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dc.contributor.advisorDixon, J. B.
dc.creatorCarty, David
dc.date.accessioned2022-04-01T16:01:56Z
dc.date.available2022-04-01T16:01:56Z
dc.date.issued1977
dc.identifier.urihttps://hdl.handle.net/1969.1/CAPSTONE-CohenW_1982
dc.descriptionProgram year: 1976/1977en
dc.descriptionDigitized from print original stored in HDRen
dc.description.abstractCesium selectivity (kg) exponentially increased as Cs saturation decreased in the <0.2μm clay fraction and possibly in the 2-0.2μm clay and 20-2μm silt fractions of the lignite associated shale. The <0.2μm clay fraction had a high selectivity up to about 10% Cs saturation. Larger particle sizes had the highest selectivity. The total number of Cs ions fixed was higher in the smaller size fractions. Additional analyses must be performed to accurately determine the mineralogical composition of the shale and the ultimate disposition of the Cs ions introduced into the mineral system.en
dc.format.extent46 pagesen
dc.format.mediumelectronicen
dc.format.mimetypeapplication/pdf
dc.subjectCesium selectivityen
dc.subjectlignite associated shaleen
dc.subjectclayen
dc.subjectparticle sizeen
dc.subjectmineralogical compositionen
dc.subjectCs ionsen
dc.titleCesium Selectivity Of A Lignite Associated Shale Strata In Texasen
dc.title.alternativeCESIUM SELECTIVITY OF A LIGNITE ASSOCIATED SHALE STRATA IN TEXASen
dc.typeThesisen
thesis.degree.departmentSoil and Crop Sciencesen
thesis.degree.grantorUniversity Undergraduate Fellowen
thesis.degree.levelUndergraduateen
dc.type.materialtexten


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