Articles | Volume 25, issue 1
https://doi.org/10.5194/hess-25-291-2021
https://doi.org/10.5194/hess-25-291-2021
Research article
 | 
19 Jan 2021
Research article |  | 19 Jan 2021

Modelling the hydrological interactions between a fissured granite aquifer and a valley mire in the Massif Central, France

Arnaud Duranel, Julian R. Thompson, Helene Burningham, Philippe Durepaire, Stéphane Garambois, Robert Wyns, and Hervé Cubizolle

Viewed

Total article views: 4,130 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,690 1,339 101 4,130 385 121 137
  • HTML: 2,690
  • PDF: 1,339
  • XML: 101
  • Total: 4,130
  • Supplement: 385
  • BibTeX: 121
  • EndNote: 137
Views and downloads (calculated since 14 May 2020)
Cumulative views and downloads (calculated since 14 May 2020)

Viewed (geographical distribution)

Total article views: 4,130 (including HTML, PDF, and XML) Thereof 3,885 with geography defined and 245 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 11 May 2026
Download
Short summary
Peat-forming wetlands (mires) provide multiple ecosystem services, which depend on peat remaining waterlogged. Using hydrological modelling, we show that, contrary to a common assumption, groundwater inflow can be a quantitatively important and functionally critical element of the water balance of mires in hard-rock upland and mountain areas. This influence is such that patterns of groundwater upwelling and seepage explain the spatial distribution of mires in the landscape.
Share