iii eXECUTIVE SUMMARY Pacific Northwest Laboratory (PNL) used a methodology for predicting the migration and fate of radionuclides in the environment to assess 239pu migration in the vicinity of Los Alamos National Laboratory (LANL). The MCEA (Multimedia ~ontaminant ~nvironmental Exposure Assessment) methodology, which was jointly developed by PNL and LANL, assesses exposures to air, water, soil, and plants from contaminants released into the environment by simulating dominant mechanisms of contaminant migration and fate. The methodology is more sophisticated than those for a basic worst-case scenario analysis, but less sophisticated than a full-scaled, extremely detailed, expensive and timeconsuming onsite survey. The methodology encompasses five different pathways (i.e., atmospheric, terrestrial, overland, subsurface, and surface water) and combines them into a highly flexible tool. The flexibility of the MCEA methodology is demonstrated in this study by encompassing two of the pathways (i.e., overland and surface water) into an effective tool for simulating the migration and fate of radionuclides released into the Los Alamos, New Mexico region.The purpose of this study was to assess the potential migration and fate of radionuclides in Los Alamos and Pueblo Canyons. Specifically, a precipitation-generated flood event with a recurrence interval of 50 yr was simulated in Los Alamos and Pueblo Canyons to simulate the degree to which radionuclides would migrate into lower Los Alamos Canyon. PNL performed this work in cooperation with LANL.The MCEA methodology was employed to simulate the resuspension, deposition, sorption, migration, and fate of 239Pu adsorbed onto bed sediments. The scenario studied herein assumed the 239pu concentrations currently existing at the modeling site as the initial conditions. A temporally varying, spatially uniform precipitation event representing a possible 50-yr flood event was used in the modeling scenario. The 50-yr event was chosen in an attempt to simulate a critical event (i.e., one which may transport significant amounts of 239pu downstream and deposit them into lower v Los Alamos Canyon). Overland runoff events transported water and sediment to the channel 's edge as lateral inflow. The movement of water and sediment along with contaminated bed sediment entrained into the flow were simulated for the precipitation-generated flood event.The study revealed that a) the 239 pu inventory in lower Los Alamos Canyon increased by approximately 1.1 times for the 50-yr flood event; b) the average contaminant 239pu concentrations (i.e., weighted according to the depth of the respective bed layer) in lower Los Alamos Canyon for the 50-yr flood event decreased by 5.4%; c) ~27% of the total 239pu contaminaton resuspended from the entire bed (based on the assumed cross sections) for the 50-yr flood event originated from lower Pueblo Canyon; d) an increase in the 239pu contaminaton of the bed followed the general deposition patterns experienced by the sediment in Pueblo-lower Los Alamos Canyo...