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<br />The major objective of this study was determination of the trends <br />and responses of riparian plant communities, along Rock Creek in the uinta <br />Mountains of Utah, to the different combinations of 1) soil moisture and <br />salinity, 2) solar irradiation as affected by adjacent mountains, and 3) <br />stream action. In addition, unique features of the stream hydrology and <br />riparian vegetation along the Lake Fork and Yellowstone Rivers must be <br />considered to clarify relations between the vegetation and physical factors <br />of the environment along Rock Creek. <br />The annual discharge of Rock Creek is approximately 115,700,984 cubic <br />meters, and it drains a watershed of approximately 622 square kilometers <br />(240 square miles). Spring runoff contributes most of this water during <br />the months of May and June, with average daily flows ranging from 17.0 <br />to 22 cubic meters per second. Stream flows during the remainder of the <br />year are generally below three cubic meters per second. Elevations of <br />the stream segments studied ranged from 1,830 meters (6000 feet) to 2,430 <br />meters (8000 feet). Average annual precipitation for these segments ranged <br />from 25 cm (10 in.) to 75 cm (30 in.). Lowest precipitation occurred during <br />the months of March and April and greatest precipitation occurred during <br />August and September. <br /> <br />METHODS <br /> <br />A detailed description of methods used is presented elsewhere (Hansen, <br />1977). Only a brief description is provided here. <br />Field research was conducted during the summers of 1975 and 1976. <br />Vegetative parameters such as c~ver, production, and density were measured <br />for2species in each of five 5 m plots (shrub and tree strata) and ten <br />1 m plots (herb strata) in each of 71 vegetative communities adjacent <br />to Rock Creek. Other parameters measured were temperature, relative <br />humidity, plant water potential, distance above and to the stream, and <br />soil depth or stoniness as assessed by 1 m x 1 cm metal rod pushed as far <br />as possible into the ground. Soil samples were analyzed for bulk density, <br />soil moisture, pH, electrical conductivity, and texture. <br />Computer and statistical analyses were performed using MIDAS programs <br />at the University of Michigan. The types of analyses included: cluster <br />analyses, one-way analysis of variance, stepwise multiple regression <br />analysis, discriminant analysis, principal component analysis and other <br />descriptive statistics. <br /> <br />RESULTS <br /> <br />Cluster analysis based on importance values (canopy cover and relative <br />abundance) resulted in the selection of eight major groupings of riparian <br />communities. Names were assigned to these groupings based on the dominant <br />species (species with the highest average importance value): alder, willow, <br />birch, conifer, cottonwood, aspen, hawthorn, and buffaloberry. Cluster <br />analysis of the herb strata, based on importance values of presence and <br />absence of a species, resulted in selection of different groups. This <br />suggests that understory species are not restricted to a particular overstory <br />species, but may be distributed according to similar environmental conditions, <br />particularly soil moisture. For example, 1) the birch, alder, and willow; <br /> <br />61 <br />