My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
Pagosa Springs San Juan/Delores River Div 7 Response Letter
CWCB
>
Water Supply Protection
>
DayForward
>
7001-8000
>
Pagosa Springs San Juan/Delores River Div 7 Response Letter
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
11/6/2014 12:00:03 PM
Creation date
10/27/2014 11:54:50 AM
Metadata
Fields
Template:
Water Supply Protection
Description
Dave Rosgen respone letter on the San Juan River in Pagosa Springs, CO
State
CO
Basin
San Juan/Dolores
Water Division
7
Date
1/1/2007
Author
Dave Rosgen
Title
Pagosa Springs WWP, San Juan/Delores Division 7 Dave Rosgen's response letter
Water Supply Pro - Doc Type
Correspondence
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
46
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
diversions. The flatter and smaller vane angle arm will extend farther upstream to intercept <br /> proportionately more water and increase the length of bank protected. <br /> Vane slope. The slope of the vane extending from the bankfull stage bank should vary between <br /> 2-7 percent. Vane slope is defined by the ratio of bank height/vane length. For installation in <br /> meander bends,ratios of J-Hook Vane length/bankfull width is calculated as a function of the <br /> ratio of radius of curvature/bankfull width and departure angle (Table 1). Equations for <br /> predicting ratios of J-Hook Vane spacing/bankfull width on meander bends based on ratio of <br /> radius of curvature/bankfull width and departure angle is shown in Table 2. Vane length is the <br /> distance measured from the bankfull bank to the intercept with the invert elevation of the <br /> streambed at 1/3 of the bankfull channel width for either Cross-Vanes or J-Hook Vanes. For <br /> very large rivers,where it is impractical to extend the vane length to 1/3 of the bankfull width, <br /> vane slope is calculated based on the specified angle of departure and the ratio of bank <br /> height/vane length where the vane arm intercepts the proposed invert of the structure. <br /> Table 1. Equations for predicting ratio of vane length/bankfull width (VI) as a function of ratio <br /> of radius of curvature/width and departure angle, where W=bankfull width. (SI units) <br /> Rc/W Departure Angle (degrees) Equation <br /> 3 20 VL=0.0057 W+0.9462 <br /> 3 30 VL=0.0089 W+0.5933 <br /> 5 20 VL =0.0057 W+ 1.0462 <br /> 5 30 VL=0.0057 W+0.8462 <br /> Table 2. Equations for predicting ratio of vane spacing/width (Vs) as a function of ratio of <br /> radius of curvature/width and departure angle, where W= bankfull width (SI units) <br /> Rc/W Departure angle (degrees) Equation <br /> 3 20 Vs= -0.006 W+2.4781 <br /> 3 30 Vs=-0.0114 W+ 1.9077 <br /> 5 20 Vs=-0.0057 W+2.5538 <br /> 5 30 Vs=-0.0089 W+2.2067 <br /> The spacing of.T-Hook Vanes can be increased by 0.40W if there exists a low bank erosion <br /> hazard rating(BEHI)of less than 30(Rosgen, 1996, 2001). <br /> Bank height. The structure should only extend to the bankfull stage elevation. If the bank is <br /> higher, a bankfull bench is constructed adjacent to the higher bank and the structure is integrated <br /> into the bench. The use of a Cross-Vane is shown in Figure 8 where a bankfull bench is created <br /> adjacent to a terrace bank. <br /> Footers. The minimum footer depth at the invert for cobble and gravel bed streams is associated <br /> with a ratio of 3 times the protrusion height of the invert rock. This is applicable to all three <br /> structures and is shown in Figure 9 for a J-Hook Vane. For sand bed streams,the minimum <br /> depth is doubled due to the deeper scour depths that occur. All rocks for all three structures <br /> require footers. If spaces are left between the invert rocks for Cross-Vane and W Weirs, then the <br /> top of the footer rocks becomes the invert elevation for grade control. If no gaps are left,then <br /> the top of the surface rock becomes the base level of the stream. <br /> 12 <br />
The URL can be used to link to this page
Your browser does not support the video tag.