Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
The Leading Edge Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

The Leading Edge; July 2005; v. 24; no. 7; p. 724-728; DOI: 10.1190/1.1993267
© 2005 Society of Exploration Geophysicists
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Submit a response
Right arrow Alert me when this article is cited
Right arrow Alert me when eLetters are posted
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Park, C. B.
Right arrow Articles by Christian, H.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Underwater MASW to evaluate stiffness of water-bottom sediments

Choon B. Park, Richard D. Miller, Jianghai Xia and Julian Ivanov

Kansas Geological Survey, Lawrence, USA

Gary V. Sonnichsen, James A. Hunter, R.L. Good and R.A. Burns

Geological Survey of Canada, Ottawa

Harold Christian

Christian Situ Geoscience, Dartmouth, Nova Scotia, Canada

Corresponding author: park{at}kgs.ku.edu

Stiffness measurements are often necessary for geotechnical characterization of an underwater site. Seismically, these measurements can be made through the dispersion analysis of the Rayleigh-type surface waves. Successful terrestrial application of this method has been reported by many investigators using spectral analysis of surface waves (SASW) and more recently using multichannel analysis of surface waves (MASW). The MASW method was originally developed as a land survey method to investigate the near-surface materials for their elastic properties: for example, the shear-wave velocity (VS), by recording and analyzing Rayleigh-type surface waves using a vertical (impulsive) seismic source and receivers. The acquired data are first analyzed for dispersion characteristics and, from these the shear-wave velocity is estimated using an inversion technique.




This article has been cited by other articles:


Home page
J ENVIRON ENG GEOPHYSHome page
P. Anbazhagan and T. G. Sitharam
Mapping of Average Shear Wave Velocity for Bangalore Region: A Case Study
Journal of Environmental & Engineering Geophysics, June 1, 2008; 13(2): 69 - 84.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Society of Exploration Geophysicists