Water balance in North America, 1969

Water balance in North America, 1969

Journal of Hydrology 11 (1970) 215-216; © North-HollandPublishing Co., Amsterdam BOOK REVIEWS Water Balanee in North America, 1969. Proceedings of t...

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Journal of Hydrology 11 (1970) 215-216; © North-HollandPublishing Co., Amsterdam

BOOK REVIEWS

Water Balanee in North America, 1969. Proceedings of the Symposium on Water Balance in North America, sponsored by the American Water Resources Association and held at the Banff School of Fine Arts, Banff, Alberta, Canada, June 23-25, 1969. AWRA, Urbana, Illinois, 1969.330 p. $15.

Fifth American Water Resources Conference, 1969. Proceedings of the Fifth American Water Resources Conference, sponsored by the American Water Resources Association and held at E1 Tropicano Motor Hotel, San Antonia, Texas, October 26-30, 1969. Published in four parts in the 1970 Water Resources Bulletin. AWRA, Urbana, Illinois. $15.

E. A. MOULDERand C. T. JENKINS: Analog-Digital Models of Stream-Aquifer Systems. Ground Water, Vol. 7, No. 5, p. 19-24, Sept.-Oct. 1969.6p., 8 fig. The best features of analytical and digital computers were combined to make a management model of a stream-aquifer system. The analytical model provided a means for synthesizing, verifying and summarizing aquifer properties; the digital model permits rapid calculation of the effect of watermanagement practices. Given specific management alternatives, a digital program can be written that will optimize operational plans of streamaquifer systems. The techniques are demonstrated by application to a study of the Arkansas River valley in south-eastern Colorado. Many streams are hydraulogically connected to large ground-water bodies in valley-fill deposits adjacent to and underlying the stream. In the Western United States many alluvial valleys are irrigated both by surface water and by ground-water. The Arkansas River valley in south-eastern Colorado is typical of such systems. The average yearly supply of surface water is about equal to the crop requirements, but because there are few surface storage facilities severe surface-water shortages occur during the latter part of the growing season. The ground-water reservoir offers a means of regulating the supply. Since about 1950, irrigators have installed 1200 large-capacity wells in the valley to supply late-season deficiencies. (Author's Abs. and Introduction) 215