<?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>James R. Degnan</dc:contributor>
  <dc:creator>Erick M. Boehmler</dc:creator>
  <dc:date>1997</dc:date>
  <dc:description>This report provides the results of a detailed Level II analysis of scour potential at structure 
MORRTH00060005 on Town Highway 6 crossing Bedell Brook, Morristown, 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.
The site is in the Green Mountain section of the New England physiographic province in 
north-central Vermont. The 6.28-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 consists of pasture, shrubs, and 
brushland. 
In the study area, Bedell Brook has a sinuous channel with a slope of approximately 0.01 ft/
ft, an average channel top width of 56 ft and an average bank height of 4 ft. The 
predominant channel bed material is gravel with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 35.8 mm 
(0.117 ft). The geomorphic assessment at the time of the Level I and Level II site visit on 
July 16, 1996, indicated that the reach was laterally unstable. There are wide point bars and 
cut-banks with slipping bank material noted upstream and downstream of this site.
The Town Highway 6 crossing of Bedell Brook is a 44-ft-long, two-lane bridge consisting 
of one 42-foot concrete T-beam span (Vermont Agency of Transportation, written 
communication, October 26, 1995). The bridge is supported by vertical, concrete abutments 
with wingwalls. The channel is skewed approximately 45 degrees to the opening while the 
opening-skew-to-roadway is zero degrees. 
A scour hole up to 1.5 ft deeper than the mean thalweg depth was observed along the left 
abutment and upstream and downstream left wingwalls during the Level I assessment. The 
scour protection measure at this site was type-4 stone fill (less than 60 inches diameter) on 
the left bank and left wingwall upstream, the left abutment and the downstream left 
wingwall. Additional details describing conditions at the site are included in the Level II 
Summary and Appendices D and E.
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.
Contraction scour for all modelled flows ranged from 1.1 to 2.0 feet. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 3.9 to 
8.6 feet. The worst-case abutment scour occurred at the 500-year event. 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. 
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.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr97793</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 5 (MORRTH00060005) on Town Highway 6, crossing Bedell Brook, Morristown, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>