The effect of climatic and edaphic factors on soil organic carbon turnover in hummocks based on δ

Carbon isotope Climate change Hummock Soil organic carbon turnover

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
01 Nov 2020
Historique:
received: 08 03 2020
revised: 25 05 2020
accepted: 10 06 2020
pubmed: 3 7 2020
medline: 3 7 2020
entrez: 3 7 2020
Statut: ppublish

Résumé

Hummocks (thúfur, pounus) are peculiar landforms usually formed by repeated freeze-thaw processes and differential frost heave, and are common in frost soil regions, especially in the Qinghai-Tibet Plateau. However, little is known about the response of δ

Identifiants

pubmed: 32615420
pii: S0048-9697(20)33662-7
doi: 10.1016/j.scitotenv.2020.140141
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

140141

Informations de copyright

Copyright © 2020 Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of competing interest We declare that we have no financial and personal relationships with other people or organizations that can inappropriately influence our work. There is no professional or other personal interest of any nature or kind in any product, service and/or company that could be construed as influencing the position presented in, or the review of, the manuscript entitled.

Auteurs

Hanzhi Li (H)

Institute of Desertification Studies, Chinese Academy of Forestry, 100091 Beijing, China.

Feng Yan (F)

Institute of Desertification Studies, Chinese Academy of Forestry, 100091 Beijing, China. Electronic address: fyan@caf.ac.cn.

Dengfeng Tuo (D)

Institute of Desertification Studies, Chinese Academy of Forestry, 100091 Beijing, China.

Bin Yao (B)

Institute of Desertification Studies, Chinese Academy of Forestry, 100091 Beijing, China.

Junhan Chen (J)

Institute of Desertification Studies, Chinese Academy of Forestry, 100091 Beijing, China.

Classifications MeSH