Executive SummaryA critical unknown for long-term engineered barrier performance is the effect of wild fire during a post-institutional control environment where routine maintenance may be limited or non-existent. The objective of this study was to quantify the effects of a wildfire on the function of an engineered barrier. A controlled burn on September 26, 2008, was used to remove all the vegetation from the north side of the prototype Hanford barrier in the 200 East Area. Fire effects on barrier performance have been monitored and documented over the past year. Soil physical, chemical, and hydrologic properties; plant floristics and density; and animal-use were characterized before and after the fire with the unburned half of the barrier serving as a control.Flame heights exceeded 9 m, and temperatures ranged from 250 o C at 1.5 cm below the surface to over 700 o C at 1 m above the surface. Post-fire analysis of soil properties shows significant decreases in wettability, hydraulic conductivity, air-entry pressure, organic matter, and porosity relative to pre-fire conditions whereas dry bulk density increased. Decreases in hydraulic conductivity and wettabilty immediately after the fire are implicated in a surface runoff event that occurred in January 2009, the first in 13 years. There was a significant increase in macro-nutrients, pH, and electrical conductivity. After 1 year, hydrophobicity has returned to pre-burn levels with only 16% of the samples still showing signs of decreased wettability. Over the same period, hydraulic conductivity and air-entry pressure returned to pre-burn levels at one third of the locations but remained identical to values recorded immediately after the fire at the other two thirds. Soil nutrients, pH, and electrical conductivity remain elevated after 1 year. There were significant differences in the rate of accumulation and loss of soil moisture on the burned and unburned sections. On the burned section, water storage was higher during the fall, it increased more slowly with the onset of winter precipitation (owing to higher evaporation), and decreased more slowly in the spring (owing to lower evapotranspiration). Xylem pressure potentials were considerably higher on the burned half of the barrier in September 2009, which is consistent with observed differences in storage and suggest that not all the water in the soil profile will be removed before the fall rains begin. Species composition on the burned surface changed markedly from prior years, and this was relative to the unburned surface and two analog sites. An increase in the proportion of annuals and biennials is characteristic of burned surfaces that have become dominated by ruderal species. Greenhouse seedling emergence tests conducted to assess the seed bank of pre-and post-burn soils and of two analog sites at the McGee Ranch show no difference in the number of species emerging from soils collected before and after the fire. However, there were fewer species emerging from the seed bank on the side slopes and more speci...