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Analysis of Factors Influencing Soil Classification Using Normalized Piezocone Tip Resistance and Pore Pressure Parameters
Authors:James A Schneider  Mark F Randolph  Paul W Mayne  Nicholas R Ramsey
Affiliation:1Ph.D. Student, School of Civil and Resource Engineering, The Univ. of Western Australia, 35 Stirling Highway, Crawley, Western Australia 6009, Australia (corresponding author). E-mail: schneider@civil.uwa.edu.au
2Federation Fellow, Centre for Offshore Foundation Systems, The Univ. of Western Australia, 35 Stirling Highway, Crawley, Western Australia 6009, Australia. E-mail: randolph@civil.uwa.edu.au
3Professor, Geosystems Engineering Group, School of Civil and Environmental Engineering, Georgia Institute of Technology, 790 Atlantic Dr. N.W., Atlanta, GA 30332-0355. E-mail: paul.mayne@ce.gatech.edu
4Principal Geotechnical Engineer, Sinclair Knight Merz (SKM), P.O. Box 2500, Malvern, Victoria 3144, Australia. E-mail: nramsey@skm.com.au
Abstract:This paper discusses the development of a framework for classifying soil using normalized piezocone test (CPTU) data from the corrected tip resistance (qt) and penetration pore-water pressure at the shoulder (u2). Parametric studies for normalized cone tip resistance (Q = qcnet/σv0′) and normalized excess pressures (Δu2/σv0′) as a function of overconsolidation ratio (OCR = σvy′/σv0′) during undrained penetration are combined with piezocone data from clay sites, as well as results from relatively uniform thick deposits of sands, silts, and varietal clays from around the globe. The study focuses on separating the influence of yield stress ratio from that of partial consolidation on normalized CPTU parameters, which both tend to increase Q and decrease the pore pressure parameter (Bq = Δu2/qcnet). The resulting recommended classification chart is significantly different from existing charts, and implies that assessment of data in Q–Δu2/σv0′ space is superior to Q–Bq space when evaluating piezocone data for a range of soil types. Still, there are zones of overlap for silty soils and heavily overconsolidated clays, thus requiring that supplementary information to Q and Δu2/σv0′ be obtained in unfamiliar geologies, including variable rate penetration tests, dissipation tests, CPT friction ratio, or soil sampling.
Keywords:Soil classification  Cone penetration tests  Silts  Sand  Clays  Overconsolidated soils  
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