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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...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_d9d99cd51c9b4ba79425527611be4b80

Soil thermal properties during freeze–thaw dynamics as function of variable organic carbon and grain size distribution

About this item

Full title

Soil thermal properties during freeze–thaw dynamics as function of variable organic carbon and grain size distribution

Publisher

Madison: John Wiley & Sons, Inc

Journal title

Vadose zone journal, 2023-05, Vol.22 (3), p.n/a

Language

English

Formats

Publication information

Publisher

Madison: John Wiley & Sons, Inc

More information

Scope and Contents

Contents

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...

Alternative Titles

Full title

Soil thermal properties during freeze–thaw dynamics as function of variable organic carbon and grain size distribution

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_d9d99cd51c9b4ba79425527611be4b80

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_d9d99cd51c9b4ba79425527611be4b80

Other Identifiers

ISSN

1539-1663

E-ISSN

1539-1663

DOI

10.1002/vzj2.20252

How to access this item