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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>Tim Severance</dc:contributor>
  <dc:creator>Ronda L. Burns</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 
BURKTH00070016 on Town Highway 7 crossing Dish Mill Brook, Burke, 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 White Mountain section of the New England physiographic province in 
northeastern Vermont. The 6.0-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 forest except on the left bank 
upstream which is brushland. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, Dish Mill Brook has an incised, sinuous channel with a slope of 
approximately 0.04 ft/ft, an average channel top width of 40 ft and an average bank height 
of 6 ft. The channel bed material ranges from sand to boulder with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) 
of 94.1 mm (0.309 ft). The geomorphic assessment at the time of the Level I and Level II 
site visit on August 7, 1995, indicated that the reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 7 crossing of Dish Mill Brook is a 28-ft-long, two-lane bridge 
consisting of one 24-foot steel-beam span (Vermont Agency of Transportation, written 
communication, March 24, 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 35 degrees to the opening while the computed opening-skew-to-roadway is 35 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 and 
right abutments during the Level I assessment. In front of the upstream and downstream left 
wingwalls the scour depth was only 0.5 ft, while in front of the downstream right wingwall 
it was 0.75 ft and in front of the upstream right wingwall it was 0.3 ft. The scour 
countermeasures at the site include type-1 stone fill (less than 12 inches diameter) at the 
downstream end of the right abutment and along the downstream right wingwall. Type-2 
stone fill (less than 36 inches diameter) is along the upstream left bank, the upstream and 
downstream left wingwalls, and at the upstream end of the upstream right wingwall. 
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 0.5 ft. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 6.7 to 
9.3 ft. The worst-case abutment scour occurred at the 500-year discharge for the left 
abutment and at the incipient road-overtopping discharge for the right abutment. 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/ofr97758</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 16 (BURKTH00070016) on Town Highway 7, crossing Dish Mill Brook, Burke, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>