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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:creator>Scott A. Olson</dc:creator>
  <dc:date>1997</dc:date>
  <dc:description>&lt;p&gt;This report provides the results of a detailed Level II analysis of scour potential at structure 
CHELTH00460043 on Town Highway 46 crossing Jail Brook, Chelsea, 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.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The site is in the New England Upland section of the New England physiographic province 
in central Vermont. The 4.68-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 best described as suburban with 
homes, lawns, and a few trees.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, Jail Brook has an incised, straight channel with a slope of approximately 
0.02 ft/ft, an average channel top width of 32 ft and an average bank height of 6 ft. The 
channel bed material ranges from coarse sand to boulder with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 
43.0 mm (0.141 ft). The geomorphic assessment at the time of the Level I and Level II site 
visit on November 18, 1994, indicated that the reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 46 crossing of Jail Brook is a 27-ft-long, two-lane bridge consisting of 
one 23-foot concrete span (Vermont Agency of Transportation, written communication, 
August 25, 1994). The opening length of the structure parallel to the bridge face is 22.8 
ft.The bridge is supported by vertical, concrete abutments with wingwalls. The channel is 
skewed approximately zero degrees to the opening and the opening-skew-to-roadway is 
also zero degrees. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;Channel scour was not observed. However, the left abutment footing was exposed one foot. 
Scour countermeasures at the site consisted of type-2 stone fill (less than 36 inches 
diameter) on the banks and road embankments upstream and downstream of the bridge. 
Additional details describing conditions at the site are included in the Level II Summary 
and Appendices D and E.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;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.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;Contraction scour for all modelled flows ranged from 1.1 to 1.2 ft. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 5.0 to 
6.5 ft at the left abutment and 4.7 to 6.2 ft at the right abutment. The worst-case abutment 
scour 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. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;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.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr97386</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 43 (CHELTH00460043) on Town Highway 46, crossing Jail Brook, Chelsea, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>