Heating pulse tests under constant volumen on natural Boom clay.

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dc.contributor	Universitat Politècnica de Catalunya. Departament d'Enginyeria del Terreny, Cartogràfica i Geofísica
dc.contributor	Universitat Politècnica de Catalunya. MSR - Mecànica del Sòls i de les Roques
dc.contributor.author	Lima, Analice
dc.contributor.author	Romero Morales, Enrique Edgar
dc.contributor.author	Gens Solé, Antonio
dc.contributor.author	Muñoz, Juan Jorge
dc.contributor.author	Li, Xiangling
dc.date	2010-08-20
dc.identifier.citation	Lima, A. [et al.]. Heating pulse tests under constant volumen on natural Boom clay.. "Journal of rock mechanics and geotechnical engineering", 20 Agost 2010, vol. 2, núm. 2, p. 124-128.
dc.identifier.citation	1674-7755
dc.identifier.citation	10.3724/SP.J.1235.2010.00124
dc.identifier.uri	http://hdl.handle.net/2117/15163
dc.language.iso	eng
dc.publisher	Science Press
dc.relation	http://pub.chinasciencejournal.com/article/getArticle.action?articleId=16805
dc.rights	info:eu-repo/semantics/openAccess
dc.subject	Àrees temàtiques de la UPC::Enginyeria civil::Geotècnia::Mecànica de sòls
dc.subject	Clay soils -- Analysis
dc.subject	Natural Boom Clay
dc.subject	Argila -- Assaigs de materials
dc.title	Heating pulse tests under constant volumen on natural Boom clay.
dc.type	info:eu-repo/semantics/publishedVersion
dc.type	info:eu-repo/semantics/article
dc.description.abstract	Boom clay formation is a potential natural host rock for geological disposal of high-level nuclear waste in Belgium. Heating pulse tests with controlled power supply (maximum temperature was limited to 85°C) and controlled hydraulic boundary conditions were performed under nearly constant volume conditions to study the impact of thermal loading on the clay formation. Selected test results of intact borehole samples retrieved in horizontal direction are presented and discussed. The study focuses on the time evolution of temperature and pore water pressure changes along heating and cooling paths, i.e. pore pressure build-up during quasi-undrained heating and later dissipation at constant temperature.
dc.description.abstract	Peer Reviewed

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