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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>Michael A. Ivanoff</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 
CAMBTH00460028 on Town Highway 46 crossing the Seymour River, Cambridge, 
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 Green Mountain section of the New England physiographic province in 
northwestern Vermont. The 9.94-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 while the immediate 
banks have dense woody vegetation. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, the Seymour River has an incised, straight channel with a slope of 
approximately 0.02 ft/ft, an average channel top width of 81 ft and an average bank height 
of 5 ft. The channel bed material ranges from gravel to boulder with a median grain size 
(D&lt;sub&gt;50&lt;/sub&gt;) of 62.0 mm (0.204 ft). The geomorphic assessment at the time of the Level I and 
Level II site visit on July 11, 1995, indicated that the reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 46 crossing of the Seymour River is a 38-ft-long, one-lane bridge 
consisting of one 33-foot steel-beam span (Vermont Agency of Transportation, written 
communication, March 8, 1995). The opening length of the structure parallel to the bridge 
face is 30.6 ft.The bridge is supported by vertical, concrete abutments with wingwalls. The 
channel is skewed approximately 5 degrees to the opening while the measured opening-skew-to-roadway is 10 degrees.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;A scour hole 0.2 ft deeper than the mean thalweg depth was observed along the upstream 
right wingwall and right abutment during the Level I assessment. The only scour protection 
measure at the site was type-1 stone fill (less than 12 inches diameter) along the upstream 
left road embankment. 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) 
for the 100- and 500-year discharges. In addition, the incipient roadway-overtopping 
discharge is determined and analyzed as another potential worst-case scour scenario. 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 0.0 to 0.8 ft. The worst-case 
contraction scour occurred at the incipient roadway-overtopping discharge. Left abutment 
scour ranged from 4.2 to 4.9 ft. The worst-case left abutment scour occurred at the 500-year 
discharge. Right abutment scour ranged from 8.8 to 9.7 ft. The worst-case right abutment 
scour occurred at the incipient roadway-overtopping 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/ofr97648</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 28 (CAMBTH00460028) on Town Highway 46, crossing the Seymour River, Cambridge, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>