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Grant: Discovery Grants Program - Individual

Laurentian University of Sudbury

$24,000.00

Uptake and release of heavy metals by minerals and rock coatings

EF 2009-10

Résumé
The financial wealth of many countries is tied to their resources and manufacturing industries. In Canada, the processing of mining materials and waste disposal are key sources of the release of heavy metals into the environment. Accumulations of these elements in air, water and soils have a severe impact on the health of the environment. Therefore, understanding the fate of a heavy metal in the environment is critical to predict the presence of contaminants in air, water and soil. Predictive understanding requires knowledge regarding the interaction of a specific element-bearing material with the environment and once the element is released, its interaction with geological and barrier materials. My research focuses on the characterization of the release and uptake of heavy metals by minerals and coatings on rocks and minerals. In my ongoing research, I examine the release of Uranium via the dissolution of secondary uranium minerals, a scenario that would likely occur when nuclear waste comes in contact with Oxygen-rich solutions. A short-term goal of this part of my research is a general understanding between the dissolution properties of a secondary uranium mineral (features and kinetic) and its structure and the crystal-chemical properties of the elements in solution. The major part of my future research will be the characterization of the uptake of heavy metals by coatings and alteration phases. The uptake of heavy metals by minerals was dominantly studied using non-altered surfaces. However, mineral surfaces exposed to the atmosphere can be altered or covered by coatings and their interaction with heavy metal thus depends on the composition and structural features of alteration layers or alteration phases in proximity to the "parent" minerals. These examinations will include laboratory experiments on the uptake of heavy metals by alteration layers on silicate minerals. Furthermore, coatings and alteration phases will be studied in mine tailings and acidic soils around Sudbury and in the U-deposits of Elliot Lake and Pena Blanca, Mexico. The results from the studies at the U-deposits will give a better understanding on the mobilization of Uranium in mine tailings or nuclear waste repositories that are hosted in silica-rich lithologies.
Programme
Discovery Grants Program - Individual
Emplacement
Ontario, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data

Tel que publié

Application id
355232-2008
Name nom
Schindler, Michael
Department département
Earth Sciences
Organization id
26
Institution établissement
Laurentian University of Sudbury
Province en
Ontario
Province fr
Ontario
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2009
Competition year année de concours
2008
Award amount
24000
Program id
RGPIN
Program nane 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
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
4001
Research subject group en
Earth science
Research subject group fr
Sciences de la terre
Research subject en
Mineralogy, crystal chemistry and crystallography
Research subject fr
Minérologie, chimie des cristaux et cristallographie
Partie
2
Nb partie
5
Application title
Uptake and release of heavy metals by minerals and rock coatings
Keyword
NA
Application summary
The financial wealth of many countries is tied to their resources and manufacturing industries. In Canada, the processing of mining materials and waste disposal are key sources of the release of heavy metals into the environment. Accumulations of these elements in air, water and soils have a severe impact on the health of the environment. Therefore, understanding the fate of a heavy metal in the environment is critical to predict the presence of contaminants in air, water and soil. Predictive understanding requires knowledge regarding the interaction of a specific element-bearing material with the environment and once the element is released, its interaction with geological and barrier materials. My research focuses on the characterization of the release and uptake of heavy metals by minerals and coatings on rocks and minerals. In my ongoing research, I examine the release of Uranium via the dissolution of secondary uranium minerals, a scenario that would likely occur when nuclear waste comes in contact with Oxygen-rich solutions. A short-term goal of this part of my research is a general understanding between the dissolution properties of a secondary uranium mineral (features and kinetic) and its structure and the crystal-chemical properties of the elements in solution. The major part of my future research will be the characterization of the uptake of heavy metals by coatings and alteration phases. The uptake of heavy metals by minerals was dominantly studied using non-altered surfaces. However, mineral surfaces exposed to the atmosphere can be altered or covered by coatings and their interaction with heavy metal thus depends on the composition and structural features of alteration layers or alteration phases in proximity to the "parent" minerals. These examinations will include laboratory experiments on the uptake of heavy metals by alteration layers on silicate minerals. Furthermore, coatings and alteration phases will be studied in mine tailings and acidic soils around Sudbury and in the U-deposits of Elliot Lake and Pena Blanca, Mexico. The results from the studies at the U-deposits will give a better understanding on the mobilization of Uranium in mine tailings or nuclear waste repositories that are hosted in silica-rich lithologies.