<?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:contributor>Scott A. Olson</dc:contributor>
  <dc:creator>Joseph D. Ayotte</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>&lt;p&gt;This report provides the results of a detailed Level II analysis of scour potential at structure 
BRIDTH00650057 on Town Highway 65 crossing Broad Brook, Bridgewater, 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). A Level I study is included in Appendix E of this report. A Level I study provides 
a qualitative geomorphic characterization of the study site. Information on the bridge, 
available from VTAOT files, was compiled prior to conducting Level I and Level II 
analyses and can be found in Appendix D.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The site is in the Green Mountain physiographic province of central Vermont in the town of 
Bridgewater. The 26.9-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 US left bank is forested; DS left bank is shrub and 
brushland; US right bank is lawn and the DS right bank has very little vegetation and is 
largely coincident with the Ottauquechee River.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, Broad Brook has an incised channel with a slope of approximately 0.0067 
ft/ft, an average channel top width of 60 ft and an average channel depth of 3 ft. The 
predominant channel bed material is gravel (D&lt;sub&gt;50&lt;/sub&gt; is 46.2 mm or 0.151 ft). The geomorphic 
assessment at the time of the Level I and Level II site visit on October 25, 1994, indicated 
that the reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 65 crossing of Broad Brook is a 47-ft-long, one-lane bridge consisting 
of one 44-ft steel-beam span with a timber deck, supported by vertical concrete abutments 
with wingwalls on the upstream and downstream sides (Vermont Agency of Transportation, 
written commun., August, 1994). The US right wingwall and road approach is protected by 
stone fill. The US and DS right wingwalls and the right abutment are reported as having 1.0 
to 1.5 ft of scour at the time of the Level one assessment on 10/25/94. Erosion from road 
wash affects all road approach embankments. Broad Brook flows into the Ottauquechee 
River approximately 30 ft downstream of the bridge. The channel approach to the bridge is 
straight with the bridge skewed 20 degrees to flow and the opening skew-to-roadway is 0 
degrees. 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 rock rip-rap sizes were computed using the general guidelines described 
in Hydraulic Engineering Circular 18 (Richardson and others, 1993).
Total scour at a highway crossing is comprised of three components: 1) long-term 
aggradation or degradation; 2) contraction scour (due to reduction in flow area caused by 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 scour depths 
for contraction and local scour and a summary of the results follows.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;Contraction scour for all modelled flows ranged from 0.4 ft to 1.5 ft and the worst-case 
contraction scour occurred at the incipient overtopping discharge. Abutment scour ranged 
from 6.0 ft to 14.6 ft and the worst-case abutment scour occurred at the 100-year discharge. 
Scour depths and depths to armoring are summarized on p. 14 in the section titled “Scour 
Results”. Scour elevations, based on the calculated depths are presented in tables 1 and 2; 
a graph of the scour elevations 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;For all scour presented in this report, “the scour depths adopted [by VTAOT] may differ 
from the equation values based on engineering judgement” (Richardson and others, 1993, p. 
21, 27). It is generally accepted that the Froehlich equation (abutment scour) gives 
“excessively conservative estimates of scour depths” (Richardson and others, 1993, p. 48). 
Many factors, including historical performance during flood events, the geomorphic 
assessment, and the results of the hydraulic analyses, must be considered to properly assess 
the validity of abutment scour results.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr96232</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 57 (BRIDTH00650057) on Town Highway 65, crossing Broad Brook, Bridgewater, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>