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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>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 
STAMVT01000002 on State Route 100 crossing Roaring Brook, Stamford, 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 
Southwestern Vermont. The 8.26-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 houses with grass lawns, 
and trees on the right overbank areas upstream and downstream of the bridge. The left 
overbank areas upstream and downstream of the bridge are covered with trees and brush.
In the study area, Roaring Brook has a straight channel with a slope of approximately 0.02 
ft/ft, an average channel top width of 56 ft and an average bank height of 5 ft. The channel 
bed materials range from gravel to boulders with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 53.7 mm 
(0.176 ft). The geomorphic assessment at the time of the Level I and Level II site visit on 
July 31, 1996, indicated that the reach was aggraded.
The State Route 100 crossing of Roaring Brook is a 44-ft-long, two-lane bridge consisting 
of one 42-foot steel-beam span (Vermont Agency of Transportation, written 
communication, September 28, 1995). The bridge is supported by vertical, concrete 
abutments with wingwalls. The channel is skewed approximately 5 degrees to the opening 
and the opening-skew-to-roadway is 5 degrees. 
Scour protection measures at the site were type-2 stone fill (less than 36 inches diameter) on 
the upstream banks and wingwalls, type-3 (less than 48 inches diameter) on the downstream 
wingwalls, and artificial levees made from a variety of materials on the downstream banks. 
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 0.8 feet. The worst-case 
contraction scour occurred at the 100-year discharge. Abutment scour ranged from 4.2 to 
9.3 feet. The worst-case abutment scour occurred at the 500-year discharge at the left 
abutment. 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/ofr97211</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 2 (STAMVT01000002) on State Route 100 crossing Roaring Brook, Stamford, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>