Water-Resources Investigation Report 03-4064
U.S. Geological Survey Water-Resources Investigation Report 03-4064, 137 pages (Published 2003)
Stephen T. Benedict
In cooperation with the South Carolina Department of Transporation
This report is available online in pdf format (8 MB): USGS WRIR 03-4064
Appendix A contains a description of the SCBSD automated reports, raw data tables, and variable definitions.
The U.S. Geological Survey, in cooperation with the South Carolina Department of Transportation, collected observations of clear-water abutment and contraction scour at 146 bridges in the Coastal Plain and Piedmont of South Carolina. Scour depths ranged from 0 to 23.6 feet. Theoretical scour depths were computed at each bridge and compared with observed scour. This comparison showed that theoretical scour depths, in general, exceeded the observed scour depths and often were excessive. A comparison of field data with dimensionless relations for laboratory data showed that the range of dimensionless variables used in laboratory investigations was outside of the range for field data in South Carolina, suggesting laboratory relations may not be applicable to field conditions in South Carolina. Variables determined to be important in developing scour within laboratory studies were investigated to understand their influence within the South Carolina field data, and many of these variables appeared to be insignificant under field conditions found in South Carolina. The strongest explanatory variables were embankment length, geometric-contraction ratio, approach velocity, and soil cohesion. Envelope curves developed with the field data are useful tools for assessing reasonable ranges of scour depth in South Carolina. These tools are simple to apply and are an improvement over the current methods for predicting theoretical scour.
Data from this study have been compiled into a database that includes photographs, figures, observed scour depths, theoretical scour depths, limited basin characteristics, limited soil data, and theoretical hydraulic data. The database can be used to compare studied sites with unstudied sites to assess the potential for scour at the unstudied sites. In addition, the database can be used to assess the performance of various theoretical methods for predicting clear-water abutment and contraction scour.
Selected data generated from this study has been compiled into a database called the South Carolina Bridge Scour Database (SCBSD), and can be viewed using Microsoft Access. The SCBSD includes photographs, figures, selected field data, variables used to compute theoretical scour, computed scour depths, limited basin characteristics, limited soil data, and selected hydraulic data estimated with the WSPRO model (Shearman, 1990). These raw data are compiled in various data tables within the database, and automated reports have been developed to allow extraction of selected data for a chosen bridge. The SCDOT assigns a unique 12-digit number for each bridge under its jurisdiction and these numbers are used in the database as the primary search variable for extracting selected data from the raw data tables for display in the automated reports. Appendix A contains a description of the SCBSD automated reports, raw data tables, and variable definitions.
The SCBSD is a valuable tool for use in investigating clear-water abutment scour and contraction scour. For one who is assessing scour at bridges in South Carolina, the SCBSD provides a tool for making site comparisons. Sites under investigation, but not included in the current study, can be compared with sites in the SCBSD to gain insights about the range of anticipated scour depths. The SCBSD also provides a source of data to assess various theoretical methods for predicting clear-water abutment and contraction scour. Most equations for predicting scour are driven by hydraulic variables, such as flow depth and velocity. These variables can be extracted from the SCBSD and used in various theoretical equations to compute theoretical scour depths. The theoretical scour depths can then be compared with observed scour, as well as the field-data envelope curves, to assess the chosen equation's performance. (Hydraulic data in the SCBSD may need to be manipulated to obtain specific variables required for a given theoretical equation.)
One should keep in mind that the hydraulic data in the SCBSD were generated from a model and, therefore, do not necessarily represent the flow conditions that created the observed scour. As a result, some error is likely to be introduced into the comparison of theoretical scour with observed scour because of inaccuracies in the hydralic data. However, the abundance of data points in the SCBSD will allow such comparisons to show the general trends of the theoretical equation and will provide some indication of the equation's performance.
The SCBSD provides only limited information at each study site and, therefore, cannot be relied upon to provide a complete understanding of the sites. If more detailed information is required to understand conditions at a given site, then other data sources, such as topographic maps and bridge plans, should be consulted. Under certain circumstances, site visits may be required to gain a full appreciation of the observed scour and the conditions that created it.
TO INSTALL SCBSD:
The SCBSD was developed using Microsoft Access 2000. The electronic file for the database requires approximately 638 megabytes of computer storage. To install the database, the file "scour.mdb" should be copied to a directory of the user's choice. After copying this file to the computer, the properties of the file should be changed from "Read-only" by
(1) right clicking on the file and selecting "Properties" on the popup menu,
(2) unselecting the "Read-only" option in the Properties menu box, and then
(3) clicking "OK" at the bottom of the menu box.
TO INVOKE SCBSD
The file "scour.mdb" should be opened in Access. Upon opening this file, a menu box titled, "Bridge-Scour Data Reports," will appear. This menu box lists the 10 automated reports described in Appendix A and allows the user to generate the automated reports for a selected bridge. Near the top of this menu box is a drop-down menu designated by a menu button with a downward pointing arrowhead. Clicking on this button will produce a list of sites included in this study. From this list, the user should select a bridge of interest. Once a specific bridge has been selected, the user can view the various automated reports, for the bridge of interest, by selecting the "View Selected Record" menu button that is to the right of the report of interest. Selecting the "View All Reports" menu button will generate, in numeric order, the corresponding report for all bridges.
TO OBTAIN SCBSD (638MB), Please e-mail Pubs Information
Abstract
Introduction
Purpose and Scope
Acknowledgments
Previous Investigations
Description of Study Area
Data Assumptions
Justification for the Assumption of Large Flood Flows
Justification for the Assumption of Equilibrium-Scour Conditions
Basin Equilibrium Scour
Site selection
SCDOT List of Bridges with Observed Scour
Selection of Previously Studied Level 2 Bridge-Scour Sites
Selection of Piedmont Sites Influenced by the August 1995 Flood
Selection of Piedmont Bridges with Wide, Flat Floodplains
Selection of Coastal Plain Sites Influenced by the September 1999 Flood
Techniques for the Collection and Interpretation of Field Data
Data Collection in the Coastal Plain
Data Collection in the Piedmont
Flow Model Data
Sediment Samples
Contraction Scour in the Abutment Area
Pier Scour in the Abutment Area
Estimating Hydraulic Data
Development of WSPRO Models
Estimates of Hypothetical Flows
Historical Flows
Flood of October 1992
Flood of August 1995
Flood of September 1999
Development of Theoretical Bridge-Scour Database
Theoretical Pier Scour
Theoretical Live-Bed Contraction Scour
Theoretical Clear-Water Contraction Scour
Theoretical Abutment Scour
Variables Influencing Abutment Scour
Time and Flow Duration
Flow Velocity
Flow Depth
Sediment Size
Sediment Gradation
Embankment Length
Abutment Shape
Embankment Skew
Channel Geometry
Geometric-Contraction Ratio
Conclusions
Abutment Scour in the Piedmont
Comparison of Observed and Theoretical Abutment-Scour Depths
Piedmont Floodplain Geometry as an Indicator of Potential Scour
Embankment Length as an Indicator of Potential Scour
Geometric-Contraction Ratio as an Indicator of Potential Scour
Floodplain Land Cover as an Indicator of Potential Scour
Abutment Scour in the Coastal Plain
Abutment-Scour Hole Patterns
Comparison of Observed and Theoretical Abutment-Scour Depths
Embankment Length as an Indicator of Potential Scour
Geometric-Contraction Ratio as an Indicator of Potential Scour
Bridges 240 Feet or Less in Length.
Floodplain Land Cover as an Indicator of Potential Scour
Effect of Upstream Channel Alignment on Abutment Scour
Guidance for Assessing Abutment-Scour Depth Using the Envelope Curves
Selecting a Reference Surface for Abutment-Scour Depth
Estimating the Embankment Length and the Geometric-Contraction Ratio
Selecting the Appropriate Abutment-Scour Depth Envelope
Single-Bridge Openings
Multiple-Bridge Openings
Contraction and Pier Scour within the Abutment-Scour Area
Limitations of the Abutment-Scour Depth Envelope Curves
Guidance for Assessing Abutment-Scour Hole Location, Width, and Shape
Lateral Reference for Scour Hole
Scour-Hole Top Width
Scour-Hole Longitudinal Location
Scour-Hole Shape
Clear-Water Contraction Scour in the Piedmont
Comparison of Observed and Theoretical Contraction-Scour Depths
Geometric-Contraction Ratio as an Indicator of Potential Scour
Selecting a Reference Surface for Clear-Water Contraction Scour
Pier Scour Within Clear-Water Contraction-Scour Areas
Estimate of Clear-Water Contraction-Scour Hole Location
Permissible Velocities for Clear-Water Contraction Scour
The South Carolina Bridge-Scour Database
Summary
Selected References
This report is available online in pdf format (8 MB): USGS WRIR 03-4064
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For more information, contact the South Carolina Publications Unit.
USGS South Carolina Publications • South Carolina Water Science Center