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). These differences are the result of secondary processes such as conductive cooling,...
Na minha lista:
| Publicado no: | Geologica Acta: an international earth science journal |
|---|---|
| Principais autores: | , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Universitat de Barcelona
2017
|
| Assuntos: | |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=50551303001 https://www.redalyc.org/journal/505/50551303001/ https://www.redalyc.org/journal/505/50551303001/html/ https://www.redalyc.org/journal/505/50551303001/50551303001.epub https://www.redalyc.org/journal/505/50551303001/movil |
| Tags: |
Sem tags, seja o primeiro a adicionar uma tag!
|