Geotechnical site characterization in the greater Memphis area using cone penetration tests

Citation
Ja. Schneider et al., Geotechnical site characterization in the greater Memphis area using cone penetration tests, ENG GEOL, 62(1-3), 2001, pp. 169-184
Citations number
31
Categorie Soggetti
Geological Petroleum & Minig Engineering
Journal title
ENGINEERING GEOLOGY
ISSN journal
00137952 → ACNP
Volume
62
Issue
1-3
Year of publication
2001
Pages
169 - 184
Database
ISI
SICI code
0013-7952(200110)62:1-3<169:GSCITG>2.0.ZU;2-6
Abstract
The determination of seismic ground hazards in Memphis and Shelby County, T ennessee is facilitated by the use of electronic cone penetration tests tha t can provide up to four independent readings with depth from a single soun ding. One series of soundings is being performed for site-specific mapping to determine the presence and extent of potentially-liquefiable sediments, in-situ soil resistance to liquefaction, and initial soil stiffness for gro und motion amplification studies. Another series of soundings is being cond ucted in conjunction with field paleoliquefaction mapping in the New Madrid seismic zone to better define the intensity, magnitude, and geographic ext ent of ground failures caused by large past earthquake events, as well as i nformation about the source sands. In this paper, an overview is given on t he types of multi-channeled penetrometer data that are being collected, inc luding vertical profiles of cone tip stress (q(t)), sleeve friction (f(s)), penetration porewater pressure (u(1) or u(2)) downhole shear wave velocity (V-s) and/or electrical conductivity (k(c)). Representative soundings are presented from select sites to illustrate repeatability, data post-processi ng methods, and that derived downhole V-s profiles are generally in good ag reement with non-invasive surface techniques at two Memphis test sites. Cyc lic stress based procedures for liquefaction are discussed with relation to data from a paleoliquefaction site in Germantown, Tennessee, and estimates of the minimum magnitude of the historic event are discussed. While estima tes of the earthquake magnitude are preliminary pending additional study on attenuation relationships and site response in the deep soils of the Missi ssippi Embayment, it is inferred from evaluation of in-situ test data using cyclic stress based techniques that the December 1811 New Madrid earthquak e was likely larger than a M-W = 7.5 event. (C) 2001 Elsevier Science B.V. All rights reserved.