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Grant: Discovery Grants Program - Individual

University of British Columbia

$67,000.00

From mantle geodynamics to environmental processes: a geochemical perspective

EF 2015-16

Résumé
Modern geochemistry is concerned with quantifying and explaining the transfer of elements within and between the different major geological reservoirs of the Earth, including the mantle, the crust, the oceans, and the atmosphere. Geochemistry provides answers and tools for the fundamental understanding of our planet, including the environment, global change, resources, human health and natural hazards. Such research requires precise analysis of isotopic ratios and elemental concentrations in rocks, minerals, water, or organic matter. Multiple collector inductively coupled plasma mass spectrometers dramatically expand the potential isotopic systems that can be measured and allow for unprecedented sensitivity and precision. I propose to investigate three main themes of geochemical applications: 1) Earth's mantle and solid earth, 2) environmental impact, and 3) analytical developments in mass spectrometry. As the Earth's deep interior cannot be sampled directly, geochemists rely on analyzing basalts to infer the composition of the mantle. I propose to study two of the largest modern mantle plumes (Hawaii and Kerguelen) that originate in the deep mantle and, as well as Cascade Arc volcanoes and sediments to model the amount of recycling into the mantle. The results of this research will contribute to the global understanding of the composition and distribution of components in the mantle and their variation over geologic time. In the environmental theme, I will use heavy stable isotope systems (Cd, Zn, Si coupled with Pb) to investigate element cycling and metal pollution in marine and terrestrial systems. This work will increase our understanding of ancient climates and oceanographic conditions and has implications for British Columbia fisheries and aquaculture industry. Research within the third theme includes systematic studies to characterize reference materials and identify problematic matrix effects during mass spectrometry. This work will lead to an invaluable reference database and methodology for the scientific community. The overall objective of the proposed 5-year research program is to evaluate the geochemical evolution of our planet and its environment through the use of new analytical possibilities in isotopic geochemistry.
Programme
Discovery Grants Program - Individual
Emplacement
British Columbia, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data

Tel que publié

Application id
249476-2013
Name nom
Weis, Dominique
Department département
Earth, Ocean and Atmospheric Sciences
Organization id
2
Institution établissement
University of British Columbia
Province en
British Columbia
Province fr
Colombie-Britannique
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2015
Competition year année de concours
2013
Award amount
67000
Program id
RGPIN
Program name en
Discovery Grants Program - Individual
Program name fr
Programme de subventions à la découverte - individuelles
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
1506
Committee name en
Geosciences
Committee name fr
Géosciences
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
3
Nb partie
5
Application title
From mantle geodynamics to environmental processes: a geochemical perspective
Keyword
NSERC
Application summary
Modern geochemistry is concerned with quantifying and explaining the transfer of elements within and between the different major geological reservoirs of the Earth, including the mantle, the crust, the oceans, and the atmosphere. Geochemistry provides answers and tools for the fundamental understanding of our planet, including the environment, global change, resources, human health and natural hazards. Such research requires precise analysis of isotopic ratios and elemental concentrations in rocks, minerals, water, or organic matter. Multiple collector inductively coupled plasma mass spectrometers dramatically expand the potential isotopic systems that can be measured and allow for unprecedented sensitivity and precision. I propose to investigate three main themes of geochemical applications: 1) Earth's mantle and solid earth, 2) environmental impact, and 3) analytical developments in mass spectrometry. As the Earth's deep interior cannot be sampled directly, geochemists rely on analyzing basalts to infer the composition of the mantle. I propose to study two of the largest modern mantle plumes (Hawaii and Kerguelen) that originate in the deep mantle and, as well as Cascade Arc volcanoes and sediments to model the amount of recycling into the mantle. The results of this research will contribute to the global understanding of the composition and distribution of components in the mantle and their variation over geologic time. In the environmental theme, I will use heavy stable isotope systems (Cd, Zn, Si coupled with Pb) to investigate element cycling and metal pollution in marine and terrestrial systems. This work will increase our understanding of ancient climates and oceanographic conditions and has implications for British Columbia fisheries and aquaculture industry. Research within the third theme includes systematic studies to characterize reference materials and identify problematic matrix effects during mass spectrometry. This work will lead to an invaluable reference database and methodology for the scientific community. The overall objective of the proposed 5-year research program is to evaluate the geochemical evolution of our planet and its environment through the use of new analytical possibilities in isotopic geochemistry.