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FLOOD04543
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Last modified
1/25/2010 6:46:33 PM
Creation date
10/5/2006 12:44:04 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Community
Harrison County, Iowa
Basin
Statewide
Title
California Bend Missouri River Fish and Wildlife Mitigation
Date
11/1/1994
Prepared For
US Army Corps of Engineers
Prepared By
Greenhorne & O'Mara, Inc.
Floodplain - Doc Type
Data (general)
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<br />I <br />I <br /> , <br /> ., <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 />____ ___n_ <br /> <br />KISSOURI RIVER KITIGATIOR <br />CALIFORIUA BElID PROJECT <br /> <br />RESPONSE TO DRAFT DPR COKKENTS <br /> <br />Response to numbered comments 32 through 43 <br /> <br />32. The HEC-2 models will be extended downstream by approximately 1 mile using <br />government provided cross-section information as requested. <br /> <br />33. HEC-2 models for the floodplain analyses were calibrated to 100-year water <br />surface elevations shown on the government provided floodplain maps. The <br />CRP could not be reproduced using the existing conditions model calibrated <br />to lOO-year water surface profiles. However, the CRP was closely reproduced <br />throughout the reach by adjusting the starting energy slope. <br /> <br />Original calibration of the models was based on information and direction <br />provided to us by the Corps. Some high water mark information was later <br />transmitted to our office just prior to completion of the draft DPR. The <br />HEC-2 model calibrations, split-flow analyses, and floodplain analyses were <br />already completed based upon the information originally provided. <br />Recalibrating the models based on new information would constitute a change <br />in scope. <br /> <br />34. The chute outlet elevation was set slightly more than 5 feet below the CRP <br />so that the chute channel slope would be similar to the average river slope. <br />The chute channel has a slightly longer flow path due to the fact that it is <br />on the outside of the bend. During lower flows, the chute channel flow is <br />hydraulically disconnected from the main channel. The intent of the chute <br />channel slope was to help prevent excessive sediment deposition. <br /> <br />35. See previous comments for Number 32. <br /> <br />36. The conveyance change may cause some problems in the model. however the <br />means for modeling the chute channel should produce reasonable results. <br /> <br />37. The energy grade in the Missouri River decreases very slightly for flows <br />taken out for the chute. The HEC-2 split flow models did account for <br />discharge lost to the chute channel, and flow was reduced in the main <br />channel between the chute inlet and outlet. This is hard to distinguish on <br />the graph since the energy grade is so flat. <br /> <br />38. The EM-1110-2-1601 manual was provided to our office for use on this <br />contract. We were unaware of any updated version. <br /> <br />39. The riprap size will be checked and documented based upon your recommendation. <br /> <br />40. The rip rap size was based on the manual provided to us for use on this <br />contract. <br /> <br />41. The frequency ml.Xl.ng information was originally developed by the Corps of <br />Engineers as a general guideline. The Texas Department of Highways reprinted <br />the information developed by the Corps. In essence. this is the Corps <br />procedure. <br />
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