High-Resolution GPR Geophysical Imaging for Subsurface Dam Siting in an Ephemeral Stream within the Brazilian Semiarid Region
Underground dam; GPR; Brazilian semiarid
Ensuring water security in semi-arid regions depends on the development of social technologies tailored to the dynamics of ephemeral streams. This study evaluates the geological and physical-structural constraints for locating a subsurface dam within the bed of the Cabuji River, at the Santa Luzia Farm, in the municipality of Angicos, Rio Grande do Norte, Brazil. The study area is situated within the geotectonic context of the Borborema Province, overlying the crystalline basement of the Seridó Belt. Due to the predominance of fractured metamorphic rocks and shallow soils, the region constitutes a geologically unfavorable environment for conventional groundwater accumulation and storage in deep aquifers. Given this chronic hydrogeological limitation, developing alternative abstraction and retention technologies is essential to mitigate climate vulnerability and drive local socioeconomic development. The methodology integrated high-resolution Ground Penetrating Radar (GPR) imaging for the three-dimensional delineation of the alluvial sedimentary package thickness. Siting criteria were based on the thickness of the sedimentary package, the narrowing of the river channel, and the presence of lateral abutments for the structural anchoring of the crest/septon. The adopted geophysical model allowed the impermeable core to be positioned across the thinnest section of the alluvium, immediately downstream of a thick upstream sequence of accumulated sediments, thereby optimizing the consumption of waterproofing material and maximizing the volume of retained water. In conclusion, although the strong rheological structural control precludes a strictly orthogonal alignment of the core wall relative to the theoretical flow, the evaluated reach meets the technical requirements for implementing the Costa & Melo Model, consolidating GPR as an important tool for enabling shallow reservoirs in crystalline terrains.