My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
1997-03-19_REPORT - M1981302
DRMS
>
Day Forward
>
Report
>
Minerals
>
M1981302
>
1997-03-19_REPORT - M1981302
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
9/9/2022 3:19:17 PM
Creation date
11/26/2007 11:58:50 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1981302
IBM Index Class Name
Report
Doc Date
3/19/1997
Doc Name
INITIAL RECONNAISSANCE OF DRAINAGE NETWORK AND SOUTH BOULDER CREEKS HYDROLGOY HWY 36 TO APPROXIMATEL
From
TAGGART ENGINEERING ASSOC INC
To
URBAN DRAINAGE AND FLOOD CONTROL DISTRICT
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
93
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).
View images
View plain text
1 <br /> ' SECTION IV <br /> INITIAL HYDROLOGY MODELING OF THE WEST OVERFLOW AREA <br /> OF SOUTH BOULDER CREEK BELOW HIGHWAY 36 <br /> INTRODUCTION <br /> ' The Corps' SWMM model was adapted to model the West Valley Overflow by <br /> replacing all elements downstream of Node 44, which was estimated to be located <br /> above South Boulder Creek's confluence with Viele, and specifically assumed for <br /> present modeling purposes to be located at South Boulder Creek and Highway 36. <br /> None of the other problems observed upstream were corrected as the purpose of <br /> ' the effort was to conduct an initial reconnaissance of the general behavior of the <br /> West Valley Overflow. The Corps' rainfall was used as directed. During this <br /> portion of the investigation, comparisons with other hydrology investigations <br /> ' revealed that the Corps' rainfall was different from the other investigations. <br /> Therefore, rainfall should be investigated and corrected as part of future phases of <br /> work. <br /> ' INITIAL FLOW ESTIMATES AND METHODOLOGY <br /> Drawing 3 at the end of this report illustrates representative results of the <br /> hydrology modeling effort. The model is more complicated than the flow arrows <br /> and associated numbers indicate. For example, the flows at and across Baseline <br /> are quite complicated, with flows going under the road in a culvert, flows in both <br /> lanes traveling east, with the east storage spilling onto the roadway, with flows in <br /> ' excess of the Crossover Ditch ultimately spilling north over a two to three block <br /> area. <br /> ' The Boulder 1993 Aerial Topography (1 " = 100' scale, 2 foot contour interval, <br /> with supplementary spot elevations) was used as the base, supplemented by <br /> measurement of key hydraulic structures and limited hand level surveys to identify <br /> relative invert elevations and slopes. <br /> Typically flow splits were determined by evaluating normal depth channel capacity <br /> downstream of culverts, and then conducting culvert calculations for both inlet and <br /> outlet control. For assumed flows, upstream water surfaces and resultant splits <br /> ' were determined by assuming appropriate weir parameters. At each potential split <br /> location, a wide range of values was determined so that spills and normal <br /> conveyance pattern flows could be simulated from low to extreme flows. <br /> IV - 1 <br />
The URL can be used to link to this page
Your browser does not support the video tag.