Technical Papers
Feb 7, 2017

Two Case Histories Demonstrating the Effect of Past Earthquakes on Liquefaction Resistance of Silty Sand

Publication: Journal of Geotechnical and Geoenvironmental Engineering
Volume 143, Issue 6

Abstract

The paper compares two liquefaction case histories in California: (1) the response of the Wildlife site in the Imperial Valley to the 2010 El-Mayor Cucapah earthquake (Mw=7.2, amax=0.15  g); and (2) the response of the Treasure Island Fire Station (F.S.) site in the San Francisco Bay area to the 1989 Loma Prieta earthquake (Mw=6.9, amax=0.16  g). Both histories involve silty sand critical layers with nonplastic fines contents, FC=2427%, similar normalized shear wave velocities, Vs1=145155  m/s, low cone penetration test (CPT) cone penetration resistances, and groundwater tables at essentially the same depth. The corresponding data points plot almost on top of each other on the shear wave velocity field liquefaction charts, which predict liquefaction at both sites. While Treasure Island F.S. did liquefy during the shaking, Wildlife did not and was far from liquefaction as indicated by piezometers at the site. This paper constitutes an attempt to understand the reason for these very different pore pressure responses through a detailed analysis of similarities and differences between the two histories. It is concluded that preshaking by previous earthquakes is the most probable explanation of the higher liquefaction resistance exhibited by the Wildlife site and other sites in the Imperial Valley. While the Wildlife critical layer was subjected to about 60–70 earthquakes capable of generating significant excess pore pressures between its estimated 1907 deposition and the 2010 earthquake, the Treasure Island F.S. layer was subjected to only about two earthquakes capable of doing so between deposition in the 1930’s and the 1989 earthquake. This difference is due to the very high seismic activity in the last 100-plus years in the Imperial Valley compared with a seismically quiet San Francisco Bay Area after the 1906 earthquake. The significance of the prior seismic history is corroborated by recent results from centrifuge and large-scale experiments. These results as well as the methodology developed in the paper may be helpful when analyzing the observed high liquefaction resistance of sandy sites located in other seismic regions.

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Acknowledgments

The authors want to acknowledge the California Department of Fish and Wildlife that provides access to the monitoring site at the Wildlife Liquefaction Array. The NEES@UCSB field site facility received support from the George E. Brown, Jr. Network for Earthquake Engineering Simulation program through CMS-0217421 and CMMI-0927178. The California Geological Surveys’ Strong Motion Instrumentation Program (CSMIP) provided the ground motion observations for the Treasure Island site, and the U.S. Geological Survey National Strong Motion Instrumentation project (NSMP) provided the 1987 ground motion and pore pressure observations from the Wildlife Site. The authors also want to thank Professor R. Andrus for useful discussions about the effects of geologic age, preshaking and liquefaction, Dr. T. Holzer for his help in clarifying the types of soil deposition at the Wildlife and Treasure Island sites, and Professor S. Thevanayagam for his contribution to the experimental results included in Fig. 9.

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Journal of Geotechnical and Geoenvironmental Engineering
Volume 143Issue 6June 2017

History

Received: Sep 14, 2015
Accepted: Sep 26, 2016
Published online: Feb 7, 2017
Published in print: Jun 1, 2017
Discussion open until: Jul 7, 2017

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W. El-Sekelly, M.ASCE [email protected]
Lecturer, Mansoura Univ., Mansoura, Dakahlia Governorate 35516, Egypt (corresponding author). E-mail: [email protected]
R. Dobry, M.ASCE
Institute Professor, Dept. of Civil and Environmental Engineering, Rensselaer Polytechnic Institute, 110 8th St., JEC 4049, Troy, NY 12180.
T. Abdoun, M.ASCE
Iovino Chair Professor, Dept. of Civil and Environmental Engineering, Rensselaer Polytechnic Institute, 110 8th St., JEC 4049, Troy, NY 12180.
J. H. Steidl
Research Seismologist, Earth Research Institute, UC Santa Barbara, 6710 Ellison Hall, Santa Barbara, CA 93106-1100.

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