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Aeolian and pluvial processes represent important mechanisms for the movement of actinides and fission products at the Earth’s surface. Soil samples taken in the early 1970’s near a Department of Energy radioactive waste disposal site (the Subsurface Disposal Area, SDA, located in southeastern Idaho) provide a case study for studying the mechanisms and characteristics of environmental actinide and Cs-137 transport in an arid environment. Multi-component mixing models suggest actinide contamination within 2.5 km of the SDA can be described by mixing between 2 distinct SDA end members and regional nuclear weapons fallout. The absence of chemical fractionation between Am-241 and Pu239+240 with depth for samples beyond the northeastern corner and lack of 241Am in-growth over time (due to Pu-241 decay) suggest mechanical transport and mixing of discrete contaminated particles under arid conditions. Occasional samples northeast of the SDA (the direction of the prevailing winds) contain anomalously high concentrations of Pu with Pu-240/Pu-239 isotopic ratios statistically identical to those in the northeastern corner. Taken together, these data suggest flooding resulted in mechanical transport of contaminated particles into the area between the SDA and a flood containment dike in the northeastern corner, following which subsequent contamination spreading in the northeastern direction resulted from wind transport of discrete particles. (C) 2015 Elsevier Ltd. All rights reserved.