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Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/17659
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dc.contributor.authorDean, Gordon H.-
dc.date.accessioned2015-06-29T20:09:12Z-
dc.date.available2015-06-29T20:09:12Z-
dc.date.issued1946-05-
dc.identifier.urihttp://hdl.handle.net/11375/17659-
dc.description.abstractIn the atomic energy pile at Chalk River, heavy water (deuterium oxide, D2O) is to be used as a moderator. Early in 1944, it became evident that frequent determinations of the isotopic composition of D2O samples would be required. For this purpose, there was obtained from the American authorities a mass spectrometer specially designed for routine hydrogen isotope analysis. This instrument was assembled and put into operation at McMaster in the summer of 1944. During the course of subsequent work, two other deuterium mass spectrometers were built in this laboratory, following the design of the instrument sent from the United States; one of these has now been installed at the plant site, and a second is to follow at an early date. The studies reported below involved the determination of operating conditions, the measurement of grid leaks, of the order of 10^10 ohms, and the investigation of further applications of the deuterium mass spectrometer.en_US
dc.language.isoenen_US
dc.subjectChalk Riveren_US
dc.subjectatomic energyen_US
dc.subjectheavy wateren_US
dc.subjectdeuterium oxideen_US
dc.subjectdeuterium mass spectrometeren_US
dc.subjectMcMaster Universityen_US
dc.subjectoperating conditionsen_US
dc.subjectgrid leaksen_US
dc.subjectapplicationsen_US
dc.titleStudies With the Deuterium Mass Spectrometeren_US
dc.typeThesisen_US
dc.contributor.departmentChemistryen_US
dc.description.degreetypeThesisen_US
dc.description.degreeMaster of Science (MSc)en_US
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