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<br />002371 <br />Abstract <br /> <br />The effects of the construction and operation of Glen Canyon Dam have been studied, <br /> <br /> <br />documented, and manipulated in the downstream environment in Grand Canyon. Glen Canyon <br /> <br />Environmental Studies led 13 years of study that focused on addressing and mitigating the adverse <br /> <br />impacts of the Dam on that ecosystem. While data has been collected from Lake Powell throughout <br /> <br />its filling history, there has been no concerted effort to evaluate the impacts of dam operations on <br /> <br />the physical, biological, and chemical processes of the reservoir and downstream releases. Using <br /> <br />data from the 33-year history of water quality monitoring on Lake Powell, primarily from Bureau <br /> <br />of Reclamation efforts, we will begin to demonstrate the effect of dam operations and other factors <br /> <br />on the water quality and hydrodynamics of Lake Powell. Of special importance are the historical <br /> <br />record reflecting the flood years of 1980 to 1986, modified operations of Glen Canyon Dam which <br /> <br />began in 1991, the results from the Experimental Beach/Habitat Building Flood of the spring of <br /> <br />1996, and most recently, the high sustained releases starting in February 1997. No special data <br /> <br />collection was designed to answer the question, but rather, the stock of existing data was analyzed <br /> <br />to provide the answers and to fuel the questions that formed the assessment. The results show that, <br /> <br />combined with other influences, dam operations have an undeniable effect upon the stratification <br /> <br />and mixing of the reservoir, and those effects are consequently passed downstream through the <br /> <br />dam. Not all aspects of dam operations could be answered or analyzed under the scope of the nine <br /> <br />months allowed for the assessment. The experimental flood demonstrated the effects of using <br /> <br />alternate structures for the release of water, in this case, the hollow jet tubes that are positioned 100 <br /> <br />feet below the penstock withdrawal ports. The historic record of the 1980's indicated that the <br /> <br />combination of high and repeated spring floods and high and sustained discharge from penstocks as <br /> <br />well as spillways and hollow jet tubes caused substantial mixing of the reservoir. The recent <br /> <br />06/02/98 <br /> <br />DRAFT <br /> <br />Page iv of62 <br />