<?xml version='1.0' encoding='utf-8'?>
<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:creator>Michael A. Ivanoff</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>This report provides the results of a detailed Level II analysis of scour potential at structure 
POMFTH00020013 on town highway 2 crossing Barnard Brook, Pomfret, 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 study 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 can be found in 
Appendix D.
The site is in the New England Upland section of the New England physiographic province 
of east-central Vermont in the town of Pomfret. The 7.98-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 
primarily field grasses with some brush on the immediate banks.
In the study area, Barnard Brook has an incised, sinuous channel with a slope of 
approximately 0.006 ft/ft, an average channel top width of 32 ft and an average channel 
depth of 4 ft. The predominant channel bed materials are gravel and cobbles with a median 
grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 51.0 mm (0.167 ft). The geomorphic assessment at the time of the Level 
I and Level II site visit on September 15, 1994, indicated that the reach was stable.
The town highway 2 crossing of Barnard Brook is a 23-ft-long, two-lane bridge consisting 
of one 20-foot concrete span (Vermont Agency of Transportation, written communication, 
August 22, 1994). The bridge is supported by vertical, concrete abutments with wingwalls. 
The channel is skewed approximately 30 degrees to the opening while the opening-skew-toroadway is 0 degrees. 
Scour, 2.5 ft deeper than the mean thalweg depth, was observed along the left abutment 
during the Level I assessment. The only scour protection measure at the site was type-2 
stone fill (less than 36 inches diameter) along the base and upstream of the upstream left 
wingwall. Additional details describing conditions at the site are included in the Level II 
Summary and Appendices D and E.
Scour depths and rock rip-rap sizes were computed using the general guidelines described 
in Hydraulic Engineering Circular 18 (Richardson and others, 1995). 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 100-year discharge. Abutment scour ranged from 7.2 to 
12.6 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”. Scoured-streambed 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 particle-size 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/ofr96583</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 13 (POMFTH00020013) on Town Highway 2, crossing Barnard Brook, Pomfret, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>