<?xml version='1.0' encoding='utf-8'?>
<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>James R. Degnan</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 
FFIETH00030012 on Town Highway 3 crossing the Fairfield River, Fairfield, 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 
north-western Vermont. The 7.34-mi&lt;sup&gt;2&lt;/sup&gt; drainage area is in a predominantly rural basin with 
forest on the valley walls and pasture/row crops on the valley bottom. In the vicinity of the 
study site, the surface cover is row crops with a few trees on the immediate banks.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;In the study area, the Fairfield River has a meandering channel with a slope of 
approximately 0.005 ft/ft, an average channel top width of 37 ft and an average channel 
depth of 6 ft. The predominant channel bed materials are sand and gravel with a median 
grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 32.5 mm (0.107 ft). The geomorphic assessment at the time of the Level 
I and Level II site visit on June 16, 1995, indicated that the reach was stable.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;The Town Highway 3 crossing of the Fairfield River is a 24-ft-long, one-lane bridge 
consisting of one 20-foot concrete span (Vermont Agency of Transportation, written 
communication, March 8, 1995). The bridge is supported by vertical, concrete abutments 
with wingwalls. The channel is skewed approximately 40 degrees to the opening. Although 
bridge records show an opening-skew-to-roadway of 45 degrees, the skew measured from 
surveyed points was 30 degrees. &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;At the time of the level I assessment, the left abutment had been undermined and settled 
into a scour hole at the upstream end. The right abutment footing was exposed but not 
undermined. The scour protection measures at the site were type-1 stone fill (less than 12 
inches diameter) on the downstream right bank, and type-2 stone fill (less than 36 inches 
diameter) along the entire base of the upstream right wingwall, the upstream banks, and
downstream left bank. The type-2 stone fill on the left bank downstream changes to type-1 
about 55 feet downstream of the bridge. 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 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 3.0 ft. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 3.2 to 
4.0 ft. at the left abutment and 9.7 to 11.7 feet at the right abutment. The worst-case left 
abutment scour occurred at the incipient over-topping discharge, which was less than the 
100-year discharge. The worst-case right 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/ofr97108</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 12 (FFIETH00030012) on Town Highway 3, crossing the Fairfield River, Fairfield, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>