Trends in productivity and mineral content of herbaceous vegetation in Ponderosa pine and montane grassland over a 4-year period are reported. Dry matter production on burned areas was 1.4, 1.3, 2.2 and 1.6 times that on unburned sites in the four successive years following the fire. Annual forbs and annual grasses contributed 56% of total dry matter the first year following fire. Perennial forbs contributed 40, 75, 75, and 77% of dry matter on the burned sites in successive years following the fire, compared with 66% on the unburned site. Herbage mineral concentrations did not change appreciably following fire, although low values for nitrogen and potassium were apparent in the first year.Responses of herbaceous understories in Ponderosa pine (Pinus ponderosa) communities to fire in the northern Rocky Mountains have not been extensively evaluated. Although investigations in Arizona by Pearson et al. (1972), Campbell et al. (1977, and in central Washington (Weaver 1951) have been made, Mueggler (1976) concluded that generalizations are difficult because each combination of climate, vegetation, and soil must be considered separately. Further, none of these investigations evaluated trends in productivity, vegetative composition, and nutrient content simultaneously.A lightning-caused fire in Ponderosa pine and adjacent montane grassland on August 10, 1973, in the Upper Selway River (White Cap Creek), Idaho, provided opportunities to assess understory responses. It burned for 43 days over an 1,100-ha area, when it was extinguished by rain (Mutch 1974). The area is a portion of a fire management zone in the Selway-Bitterroot Wilderness where fires are allowed to burn under most natural conditions.Objectives of this study were to follow changes in vegetative production, composition, and mineral content on the burned area and compare with adjacent unburned sites.
Study AreaElevations on the burn ranged from 935-1,830 m, with all study plots on south-facing slopes at 1,000-1,300 m above sea level. Soils were derived from Idaho batholith parent material consisting of decomposed granite, gneiss, and rhyolite (Greenwood and Morrison 1967). Habeck (1972) characterized these soils as low in fertility, water holding capacity and of weak structure. Average annual precipitation was 76 cm with peaks occurring November-January and April-June (Finklin 1977 The fire occurred under extremely dry conditions, with relative humidity as low as 11%, maximum temperatures to 32° C, and winds gusting to 45 km/ hr. Ground cover on south-exposed slopes was sparse and unevenly distributed. Burned study sites showed evidence of burned stubble but no litter. The fire burned rapidly over these sites and left little ash. Adjacent unburned slopes of similar topographic characteristics were used for comparisons.Elk (Cervus elaphus) and deer (Odocoileus hemionus, 0. virginianus) used these areas as winter-spring range. McCulloch (1955) reported heavy utilization of browse by elk on adjacent shrub winter ranges in the early 1950's, and pr...