2006Journal of Geotechnical and Geoenvironmental EngineeringRequires access

Index Properties-Based Criteria for Liquefaction Susceptibility of Clayey Soils: A Critical Assessment

David Kun Li, C. Hsein Juang, Ronald D. Andrus, William M. Camp

Open publisher page 29 citations

Abstract

The Cooper marl in Charleston, S.C., a deep layer of clayey soils approximately 5– 21m below the ground surface, is generally recognized as nonliquefiable material. Data from field cone penetration tests and laboratory tests of samples taken from the Cooper marl are used to investigate the adequacy of index properties-based criteria for assessing liquefaction susceptibility of clayey soils. In particular, the criterion based on soil behavior type index (Ic) and that based on Atterberg limits are examined. The results show that the Atterberg limits-based criterion adequately reflected the characteristics of the marl, whereas the Ic -based criterion erroneously identified the marl as being liquefiable. A possible reason for the deficiency of Ic and a modification to overcome this deficiency are presented.

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What this paper is about

The Cooper marl in Charleston, S.C., a deep layer of clayey soils approximately 5– 21m below the ground surface, is generally recognized as nonliquefiable material. Data from field cone penetration tests and laboratory tests of samples taken from the Cooper marl are used to investigate the adequacy of index properties-based criteria for assessing liquefaction susceptibility of clayey soils. In particular, the criterion based on soil behavior type index (Ic) and that based on Atterberg limits are examined. The results show that the Atterberg limits-based criterion adequately reflected the characteristics of the marl, whereas the Ic -based criterion erroneously identified the marl as being liquefiable. A possible reason for the deficiency of Ic and a modification to overcome this deficiency are presented.

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Available abstract

The Cooper marl in Charleston, S.C., a deep layer of clayey soils approximately 5– 21m below the ground surface, is generally recognized as nonliquefiable material. Data from field cone penetration tests and laboratory tests of samples taken from the Cooper marl are used to investigate the adequacy of index properties-based criteria for assessing liquefaction susceptibility of clayey soils. In particular, the criterion based on soil behavior type index (Ic) and that based on Atterberg limits are examined. The results show that the Atterberg limits-based criterion adequately reflected the characteristics of the marl, whereas the Ic -based criterion erroneously identified the marl as being liquefiable. A possible reason for the deficiency of Ic and a modification to overcome this deficiency are presented.

Key concepts: Marl, Atterberg limits, Geotechnical engineering, Liquefaction, Penetration test, Soil water, Clay soil, Geology

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