Intrusión de agua salada en Dinamarca
DOI:
https://doi.org/10.21701/bolgeomin/133.1/002Palabras clave:
Acuíferos costeros, Intrusión marina, Acuíferos fracturados, Lentes de agua dulce, Métodos electromagnéticos aéreosResumen
Se han revisado los estudios que han investigado la intrusión marina en Dinamarca para identificar las principales características que afectan a los acuíferos costeros en su interacción con el mar. Tradicionalmente, en regiones con clima húmedo, la intrusión marina no es considerada como un problema frecuente ya que se suele asociar con áreas afectadas por la escasez de agua. Sin embargo, se han identificado múltiples factores que pueden generar la salinización de acuíferos costeros en Dinamarca como la presencia de tierras bajas drenadas a lo largo de la costa con niveles freáticos por debajo del nivel del mar o el flujo preferente a través de morfologías kársticas o paleovalles en acuíferos carbonatados o detríticos respectivamente. Los cambios eustáticos han jugado también un papel importante en la salinización de acuíferos, en acuíferos profundos se pueden llegar a identificar aguas connatas antiguas y en islas de reducido tamaño, se establece un delicado equilibrio con lentes de agua dulce sobre aguas salinas. Debido a que este país depende casi exclusivamente de las aguas subterráneas para el abastecimiento de la población, la intrusión marina podría poner en riesgo los recursos subterráneos de agua dulce en las zonas costeras. La revisión de casos estudiados plantea una serie de cuestiones acerca de la magnitud de los problemas existentes y las perspectivas futuras considerando cambios climáticos. Con esta revisión se ha puesto en contexto el estado actual de conocimiento acerca de la intrusión marina en el país y se han identificado los desafíos que podría ser necesario acometer en el futuro.
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