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Medical Hydrology and Balneology: Environmental Aspects

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Mineral waters in Azores isl<strong>and</strong>s: hydrogeo<br />

logical approach <strong>and</strong> therapeutical applications<br />

Carreiro-Nunes JC (1-2) , Carvalho JM (2) , Oliveira LC (2) , Carvalho MR (3)<br />

(1) INOVA Institute. Ponta Delgada, Azores, Portugal<br />

(2) Geosciences Department, Azores University, Portugal<br />

(3) Lisbon University, Sciences Faculty, Geology Department, Lisbon, Portugal<br />

jcnunes@uac.pt<br />

Introduction <strong>and</strong> Objectives<br />

In Azores Isl<strong>and</strong>s, located 1,815 km W of Portugal Mainl<strong>and</strong>, in the North Atlantic<br />

Ocean <strong>and</strong> at the Azores triple tectonic junction, occur several mineral <strong>and</strong><br />

thermal waters related to volcanism <strong>and</strong> circulation in volcanic formations (e.g.,<br />

Carvalho et al., 2005; Carvalho et al., 2006; Cruz, 2004; Cruz & França, 2006;<br />

Cabeças et al., 2010). Some of them are or were classified as natural mineral water<br />

(Nunes et al., 2007) as, i) the Lombadas <strong>and</strong> Serra do Trigo CO2-rich waters, <strong>and</strong> ii)<br />

waters used for balneotherapy <strong>and</strong> balneology as Furnas, Ferraria <strong>and</strong> Caldeiras da<br />

Ribeira Gr<strong>and</strong>e (São Miguel Isl<strong>and</strong>), Varadouro ( Faial Isl<strong>and</strong>) <strong>and</strong> Carapacho<br />

(Graciosa Isl<strong>and</strong>). In the commercial market it is also present the spring water<br />

Gloria Patri (low mineralization) at São Miguel Isl<strong>and</strong>.<br />

Materials <strong>and</strong> Methods<br />

Typology of chemical composition is quite broad, resulting hydrogeological<br />

conceptual models of several nature (Cruz, 2007), namely (Figure 1): (i) NaCl<br />

thermal springs from the basal aquifer; (ii) thermal springs, boiling pools, fumaroles<br />

<strong>and</strong> cold CO2-rich springs associated to hydrothermal systems. To those types must<br />

be associated other springs resulting from suspended aquifers, spurring from paleosoils,<br />

dykes, lithological contacts or other structures.<br />

Current development projects (Nunes et al., 2007) are being carried out mainly<br />

over thermal springs at sea level (e.g. Varadouro, Carapacho, <strong>and</strong> Ferraria) associated<br />

with the basal aquifer <strong>and</strong> sea water heating.<br />

At those sites several studied <strong>and</strong> works are in due course <strong>and</strong> include hydrogeological<br />

surveys, isotopic <strong>and</strong> classical geochemistry, geophysical surveys <strong>and</strong><br />

evaluation <strong>and</strong> production drilled wells. The scope is to get resources able to be<br />

recognized as natural mineral natural according to European <strong>and</strong> national law <strong>and</strong><br />

with the modern hygienical <strong>and</strong> sanitary st<strong>and</strong>ards.<br />

Results<br />

Those mineral waters have electrical conductivities from 6 to 47 mS/cm <strong>and</strong><br />

temperatures from 35ºC (Varadouro old spring), to 41ºC (Carapacho) <strong>and</strong> 62ºC<br />

Balnea<br />

2012, núm. 6, 231-232<br />

231<br />

ISBN: 978-84-669-1887-0<br />

978-84-669-3482-4

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