Groundwater recharge is difficult to estimate, especially in fractured aquifers, because of the spatial variability of the soil properties and because of the lack of data at basin scale. A …
MSM Oliveira, MA Neves, FA Caxito… - Journal of South American …, 2022 - Elsevier
Abstract The 18 O, 2 H and ³H isotopes have been used to identify recharge and circulation patterns in aquifer systems by determining the relationships between isotopic signatures of …
Les réactions chimiques souterraines jouent un rôle crucial dans la dynamique de la zone critique. La cinétique des réactions chimique est généralement déterminée à partir …