Battle Flat Pilot Watershed Project - Description and History
Following 20 years of research on small experimental watersheds in the
chaparral shrublands, planning began for a joint pilot application project
in 1976 between the Southwestern Region of the USDA Forest Service and
the Rocky Mountain Forest and Range Experiment Station
(Bolander
1986, Hassell
1976, Krebill
and Tackle 1978). The objective of this pilot application program
was to test the state-of-the art technology on a larger, operational-scale
chaparral watershed. Management techniques aimed at improving the production
of water, maintaining water quality, increasing livestock and wildlife
forage, enhancing wildlife habitat, reducing fire hazard and erosion,
and determining the economic feasibility of chaparral management was to
be evaluated and refined. This program also provided research opportunities
for studying fire effects on nutrients, erosion and sedimentation rates,
plant productivity and growth, and fire history (DeBano
et al. 1999b).
Study Area
A 3,780-ac watershed (Battle Flat) on the Prescott National Forest in
central Arizona was designated as a pilot application area in chaparral
shrublands in July 1977 (Hassell
1976). The Battle Flat Demonstration Area in the Bradshaw Mountains
was chosen to test the current knowledge of managing chaparral shrublands
on an operational-size watershed (Bolander
1986). The results of all information gained on experimental chaparral
watersheds (both in Arizona and in California) were used to design treatments.
The demonstration area consists of two adjacent watersheds. The southern-most
watershed (1,600 ac) is drained by the northeast trending Tuscumbia Creek;
the northern-most watershed (2,174 ac) is drained by the east-southeast
trending Battle Flat Creek. The elevation at the point of junction of
the two stream channels is 4,969 ft.
The topography is highly dissected and rugged. Most of the watershed
faces southeast with slopes ranging from 8 to 30 degrees. Parent rock
materials in the study area consists of granitics, volcanics, and alluvium.
The Battle Flat watershed contains 11 different soil map units (Humbert
et al., 1981) whose texture range from sandy loams to very gravelly
coarse loams. These soils are located on slopes from 0 to 60% and are
all less than 16 inches deep. Runoff on these slopes is rapid and erosion
hazard is moderate to high.
Annual precipitation averaged 27 inches over a 10-year period. The watersheds
were dominated by shrub live oak (48%), birchleaf mountainmahogany (27%),
and pointleaf manzanita (19%). The remaining 6% cover was made up of several
other species.
Cooperators
In collaboration with the pilot application program, several research
studies were initiated by Rocky Mountain Forest and Range Experiment Station
scientists and other scientists from Arizona State University and the
University of Arizona. These studies included establishing baseline information
on streamflow, erosion and sedimentation, shrub biomass, scenic beauty,
effects of fire on nutrient cycling, fire history, and the effect of fire
on erosion. Streamflow, precipitation, and sediment measurements were
a joint effort between the Rocky Mountain Research Station and the Prescott
National Forest. Overall program management was jointly shared by a project
leader for the Rocky Mountain Research Station, the supervisor of the
Prescott National Forest, and the lead hydrologist for the Southwestern
Region of the Forest Service.