Liquefaction of Silty Soils
Abstract
Liquefaction during earthquakes has been a significant cause of failure of onshore as well as offshore structures. The phenomenon of liquefaction has been studied extensively for the case of cohesionless soils. Fine- grained soils, such as silts and sands with fines, have generally been considered non-liquefiable in the past. Recent studies have shown that fine-grained soils in certain situations may be susceptible to liquefaction. This paper presents the results of an experimental investigation conducted to determine the liquefaction susceptibility of a low-plasticity silty soil. Cyclic triaxial tests were conducted on undisturbed and reconstituted specimens for this purpose. The results of the study indicate that low-plasticity specimens used in this test program were susceptible to failure by large axial deformations even though liquefaction defined in terms of loss of initial effective confining pressure may not occur.
Recommended Citation
V. K. Puri et al., "Liquefaction of Silty Soils," International Journal of Offshore and Polar Engineering, vol. 6, no. 4, pp. 308 - 312, Dec 1996.
Department(s)
Civil, Architectural and Environmental Engineering
Keywords and Phrases
Earthquake; Fine-grained soils; Liquefaction; Low plasticity; Potential for deformation; Silts; Wave action
International Standard Serial Number (ISSN)
1053-5381
Document Type
Article - Journal
Document Version
Citation
File Type
text
Language(s)
English
Rights
© 2024 The Authors, All rights reserved.
Publication Date
01 Dec 1996