Low-temperature dielectric measurements of confined water in porous granites
Main Author: | |
---|---|
Publication Date: | 2014 |
Other Authors: | , , , , , , , , , |
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 |
id |
RCAP_746b2ecb0e5836f2865b8cedd8e8cfbc |
---|---|
oai_identifier_str |
oai:dspace.uevora.pt:10174/13624 |
network_acronym_str |
RCAP |
network_name_str |
Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) |
repository_id_str |
https://opendoar.ac.uk/repository/7160 |
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 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/conferenceObject |
format |
conferenceObject |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10174/13624 http://hdl.handle.net/10174/13624 |
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 nao nao sim nd nd nd nd nd nd pmoita@uevora.pt nd nd nd nd 250 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.source.none.fl_str_mv |
reponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologia instacron:RCAAP |
instname_str |
FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologia |
instacron_str |
RCAAP |
institution |
RCAAP |
reponame_str |
Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) |
collection |
Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) |
repository.name.fl_str_mv |
Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologia |
repository.mail.fl_str_mv |
info@rcaap.pt |
_version_ |
1833592497458118656 |