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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>Emily C. Wild</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 
WNDHTH00020010 on Town Highway 2 crossing the Middle Branch Williams River, 
Windham, 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 
south central Vermont. The 1.44-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 predominate surface cover upstream of the bridge 
is pasture on the left bank and forest on the right bank. Downstream of the bridge the 
surface cover consists of forest on the right bank and grass on the left bank.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, the Middle Branch Williams River has an incised, sinuous channel with a 
slope of approximately 0.03 ft/ft, an average channel top width of 28 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 61.4 mm (0.201 ft). The geomorphic assessment at the time of the Level I and 
Level II site visit on August 22, 1996, indicated that the reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 2 crossing of the Middle Branch Williams River is a 
25-ft-long, two-lane bridge consisting of one 22-foot concrete slab span (Vermont Agency 
of Transportation, written communication, March 31, 1995). The bridge is supported by 
vertical, concrete abutments with wingwalls. The channel is skewed approximately 60 
degrees to the opening while the opening-skew-to-roadway is 50 degrees. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The scour protection measures at the site included type-2 stone fill (less than 36 inches 
diameter) along both upstream banks. The scour protection measures downstream were type 
-1 stone fill (less than 12 inches diameter) on the left bank and type-3 stone fill (less than 48 
inches diameter) on the right bank. Scour protection measures do not exist underneath 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 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 modelled flows ranged from 0.9 to 2.2 ft. The worst-case contraction 
scour occurred at the 500-year discharge. Abutment scour ranged from 8.5 to 8.8 ft along 
the right abutment and from 8.7 to 10.1 ft along the left abutment. The worst-case abutment 
scour at the right abutment occurred at the 100-year discharge and at the left 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/ofr97387</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 10 (WNDHTH00020010) on Town Highway 2, crossing the Middle Branch of the Williams River, Windham, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>