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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>Erick M. Boehmler</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 
MONKTH00340021 on Town Highway 34 crossing Little Otter Creek, Monkton, 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 D 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 C.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The site is in the Champlain section of the Saint Lawrence Valley physiographic province 
in northwestern Vermont. The 34.1-mi&lt;sup&gt;2&lt;/sup&gt;
 drainage area is in a predominantly rural and 
forested basin with pasture in the valleys. In the vicinity of the study site, the surface cover 
consists of pasture. The most significant tree cover is immediately adjacent to the channel 
on the right bank downstream.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, Little Otter Creek has a sinuous channel with a slope of approximately 
0.008 ft/ft, an average channel top width of 92 feet and an average bank height of 6 feet. 
The predominant channel bed materials are silt and clay. Sieve analysis indicates that 
greater than 50% of the sample is silt and clay and thus a median grain size by use of sieve 
analysis was indeterminate. Therefore, the median grain size was assumed to be medium 
silt with a size (D&lt;sub&gt;50&lt;/sub&gt;) of 0.0310 mm (0.000102 ft). The geomorphic assessment at the time of 
the Level I and Level II site visit on June 19 and June 20, 1996, indicated that the reach was 
stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 34 crossing of Little Otter Creek is a 50-ft-long, one-lane bridge 
consisting of one 26-foot concrete span and three “boiler tube” smooth metal pipe culverts 
through the left road approach (Vermont Agency of Transportation, written 
communication, December 15, 1995). The opening length of the bridge parallel to the 
bridge face is 25.1 feet. The bridge is supported by vertical, concrete abutments with 
wingwalls on the right abutment only. The channel is skewed approximately 25 degrees to 
the opening. The VTAOT records indicate the opening-skew-to-roadway is 20 degrees but 
measurement from surveyed data suggests the skew is five degrees.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The scour protection measures at the site were type-1 stone fill (less than 12 inches 
diameter) on the upstream and downstream embankments of the left road approach and 
type-2 stone fill (less than 36 inches diameter) surrounding the entrance of each culvert. 
Additional details describing conditions at the site are included in the Level II Summary 
and Appendices C and D.&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 10.3 to 12.3 feet. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 8.6 to 
22.5 feet. The worst-case abutment scour occurred at the 500-year discharge for the left 
abutment and at the incipient 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/ofr97672</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 21 (MONKTH00340021) on Town Highway 34, crossing Little Otter Creek, Monkton, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>