The input signal to a carbonate aquifer highlights recharge processes and climate evolution under temperate Atlantic conditions-Reference-Cited by-同舟云学术

The input signal to a carbonate aquifer highlights recharge processes and climate evolution under temperate Atlantic conditions

Published:2022-06-06 Issue:8 Volume:67 Page:1238-1252
ISSN:0262-6667
Container-title:Hydrological Sciences Journal
language:en
Short-container-title:Hydrological Sciences Journal

Author:

Cao Feifei¹²^ORCID,Jaunat Jessy¹^ORCID,Huneau Frédéric³⁴^ORCID,Négrel Philippe⁵,Garel Emilie³⁴,Mattei Alexandra³⁴,Celle Hélène⁶,Ollivier Patrick⁵^ORCID

Affiliation:

1. Université de Reims Champagne-Ardenne, EA 3795 – GEGENAA, 2 esplanade Roland Garros, Reims, France

2. Department of Physical Geography, Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden

3. Université de Corse Pascal Paoli, Faculté des Sciences et Techniques, Laboratoire d’Hydrogéologie, Campus Grimaldi, Corte, France

4. CNRS, UMR 6134 SPE, BP 52, Corte, France

5. BRGM, 3 av. C. Guillemin, BP 36009, Orléans, France

6. Université de Bourgogne Franche-Comté, CNRS, UMR 6249 Chrono-Environnement, Besançon Cedex, France

Funder

Agence de l’Eau Seine-Normandie

Publisher

Informa UK Limited

Subject

Water Science and Technology

Link

https://www.tandfonline.com/doi/pdf/10.1080/02626667.2022.2072222

Reference109 articles.

1. Allen, D.J. et al. 1997. The physical properties of major aquifers in England and Wales. British Geological Survey, Technical Report No. WD/97/34, p. 312

2. Rapid karstic bypass flow in the unsaturated zone of the Yorkshire chalk aquifer and implications for contaminant transport

3. The application of environmental isotopes to conceptualize groundwater recharge in a coastal aquifer system: Case study of the West Coast Aquifer System, South Africa

4. Atmospheric factors controlling the stable isotopes (δ18O and δ2H) of the Indian summer monsoon precipitation in a drying region of Eastern India