Low-temperature dielectric measurements of confined water in porous granites

Bibliographic Details
Main Author: Silva, Hugo
Publication Date: 2014
Other Authors: Prezas, Pedro, Vinagre, Ana, Graça, Manuel F., Monteiro, Jorge H., Tlemçami, Mouhadyne, Moita, Patrícia, Pinho, António, Bezzeghoud, Mourad, Sushil, Mendiratta, Rosa, Rui
Format: Conference object
Language: por
Source: Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
Download full: http://hdl.handle.net/10174/13624
Summary: Three different granitic rocks extracted from Évora (in the south of Portugal) where used to perform dielectric measurements in the frequency range from 100 Hz to 1 MHz and temperatures 100 − 350 K. Thin cylindrical samples were prepared and circular electrodes were established using silver conductive paint. A clear anomaly appears, for T ⇠ 200 − 220 K, in the dielectric measurements of the samples studied. This anomaly occurs in different materials and coincides with a phase transition of supercooled water. Tightly bounded water confined in the pores of the rock do not crystallize at 273 K, but form a metastable liquid down to 200−220 K increasing water polarization. Below this temperature water molecules solidify and polarizability decreases. The rock presenting the most sizeable anomaly has a very low specific surface area, ⇠ 0.09 m2g
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spelling Low-temperature dielectric measurements of confined water in porous granitesdielectric measurementsgranitesThree different granitic rocks extracted from Évora (in the south of Portugal) where used to perform dielectric measurements in the frequency range from 100 Hz to 1 MHz and temperatures 100 − 350 K. Thin cylindrical samples were prepared and circular electrodes were established using silver conductive paint. A clear anomaly appears, for T ⇠ 200 − 220 K, in the dielectric measurements of the samples studied. This anomaly occurs in different materials and coincides with a phase transition of supercooled water. Tightly bounded water confined in the pores of the rock do not crystallize at 273 K, but form a metastable liquid down to 200−220 K increasing water polarization. Below this temperature water molecules solidify and polarizability decreases. The rock presenting the most sizeable anomaly has a very low specific surface area, ⇠ 0.09 m2g2015-03-26T12:25:37Z2015-03-262014-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjecthttp://hdl.handle.net/10174/13624http://hdl.handle.net/10174/13624porSilva et al (2014)Low-temperature dielectric measurements of confined water in porous granites, Geophysical Research Abstracts, vol, 16, EGU2014-12625. EGU General Assemblynaonaosimndndndndndndpmoita@uevora.ptndndndnd250Silva, HugoPrezas, PedroVinagre, AnaGraça, Manuel F.Monteiro, Jorge H.Tlemçami, MouhadyneMoita, PatríciaPinho, AntónioBezzeghoud, MouradSushil, MendirattaRosa, Ruiinfo:eu-repo/semantics/openAccessreponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiainstacron:RCAAP2024-01-03T18:58:35Zoai:dspace.uevora.pt:10174/13624Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireinfo@rcaap.ptopendoar:https://opendoar.ac.uk/repository/71602025-05-28T12:04:47.179967Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiafalse
dc.title.none.fl_str_mv Low-temperature dielectric measurements of confined water in porous granites
title Low-temperature dielectric measurements of confined water in porous granites
spellingShingle Low-temperature dielectric measurements of confined water in porous granites
Silva, Hugo
dielectric measurements
granites
title_short Low-temperature dielectric measurements of confined water in porous granites
title_full Low-temperature dielectric measurements of confined water in porous granites
title_fullStr Low-temperature dielectric measurements of confined water in porous granites
title_full_unstemmed Low-temperature dielectric measurements of confined water in porous granites
title_sort Low-temperature dielectric measurements of confined water in porous granites
author Silva, Hugo
author_facet Silva, Hugo
Prezas, Pedro
Vinagre, Ana
Graça, Manuel F.
Monteiro, Jorge H.
Tlemçami, Mouhadyne
Moita, Patrícia
Pinho, António
Bezzeghoud, Mourad
Sushil, Mendiratta
Rosa, Rui
author_role author
author2 Prezas, Pedro
Vinagre, Ana
Graça, Manuel F.
Monteiro, Jorge H.
Tlemçami, Mouhadyne
Moita, Patrícia
Pinho, António
Bezzeghoud, Mourad
Sushil, Mendiratta
Rosa, Rui
author2_role author
author
author
author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Silva, Hugo
Prezas, Pedro
Vinagre, Ana
Graça, Manuel F.
Monteiro, Jorge H.
Tlemçami, Mouhadyne
Moita, Patrícia
Pinho, António
Bezzeghoud, Mourad
Sushil, Mendiratta
Rosa, Rui
dc.subject.por.fl_str_mv dielectric measurements
granites
topic dielectric measurements
granites
description Three different granitic rocks extracted from Évora (in the south of Portugal) where used to perform dielectric measurements in the frequency range from 100 Hz to 1 MHz and temperatures 100 − 350 K. Thin cylindrical samples were prepared and circular electrodes were established using silver conductive paint. A clear anomaly appears, for T ⇠ 200 − 220 K, in the dielectric measurements of the samples studied. This anomaly occurs in different materials and coincides with a phase transition of supercooled water. Tightly bounded water confined in the pores of the rock do not crystallize at 273 K, but form a metastable liquid down to 200−220 K increasing water polarization. Below this temperature water molecules solidify and polarizability decreases. The rock presenting the most sizeable anomaly has a very low specific surface area, ⇠ 0.09 m2g
publishDate 2014
dc.date.none.fl_str_mv 2014-01-01T00:00:00Z
2015-03-26T12:25:37Z
2015-03-26
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
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url http://hdl.handle.net/10174/13624
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv Silva et al (2014)Low-temperature dielectric measurements of confined water in porous granites, Geophysical Research Abstracts, vol, 16, EGU2014-12625. EGU General Assembly
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nao
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pmoita@uevora.pt
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250
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