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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 
WALDTH00020007 on Town Highway 2 crossing Coles Brook, Walden, Vermont (figures 
1–8). Coles Brook is also referred to as Joes Brook. 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 north-eastern Vermont. The 12.8-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 shrub and 
brushland.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, Coles Brook has a sinuous channel with a slope of approximately 0.005 ft/
ft, an average channel top width of 37 ft and an average bank height of 4 ft. The channel bed 
material ranges from sand to cobble with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 32.9 mm (0.108 ft). 
The geomorphic assessment at the time of the Level I and Level II site visit on August 9, 
1995, indicated that the reach was laterally unstable due to cut-banks, point bars, and loose 
unconsolidated bed material.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 2 crossing of Coles Brook is a 74-ft-long, two-lane bridge consisting of 
one 71-foot steel-beam span (Vermont Agency of Transportation, written communication, 
April 5, 1995). The opening length of the structure parallel to the bridge face is 69.3 ft. The 
bridge is supported by spill-through abutments. The channel is skewed approximately 35 
degrees to the opening while the measured opening-skew-to-roadway is 15 degrees. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;A scour hole 1.5 ft deeper than the mean thalweg depth was observed from 60 ft. to 100 ft. 
downstream during the Level I assessment. Scour protection measures at the site include: 
type-1 stone fill (less than 12 inches diameter) along the right bank upstream, at the 
downstream end of the downstream left wingwall and downstream right wingwall; and 
type-2 stone fill (less than 36 inches diameter) along the left bank upstream, at the upstream 
end of the upstream right wingwall, and along the entire base of the left and right 
abutments. 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 0.0 to 0.8 ft. The worst-case 
contraction scour occurred at the incipient roadway-overtopping discharge. Abutment scour 
ranged from 5.7 to 12.9 ft. 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/ofr97632</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 7 (WALDTH00020007) on Town Highway 2, crossing Coles Brook, Walden, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>