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FLOOD06381
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Last modified
1/25/2010 7:08:50 PM
Creation date
10/5/2006 2:13:26 AM
Metadata
Fields
Template:
Floodplain Documents
County
Otero
Community
La Junta
Stream Name
Arkansas River & Tributaries
Basin
Arkansas
Title
La Junta, Colorado Local Protection Project Phase I GDM Sediment Investigation
Date
9/1/1985
Prepared For
US Army Corps of Engineers
Prepared By
The Hydrologic Engineering Center
Floodplain - Doc Type
Project
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<br />Project #4 conditions indicated rates of deposition of 3.2, 9.7 and 31. 5 <br />ft/day for the 50-year, 100-year and standard project flood respectively: <br />roughly twice the values for project #3. Although actual depths of scour or <br />deposition for single flood events cannot be predicted with certainty, the <br />above analysis indicates that the project #4 levee configuration has greater <br />potential for deposition. <br /> <br />A reach of scour (near river mile 1198.9) was also analyzed. The hand <br />computations showed the following scour rates for existing conditions: 0.1, <br />Q.l, and 0.3 ft/day corresponding to 50-year, 100-year and standard project <br />flood. Project #3 conditions indicated scour rates of 1.9, 3.4 and 14.1 <br />ft/day. Project #4 conditions indicated rates of scour of 4.9, 9 ~l and 31.3 <br />ft/day. From this analysis it can be seen that the project #4 levee <br />configuration has greater potential for scour than the project #3 levees. The <br />analysis also showed that significantly more local scour and deposition may <br />occur under project conditions as compared to existing conditions. <br /> <br />The rates of scour and deposition calculated above are based on the <br />conditions at peak flow, which exist for only a few hours. As the bed adjusts <br />and hydraulic conditions change, scour and deposition will occur at different <br />rates. To estimate a depth of deposit/scour, the rate is multiplied by the <br />duration of the peak flow. This approach will give an upper bound for the <br />actual expected depths of deposit/scour. <br /> <br />5.6 Intet'Pretation of simulation Results and Conclusions <br /> <br />The channel response due to a single flood event is affected by many <br />factors. Some of these factors (such as sediment inflow from local drainage <br />and changes in watershed conditions) were not incorporated in the above <br />analysis. For this reason, the simulated results should be interpreted as <br />showing general trends of aggradation and degradation in the main river <br />channel. The actual magnitudes of bed changes in the results should be <br />considered as approximate values for the general scour or depositional trends <br />the river may have for these kinds of single events. <br /> <br />Appendix F presents plotted results of channel deposition vs. time at each <br />cross section for existing, project #3 and project #4 conditions. Examination <br />of these results shows that at many locations within the project reach, both <br />project #3 and project #4 conditions caused channel scouring to occur where <br />little or no scour had occurred under present natural conditions. In addition <br />to increased scouring within the project reach, greater depths of deposit occur <br />just downstream from the project for both project #3 and #4 conditions, <br />compared to existing conditions. <br /> <br />Conclusions reached from analyzing the simulation results are highlighted <br />below: <br /> <br />. The river bed appeared to be fairly stable for existing conditions. <br /> <br />, Both project conditions (project #3 and project #4) indicated <br />significant scour in the project reach between cross sections ll96.9 <br />and 1198.9. The levee configuration for project #4 resulted in more <br />scour upstream from the project. The maximum water depth for the SPF <br />was about three feet greater for project #4 conditions than for <br />project #3 conditions. This is because the levees are closer together <br />for proj ect #4. <br /> <br />61 <br />
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