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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>Laura Medalie</dc:contributor>
  <dc:creator>Michael A. Ivanoff</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 
TROYTH00290015 on Town Highway 29 crossing Beetle Brook, Troy, 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 8.97-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 forest except for the downstream 
right bank which is grass.
In the study area, Beetle Brook has an incised, sinuous channel with a slope of 
approximately 0.02 ft/ft, an average channel top width of 41 ft and an average bank height 
of 4 ft. The channel bed material ranges from gravel to boulder with a median grain size 
(D&lt;sub&gt;50&lt;/sub&gt;) of 118 mm (0.387 ft). The geomorphic assessment at the time of the Level I and Level 
II site visit on June 7, 1995, indicated that the reach was stable.
The Town Highway 29 crossing of Beetle Brook is a 30-ft-long, one-lane bridge consisting 
of one 25-foot steel-beam span (Vermont Agency of Transportation, written 
communication, March 7, 1994). The opening length of the structure parallel to the bridge 
face is 23.4 ft. The bridge is supported by vertical, concrete abutments with wingwalls. The 
channel is skewed approximately 15 degrees to the opening while the opening-skew-toroadway is 0 degrees.
A scour hole 0.5 ft deeper than the mean thalweg depth was observed along the right 
abutment during the Level I assessment. Scour counter measures at the site include type-3 
stone fill (less than 48 inches diameter) at the downstream end of the downstream right 
wingwall, type-2 stone fill (less than 36 inches diameter) along the downstream left 
wingwall and the upstream left road embankment, and type-1 stone fill (less than 12 inches 
diameter) at the upstream right road embankment. 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 0.0 to 0.6 ft. The worst-case 
contraction scour occurred at the incipient-overtopping discharge. Left abutment scour 
ranged from 8.0 to 8.9 ft. The worst-case left abutment scour occurred at the 500-year 
discharge. Right abutment scour ranged from 15.4 to 16.5 ft. The worst-case right abutment 
scour occurred at the incipient-overtopping discharge. Additional information on scour 
depths and depths to armoring are included in the section titled “Scour Results”. Scouredstreambed 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 particlesize 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/ofr97408</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 15 (TROYTH00290015) on Town Highway 29, crossing Beetle Brook, Troy, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>