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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>Donald L. Song</dc:contributor>
  <dc:creator>Erick M. Boehmler</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 
BRNATH00470030 on Town Highway 47 crossing Locust Creek, Barnard, 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 Green Mountain section of the New England physiographic province in 
central Vermont. The 4.18-mi&lt;sup&gt;2&lt;/sup&gt;
 drainage area is a predominantly rural and forested basin. In 
the vicinity of the study site, the surface cover consists of trees, shrubs, and brush.
In the study area, Locust Creek has an incised, sinuous channel with a slope of 
approximately 0.02 ft/ft, an average channel top width of 32 ft and an average bank height 
of 4 ft. The predominant channel bed material is gravel with a median grain size (D&lt;sub&gt;50&lt;/sub&gt;) of 
49.5 mm (0.162 ft). The geomorphic assessment at the time of the Level I and Level II site 
visit on October 13, 1994, indicated that the reach was stable.
The Town Highway 47 crossing of Locust Creek is a 28-ft-long, one-lane bridge consisting 
of one 25-foot concrete span (Vermont Agency of Transportation, written communication, 
August 23, 1994). The bridge is supported by vertical, concrete abutments with wingwalls. 
The channel is skewed approximately 40 degrees to the opening. Historical bridge data 
indicates that the opening-skew-to-roadway is 45 degrees, but 35 degrees was computed by 
use of survey data from this study.
A minor scour hole, 0.5 ft deeper than the mean thalweg depth was observed along the left 
abutment wall during the Level I assessment. The scour protection measures at the site were 
type-2 stone fill (less than 36 inches diameter) on the upstream wingwalls. There also is 
type-3 stone fill on the downstream right wingwall. 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). 
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 1.4 feet. The worst-case 
contraction scour occurred at the 500-year discharge. Abutment scour ranged from 2.3 to 
8.9 feet. The worst-case abutment scour occurred at the 100-year discharge at 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. 
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/ofr97210</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Level II scour analysis for Bridge 30 (BRNATH00470030) on Town Highway 47, crossing Locust Creek, Barnard, Vermont</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>