Soil thermal properties during freeze–thaw dynamics as function of variable organic carbon and grain...
Soil thermal properties during freeze–thaw dynamics as function of variable organic carbon and grain size distribution
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Madison: John Wiley & Sons, Inc
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English
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Madison: John Wiley & Sons, Inc
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Permafrost regions are experiencing increasing air temperatures, accelerating the thawing process, and thickening the active layer in summer. This can accelerate the release of greenhouse gasses into the atmosphere from the organic carbon stored in the permafrost. The long‐term thawing rates of permafrost below the active layer are governed by the...
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Soil thermal properties during freeze–thaw dynamics as function of variable organic carbon and grain size distribution
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TN_cdi_doaj_primary_oai_doaj_org_article_d9d99cd51c9b4ba79425527611be4b80
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_d9d99cd51c9b4ba79425527611be4b80
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ISSN
1539-1663
E-ISSN
1539-1663
DOI
10.1002/vzj2.20252