<?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:creator>Scott A. Olson</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>This report provides the results of a detailed Level II analysis of scour potential at structure 
HARDTH00490024 on Town Highway 49 crossing Nichols Brook at Mackville Pond 
Outlet, Hardwick, 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 New England Upland section of the New England physiographic province 
in north-central Vermont. The 10.7-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 best described as 
suburban with residences, lawns, trees and roadways.
There is a dam 54 feet downstream of the bridge which controls Mackville Pond upstream 
of the bridge. The vertical drop over the dam is 15 feet. Immediately upstream of the bridge 
the width of the waterway is 146 feet. The predominant channel bed material is sand with a 
median grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 0.576 mm (0.00189 ft). The geomorphic assessment at the time 
of the Level I and Level II site visit on July 25, 1995, indicated that the reach was stable.
The Town Highway 49 crossing of Nichols Brook at Mackville Pond Outlet is a 42-ft-long, 
two-lane bridge consisting of one 38-foot steel-beam span (Vermont Agency of 
Transportation, written communication, April 3, 1995). The bridge is supported by vertical, 
concrete abutments with wingwalls on the downstream end of the left abutment and 
upstream and downstream ends of the right abutment. The channel is not skewed to the 
opening, but the opening-skew-to-roadway is 5 degrees.
Scour protection measures at the site include type-3 stone fill (less than 48 inches diameter) 
on the upstream side of the left roadway embankment and at the upstream end of the left 
abutment. Type-2 stone fill (less than 36 inches diameter) was on the upstream right 
roadway embankment. Additional details describing conditions at the site are included in 
the Level II Summary and Appendices 
D and E.
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.
Contraction scour for all modelled flows ranged from 4.7 to 21.0 ft. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour at the left abutment 
ranged from 13.3 to 15.8 ft. with the worst-case occurring at the 500-year discharge. 
Abutment scour at the right abutment ranged from 8.1 to 9.8 ft. with the worst-case 
occurring at the incipient roadway-overtopping discharge. Additional information on scour 
depths and depths to armoring are included in the section titled “Scour Results”. Scouredstreambed 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 particlesize distribution. 
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.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr96637</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 24 (HARDTH00490024) on Town Highway 49, crossing Nichols Brook at Mackville Pond Outlet, Hardwick, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>