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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>Matthew A. Weber</dc:contributor>
  <dc:creator>Ronda L. Burns</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 
ROYATH00550025 on Town Highway 55 crossing Broad Brook, Royalton, 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 New England Upland section of the New England physiographic province 
in central Vermont. The 11.6-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 on the upstream and 
downstream left overbanks and forest on the upstream and downstream right overbanks.
In the study area, Broad Brook has an incised, sinuous channel with a slope of 
approximately 0.01 ft/ft, an average channel top width of 41 ft and an average bank height 
of 5 ft. The channel bed material ranges from sand to boulder with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) 
of 58.3 mm (0.191 ft). The geomorphic assessment at the time of the Level I site visit on 
April 13, 1995 indicated that the reach was laterally unstable. The stream impacts the 
upstream left bank where there is a cut bank. 
The Town Highway 55 crossing of the Broad Brook is a 35-ft-long, two-lane bridge 
consisting of one 31-foot steel-beam span (Vermont Agency of Transportation, written 
communication, March 22, 1995). The opening length of the structure parallel to the bridge 
face is 32 ft. The bridge is supported by vertical, concrete abutments with wingwalls. The 
channel is skewed approximately 20 degrees to the opening, while the opening-skew-toroadway is zero degrees. 
A scour hole 1.0 ft deeper than the mean thalweg depth was observed along the left 
abutment and the downstream left wingwall during the Level I assessment. The scour 
countermeasure at the site was type-2 stone fill (less than 36 inches diameter) along the 
upstream and downstream left banks that extended to the ends of the wingwalls. 
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 0.6 to 1.5 ft. The worst-case 
contraction scour occurred at the incipient-overtopping discharge which was less than the 
100-year discharge. Abutment scour ranged from 3.5 to 8.9 ft. The worst-case abutment 
scour occurred at the incipient road-overtopping discharge for the left abutment and at the 
100-year discharge for the right 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 crosssection 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/ofr97422</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 25 (ROYATH00550025) on Town Highway 55, crossing Broad Brook, Royalton, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>