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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>Timothy Severance</dc:contributor>
  <dc:creator>R.L. Burns</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 
NEWBTH00500065 on Town Highway 50 crossing Peach Brook, Newbury, 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 east-central Vermont. The 15.3-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 forest upstream of the bridge and 
shrub and brushland downstream of the bridge.
In the study area, Peach Brook has an incised, sinuous channel with a slope of 
approximately 0.005 ft/ft, an average channel top width of 40 ft and an average bank height 
of 8 ft. The channel bed material ranges from cobble to boulder with a median grain size 
(D50) of 83.1 mm (0.273 ft). The geomorphic assessment at the time of the Level I and 
Level II site visit on August 29, 1995, indicated that the reach was stable.
The Town Highway 50 crossing of the Peach Brook is a 29-ft-long, two-lane bridge 
consisting of one 25-foot steel-beam span (Vermont Agency of Transportation, written 
communication, March 27, 1995). The opening length of the structure parallel to the bridge 
face is 24.9 ft. The bridge is supported by vertical, concrete abutments with wingwalls. The 
channel is skewed approximately 50 degrees to the opening while the computed openingskew-to-roadway is 20 degrees.
A channel scour hole 0.75 ft deeper than the mean thalweg depth was observed under the 
bridge during the Level I assessment. Also observed was channel scour 0.75 ft deeper than 
the mean thalweg at the upstream face of the bridge and channel scour 0.25 ft deeper than 
the mean thalweg along the right bank downstream. The scour protection measures at the 
site included type-1 stone fill (less than 12 inches diameter) along the upstream and 
downstream right wingwalls and type-2 stone fill (less than 36 inches diameter) along the 
upstream right bank and along the downstream left wingwall and bank. In addition, there 
are four 3 ft square concrete blocks at the corner where the upstream right wingwall joins 
the right abutment. The upstream left wingwall and upstream half of the left abutment were 
constructed on top of a bedrock outcrop. 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) 
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.
Contraction scour for all modelled flows ranged from 0.0 to 1.3 ft. The worst-case 
contraction scour occurred at the incipient roadway-overtopping discharge, which was less 
than the 100-year discharge. The right abutment scour ranged from 6.1 to 7.2 ft. The worstcase right abutment scour occurred at the incipient roadway-overtopping discharge. The left 
abutment scour ranged from 7.1 to 10.3 ft. The worst-case left 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. 
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 he</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr97804</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 65 (NEWBTH00500065) on Town Highway 50, crossing Peach Brook, Newbury, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>