Water quality, substratum and biotic responses of five central Idaho (USA)streams during the first year following the Mortar Creek fire

The Mortar Creek Fire burned 26 000 ha of mixed-conifer Rocky Mountain fore st in July-August 1979. Changes in burn stream conditions were examined rel ative to reference streams for various ecological factors on two to six occ asions, from October 1979 to August 1980. Factors included major ions and n utrients, suspended and benthic particulate matter, periphyton (algae), and macroinvertebrates. Elevated levels of most dissolved chemicals in the bur n streams were evident soon after the fire and again during spring runoff. However, there were no major disruptions in the relative composition of cat ions (and presumably of anions also) in the burn streams during the study. Concentration (mg/L) and load (g/s) of some constituents were higher (e.g. NO3-N) and of others (e.g. Ca) were lower in the burn than in the reference streams during spring runoff, depending on whether they were normally unde r biological or geological control, respectively. Suspended sediment and pa rticulate organic matter generally were higher in burn streams, especially during snow-melt runoff or following heavy rain storms. Benthic organic mat ter was higher in burn streams and was mainly charcoal, compared to the usu al leaf litter found in the reference streams. Fine sediments increased and periphyton decreased in the burn streams. The fire increased the sensitivi ty of the burn streams to more routine smaller-scale disturbances, such as rainstorms, which had major impacts on the burn streams but not on the refe rence streams. The macro invertebrate assemblage showed little direct effec t from the fire but was severely altered in composition and abundance by th e subsequent runoff, scouring, and channel alteration initiated by spring r unoff. The burn streams showed considerable individuality in their response to fire depending on the particular set of conditions to which they were e xposed.