EARTHQUAKE SIMULATION IN GEOTECHNICAL ENGINEERING: APPLICATIONS AND RESEARCH NEEDS TO IMPROVE STATE OF PRACTICE K. Arulmoli Earth Mechanics, Inc., Fountain Valley, California ABSTRACT During the past decade or so, significant progress has been made in the area of understanding soil behavior during earthquakes. With the advent of faster and cheaper microcomputers, use of recent advanced computer programs for site response and soil-structure interaction evaluation has become more affordable thus making it possible to accommodate these analyses into projects with limited budgets and demanding schedules. However, clarification or additional work is still needed in many areas to improve the current state of practice. In the future, as the geotechnical profession is challenged to develop more efficient designs, researchers will be faced with the task of supplying the profession with appropriate tools to face these challenges. An additional challenge for geotechnical engineers is to understand the structural design implications of the geotechnical recommendations since in most cases the end users of geotechnical recommendations are structural engineers. Efforts should be focused on overcoming these challenges through effective collaboration between geotechnical and structural researchers and practitioners. INTRODUCTION Significant strides have been made in the area of understanding soil behavior during earthquakes in the recent past. Under the sponsorship of the National Science Foundation, significant improvements have been made in the area of earthquake simulation in geotechnical engineering allowing practitioners to better evaluate geotechnical earthquake engineering problems. In the early 1990s, the VELACS program was instrumental in highlighting the use of centrifuge modeling to verify numerical codes through collaborative efforts among geotechnical researchers and practitioners (Arulanandan and Scott 1993). For the first time ever, consensus has been reached by the geotechnical community regarding the use of cone penetration testing and shear wave velocity measurements, in addition to standard penetration testing, to evaluate liquefaction potential, as documented in a 1997 NCEER publication (Youd and Idriss 1997) and later published in the ASCE Geotechnical and Geoenvironmental Engineering Journal (Youd et al. 2001). With the advent of faster and cheaper microcomputers, use of recent advanced computer programs for site response and soil-structure interaction evaluation has become more affordable making it possible to accommodate these analyses into projects with limited budgets and demanding schedules. Recently, guidelines for evaluating and mitigating earthquake-induced induced hazards such as liquefaction (Martin and Lew 1999) and landslides (Blake et al. 2002) have been developed to help the practicing geotechnical engineers and the reviewing agencies of Southern California. In spite of the significant progress in geotechnical earthquake engineering practice in the recent past, clarification or additional work is still needed in certain areas to improve the current state of practice. Some areas needing immediate attention to develop guidelines include, (1) Liquefaction potential and seismic settlement of silty soils, (2) Liquefaction potential of deep soil deposits, (3) Lateral soil springs (p-y curves) during seismic loading, (4) Seismic earth pressures, and (5) Faster computer programs for seismic soil-structure interaction evaluations. Some example situations are highlighted in the following paragraphs where guidelines are needed for the practicing engineers to tackle real-world geotechnical earthquake engineering design problems. LIQUEFACTION POTENTIAL AND SEISMIC SETTLEMENT OF SILTY SOILS While the 1997 NCEER publication provides recommended procedures for evaluation of liquefaction potential of clean sands and sandy soils with fines, the authors are not aware of any clear guidelines for liquefaction potential evaluation for silty soils, especially containing nonplastic fines. The same is also true for evaluation of seismically induced settlements of silty soils. Evaluation of liquefaction potential and seismically induced settlement of silty soils deserves attention from the geotechnical earthquake engineering research community. LIQUEFACTION POTENTIAL OF DEEP SOIL DEPOSITS The geotechnical engineer often encounters subsurface conditions where Holocene soil deposits deeper than 15 m (50 ft.) are present. Recommended procedures for evaluation of liquefaction potential of deep soil deposits (Youd and Idriss 1997; Youd et al. 2001) are based on simplified procedures verified using case histories of known liquefaction (or no liquefaction) of soils within depths less than 15 m (50 ft.). Using the same procedures to evaluate liquefaction potential of deep soil deposits often leads to questionable results. As an example, a clean sand deposit located 30 m (100 ft.) below ground surface with a field SPT blow count (N60) of 50 or more would be characterized as “dense to very dense” implying that this layer would be nonliquefiable under a moderate earthquake shaking. Using the overburden correction recommended by the NCEER document, the overburden-corrected blow count (N1)60 was estimated to be about 22 (assuming the water table depth of 6 m and typical soil unit weights). 22 FIG. 1 SPT Clean Sand Base Curve for M=7.5 Earthquakes (Youd and Idriss 1997) It can be seen in Figure 1 that the sand deposit would be considered liquefiable, contradicting the generally accepted notion that a field blow count of 50 or more is a very competent soil. The implication of this conflict becomes even more significant when pile foundations are tipped into deep “dense to very dense” sand deposits. LATERAL SOIL SPRINGS DURING SEISMIC LOADING This is another area where guidelines are needed for the practitioners. Lateral soil springs are used in soil-structure interaction problems where pile foundation is used to support structures such as bridges, buildings, wharves, and other structures. Selection of appropriate lateral soil springs (p-y springs) during seismic loading should consider various factors that affect the lateral behavior of piles. They include, pile diameter effects, pile group effects, depth effects, liquefaction and soft soil effects, gapping effects, and sloping ground conditions (level ground, upslope, and downslope). Although significant research efforts have been and are on going, recommendations regarding the use of lateral soil springs in practice are lacking. SEISMIC EARTH PRESSURES Seismic earth pressures on retaining structures (walls, abutments etc.) are estimated using the Mononabe-Okabe (M-O) equation (Seed and Whitman 1970). One of the limitations of the M-O equation is that it “blows up” for cases of large ground acceleration and/or steeper slopes. In such cases, the geotechnical designers are left with the option of having to select seismic earth pressures based on the individual’s experience and judgment. Clarification is needed on the use and limitations of the M-O equation for estimating seismic earth pressures. When the M-O equation is not applicable, alternate recommendations are needed. The seismic passive earth pressure is used in the design of bridge abutments in California (Caltrans 2001). At present, Caltrans recommends 239 kPa (5.0 ksf) as the maximum passive pressure during earthquake for a 1.7 m (5.5 ft.) high abutment. This value is based on the results of limited full-scale tests performed on a 1.7 m (5.5 ft.) high abutment at the University of California, Davis (Romstad et al. 1995). For abutment heights other than 1.7 m (5.5 ft.), the earth pressures are estimated by interpolation. Due to the limited amount of data that the current passive pressure recommendation is based on, it is desirable to have additional data points to verify or modify this value. FASTER COPMUTER PROGRAMS With the advent of faster and cheaper microcomputers, use of recent advanced computer programs for site response and soil-structure interaction evaluation has become more affordable thus making it possible to accommodate these analyses into projects with limited budgets and demanding schedules. However, time-history analyses can still be slow and time consuming. Furthermore, the results from time-history analyses are voluminous and can overwhelm the user. Faster and user-friendly computer programs for seismic soil-structure interaction evaluations with effective pre-processors for data input and post-processors/animation techniques for visualization and presentation of results are needed to advance the state of practice. CONCLUSIONS Additional research effort must be focused on many areas of geotechnical earthquake engineering to improve the current state of practice. Some areas needing immediate attention to develop guidelines were discussed in this paper. In the future, as the geotechnical profession is challenged to develop more efficient designs, researchers will in turn be challenged to focus their efforts on new areas in order to supply the profession with appropriate tools. Potential long-term research areas include, evaluation of unsaturated soil behavior under earthquakes and dynamic modeling of three-dimensional problems. An additional challenge for the geotechnical engineers is to understand the structural design implications of the geotechnical recommendations since in most cases, the end user of the geotechnical recommendations are structural engineers. Efforts should be focused on overcoming these challenges through effective collaboration between geotechnical and structural researchers and practitioners. REFERENCES Arulanandan, K., and Scott, R. F. 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