E03 : Diffusion Mechanism of Pu+3 in Sedimentary Repository Conditions: Ab Initio Molecular Dynamics Study


Students Becca Barbera
School HWCD - Cathedral High School - Hamilton
Level Senior 11/12 - Grade 11
Group Group 15 - Earth and Environmental III
Abstract The purpose of this experiment is to determine the diffusion coefficient of Pu+3 through MX-80 bentonite clay, alongside the interference of the SR-270-PW brine solution found within sedimentary rock formations. This study has many valuable applications and provides the Nuclear Waste Management Organization with specific data to be considered upon when deciding on the deep geological repository host location and storage methods, alongside performance and safety assessments, which will both ensure public protection and support zero-emission clean-energy production.
Project Video Video Link
Awards
Group Award Prize
Canadian Institute of Mining Metallurgy and Petroleum (Hamilton Branch) AwardsCanadian Institute of Mining Metallurgy and Petroleum (Hamilton Branch) Award$ 100
International Science & Engineering Affiliated Fair AwardsAssociation for Women Geoscientists Awardcertificate
International Science & Engineering Affiliated Fair AwardsRicoh USA Inc. Awardcertificate
Rotary Club of Hamilton Stoney Creek AwardsRotary Club of Hamilton Stoney Creek Award - First$ 250
Merit AwardsGold Merit Award$ 100
ArcelorMittal Dofasco AwardsArcelorMittal Dofasco Central Trades & Services Department Award$ 100
Primary Fluid Systems AwardsPrimary Fluid Systems Award$ 100
ISEF Trip AwardsISEF Trip Award
McMaster University School of Earth Environment and SocietyEarth and Environmental Sciences Award$ 100
McMaster University MGD Institute for Infectious Disease Research AwardsMichael G. DeGroote Institute for Infectious Disease Research Award - Bronze$ 50
Harrison Family Chemistry AwardHarrison Family Chemistry Award$ 100