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

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Cited articles

Ahmed, S. and Sreedevi, P. D.: Simulation of flow in weathered-fractured aquifer in a semi-arid and over-exploited region, in: Groundwater dynamics in hard rock aquifers: sustainable management and optimal monitoring network design, edited by: Ahmed, S., Jayakumar, R., and Salih, A., 219–233, Springer, Dordrecht, The Netherlands, 2008. 
Ala-aho, P., Soulsby, C., Wang, H., and Tetzlaff, D.: Integrated surface-subsurface model to investigate the role of groundwater in headwater catchment runoff generation: A minimalist approach to parameterisation, J. Hydrol., 547, 664–677, https://doi.org/10.1016/j.jhydrol.2017.02.023, 2017. 
Al-Khudhairy, D. H. A., Thompson, J. R., Gavin, H., and Hamm, N. A. S.: Hydrological modelling of a drained grazing marsh under agricultural land use and the simulation of restoration management scenarios, Hydrol. Sci. J., 44, 943–971, https://doi.org/10.1080/02626669909492291, 1999. 
Allen, R. G. and Pereira, L. S.: Estimating crop coefficients from fraction of ground cover and height, Irrig. Sci., 28, 17–34, https://doi.org/10.1007/s00271-009-0182-z, 2009. 
Allen, R. G., Pereira, L. S., Raes, D., and Smith, M.: Crop evapotranspiration – Guidelines for computing crop water requirements, FAO irrigation and drainage paper, Food and Agriculture Organization, Rome, Italy, 300 pp., 1998. 
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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.