Deciphering groundwater flow-paths in fault-controlled semiarid mountain front zones (Central Chile)
Résumé
The Mountain-Block Recharge (MBR), also referred to as the hidden recharge, consists of groundwater inflows
from the mountain block into adjacent alluvial aquifers. This is a significant recharge process in arid environments,
but frequently discarded since it is imperceptible from the ground surface. In fault-controlled Mountain
Front Zones (MFZs), the hydrogeological limit between the mountain-block and adjacent alluvial basins is complex
and, consequently, the groundwater flow-paths reflect that setting. To cope with the typical low density of
boreholes in MFZs hindering a proper assessment of MBR, a combined geoelectrical-gravity approach was proposed
to decipher groundwater flow-paths in fault-controlled MFZs. The study took place in the semiarid
Western Andean Front separating the Central Depression from the Principal Cordillera at the Aconcagua Basin
(Central Chile). Our results, corroborated by field observations and comparedwithworldwide literature, indicate
that: (i) The limit between the two domains consists of N-S-oriented faults with clay-rich core (several tens of
meters width low electrical-resistivity subvertical bands) that impede the diffuse MBR. The “hidden recharge”
along theWestern Andean Front occurs through (ii) focused MBR processes by (ii.a) open and discrete basement
faults (mass defect and springs) oblique to the MFZ that cross-cut the N-S-oriented faults, and (ii.b) highhydraulic
transmissivity alluvial corridors in canyons. Alluvial corridors host narrow unconfined mountain aquifers,
which are recharged by indirect infiltration along ephemeral streams and focused inflows from oblique
basement faults. This study also revealed seepage from irrigation canals highlighting their key role in the recharge
of alluvial aquifers in the Central Depression. The proposed combined geophysical approach successfully incorporated (hydro)geological features and geophysical forward/inverse modelling into a robust
hydrogeological conceptualmodel to decipher groundwater flow-paths in fault-controlledMFZs, even in the absence
of direct observation points.