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dc.contributor.advisorHarding, K. E.
dc.creatorSwolfs, Henri Samuel
dc.date.accessioned2020-01-08T17:52:00Z
dc.date.available2020-01-08T17:52:00Z
dc.date.created1971
dc.date.issued1974
dc.identifier.urihttps://hdl.handle.net/1969.1/DISSERTATIONS-173251
dc.description.abstractTo evaluate the effect of chemical solutions on the strength properties of porous rocks, triaxial and uniaxial compression experiments have been made on Coconino sandstone injected with distilled water and dilute solutions of aluminum and ferric chloride. Confining pressure and internal pore pressure were applied and measured independently. Temperature was varied from 24° to 200°C. Results indicate that the strength and ductility of the sandstone are dependent on the type and concentration of the cations in the aqueous phase. Dilute solutions of aluminum and ferric iron salts, in addition to water, react with the surface structure of quartz and probably other silicates, and weaken the surface silicon-oxygen bonds by hydrolysis. This leads to a reduction in surface energy, surface cohesion, and breaking strength. ...en
dc.format.extent65 leavesen
dc.format.mediumelectronicen
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.rightsThis thesis was part of a retrospective digitization project authorized by the Texas A&M University Libraries. Copyright remains vested with the author(s). It is the user's responsibility to secure permission from the copyright holder(s) for re-use of the work beyond the provision of Fair Use.en
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.titleInfluence of pore-fluid chemistry and temperature on fracture of sandstone under confining pressureen
dc.typeThesisen
thesis.degree.disciplineGeologyen
thesis.degree.grantorTexas A&M Universityen
thesis.degree.nameDoctor of Philosophyen
thesis.degree.levelDoctoralen
dc.type.genredissertationsen
dc.type.materialtexten
dc.format.digitalOriginreformatted digitalen
dc.publisher.digitalTexas A&M University. Libraries


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