Álvaro M. Sáinz García, Jorge J. Molinero Huguet, Maarten W. Saaltink
Coastal karst features are supposed to be generated by the coupling between the infiltration of undersaturated rain water together with mixing from the fresh-saltwater interface. A coupled density-driven flow and reactive solute transport numerical model is presented which is able to duplicate conditions in such a morphogenetic conceptual model.
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