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FLOOD04719
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Last modified
1/25/2010 6:47:03 PM
Creation date
10/5/2006 12:54:56 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Community
Harrison County, Iowa
Stream Name
Missouri River Miles 651-64905
Basin
Statewide
Title
California Bend Habitat Restoration/Preservation Project Volume 2
Date
10/1/1994
Prepared For
US Army Corps of Engineers
Prepared By
Greenhorne & O'Mara, Inc.
Floodplain - Doc Type
Project
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />the main channel due to the chute channel split flows was minimal. For low to moderate Missouri River flows, the <br />chute channel flows are relatively small, and therefore the split flow determination followed a slightly different <br />procedure. For each pilot channel width, the energy elevation of the Missouri River was plotted for each of the <br />four flows modeled, and then the chute channel energy curve was plotted on the same graph. The point at which <br />the two curves cross (i.e. equal energy) was used to find the corresponding chute discharge. <br /> <br />The ultimate chute channel hydraulic design followed the same split flow analysis procedure as described above. <br />The ultimate bottom width was developed by trial and error keeping in mind the constraints on chute channel <br />velocities and impacts on navigation. Assumed criteria for the chute channel specify that water surface elevations <br />in the main channel should not be decreased by more than 1. 0 foot under any flow condition. The average <br />velocities in the chute channel should be in the range of 1.0 to 5.0 feet/second, which is a rough guide for channel <br />stability purposes given the soil types found at California Bend. Through the modeling process, it was determined <br />that a 150' bottom width and 3H to IV side slopes would be a reasonable geometric design for the ultimate chute <br />channel. <br /> <br />Figure I presents a tabular summary of the split flow analysis. while Figure 2 displays chute channel discharge vs. <br />total river discharge for the 150' wide ultimate chute channel. Figure 3 shows average channel velocities along the <br />150' wide ultimate chute channel for Missouri River discharges of 31,000 and 40,000 cfs. Rating curves developed <br />for each of the split flow models are also included in this section. HEC-2 output files for the 150' wide chute <br />channel split flow runs (Q=40,000 cfs) are also included in this section. <br /> <br />As a revision to the draft DPR, the HEC-2 models for the calibration and floodplain runs were extended <br />downstream to river mile 647.4 at the request of the Corps. The computed water surfaces for the "revised" existing <br />conditions models were within 0.02 feet of the previous (draft) models. Therefore, cross-sections for the split flow <br />models for the chute analysis were not extended downstream based upon the results of the existing conditions <br />model. The split flow analysis for this report is identical to the split flow analysis in the draft report. <br /> <br />Floodplain Analysis: Impacts to the 100-year water surface elevations in the Missouri River were evaluated for <br />the proposed 10', 25', and 50' wide pilot channels using HEC-2 backwater models. The excavated pilot channels <br />for each width were modeled by adjusting the OR data in the left overbank along the proposed channel alignment. <br />In addition, the excavated material was coded into the cross-sections as a benn with a top width equaI to 2 times <br />the pilot channel bottom width, and side slopes of 2H to I V. For each case, the maximum change in water surface <br />from existing conditions was much less than 1. 0 foot. The computed water surface elevations for proposed <br />conditions upstream of the chute outlet were actually higher than the existing conditions water surfaces. This can <br />probably be attributed to the disposal berms along the pilot channels. <br /> <br />Impacts to the 100-year water surface elevations in the Missouri River were also evaluated for the proposed <br />backwater/wetland complex alternatives. Flood profile impacts would be maiuly due to the proposed backwater <br />areas at the southern and eastern portions of the site. Proposed open water areas would have a water surface <br />elevation of approximately 9%.0 feet Oow sill elevation). The areas of standing water were considered to be <br />ineffective flow areas, and the left overbank was therefore modeled with a minimum elevation of 996.0 feet. The <br />computed water surface elevations for the backwater/wetland option were easily within one foot of the existing <br />water surface elevations. Floodplain impacts from the proposed alternative water supply system were assumed to <br />be negligible. Figure 4 presents a tabular summary of the computed loo-year water surface profiles for existing <br />and proposed conditions. Figure 5 shows the same information in graphical format. HEC-2 output files for the <br />proposed 50' wide pilot channel and the backwater/sill loo-year floodplain runs are also included in this section. <br /> <br />Summary: If the flow-through chute option is selected, the recommended pilot channel is trapezoidal in geometry <br />with a 50' bottom width and 2H to I V side slopes. This geometry would require more excavation than the 10' or <br />25' pilot channels, but the smaller pilot channel widths may not enlarge rapidly enough, or possibly not at all due <br />to the lower velocities. The estimated ultimate channel would be a chute with a 150' bottom width and 3H to IV <br />side slopes. <br />
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