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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>Erick M. Boehmler</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 
GLOVTH00410023 on Town Highway 41 crossing Sherburne Brook, Glover, 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 New England Upland section of the New England physiographic province 
in northern Vermont. The 2.57-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 forest with small areas 
of lawn and a home on the right overbank and a gravel roadway along the upstream left 
bank.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, Sherburne Brook has an incised, sinuous channel with a slope of 
approximately 0.03 ft/ft, an average channel top width of 33 ft and an average bank height 
of 6 ft. The channel bed material ranges from gravel to boulder with a median grain size 
(D&lt;sub&gt;50&lt;/sub&gt;) of 57.3 mm (0.188 ft). The geomorphic assessment at the time of the Level I and 
Level II site visit on October 24, 1994, indicated that the reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 41 crossing of Sherburne Brook is a 24-ft-long, one-lane bridge 
consisting of one 21-foot steel-beam span with a timber deck (Vermont Agency of 
Transportation, written communication, August 4, 1994). The opening length of the 
structure parallel to the bridge face is 20.3 ft. The bridge is supported by vertical, granite 
block abutments. The channel is skewed approximately 55 degrees to the opening while the 
measured opening-skew-to-roadway is 30 degrees. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;One foot of scour below the mean thalweg depth was observed along the right abutment 
undermining the abutment by 0.5 feet vertically. 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 for all modelled flows ranged from 0.4 to 0.8 ft. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 4.6 to 
7.2 ft. The worst-case abutment scour also 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. &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/ofr97388</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 23 (GLOVTH00410023) on Town Highway 41, crossing Sherburne Brook, Glover, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>