My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD08394
CWCB
>
Floodplain Documents
>
Backfile
>
7001-8000
>
FLOOD08394
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/25/2010 7:14:26 PM
Creation date
10/5/2006 3:35:36 AM
Metadata
Fields
Template:
Floodplain Documents
County
Pueblo
Community
Pueblo
Stream Name
Fountain Creek
Basin
Arkansas
Title
Fountain Dam and Reservoir Design Memorandum Number 1: Hydrology, Part 1
Date
2/9/1978
Prepared For
Pueblo
Prepared By
MSM Consultants, Inc.
Floodplain - Doc Type
Project
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
56
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 />curves were developed by adjusting the curve at Nepest8 hy the ratin <br />of their respective standard project floods to the Srl' at Nepl'stn. <br />The Nepesta site was chosen because of its central location in thin <br />reach of the Arkansas River. This procedure yielded consistent re- <br />sults of flows in the Arkansas River from Pueblo to Las Animas. <br />Also, a reasonable relationship between floods of designated fre- <br />quency and the standard project flood was maintained throughout the <br />study reach. <br /> <br />. <br /> <br />. <br /> <br />DEVELOPMENT OF DESIGN FLOODS <br /> <br />30. FLOOD ROUTING CRITERIA. Flood routings were required for <br />development of the standard project flood at several locations alonr, <br />the Arkansas River. Routings were performed by the Modified PuIs <br />method. Storage-outflow curves at selected cross sections from <br />Fountain Creek to the St. Charles River were developed by HEC-2 <br />backwater computations. Cross section data for this reach were.ob- <br />tained from digitized sections from 2-foot contour interval mappinr. <br />Storage-outflow curves for the reach from the St. Charles River to <br />Las Animas were obtained from normal denth computations at selected <br />cross sections. These sections were developed from field surveys <br />and 7-l/2-minute USGS quadrangle maps. The HEC-I computer program <br />was utilized for these flood routings. The HEC-I model was cali- <br />brated for the .reach from Pueblo to below Chico Creek. Flood hydro- <br />graph data were not available for the reach to Las Animas. Plates <br />10 and 11 show two 1921 flood hydrographs that were reproduced by <br />the HEC-l model. The reproduced peaks are ahout 10 percent low <br />which is probably due to unrecorded tributary inflows missinr. from <br />the model. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />31. UNIT HYIlROGRAPIIS. Unit hydrorraphs were developed by syn- <br />thetic methods because of lack of rainfall-discharge data to sub- <br />stantiate natural unit hydrographs. The synthetic unit hydrorraphs <br />were determined by use of the following two formulas: ' <br /> <br />. <br /> <br />qp a 12,650 (Sst+ 0.00109)1.08 <br /> <br /> <br />" . 0.074 ['~:~.)0.3J 0.669 <br /> <br />u <br />II <br /> <br />. <br /> <br />. <br /> <br />These formulas were developed by regression analyses during the <br />studies of the Purgatoire River at Trinidad, Colorado. The results <br />of those regression analyses are presented as Plates 12 and 13. <br />Plotted on these plates are qp and tp for Willow Creek above Heron <br />Reservoir, near Park View, New Mexico. Values of qp and tp for <br /> <br />.. <br /> <br />12 <br /> <br />. <br />
The URL can be used to link to this page
Your browser does not support the video tag.