TY - GEN
T1 - Accommodating transient velocities in time-domain particle tracking simulations of radionuclide transport
AU - Painter, Scott
PY - 2008
Y1 - 2008
N2 - Particle tracking in the time domain has previously been shown to be a robust and efficient technique for simulating radionuclide transport in the subsurface. In time-domain particle methods, particles representing packets of radionuclide mass are moved along predefined pathways using random residence time distributions developed from the underlying physicochemical retention processes. Time-domain particle tracking is extended here to accommodate pathway properties that are piecewise constant in time. Advection in flowing fractures and diffusion/sorption in the surrounding rock matrix is considered. In the new algorithm, a particle's distance away from a flowing fracture is sampled at the end of a constant-velocity flow period. Given this position in the matrix, the time required to diffuse back to the flowing fracture is then sampled. The particle is then restarted in the fracture using the new pathway velocity. Numerical verification tests demonstrate that the new approach is sufficiently accurate for use in assessing geological barriers in high-level nuclear waste repositories.
AB - Particle tracking in the time domain has previously been shown to be a robust and efficient technique for simulating radionuclide transport in the subsurface. In time-domain particle methods, particles representing packets of radionuclide mass are moved along predefined pathways using random residence time distributions developed from the underlying physicochemical retention processes. Time-domain particle tracking is extended here to accommodate pathway properties that are piecewise constant in time. Advection in flowing fractures and diffusion/sorption in the surrounding rock matrix is considered. In the new algorithm, a particle's distance away from a flowing fracture is sampled at the end of a constant-velocity flow period. Given this position in the matrix, the time required to diffuse back to the flowing fracture is then sampled. The particle is then restarted in the fracture using the new pathway velocity. Numerical verification tests demonstrate that the new approach is sufficiently accurate for use in assessing geological barriers in high-level nuclear waste repositories.
UR - http://www.scopus.com/inward/record.url?scp=70449122009&partnerID=8YFLogxK
M3 - Conference contribution
AN - SCOPUS:70449122009
SN - 9781605604862
T3 - American Nuclear Society - 12th International High-Level Radioactive Waste Management Conference 2008
SP - 14
EP - 19
BT - American Nuclear Society - 12th International High-Level Radioactive Waste Management Conference 2008
T2 - 12th International High-Level Radioactive Waste Management Conference 2008
Y2 - 7 September 2008 through 11 September 2008
ER -