Dual carbon isotopes (δ

Dissolved inorganic carbon Dual carbon isotopes Input flux Karst reservoir Source tracing

Journal

Environmental research
ISSN: 1096-0953
Titre abrégé: Environ Res
Pays: Netherlands
ID NLM: 0147621

Informations de publication

Date de publication:
02 Sep 2024
Historique:
received: 11 06 2024
revised: 09 08 2024
accepted: 31 08 2024
medline: 5 9 2024
pubmed: 5 9 2024
entrez: 5 9 2024
Statut: aheadofprint

Résumé

In karst areas, the dissolved inorganic carbon (DIC) concentrations in aquatic systems are typically higher than that in non-karst areas due to intensive carbonate rock weathering. Understanding the sources and input fluxes of DIC in karst reservoirs is crucial for regional carbon cycle studies. This study utilized dual carbon isotopes (δ

Identifiants

DOI: 10.1016/j.envres.2024.119905 PMID: 39233028
pubmed: 39233028
pii: S0013-9351(24)01810-3
doi: 10.1016/j.envres.2024.119905
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

119905

Informations de copyright

Copyright © 2024. Published by Elsevier Inc.

Déclaration de conflit d'intérêts

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. ☐ The authors declare the following financial interests/personal relationships which may be considered as potential competing interests:

Auteurs

Zeqiong Qiu (Z)

College of Resources and Environmental Engineering, Guizhou Institute of Technology, Guian New District 550003, China; Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China.

Qinlin Wang (Q)

College of Resources and Environmental Engineering, Guizhou Institute of Technology, Guian New District 550003, China.

Hao Liu (H)

College of Resources and Environmental Engineering, Guizhou Institute of Technology, Guian New District 550003, China.

Xia Yu (X)

College of Resources and Environmental Engineering, Guizhou Institute of Technology, Guian New District 550003, China; Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China; State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi'an 710061, China; Shanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi'an 710061, China. Electronic address: yuxia@git.edu.cn.

Qixin Wu (Q)

Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China.

Yanling An (Y)

College of Resources and Environmental Engineering, Guizhou Institute of Technology, Guian New District 550003, China; Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China.

Peng Cheng (P)

State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi'an 710061, China; Shanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi'an 710061, China.

Jie Zeng (J)

Key Laboratory of Karst Georesources and Environment (Guizhou University), Ministry of Education, College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China.

Classifications MeSH