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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:creator>Ronda L. Burns</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 
HUNTTH00220032 on Town Highway 22 crossing Brush Brook, Huntington, 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 
central Vermont. The 5.7-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 forest except on the downstream right 
overbank which is pasture. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, Brush Brook has an incised, straight channel with a slope of 
approximately 0.05 ft/ft, an average channel top width of 58 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 127 mm (0.416 ft). The geomorphic assessment at the time of the Level I and Level 
II site visit on June 25, 1996, indicated that the reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 22 crossing of Brush Brook is a 36-ft-long, one-lane bridge consisting 
of one 34-foot steel-beam span and a timber deck (Vermont Agency of Transportation, 
written communication, December 12, 1995). The opening length of the structure parallel to 
the bridge face is 35.7 ft. The bridge is supported by vertical, concrete abutments with 
wingwalls on the left. The channel is skewed approximately 50 degrees to the opening 
while the measured opening-skew-to-roadway is 15 degrees. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;A scour hole 1.0 ft deeper than the mean thalweg depth was observed along the left 
abutment and downstream left wingwall 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 
upstream right bank. 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 0.0 to 0.2 ft. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 6.4 to 
10.2 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. &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/ofr97651</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 32 (HUNTTH00220032) on Town Highway 22, crossing Brush Brook, Huntington, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>