<?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>Robert E. Hammond</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 
POMFTH00010017 on Town Highway 1 crossing Mill Brook, Pomfret, 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 
central Vermont. The 8.11-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 pasture.
In the study area, Mill Brook has a sinuous channel with a slope of approximately 0.009 ft/
ft, an average channel top width of 30 ft and an average channel depth of 3 ft. The 
predominant channel bed materials are gravel and cobbles with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 
71.9 mm (0.236 ft). The geomorphic assessment at the time of the Level I and Level II site 
visit on July 25, 1996, indicated that the reach was stable.
The Town Highway 1 crossing of Mill Brook is a 54-ft-long, two-lane bridge consisting of 
one 52-foot steel-beam span (Vermont Agency of Transportation, written communication, 
August 23, 1994). The bridge is supported by vertical, concrete abutments with spillthrough embankments. The channel is skewed approximately 15 degrees to the opening and 
the opening-skew-to-roadway is 15 degrees. 
The scour protection measures at the site were type-3 stone riprap (less than 48 inches 
diameter) on the spill-through embankments of each abutment and type-2 stone fill (less 
than 24 inches diameter) on the banks downstream. Additional details describing conditions 
at the site are included in the Level II Summary and Appendices D and E.
Scour depths and 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 0.0 to 0.9 ft. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 3.6 to 
7.1 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. 
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/ofr972</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 17 (POMFTH00010017) on Town Highway 1 (FAS 166) crossing Mill Brook, Pomfret, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>