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Last modified
11/23/2009 1:02:55 PM
Creation date
10/4/2006 9:51:31 PM
Metadata
Fields
Template:
Floodplain Documents
County
Pueblo
Community
Pueblo
Stream Name
Fountain Creek
Title
Pueblo Flood Control Project
Date
1/1/1990
Prepared For
Pueblo County
Prepared By
US Army Corps of Engineers
Floodplain - Doc Type
Project
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<br />. <br /> <br />. <br /> <br />:. <br />I <br />-''; <br /> <br />of the General Design Conference held 7 December 1983 prompted several design <br />changes from the plan presented in the Phase I Report. <br /> <br />3-10. Hvdraulic Design-Procedural Summarv. A channel baseline was set and <br />appropriate bridge data coded and inserted into the cross section data to, form <br />the basic HEC-2 model. Encroachment stations were added to the model to <br />simulate the location of the levees proposed in the Phase I study. Numerous <br />trials involving excavation and levee alternatives to finalize the Phase II <br />design are discussed in subsequent paragraphs. <br /> <br />3-11. Hvdraulic Losses. Mannings' roughness factors used in this study were <br />the same as used in the Phase I report. Left overbank values ranged from 0.08 <br />to 0.10; right overbank values ranged from 0.05 to 0.06. Channel values from <br />0.03 to 0.035. After a site visit to Pueblo, it was found that these values <br />Were a little high. Additional HEC-2 backwater runs were made using a maximum <br />n value of 0.07 in the overbanks and 0.03 in the channel. The sensitivity of <br />stage and velocity to the roughness factors proved negligible, with water <br />surface elevations decreasing an average of only 0.03 feet. Contraction and <br />expansion coefficients used between cross sections On Fountain Creek were 0.1 <br />and 0.3, respectively, which apply to gradual transitions. Bridge sections <br />used contraction and expansion coefficients of 0.3 and 0.5, respectively. <br />Because changes in the direction of flow are more abrupt at the confluence <br />withfhe Arkansas River, values of 0.3 and 0.6 were used for the cross <br />sections at the Highway 227 bridge. <br /> <br />3-12. Standard Pro;ect Flood. Pre-Pro;ect Conditions. Since the proposed <br />channel improvement provides less than SPF protection, the consequences of <br />flows exceeding the channel capacity, up to and including the SPF, were <br />investigated. The standard project flood is 152,000 cfs for Fountain Creek at <br />Pueblo. The existing condition analysis indicated that 44,000 cfs split from <br />the main flow around 13th Street and headed through downtown Pueblo. The <br />split flow traveled through the downtown area to the Arkansas River, where it <br />joined with a coincidental flow of 8,000 cfs a short distance above the mouth <br />of Fountain Creek. <br /> <br />3-13. Standard Pro;ect Flood. Post-Pro;ect Conditions. The proposed project <br />greatly reduces flooding from the SPF. A "worst case" scenario was ana lyzed <br />in which levees broke above the 8th Street and Atchison Topeka and Santa Fe <br />(ATSF) bridges. Flow broke out of the channel at 13th Street where 1700 cfs <br />went under 1-25 to the west. The east levee above the 8th Street broke for a <br />distance of 500 feet downstream from its start. A flow of 10,000 cis went <br />into the east overbank from this break. Immediately above 8th Street bridge <br />the earthen levee On the west side broke and sent 14,500 cfs to the west. The <br />soil-cement levee On the east side was overtopped and experienced failure of <br />the parapet wall. A flow of 6500 cfs joined the 10,000 cfs already on the <br />east side. About 1,800 feet upstream of the AT&SF bridge the east levee was <br />overtopped and partially eroded, sending 6500 cfs into the east overbank. <br />Immediately above the AT&SF bridge the east levee broke for a distance of 100 <br />feet sending 2,800 cfs to the east. In the area of the Missouri Pacific <br />Railroad (MPRR) bridge, flow overtopped the tracks running parallel to the <br />creek on the west bank. The 16,200 cfs which split off to the west flowed <br />through the downtown area and on down to the Arkansas River just above the <br />mouth of Fountain Creek. The 25,800 cfs which split off to the east stayed <br />between the levee and high ground to the east. This flow ran parallel to the <br /> <br />III-3 <br />
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