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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>James R. Degnan</dc:contributor>
  <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 
HUNTTH00220033 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 8.65-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 0.04 ft/ft, an average channel top width of 42 ft and an average bank height 
of 3 ft. The channel bed material ranges from gravel to boulder with a median grain size 
(D&lt;sub&gt;50&lt;/sub&gt;) of 76.7 mm (0.252 ft). The geomorphic assessment at the time of the Level I and 
Level II site visit on June 26, 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 40-ft-long, two-lane bridge consisting 
of one 23.5-foot concrete slab span (Vermont Agency of Transportation, written 
communication, November 30, 1995). The opening length of the structure parallel to the 
bridge face is 36.9 ft. The bridge is supported by vertical, concrete abutments with 
wingwalls. The channel is skewed approximately 35 degrees to the opening while the 
opening-skew-to-roadway is 30 degrees. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The scour protection measure at the site was type-2 stone fill (less than 36 inches diameter) 
along the left and right banks upstream that extended through the bridge and along the 
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) 
for the 100- and 500-year discharges. In addition, the incipient roadway-overtopping 
discharge is analyzed since it has the potential of being the 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.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;Contraction scour for all modelled flows ranged from 0.0 to 1.1 ft. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 6.5 to 
14.9 ft. The worst-case abutment scour occurred at the incipient roadway-overtopping 
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/ofr97664</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 33 (HUNTTH00220033) on Town Highway 22, crossing Brush Brook, Huntington, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>