Grant: Research Tools and Instruments - Category 1 (<$150,000)
Dalhousie University
$148,822.00
Low-background vacuum extraction and graphitisation system for 14C
EF 2007-08
Résumé
Radiocarbon, C-14, is a naturally ubiquitous isotope that has many uses. It is most known for its use as a dating technique. It is also widely used as a tracer in biomedical experiments where the C-14 is substituted for non-radioactive C-12. We wish to explore two other uses of C-14 using the proposed equipment. When cosmic rays interact with exposed atoms in rock and soil, one of the many isotopes produced is C-14. Only 15 atoms of C-14 are produced per year in a 1 g quartz crystal, exposed for instance, on a beach in the Arctic. If we can build a vacuum system that allows negligible contamination (no lab air, no C from fixtures of the system) it is possible to count the low concentration of C-14 in 5 to 7 g of quartz that has been exposed for thousands of years. The concentration provides information about the exposure age and erosion history of the rock, with which we can answer important questions regarding , for instance, the frequency of storms and earthquakes, the history of climate changes, and timing of human occupancy. Our second use of extremely low abundances of C-14 is in the study of specific organic molecules and their application to environmental science and paleoceanography. For instance, by measuring the C-14 abundance in fatty acids of microbes, it is possible to determine if the microbes are biograding specific pollutants and petroleum contaminants in various aquatic and terrestrial environments (there is no C-14 in petroleum due to radioactive decay). However, the extraction of such small masses (tens of micrograms of C-14) requires a low-background vacuum line that does not yet exist in Canada and is not readily accessible at the few possible facilities worldwide. In addition to two technicians, students and visitors will receive training in vacuum systems, isotope and environmental geochemistry, and geochronology. The system will be unique to Canada and will help these researchers and their teams to assume leadership in designing innovative C-14 experiments.
Programme
Research Tools and Instruments - Category 1 (<$150,000)
Bénéficiaire
Emplacement
Nova Scotia, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data
Tel que publié
Application id
358955-2008
Name nom
Gosse, John
Department département
Earth Sciences
Organization id
79
Institution établissement
Dalhousie University
Province en
Nova Scotia
Province fr
Nouvelle-Écosse
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2007
Competition year année de concours
2008
Award amount
148822
Program id
EQPEQ
Program name en
Research Tools and Instruments - Category 1 (<$150,000)
Program name fr
Outils et instruments de recherche - catégorie 1 (<150 000$)
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
8
Committee name en
Solid Earth Sciences
Committee name fr
Sciences de la Terre solide
Area of application code
1203
Area of application group en
Advancement of knowledge
Area of application group fr
Avancement des connaissances
Area of application en
Earth sciences
Area of application fr
Sciences de la terre
Research subject code
4200
Research subject group en
Geochemistry and geochronology
Research subject group fr
Géochimie et géochronologie
Research subject en
Geochemistry and geochronology
Research subject fr
Géochimie et géochronologie
Partie
1
Nb partie
1
Application title
Low-background vacuum extraction and graphitisation system for 14C
Keyword
NA
Application summary
Radiocarbon, C-14, is a naturally ubiquitous isotope that has many uses. It is most known for its use as a dating technique. It is also widely used as a tracer in biomedical experiments where the C-14 is substituted for non-radioactive C-12. We wish to explore two other uses of C-14 using the proposed equipment. When cosmic rays interact with exposed atoms in rock and soil, one of the many isotopes produced is C-14. Only 15 atoms of C-14 are produced per year in a 1 g quartz crystal, exposed for instance, on a beach in the Arctic. If we can build a vacuum system that allows negligible contamination (no lab air, no C from fixtures of the system) it is possible to count the low concentration of C-14 in 5 to 7 g of quartz that has been exposed for thousands of years. The concentration provides information about the exposure age and erosion history of the rock, with which we can answer important questions regarding , for instance, the frequency of storms and earthquakes, the history of climate changes, and timing of human occupancy. Our second use of extremely low abundances of C-14 is in the study of specific organic molecules and their application to environmental science and paleoceanography. For instance, by measuring the C-14 abundance in fatty acids of microbes, it is possible to determine if the microbes are biograding specific pollutants and petroleum contaminants in various aquatic and terrestrial environments (there is no C-14 in petroleum due to radioactive decay). However, the extraction of such small masses (tens of micrograms of C-14) requires a low-background vacuum line that does not yet exist in Canada and is not readily accessible at the few possible facilities worldwide. In addition to two technicians, students and visitors will receive training in vacuum systems, isotope and environmental geochemistry, and geochronology. The system will be unique to Canada and will help these researchers and their teams to assume leadership in designing innovative C-14 experiments.