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• <br />CHAPTER VI. CONCLUSIONS <br />Conclusions <br />Bureau of Land Management Sites <br />During the 1996 runoff season for the Green River near Vernal, Utah, several objectives were met <br />regarding potential floodplain habitat restoration activities. Across section monitoring program for reaches <br />adjacent to five selected BLM bottomland sites was established. Stage/Discharge relationships were <br />developed for each site. From these relationships flooding discharges which will significantly fill the <br />bottomlands were discerned at each site. The flooding discharges ranged from 12,900 cfs at the Above <br />Brennan bottomland to 26,500 cfs at the Baeser Bend Bottomland site. An average flooding discharge of <br />20,500 cfs was determined. <br />In order to restore historical flooding frequencies and durations, levee removal strategies were <br />designed for each bottomland site. Topographic surveys were conducted at each site. Mapping with 2 foot <br />contours were created which identified levees, bottomland configurations, and inlets or low spots which could <br />be modified to increase flooding frequencies. At each site, an existing inlet was located and/or the feasibility <br />of a large scale levee removal was assessed. Unique levee removal strategies were proposed for each site <br />with varying widths and lengths, locations relative to the bottomlands, and channel morphology characteristics. <br />Each site was designed to flood at 13,000 cfs, which will occur 2 out of every 3 years, for 11 days based on <br />post-1963 hydrology. The duration of flooding should range from no flooding in dry years to 1-3 weeks during <br />average years, or 4-8 weeks during wet years. Under existing conditions, on the average, the sites will only <br />flood approximately 2 out of 7 years on average and the duration of flooding would be only 3.5 days <br />• statistically. The flooding return periods ranged from a 1.4-year return period at the Above Brennan <br />bottomland to a 15-year return period at the Baeser Bend bottomland. In order to significantly fill the <br />bottomlands, a discharge above the flooding discharge would have to occur for several days to a week. For <br />example, flows over 19,700 cfs, the flooding discharge at Bonanza Bridge, were experienced during the 1996 <br />runoff season for approximately 4 days. However, the bottomland did not completely fill and fish passage was <br />limited due to a short duration. <br />• <br />Levee removal designs have been proposed for each of the five BLM sites. Favorable flooding <br />locations were identified in the field, and the sites were designed to flood at 13,000 cfs utilizing different design <br />parameters for each site. The frequency and duration of flooding will be returned to an assumed historic <br />frequency and duration as a result of the designs. <br />The areas of inundation for the BLM bottomlands were determined utilizing the stage/discharge <br />relationships. Table 14 gives a comparison of the areas of inundation under existing and proposed conditions. <br />Under existing conditions, flooding with a hydraulic connection is limited to approximately 50 acres for flows <br />up to 18,000 cfs (all in Above Brennan). Under proposed conditions, approximately 140 acres at five different <br />sites would occur when flows exceeded 13,000 cfs. For comparison, that area would be increased to 173 <br />acres at 18,000 cfs after levee removal versus 50 acres under existing conditions. Under proposed <br />conditions, these sites will flood more frequently and the value of these bottomland sites as floodplain habitat <br />can more readily be assessed. These sites can be monitored to evaluate sedimentation, rates of filling and/or <br />draining, and temperature. These parameters need to be evaluated in relation to biological concerns and how <br />they relate to endangered fish species. <br />59 <br />