Relations of Main-Stem Reservoir Operations and Specific Conductance in the Lower Arkansas River, Southeastern Colorado
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Two main-stem reservoirs on the lower Arkansas River, Pueblo Reservoir and John Martin Reservoir, are used to regulate and manage streamflow for irrigation and domestic water supplies, flood control, and recreation. Water storage and release operations for these reservoirs can affect streamflow and water quality of the downstream river. One water-quality property that can be affected is specific conductance. In 1996, the U.S. Geological Survey completed a study of the effects of Pueblo Reservoir and John Martin Reservoir operations on specific conductance at five sites located on the Arkansas River between Pueblo Reservoir and Lamar (fig. 1). This fact sheet presents an overview of the study findings. A detailed discussion of the study results is presented in Lewis and Brendle (1998).
[1] D. Thorne. Diagnosis and Improvement of Saline and Alkali Soils , 1954 .
[2] D. Brendle,et al. Relations of streamflow and specific-conductance trends to reservoir operations in the lower Arkansas River, southeastern Colorado , 1998 .
[3] Doug Cain. RELATIONS OF SPECIFIC CONDUCTANCE TO STREAMFLOW AND SELECTED WATER-QUALITY CHARACTERISTICS OF THE ARKANSAS RIVER BASIN, COLORADO , 1987 .