc.date.accessioned
2024-05-09T19:05:48Z
dc.date.available
2024-05-09T19:05:48Z
dc.date.issued
2024-04-11
dc.date.submitted
2023-09-06
dc.description.abstract - en
Climate change-related warming and increased precipitation may alter winter snow cover and thawing events, and therefore, may carry significant consequences for nitrous oxide (N2O) production pathways such as denitrification, and the abundance and expression of denitrifying microorganisms. We used a soil microcosm study to investigate the combined effect of soil thaw temperature, initial water filled pore space (WFPS) prior to soil freezing, and snowmelt infiltration simulated by the addition of water on N2O emission and denitrification rates, soil respiration rate, and the abundance and transcription of denitrifying (nirK, nirS, and nosZ) bacteria during a single freeze-thaw event. Soil respiration rate was primarily controlled by an increase in soil thaw temperature, whereas soil N2O emission and denitrification rates were generally greater in soils with a higher initial WFPS and soil thaw temperature. In contrast, snowmelt infiltration generally had a negligible effect on these rates, which may be related to pre-existing soil conditions that were already conducive to denitrification. Unexpectedly, the nosZ transcript/nosZ gene abundance ratio was lower in soils thawed at 8.0 °C compared to 1.5 °C; however, this may have resulted in a lower N2O reduction, thus explaining the greater levels of N2O emitted from soils thawed at 8.0 °C. Overall, this study demonstrated that increased N2O production during a single freeze-thaw event was primarily linked to antecedent conditions of high initial WFPS, soil thaw temperature, and a synergistic interplay between these two environmental parameters, and provides evidence that an increase in annual temperature and precipitation, along with the timing of precipitation, may further stimulate N2O production pathways.
dc.identifier.citation
Sennett, L. B., Brin, L. D., Goyer, C., Zebarth, B. J., & Burton, D. L. (2024). Effects of soil water content at freezing, thaw temperature, and snowmelt infiltration on N2O emissions and the abundance and gene expression of denitrifier communities during a single freeze-thaw event. Biology and Fertility of Soils, 60, 577-591. https://doi.org/10.1007/s00374-024-01817-w
dc.identifier.doi
https://doi.org/10.1007/s00374-024-01817-w
dc.identifier.issn
0178-2762
dc.identifier.uri
https://open-science.canada.ca/handle/123456789/2482
dc.language.iso
en
dc.publisher
Springer Nature
dc.rights - en
Creative Commons Attribution 4.0 International (CC BY 4.0)
dc.rights - fr
Creative Commons Attribution 4.0 International (CC BY 4.0)
dc.rights.openaccesslevel - en
Green
dc.rights.openaccesslevel - fr
Vert
dc.rights.uri - en
https://creativecommons.org/licenses/by/4.0/
dc.rights.uri - fr
https://creativecommons.org/licenses/by/4.0/deed.fr
dc.subject - en
Agriculture
dc.subject - fr
Agriculture
dc.subject.en - en
Agriculture
dc.subject.fr - fr
Agriculture
dc.title - en
Effects of soil water content at freezing, thaw temperature, and snowmelt infiltration on N2O emissions and the abundance and gene expression of denitrifier communities during a single freeze-thaw event
dc.type - en
Article
dc.type - fr
Article
local.article.journaltitle
Biology and Fertility of Soils
local.article.journalvolume
60
local.pagination
577-591
local.peerreview - en
Yes
local.peerreview - fr
Oui
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