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<br />, '.., ~ i <br />[) n C4"'S"" <br /> <br />90. Bathurst, J,c., and others, 1985, Sediment supply and unsteady transport in a mountain river; <br />the Roaring River, Colorado: Institute of Hydrology, UK report and NATO Grant 092/84, 208 p. <br /> <br />91. Bathurst, J.c., Leeks, GJ and Newson, M.D., 1986, Relationship between sediment supply and <br />sediment transport for the Roaring River, Colorado, USA, in Drainage basin sediment delivery, <br />Proceedings IntL Assoc. HydroL Sci., Alburquerque Symposium: v. 159, IAHS, p. 105-117. <br /> <br />92. Bauman, R.W., Gaufin, A.R., and Surdick, R.F., 1977, The stoneflies (Plecoptera) of the Rocky <br />Mountains: Mem. Am. EntomoL Soc., v. 31, p. 1-208. <br /> <br />93. Bazata, K., 1991, Nebraska stream classification study: Lincoln, Nebraska, Surface Water <br />Section, Water Quality Division Department of Environmental Control, State of Nebraska, 342 <br /> <br />p. <br /> <br />94. Beckman, W.c., 1952, A guide to the fishes of Colorado: University of Colorado Museum <br />Leaflet 11. <br /> <br />95. Bedinger, M.S., and Sniegocki, R.T., 1976, Summary appraisals of the Nation's ground-water <br />resources--Arkansas- White-Red Region: U.S. Geological Survey Professional Paper813-H,31 p. <br /> <br />The Arkansas-White-Red Region, an area of 265,000 square miles is characterized <br />by diversity in geography, climate, and geology and, in turn, by diversity in water <br />resources and water problems. The western semiarid part of the region is water <br />deficient, that is, potential evapotranspiration exceeds precipitation. The eastern, <br />humid part has a surplus. Water use in the region in 1970 averaged 10 billion gallons <br />per day, of which more than 65 percent was ground water. The largest use of ground <br />water was for irrigation of crops, mostly in the water-deficient areas of Texas, <br />Oklahoma, Kansas, and Colorado. Because of its ready availability and widespread <br />occurrence, ground water is used throughout the region to supply municipal and <br />rural water needs. The most productive aquifers, capable of yielding more than 50 <br />gallons per minute to individual wells are alluvium, carbonate rocks, gypsum, and <br />sandstone. Fresh water in storage in aquifers in the region is estimated to be 2 <br />billion acre-feet. In addition, a large unmeasured volume of saline water (containing <br />more than 1,000 mg/liter of dissolved solids) underlies the fresh water at depths <br />generally less than 500 feet. <br /> <br />96. Behnke, R.J., 1978, Grazing and the riparian zone: impact on aquatic values, in Graul, W.D., and <br />Bissell, S.J., eds., Lowland river and stream habitat in Colorado: a symposium: Greeley, Colo., <br />Colorado Chapter of WildL Soc. and Colorado Audubon Council, p. 126-132. <br /> <br />97. Beidleman, R. G., 1954, The cottonwood riverbottom community as a vertebrate habitat: <br />Boulder, Colo., University of Colorado, Ph.D. dissertation, 358 p. <br /> <br />98. Beiswenger, R.E., 1983, Water management in the arid west: The Cheyenne water project: The <br />Environmental Professional, v. 5, no. 1. <br /> <br />99. Belitz, K.R., and Bredehoeft, J.D., 1988, Hydrodynamics of Denver Basin; explanation of <br />subnormal fluid pressures: AAPG Bulletin, v. 72, no. 11, p. 1334-1359. <br /> <br />BIBLIOGRAPHY 23 <br /> <br />