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Influences of forest cover on soil freeze-thaw dynamics and greenhouse gas emissions through the regulation of snow regimes: A comparison study of the farmland and forest plantation.

Identifieur interne : 000316 ( Main/Exploration ); précédent : 000315; suivant : 000317

Influences of forest cover on soil freeze-thaw dynamics and greenhouse gas emissions through the regulation of snow regimes: A comparison study of the farmland and forest plantation.

Auteurs : Lixin Chen [République populaire de Chine] ; Zuosinan Chen [République populaire de Chine] ; Guodong Jia [République populaire de Chine] ; Jie Zhou [République populaire de Chine] ; Jiachen Zhao [République populaire de Chine] ; Zhiqiang Zhang [République populaire de Chine]

Source :

RBID : pubmed:32320872

Descripteurs français

English descriptors

Abstract

Vegetation cover has implications for seasonally frozen soil dynamics and greenhouse gas emissions. We examined the frozen soil dynamics and N2O and CO2 efflux in a forest plantation (Populus ssp.) and farmland. The experiments were carried out at a forest reclamation site in Zhangbei county, Hebei province, China, from November 2017 to May 2018. Compared to the farmland, the forest plantation prolonged the retention of frozen soil because the shallower snow and the longer duration of snow cover in the forest contributed to a deeper frost depth and delayed soil thawing. The canopy also sheltered the frozen soil from the extreme fluctuations in freeze-thaw cycles (FTCs) during the snow-free period. Contrasting snow regimes and FTC dynamics contributed to variations in CO2 and N2O between the forest plantation and the farmland. Path analysis showed that the soil water content and soil temperature were the main regulators of N2O and CO2 emissions, respectively, in both land-use types. By contrast, soil substrate and microorganism biomass minimally influenced N2O and CO2 efflux. In conclusion, forest cover influences frozen soil dynamics and greenhouse gas emissions by buffering temperature fluctuations in both snow-covered and snow-free periods. This study further highlights the potential importance of anthropogenic land-use changes in influencing the cold season energy balance and gas efflux in future milder winter climates.

DOI: 10.1016/j.scitotenv.2020.138403
PubMed: 32320872


Affiliations:


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<term>Greenhouse Gases (MeSH)</term>
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<term>Dioxyde de carbone (analyse)</term>
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<term>Gaz à effet de serre (MeSH)</term>
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<div type="abstract" xml:lang="en">Vegetation cover has implications for seasonally frozen soil dynamics and greenhouse gas emissions. We examined the frozen soil dynamics and N
<sub>2</sub>
O and CO
<sub>2</sub>
efflux in a forest plantation (Populus ssp.) and farmland. The experiments were carried out at a forest reclamation site in Zhangbei county, Hebei province, China, from November 2017 to May 2018. Compared to the farmland, the forest plantation prolonged the retention of frozen soil because the shallower snow and the longer duration of snow cover in the forest contributed to a deeper frost depth and delayed soil thawing. The canopy also sheltered the frozen soil from the extreme fluctuations in freeze-thaw cycles (FTCs) during the snow-free period. Contrasting snow regimes and FTC dynamics contributed to variations in CO
<sub>2</sub>
and N
<sub>2</sub>
O between the forest plantation and the farmland. Path analysis showed that the soil water content and soil temperature were the main regulators of N
<sub>2</sub>
O and CO
<sub>2</sub>
emissions, respectively, in both land-use types. By contrast, soil substrate and microorganism biomass minimally influenced N
<sub>2</sub>
O and CO
<sub>2</sub>
efflux. In conclusion, forest cover influences frozen soil dynamics and greenhouse gas emissions by buffering temperature fluctuations in both snow-covered and snow-free periods. This study further highlights the potential importance of anthropogenic land-use changes in influencing the cold season energy balance and gas efflux in future milder winter climates.</div>
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<AbstractText>Vegetation cover has implications for seasonally frozen soil dynamics and greenhouse gas emissions. We examined the frozen soil dynamics and N
<sub>2</sub>
O and CO
<sub>2</sub>
efflux in a forest plantation (Populus ssp.) and farmland. The experiments were carried out at a forest reclamation site in Zhangbei county, Hebei province, China, from November 2017 to May 2018. Compared to the farmland, the forest plantation prolonged the retention of frozen soil because the shallower snow and the longer duration of snow cover in the forest contributed to a deeper frost depth and delayed soil thawing. The canopy also sheltered the frozen soil from the extreme fluctuations in freeze-thaw cycles (FTCs) during the snow-free period. Contrasting snow regimes and FTC dynamics contributed to variations in CO
<sub>2</sub>
and N
<sub>2</sub>
O between the forest plantation and the farmland. Path analysis showed that the soil water content and soil temperature were the main regulators of N
<sub>2</sub>
O and CO
<sub>2</sub>
emissions, respectively, in both land-use types. By contrast, soil substrate and microorganism biomass minimally influenced N
<sub>2</sub>
O and CO
<sub>2</sub>
efflux. In conclusion, forest cover influences frozen soil dynamics and greenhouse gas emissions by buffering temperature fluctuations in both snow-covered and snow-free periods. This study further highlights the potential importance of anthropogenic land-use changes in influencing the cold season energy balance and gas efflux in future milder winter climates.</AbstractText>
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<Keyword MajorTopicYN="N">Farmland</Keyword>
<Keyword MajorTopicYN="N">Forest plantation</Keyword>
<Keyword MajorTopicYN="N">Frozen soil</Keyword>
<Keyword MajorTopicYN="N">Greenhouse gas emission</Keyword>
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<CoiStatement>Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.</CoiStatement>
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<name sortKey="Chen, Lixin" sort="Chen, Lixin" uniqKey="Chen L" first="Lixin" last="Chen">Lixin Chen</name>
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<name sortKey="Chen, Zuosinan" sort="Chen, Zuosinan" uniqKey="Chen Z" first="Zuosinan" last="Chen">Zuosinan Chen</name>
<name sortKey="Jia, Guodong" sort="Jia, Guodong" uniqKey="Jia G" first="Guodong" last="Jia">Guodong Jia</name>
<name sortKey="Zhang, Zhiqiang" sort="Zhang, Zhiqiang" uniqKey="Zhang Z" first="Zhiqiang" last="Zhang">Zhiqiang Zhang</name>
<name sortKey="Zhao, Jiachen" sort="Zhao, Jiachen" uniqKey="Zhao J" first="Jiachen" last="Zhao">Jiachen Zhao</name>
<name sortKey="Zhou, Jie" sort="Zhou, Jie" uniqKey="Zhou J" first="Jie" last="Zhou">Jie Zhou</name>
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