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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Laura Medalie</dc:contributor>
  <dc:creator>Michael A. Ivanoff</dc:creator>
  <dc:date>1997</dc:date>
  <dc:description>This report provides the results of a detailed Level II analysis of scour potential at structure 
WALDTH00450021 on Town Highway 45 crossing Joes Brook, Walden, Vermont (figures 
1–8). A Level II study is a basic engineering analysis of the site, including a quantitative 
analysis of stream stability and scour (U.S. Department of Transportation, 1993). Results of 
a Level I scour investigation also are included in Appendix E of this report. A Level I 
investigation provides a qualitative geomorphic characterization of the study site. 
Information on the bridge, gleaned from Vermont Agency of Transportation (VTAOT) 
files, was compiled prior to conducting Level I and Level II analyses and is found in 
Appendix D. The VTAOT files state that the stream is Coles Brook, both the USGS and the 
VTAOT maps state that it is Joes Brook.
The site is in the New England Upland section of the New England physiographic province 
in central Vermont. The 18.7-mi&lt;sup&gt;2&lt;/sup&gt;
 drainage area is in a predominantly rural and forested 
basin. In the vicinity of the study site, the surface cover is pasture upstream and downstream 
of the bridge while the immediate banks have dense woody vegetation. 
In the study area, Joes Brook has an incised, sinuous channel with a slope of approximately 
0.01 ft/ft, an average channel top width of 76 ft and an average bank height of 5 ft. The 
channel bed material ranges from sand to boulder with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 75.4 
mm (0.247 ft). The geomorphic assessment at the time of the Level I and Level II site visit 
on July 27, 1995, indicated that the reach was stable.
The Town Highway 45 crossing of Joes Brook is a 35-ft-long, one-lane bridge consisting of 
one 29-foot steel-beam span with a wooden deck (Vermont Agency of Transportation, 
written communication, April 5, 1995). The opening length of the structure parallel to the 
bridge face is 26.2 ft. The bridge is supported by vertical, “laid-up” concrete block 
abutments with no wingwalls. The channel is skewed approximately zero degrees to the 
opening while the computed opening-skew-to-roadway is 5 degrees.
The scour protection measures at the site included type-1 stone fill (less than 12 inches 
diameter) along the upstream left bank and along the entire base length of the left abutment. 
There is also type-2 stone fill (less than 36 inches diameter) along the entire base length of 
the right abutment. Additional details describing conditions at the site are included in the 
Level II Summary and Appendices D
and E.
Scour depths and recommended rock rip-rap sizes were computed using the general 
guidelines described in Hydraulic Engineering Circular 18 (Richardson and others, 1995) 
for the 100- and 500-year discharges. In addition, the incipient roadway-overtopping 
discharge is determined and analyzed as another potential worst-case scour scenario. Total 
scour at a highway crossing is comprised of three components: 1) long-term streambed 
degradation; 2) contraction scour (due to accelerated flow caused by a reduction in flow 
area at a bridge) and; 3) local scour (caused by accelerated flow around piers and 
abutments). Total scour is the sum of the three components. Equations are available to 
compute depths for contraction and local scour and a summary of the results of these 
computations follows.
Contraction scour for all modelled flows ranged from 0.0 to 1.5 ft. The worst-case 
contraction scour occurred at the incipient roadway-overtopping discharge, which was less 
than the 100-year discharge. Abutment scour ranged from 12.4 to 24.4 ft. The worst-case 
abutment scour occurred at the 500-year discharge. Additional information on scour depths 
and depths to armoring are included in the section titled “Scour Results”. Scouredstreambed elevations, based on the calculated scour depths, are presented in tables 1 and 2. 
A cross-section of the scour computed at the bridge is presented in figure 8. Scour depths 
were calculated assuming an infinite depth of erosive material and a homogeneous particlesize distribution. 
It is generally accepted that the Froehlich equation (abutment scour) gives “excessively 
conservative estimates of scour depths” (Richardson and others, 1995, p. 47). Usually, 
computed scour depths are evaluated in combination with other information including (but 
not limited to) historical performance during flood events, the geomorphic stability 
assessment, existing scour protection measures, and the results of the hydraulic analyses. 
Therefore, scour depths adopted by VTAOT may differ from the computed values 
documented herein.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr97799</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 21 (WALDTH00450021) on Town Highway 45, crossing Joes Brook, Walden, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>