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dc.contributor.authorHume, Lily Annen_US
dc.date.accessioned2014-03-14T20:39:37Z
dc.date.available2014-03-14T20:39:37Z
dc.date.issued1991-05-05en_US
dc.identifier.otheretd-06082009-171119en_US
dc.identifier.urihttp://hdl.handle.net/10919/33485
dc.description.abstractChrysotile can be linked to three diseases: lung cancer, asbestosis, and mesothelioma. The duration and intensity of exposure along with fiber size appear to play an important role in the development of the diseases. Chrysotile is part of the serpentine group which has the general composition of Mg3Si205(OH)4. The fluids in lung tissue contain very low concentrations of magnesium and silicon. As a result they are quite undersaturated with respect to chrysotile and chrysotile will dissolve. Its persistence in lung tissue is simply a result of its dissolution kinetics. The purpose of this study was to estimate the lifetime of a respirable size fiber of chrysotile in lung tissue.

The dissolution reaction for chrysotile for pH's less than nine is: Mg3Si205(OH)4 + 6H+ = 3Mg2+ + 2H4Si04 + H20

This reaction proceeds in two steps. First, the magnesium hydroxide layer of the serpentine dissolves leaving behind the silica structure of the fiber. Then the silica dissolves. Therefore, the fiber lifetime depends upon the rate of silica release. Over the range of undersaturation expected for lung tissue, the rate of silica release was found to be independent of pH with the average rate being 5.94 (±3.05) x 10-10 moles m-2 sec-I. A shrinking fiber model was used to determine the relationship between dissolution time and fiber diameter. It was found that the most hazardous sized fiber of chrysotile (1 μm) would completely dissolve in about 9 months, consideration of one standard deviation above and below the mean of the rate constant gives estimates of the lifetime of a fiber ranging from 6 to 19 months.

en_US
dc.format.mediumBTDen_US
dc.publisherVirginia Techen_US
dc.relation.haspartLD5655.V855_1991.H854.pdfen_US
dc.subjectChrysotileen_US
dc.subject.lccLD5655.V855 1991.H854en_US
dc.titleThe dissolution rate of chrysotileen_US
dc.typeThesisen_US
dc.contributor.departmentGeologyen_US
dc.description.degreeMaster of Scienceen_US
thesis.degree.nameMaster of Scienceen_US
thesis.degree.levelmastersen_US
thesis.degree.grantorVirginia Polytechnic Institute and State Universityen_US
thesis.degree.disciplineGeologyen_US
dc.contributor.committeechairRimstidt, James Donalden_US
dc.contributor.committeememberCraig, James R.en_US
dc.contributor.committeememberZelazny, Lucian W.en_US
dc.identifier.sourceurlhttp://scholar.lib.vt.edu/theses/available/etd-06082009-171119/en_US
dc.date.sdate2009-06-08en_US
dc.date.rdate2013-06-03
dc.date.adate2009-06-08en_US


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