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Sustainable Water Resources Management
Erschienen in: Sustainable Water Resources Management 4/2019

26.10.2017 | Original Article

Geosciences in the assessment of thermal and mineral groundwater systems in N-Portugal: a review

verfasst von: J. M. Marques, P. M. Carreira

Erschienen in: Sustainable Water Resources Management | Ausgabe 4/2019

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Abstract

In the North of Portugal, thermal and mineral groundwater resources (e.g., Chaves CO2-rich thermal—76 °C—waters) are being used in the local Spas, and are considered one of the main sources of local/regional development/income. A multidisciplinary approach, including geological, tectonic, geochemical and isotopic (2H, 18O, 13C, 87Sr, 3H, 14C and 3He/4He) methodologies, was used to assess local/regional conceptual circulation models. In the case of the Chaves CO2-rich thermal waters, this approach provided important data to answer the most commonly asked questions so as to enable the elaboration of a robust hydrogeological conceptual model, namely (1) Chaves thermal waters belong to the HCO3/Na/CO2-rich type (with pH ≈7), in that the result of meteoric waters–granitic rocks–gas (CO2) interaction; (2) Padrela Mountain (NE-Chaves), ascribed to high-fractured rocks, is the main recharge area; the stable isotopic composition of the groundwater samples indicate a mean recharge altitude higher than 1150 m a.s.l.; (3) the mean Sr isotopic ratio of the thermomineral waters (87Sr/86Srmean = 0.722419) is similar to that of the Sr isotopic ratios of the plagioclases of the granitic rocks (e.g. 87Sr/86Sr = 0.72087; 87Sr/86Sr = 0.71261), indicating that hydrolysis of plagioclase is the main water–rock interaction process, favoured by the presence of deep-seated (mantle-derived) CO2 (δ13C values in the range of −6 to −1‰ vs. PDB, and the CO2/3He values from 5.1 × 108 to 7.5 × 109, are typical of MORB fluids); (4) the income of carbon-14 free to Chaves CO2-rich thermal waters system does not permit reliable 14C groundwater dating; (5) the geothermometric results (e.g. K2/Mg and silica geothermometers) indicate equilibrium temperatures around 120 °C, and a maximum depth of about 3.5 km reached by the Chaves CO2-rich thermal waters system was estimated. The discharge zones are mainly related to the intersection of the main local/regional fault lineaments (and conjugate structures), responsible for promoting the mineral and thermal groundwater ascent.
Vorheriger Artikel Occurrence, management and protection of mineral and thermal waters in some volcanic areas of Italy: current knowledge and future directions
Nächster Artikel Isotopes and geochemistry to assess shallow/thermal groundwater interaction in a karst/fissured-porous environment (Portugal): a review and reinterpretation

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Metadaten
Titel
Geosciences in the assessment of thermal and mineral groundwater systems in N-Portugal: a review
verfasst von
J. M. Marques
P. M. Carreira
Publikationsdatum
26.10.2017
Verlag
Springer International Publishing
Erschienen in
Sustainable Water Resources Management / Ausgabe 4/2019
Print ISSN: 2363-5037
Elektronische ISSN: 2363-5045
DOI
https://doi.org/10.1007/s40899-017-0190-8

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