New challenges in the study of coastal aquifers from numerical modeling. The case of the Motril-Salobreña aquifer
Metadatos
Mostrar el registro completo del ítemAutor
Calvache Quesada, María Luisa; Blanco Coronas, Ángela M.; López Chicano, Manuel; Sánchez Úbeda, Juan PedroEditorial
Instituto Geologico y Minero de España
Materia
Age transport modeling Coastal aquifer Global change Saltwater intrusion Acuífero costero Cambio Global Intrusión marina Modelos de transporte de calor Modelos de transporte de edad
Fecha
2022Referencia bibliográfica
Calvache, M. L., Blanco-Coronas, Á. M., Duque, C., López-Chicano, M., & Sánchez-Úbeda, J. P. (2022). New challenges in the study of coastal aquifers from numerical modeling. The case of the Motril-Salobreña aquifer. BOLETÍN GEOLÓGICO Y MINERO, 133(1), 211-225.[http://dx.doi.org/10.21701/bolgeomin/133.1/012]
Patrocinador
Proyecto CGL2016-77503-R financiado por el Ministerio de Ciencia e Innovación; Grupo de investigación de la Junta de Andalucía RNM-369Resumen
Coastal aquifers are frequently complex systems with highly heterogeneous geological charac teristics, specific flow patterns, presence of fluids with different densities, high risk of contamina tion both by salinization and by other pollutants, and highly modified by anthropic activity. Given
this situation, numerical modeling becomes the most appropriate tool to determine the potential
impact of global change on marine intrusion in this kind of aquifers. The mathematical models
traditionally used in coastal aquifers have been those of flow and mass transport with variable
density, which allow obtaining a distribution of salinities in the aquifer and reproducing the flow
pattern in the area of discharge to the sea. In addition to these models, another type of numerical
modeling can be applied that could also provide information on specific aspects of this type of
aquifers. The study of the Motril-Salobreña coastal aquifer shows, for example, how heat trans port models allow quantifying the recharge that occurs from rivers that frequently interact with
coastal aquifers; as well as the age transport models provide data on the preferential groundwa ter circulation paths and its residence time, very relevant information in these frequently hetero geneous and anisotropic aquifers. Future challenges are directed towards determining the ef fects of sea level rise on marine intrusion and establishing the degree of equilibrium of the
freshwater-saltwater contact with the current situation