Temporal variability of secondary processes in alkaline geothermal waters associated to granitic rocks: the Caldes de Boí geothermal system (Spain)

Temporal variability of secondary processes in alkaline geothermal waters associated to granitic rocks: the Caldes de Boí geothermal system (Spain)

The Caldes de Boí geothermal waters show important differences in pH (6.5–9.6) and temperature (15.9ºC–52ºC) despite they have a common origin and a very simple circuit at depth (4km below the recharge area level). Thes differences are the result of secondary processes such as conductive cooling, m...

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Bibliographic Details
Main Authors: M.P. ASTA, M.J. GIMENO, L.F. AUQUÉ, J.P. GALVE, J. GÓMEZ, P. ACERO, P. LAPUENTE
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) 2017-06-01
Series:Geologica Acta
Subjects:
Geothermal system
Secondary processes
Mixing waters
Conductive cooling
CO2 input
Geochemical modelling techniques
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/16220

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