Multidisciplinary study for the assessment of the geometry, boundaries and preferential recharge zones of an overexploited aquifer in the Atacama Desert (Pampa del Tamarugal, Northern Chile)
Résumé
Overexploited aquifers in drylands require a thorough assessment in order to get the best insight possible of their
hydrogeological behavior and groundwater resource. With this aim we develop an integrated methodology,
using the northern part of the Pampa del Tamarugal Aquifer (PTA), at the Atacama Desert, Northern Chile, as
testing site. This multidisciplinary assessment was completed including 34 direct piezometric measurements in
boreholes, 92 geophysical soundings (TDEM) and 9 stream gauging. Main results show strong correlation between
a well-defined contrast of resistivity and the water-table of the unconfined aquifer (dry unsaturated
zone≥100 Ω.m vs saline groundwater in the saturated zone≈10 Ω.m). TDEM results helped to map the piezometric
levels and reassess the limits of the PTA. The eastern limit of the aquifer, delimited up to now by the
basin floor, is repositioned from 10 to 50 km eastward in the Andean Piedmont, indicating larger groundwater
reserves than those described previously. A high-resistivity anomaly (∼200 Ω.m) in the apex of alluvial fans
reveals that frequent flood events cause rapid flows through the coarse permeable deposits leaching the vadose
zone and contributing to recharge the aquifer (temporary recharge process). However, the updated piezometric
map indicates the piedmont as the area where most of the aquifer recharge takes place. In the piedmont, at the
downstream of tectonic structures or substratum outcrops, stream discharge changes reveal perennial river losses
contributing to a located and permanent recharge of the PTA. This groundwater recharge process would be the
main contribution to the aquifer recharge. By taking into account the regional geology, the results are summarized
in a new conceptual model redefining the geometry, the spatial distribution of groundwater levels, the
boundary conditions and the complex recharge processes (different flow magnitudes) in the northern part of the
PTA. Finally, this study indicates an integrated and efficient methodology, providing original results that are
useful for the characterization of other aquifers located in arid piedmonts and hillslopes.