Calcite dissolution by mixing waters: geochemical modeling and flow-through experiments

Calcite dissolution by mixing waters: geochemical modeling and flow-through experiments

Dissolution of carbonates has been commonly predicted by geochemical models to occur at the seawater-freshwater mixing zone of coastal aquifers along a geological time scale. However, field evidences are inconclusive: dissolution vs. lack of dissolution. In this study we investigate the process of c...

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Bibliographic Details
Main Authors: E. SANZ, C. AYORA, J. CARRERA
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2011-05-01
Series:Geologica Acta
Subjects:
Calcite dissolution
Mixing waters
Flow-through experiments
Seawater intrusion
Geochemical modeling
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/2101

Internet

https://revistes.ub.edu/index.php/GEOACTA/article/view/2101

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