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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>Ronda L. Burns</dc:contributor>
  <dc:creator>Michael A. Ivanoff</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 
ANDOVT00110040 on State Route 11 crossing Lyman Brook, Andover, 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 4.18-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 pasture while the immediate 
banks have dense woody vegetation. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, Lyman Brook has an incised, straight channel with a slope of 
approximately 0.03 ft/ft, an average channel top width of 42 ft and an average bank height 
of 8 ft. The channel bed material ranges from gravel to boulder with a median grain size 
(D&lt;sub&gt;50&lt;/sub&gt;) of 86.0 mm (0.282 ft). The geomorphic assessment at the time of the Level I and 
Level II site visit on September 9, 1996, indicated that the reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The State Route 11 crossing of Lyman Brook is a 28-ft-long, two-lane bridge consisting of 
one 27-foot concrete tee-beam span (Vermont Agency of Transportation, written 
communication, March 29, 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 0 degrees to the opening while the opening-skew-to-roadway is 30 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) at the upstream end of the upstream right wingwall and the downstream ends of 
the downstream left and right wingwalls. There was also a stone wall along the top of the 
left bank from 36 to 76 feet upstream. 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 0.0 to 0.7 ft. The worst-case 
contraction scour occurred at the incipient-overtopping discharge which was more than the 
100-year discharge. Left abutment scour ranged from 1.2 to 7.5 ft. The worst-case left 
abutment scour occurred at the 500-year discharge. Right abutment scour ranged from 5.2 
to 6.7 ft. The worst-case right abutment scour occurred at the 100-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/ofr97594</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 40 (ANDOVT00110040) on State Route 11, crossing Lyman Brook, Andover, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>