TECHNICAL PAPERS
Mar 1, 1995

Shear-Wave Velocity to Evaluate In-Situ State of Ottawa Sand

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Publication: Journal of Geotechnical Engineering
Volume 121, Issue 3

Abstract

The initial state of a sand, defined by the void ratio and effective mean normal stress, can be used to predict its large-strain response. Laboratory studies have shown that the shear-wave velocity of a sand is controlled primarily by the effective confining stresses and void ratio. Since shear-wave velocity can be measured both in the field and in the laboratory, there is an increasing interest in using shear-wave velocity to define the state of a sand. This paper presents an experimental study of shear-wave velocity interpretation for clean Ottawa sand based on steady/critical state concepts. The results show that the large-strain behavior of Ottawa sand can be estimated using shear-wave velocity measurements combined with a knowledge of the in-situ effective stress. Knowledge of the state of a sand makes it possible to estimate the boundary between either a contractant or dilatant sand at large strains. Based on these findings, a preliminary method to evaluate the potential for flow liquefaction using shear-wave velocity measurements is presented.

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Go to Journal of Geotechnical Engineering
Journal of Geotechnical Engineering
Volume 121Issue 3March 1995
Pages: 262 - 273

History

Published online: Mar 1, 1995
Published in print: Mar 1995

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Authors

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P. K. Robertson, Member, ASCE
Prof., Geotech. Group, Dept. of Civ. Engrg., Univ. of Alberta, Edmonton, Alberta, Canada T6G 2G7.
S. Sasitharan
Engr., Powertech Lab. Inc., 12388-88 Avenue, Surrey, BC, Canada V3W 7R7.
J. C. Cunning
Engr., Klohn-Crippen Consultants Ltd., 10200 Shellbridge Way, Richmond, BC, Canada V6X 2W7.
D. C. Sego, Member, ASCE
Prof., Geotech Group, Dept. of Civ. Engrg., Univ. of Alberta, Edmonton, Alberta, Canada T6G 2G7.

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