“…If the gas flux is high enough, the perched aquifer can become saturated in gases. Furthermore, dissolution of H 2 S produces sulfate water with low pH, which lowers the effective solubility of CO 2 and enhances CO 2 migration towards the surface (Bogie et al, 1987). At Los Azufres and Alcaparrosa, the presence of shallow water bodies is evidenced by the chemical and isotopic composition of springs revealing meteoric water recently infiltrated in the subsurface.…”