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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:creator>Scott A. Olson</dc:creator>
  <dc:date>1997</dc:date>
  <dc:description>This report provides the results of a detailed Level II analysis of scour potential at structure 
ALBUTH00150006 on Town Highway 15 crossing Mud Creek, Alburg, 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.
The site is in the Champlain section of the St. Lawrence Valley physiographic province in 
northwestern Vermont. The 2.90-mi&lt;sup&gt;2&lt;/sup&gt;
 drainage area is in a predominantly rural and forested 
basin. However, nearly a third of the drainage, including the location of the study site, is 
wetland.
In the study area, Mud Creek has an sinuous channel through wetland with a slope of 
approximately 0.0002 ft/ft, an average channel top width of 42 ft and an average bank 
height of 2 ft. The channel bed material ranges from clay to sand with an estimated median 
grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 0.047 mm (0.00015 ft). The geomorphic assessment at the time of the 
Level I and Level II site visit on June 26, 1995, indicated that the reach was stable.
The Town Highway 15 crossing of Mud Creek is a 30-ft-long, one-lane bridge consisting of 
one 28-foot steel-beam span (Vermont Agency of Transportation, written communication, 
March 7, 1995). The opening length of the structure parallel to the bridge face is 26.7 ft. 
The bridge is supported by vertical, concrete abutments with wingwalls. The channel is 
skewed zero degrees to the opening and the opening-skew-to-roadway is also zero degrees. 
Channel scour, approximately 2 ft deeper than the mean thalweg depth, was observed in the 
middle of the channel extending from 5 to 35 ft upstream of the bridge. The only scour 
countermeasure observed at this site was some small stone, possibly type-1 stone fill (less 
than 12 inches diameter), partially covering the channel bed under the bridge. Additional 
details describing conditions at the site are included in the Level II Summary and 
Appendices D and E.
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.
Contraction scour for all modelled flows ranged from 6.2 to 7.2 ft. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 2.0 to 
2.4 ft and 2.1 to 2.6 ft on the left and right abutments respectively. 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 crosssection 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.
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.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr97397</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 6 (ALBUTH00150006) on Town Highway 15, crossing Mud Creek, Alburg, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>