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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>Erick M. Boehmler</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 
TOPSTH00570038 on Town Highway 57 crossing the Waits River, Topsham, 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 east central Vermont. The 37.3-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 pasture while the 
left bank upstream is suburban.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, the Waits River has a sinuous locally anabranched channel with a slope of 
approximately 0.01 ft/ft, an average channel top width of 76 ft and an average bank height 
of 6 ft. The channel bed material ranges from sand to cobble with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) 
of 57.2 mm (0.188 ft). The geomorphic assessment at the time of the Level I and Level II 
site visit on August 28, 1995, indicated that the reach was considered laterally unstable due 
to cut-banks upstream, mid-channel bars and lateral migration of the channel towards the 
left abutment. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 34 crossing of the Waits River is a 34-ft-long, one-lane bridge 
consisting of one 31-foot steel-beam span (Vermont Agency of Transportation, written 
communication, March 28, 1995). The opening length of the structure parallel to the bridge 
face is 30.4 ft. The bridge is supported by a vertical, stone abutment with concrete facing 
and wingwalls on the right and by a vertical, concrete abutment with wingwalls on the left. 
The channel is skewed approximately 0 degrees to the opening and the opening-skew-to-roadway is also zero degrees.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;A scour hole 2.0 ft deeper than the mean thalweg depth was observed towards the left bank 
underneath the bridge. The only scour protection measure at the site was type-2 stone fill 
(less than 36 inches diameter) along the left bank upstream, in the upstream left wing wall 
area, along the left abutment, at the downstream end of the right abutment, and in the 
downstream left wing wall area. There is type-3 stone fill (less than 48 inches diameter) in 
the downstream right wing wall area. 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 1.6 to 5.2 ft. The worst-case 
contraction scour occurred at the 100-year discharge. Abutment scour ranged from 9.8 to 
18.5 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/ofr97649</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 38 (TOPSTH00570038) on Town Highway 57, crossing Waits River, Topsham, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>