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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>Lora K. Striker</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 
MORETH00010021 on Town Highway 1 crossing Cox Brook, Moretown, 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 
north-central Vermont. The 2.85-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 predominantly forested.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, Cox Brook has an incised, sinuous channel with a slope of approximately 
0.02 ft/ft, an average channel top width of 23 ft and an average bank height of 4 ft. The 
channel bed material ranges from gravel to cobble with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 47.5 
mm (0.156 ft). The geomorphic assessment at the time of the Level I and Level II site visit 
on July 18, 1996, indicated that the reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 1 crossing of Cox Brook is a 29-ft-long, two-lane bridge consisting of 
one 27-foot steel-beam span (Vermont Agency of Transportation, written communication, 
October 13, 1995). The opening length of the structure parallel to the bridge face is 24.8 ft. 
The bridge is supported by vertical, concrete abutments with wingwalls. The channel is 
skewed approximately 60 degrees to the opening while the measured opening-skew-to-roadway is 40 degrees. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;A scour hole 1.0 ft deeper than the mean thalweg depth was observed along the left 
abutment downstream during the Level I assessment. The only scour protection measure at 
the site was type-2 stone fill (less than 36 inches diameter) along the left bank upstream. 
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-year 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 0.2 to 0.5 ft. The worst-case 
contraction scour occurred at the incipient roadway-overtopping discharge, which was less 
than the 100-year discharge. Abutment scour ranged from 2.8 to 4.0 ft. The worst-case 
abutment scour occurred at the left abutment at the 100-year discharge and at the right 
abutment 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/ofr97662</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 21 (MORETH00010021) on Town Highway 1, crossing Cox Brook, Moretown, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>