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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>Ronda L. Burns</dc:contributor>
  <dc:creator>Scott A. Olson</dc:creator>
  <dc:date>1997</dc:date>
  <dc:description>&lt;p&gt;This report provides the results of a detailed Level II analysis of scour potential at structure 
BENNUS00070010 on U.S. Route 7, also known as North Street, crossing of the 
Walloomsac River, Bennington, 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.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The site is in the Green Mountain section of the New England physiographic province in 
southwestern Vermont. The 30.1-mi&lt;sup&gt;2&lt;/sup&gt;
 drainage area is a predominantly rural and forested 
basin. The bridge site is located within an urban setting in the Town of Bennington with 
buildings, parking lots, lawns, and a playground on the overbank areas.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, the Walloomsac River has a straight channel with constructed channel 
banks through much of the reach. The channel is located on a delta and has a slope of 
approximately 0.02 ft/ft, an average channel top width of 37 ft and an average bank height 
of 5 ft. The predominant channel bed material is cobble with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 
96.0 mm (0.315 ft). The geomorphic assessment at the time of the Level I and Level II site 
visit on August 5, 1996, indicated that the constructed reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The U.S. Route 7 crossing of the Walloomsac River is a 53-ft-long, two-lane bridge 
consisting of one 50-foot steel span (Vermont Agency of Transportation, written 
communication, September 27, 1995). The bridge is supported by vertical, concrete 
abutments with wingwalls. The wingwalls are angled in toward the channel because the 
widths of the upstream and downstream constructed channel banks are narrower than the 
bridge opening. The channel is skewed approximately 5 degrees to the opening and the 
opening-skew-to-roadway is 10 degrees. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;Scour countermeasures at the site include masonry and stone walls on both the upstream 
and downstream banks. Additional details describing conditions at the site are included in 
the Level II Summary and Appendices D and E.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;Scour depths and recommended 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.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;Contraction scour computed for all modelled flows ranged from 0.0 to 0.1 ft. The worstcase contraction scour occurred at the 500-year discharge. Computed left abutment scour 
ranged from 5.9 to 6.8 ft. with the worst-case scour occurring at the 500-year discharge. 
Computed right abutment scour for all modelled flows was 6.8 ft. Total scour depths for all 
modelled flows did not exceed the depth of the abutment footings. 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.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;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.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr97580</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 10 (BENNUS00070010) on U.S. Route 7, crossing the Walloomsac River, Bennington, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>