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Article: Five test methods for porosity of completely decomposed granite in Hong Kong

TitleFive test methods for porosity of completely decomposed granite in Hong Kong
Authors
KeywordsCompletely decomposed granite
Helium instrument
Mercury injection
Porosity
SEM
Thin section
Issue Date2004
PublisherPergamon. The Journal's web site is located at http://www.elsevier.com/locate/ijrmms
Citation
International Journal Of Rock Mechanics And Mining Sciences, 2004, v. 41 SUPPL. 1, p. 1B 03 1-8 How to Cite?
AbstractThis paper presents the results of a laboratory examination of the porosity values of Hong Kong completely decomposed granites. Five methods are used to measure the porosity values. They are the conventional physical test, helium instrument, mercury injection, thin section measurement and scanning electronic microscopy (SEM). The porosity from the physical test is an absolute porosity with the largest values (average = 44.88%). The porosity from the thin section represents voids or cracks between mineral grains on a plane section and has the smallest values (average = 7.7%). The porosity from the helium instrument is an opening porosity. The porosity from the SEM also represents the voids on a SEM image. The porosity from mercury injection is an effective porosity. The porosity values from the SEM are closely between the opening and effective porosity values. They have the average values between 30% and 35%. In other words, the SEM method can be used to effectively estimate the opening or effective porosity in meso and/or micro scales. © 2004 Elsevier Ltd.
Persistent Identifierhttp://hdl.handle.net/10722/71364
ISSN
2023 Impact Factor: 7.0
2023 SCImago Journal Rankings: 2.331
References

 

DC FieldValueLanguage
dc.contributor.authorYue, ZQen_HK
dc.contributor.authorShang, YJen_HK
dc.contributor.authorHu, RLen_HK
dc.contributor.authorTu, XBen_HK
dc.date.accessioned2010-09-06T06:31:19Z-
dc.date.available2010-09-06T06:31:19Z-
dc.date.issued2004en_HK
dc.identifier.citationInternational Journal Of Rock Mechanics And Mining Sciences, 2004, v. 41 SUPPL. 1, p. 1B 03 1-8en_HK
dc.identifier.issn1365-1609en_HK
dc.identifier.urihttp://hdl.handle.net/10722/71364-
dc.description.abstractThis paper presents the results of a laboratory examination of the porosity values of Hong Kong completely decomposed granites. Five methods are used to measure the porosity values. They are the conventional physical test, helium instrument, mercury injection, thin section measurement and scanning electronic microscopy (SEM). The porosity from the physical test is an absolute porosity with the largest values (average = 44.88%). The porosity from the thin section represents voids or cracks between mineral grains on a plane section and has the smallest values (average = 7.7%). The porosity from the helium instrument is an opening porosity. The porosity from the SEM also represents the voids on a SEM image. The porosity from mercury injection is an effective porosity. The porosity values from the SEM are closely between the opening and effective porosity values. They have the average values between 30% and 35%. In other words, the SEM method can be used to effectively estimate the opening or effective porosity in meso and/or micro scales. © 2004 Elsevier Ltd.en_HK
dc.languageengen_HK
dc.publisherPergamon. The Journal's web site is located at http://www.elsevier.com/locate/ijrmmsen_HK
dc.relation.ispartofInternational Journal of Rock Mechanics and Mining Sciencesen_HK
dc.subjectCompletely decomposed graniteen_HK
dc.subjectHelium instrumenten_HK
dc.subjectMercury injectionen_HK
dc.subjectPorosityen_HK
dc.subjectSEMen_HK
dc.subjectThin sectionen_HK
dc.titleFive test methods for porosity of completely decomposed granite in Hong Kongen_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=1365-1609&volume=41&spage=393&epage=394&date=2004&atitle=Five+test+methods+for+porosity+of+completely+decomposed+granite+in+Hong+Kongen_HK
dc.identifier.emailYue, ZQ:yueqzq@hkucc.hku.hken_HK
dc.identifier.authorityYue, ZQ=rp00209en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1016/j.ijrmms.2004.03.042en_HK
dc.identifier.scopuseid_2-s2.0-3042785721en_HK
dc.identifier.hkuros85614en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-3042785721&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume41en_HK
dc.identifier.issueSUPPL. 1en_HK
dc.identifier.spage1B 03 1en_HK
dc.identifier.epage8en_HK
dc.publisher.placeUnited Kingdomen_HK
dc.identifier.scopusauthoridYue, ZQ=7102782735en_HK
dc.identifier.scopusauthoridShang, YJ=7101867915en_HK
dc.identifier.scopusauthoridHu, RL=7202640738en_HK
dc.identifier.scopusauthoridTu, XB=7102136710en_HK
dc.identifier.issnl1365-1609-

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