My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD05212
CWCB
>
Floodplain Documents
>
Backfile
>
4001-5000
>
FLOOD05212
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/25/2010 6:48:35 PM
Creation date
10/5/2006 1:20:40 AM
Metadata
Fields
Template:
Floodplain Documents
County
Larimer
Community
Fort Collins
Stream Name
Boxelder Creek, Spring Creek, Dry Creek
Basin
South Platte
Title
Flood Control for Boxelder Creek at Fort Collins
Date
2/1/1993
Prepared For
Fort Collins
Prepared By
US Army Corps of Engineers
Floodplain - Doc Type
Floodplain Report/Masterplan
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
136
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
<br />- <br /> <br />. <br /> <br />Tal>I.4.1 <br />Dry eu.k Oischarge Frequency Rrlationship <br /> <br />City of Fort Collins, and Larimer County. The efflX:ts of irrig.ation canals on peak <br />flows were also ct.arnined during the sensitivity analysis. <br /> <br />The completed model was used to develop discharge-frequency relationships at <br />specific locations along the detailed study reach from the Larimer and Weld Canal <br />to the confluence with the Poudre River for both existing and developed conditions. <br />The modeled flood peaks were not smoothed graphically due to the effects of <br />upstream diversions which create the situation where more frequent flood peaks are <br />caused by local runoff downstream of the Larimer and Weld Canal and larger less <br />frequent peaks by runoff from the entire basin. Resulting discharge frequency <br />relationships for existing and developed conditions are shown in Table 4-1. <br /> <br />Location <br /> <br />FT<'queney <br />~ <br /> <br />D/SWelctCanaJ <br /> <br />, <br />, <br />>0 <br />" <br />>0, <br />'" <br /> <br />Mouth <br /> <br />, <br />, <br />>0 <br />" <br />100 <br />'00 <br /> <br />The model for developed conditions was used to evaluate various diversion <br />altematives for protccting the detailed study reach from the Larimer and Weld Canal <br />to lheconflucnn: with the Poudre River. Diversions withca=cities for the 10- 5Q.. <br />,-' , , <br />1QCl., and 500-ycM peak flows were e....aluated at two locations: (1) at the Larimer <br />and Weld Canal and (2) just downstream of fut Vine Drive. Diversions at each <br />location were cvalualed separately and in conjunction with diversions at the other <br />location. A lotal of twelve diversion alternatives were examined. Diversions were <br />modeled with n constant flow rate once the incoming flow reached the diversion <br /> <br />cap""iiy. Fvii,w..i::;;co:n;o!~';"n of the hydrolog.ic studies. a variable diversion rating <br />curve was developed for the 30-year ilml 'lao-year diversion channels and those <br />projects were re_cvaluatcd with the HEC-l model. With the variable diversion rating <br />curve, which more aa:uratcly reflects the project operation, mor~. discharge would <br />be pass<<l down the diversion channel for events which exceed the design capadty. <br />This results in lower residual flows passing down Dry Creek. With and without <br />prujc.;( Ili:.eharf;e f~'.lenGY 1"f'1"t;on~hiF~ for the ]OO-yearand 3G-veardiversion are <br />shown in Tablc5 6-1 and 6-2. <br /> <br />. <br /> <br />4-]2 <br /> <br />4.11 <br /> <br />Peak Diocharge in d... <br />Existing <br />Condition. <br /> <br />, <br />, <br />'" <br />3110 <br />4520 <br />8910 <br /> <br />'" <br />'" <br />." <br />2170 <br />"'" <br />7M' <br /> <br />. <br /> <br />D.""lol'ed <br />Condinonl <br /> <br />, <br />, <br />700 <br />3140 <br />4550 <br />8950 <br /> <br />'00 <br />'" <br />'00 <br />"" <br />3350 <br />1160 <br /> <br />. <br />
The URL can be used to link to this page
Your browser does not support the video tag.