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<br />00ln~7 <br /> <br />. <br /> <br />. <br /> <br />National Park Service Studies to <br />Support Quantification of Reserved Water Rights at <br />Black Canyon of the Gunnison National Monument <br /> <br />Sediment Tran~rt <br /> <br />Sediment supplied to the river from side drainages and canyon walls is transported through <br />the canyon by water. As water energy levels and the volume of material exposed to moving <br />water are reduced, the volume of sediment moved through the canyon is reduced, resulting <br />in a build-up of sediment particles. The National Park Service (NPS) has contracted <br />scientists from the US Geological Survey to determine the magnitude of streamflow <br />necessary to entrain and transport existing sediment. Data collection occurred in 1994 and <br />again in 1995 following the spring peak: of nearly 10,000 cubic feet per second (cfs). Final <br />report is expected in 1997. <br /> <br />Riparian Vee:etation <br /> <br />The presence and areal extent of woody riparian vegetation is believed to have increased <br />since construction of the Aspinall Unit reservoirs. The elimination or reduction of scouring <br />flows has increased the occurrence and stability of depositional features (e.g., sediment bars, <br />debris fans). These features serve as ideal germination and establishment sites for many <br />plant species. Consequently, vegetation establishment is occurring in areas that in the past <br />would not have supponed vegetation. The NPS has contracted with scientists from the US <br />National Biological Service (NBS) to examine the relationship between streamflow and <br />riparian vegetation composition. Vegetation sampling was initially conducted in 1990, <br />repeated and expanded in 1994, and repeated again in 1995 following the unusually high <br />spring runoff. A preliminary report was produced in 1991. Final report is expected in 1997. <br /> <br />Visual Ouali ty and Aesthetics <br /> <br />As mentioned above, prior to construction of the Aspinall Unit, strearnbanks along the <br />mainstem Gunnison River were relatively devoid of vegetation. These rugged, barren <br />shorelines and banks were clearly visible from both the canyon rim and floor. The river and <br />river channel were often described as raging, turbulent, and roaring - characteristics which <br />were also easily discernable from the canyon rim, especially at high flows. In 1990, the NPS <br />contracted scientists from Colorado State University (CSU) to identify discharge-sensitive <br />aesthetic resource attributes and to evaluate the probable impacts of hypothetically altered <br />now regimes on visual quality within the canyon. A preliminary report for this study was <br />submitted in 1992. Final analysis of potential impacts to aesthetic resources will be <br />completed once the NBS' vegetation study has concluded. <br />