SEISMIC SETTLEMENT OF SHALLOW FOUNDATIONS



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10NCEE Tenth U.S. National Conference on Earthquake Engineering Frontiers of Earthquake Engineering July 21-25, 2014 Anchorage, Alaska SEISMIC SETTLEMENT OF SHALLOW FOUNDATIONS S. Prakash 1, V.K. Puri 2, and S. Kumar 3 ABSTRACT Foundations failures have been observed during several earthquakes because of excessive settlement and tilt. The problem of settlement due to dynamic loads has attracted the attention of researchers since early sixties. Shallow foundations subjected to static and seismic loads have mostly been designed using pseudo-static approach, the settlement and tilt of the foundation was also calculated using the static methods. Empirical equations for calculation of settlement and tilt of foundations subjected to static loads and moments have also been used for estimating the settlement and tilt for the seismic case. Earlier studies have indicated that the cyclic shear stresses induced by the earthquake ground motion are the main cause of seismic settlements. Vertical accelerations generally do not result in significant settlements unless they exceed about 1g. The research effort has therefore been dedicated towards determining the shear strains induced in the soil deposits and correlating these strains with the settlements. Simplified procedures similar to ones used for liquefaction analysis have also been used for estimating shear strains in soil deposits due to earthquake which is assumed equal to volumetric strain. The settlement can then be estimated using the volumetric strain and the thickness of the deposit. For the case of a layered deposit, the strain in each layer may be calculated and total settlement obtained as the cumulative settlement. The settlement calculated in this manner generally represents the settlement of soil deposits in the free field i.e. as if the foundation was not there. The foundation may experience additional settlement due to the loads and moments imposed on the foundation by the earthquake. There has been significant research effort devoted to account for such additional settlements by considering the reduction in shear modulus of soil by induced shear strains. The total settlement of the structure due to earthquake shaking obtained as the sum of these two components of settlement. Charts based on simplifying assumptions are available to determine the post volumetric strain for soils dry and partially saturated also soils that are likely to liquefy, using the normalized standard penetration data or relative density of sand and the factor of safety against liquefaction. 1 Professor Emeritus, MST Rolla, MO prakash@mst.edu 2 Professor, Department of Civil and Environmental Engineering, SIU Carbondale, IL, puri@engr.siu.edu 3 Professor and Chair, Department of Civil and Environmental Engineering, SIU Carbondale, IL, kumars@siu.edu Prakash, S., Puri, V.K. and Kumar, S. Seismic settlement of shallow foundations. Proceedings of the 10 th National Conference in Earthquake Engineering, Earthquake Engineering Research Institute, Anchorage, AK, 2014.

Seismic Settlement of Shallow Foundations S. Prakash 1, V.K. Puri 2, and S. Kumar 3 ABSTRACT Foundations failures have been observed during several earthquakes because of excessive settlement and tilt. The problem of settlement due to dynamic loads has been the subject of research since early sixties. Shallow foundations subjected to static and seismic loads have mostly been designed using pseudo-static approach, the settlement and tilt of the foundation was also calculated using the static methods. Empirical equations for calculation of settlement and tilt of foundations subjected to static loads and moments have also been used for estimating the settlement and tilt for the seismic case. Earlier studies have indicated that the cyclic shear stresses induced by the earthquake ground motion are the main cause of seismic settlements. Vertical accelerations generally do not result in significant settlements unless they exceed about 1g. The research effort has therefore been directed towards determining the shear strains induced in the soil deposits and correlating these strains with the settlements. Simplified procedures similar to ones used for liquefaction analysis have also been used for estimating shear strains in soil deposits due to earthquake which is assumed equal to volumetric strain. The settlement can then be estimated using the volumetric strain and the thickness of the deposit. For the case of a layered deposit, the strain in each layer may be calculated and total settlement obtained as the cumulative settlement. The settlement calculated in this manner generally represents the settlement of soil deposits in the free field i.e. as if the structure was not there. The foundation may experience additional settlement due loads and moments imposed on the foundation by the earthquake. There has been considerable research effort devoted to estimate these additional settlements by considering the reduction in shear modulus of soil by induced shear strains. The total settlement of the structure due to earthquake shaking may be obtained as the sum of these two components of settlement. Charts based on simplifying assumptions are available to determine the post volumetric strain for soils, both non-liquefiable and likely to liquefy using the normalized standard penetration data or relative density of sand and the factor of safety against liquefaction. Introduction Foundation failure due to earthquakes have been observed during several past and recent earthquakes. Such failures have occurred in soils prone to liquefaction as well as in soils which did not liquefy Failures of shallow foundations have been observed in Mexico City during Michoacan earthquake of 1985 [1] and in city of Adapazari due to 1999 Kocaeli earthquake [2,3 and 4]. Typical examples of bearing capacity failure in Adapazari are shown in Fig. 1. 1 Professor Emeritus, MST Rolla, MO prakash@mst.edu 2 Professor, Department of Civil and Environmental Engineering, SIU Carbondale, IL, puri@engr.siu.edu 3 Professor and Chair, Department of Civil and Environmental Engineering, SIU Carbondale, IL, kumars@siu.edu Prakash, S., Puri, V.K. and Kumar, S. Seismic settlement of shallow foundations. Proceedings of the 10 th National Conference in Earthquake Engineering, Earthquake Engineering Research Institute, Anchorage, AK, 2014.

The surface soils at the site of foundation damage belong to CL/ ML group which are generally considered non-liquefiable. Settlements of as much as 0.5-0.7m have been observed in loose sands in Hachinohe during the 1968 Tokachioki earthquake of magnitude 7.9. Settlements of 0.5-1.0 m were observed at Port and Roko Island in Kobe due to the Hygoken Nanbu (M=6.9) earthquake. Foundation failures may occur due to reduction in bearing capacity, excessive settlement and tilt, both in liquefying and non-liquefying soils. Typical examples of damage due to earthquakes are shown Figs. 1, 2 and 3. The settlement of the foundation due to applied loads is one of the most important considerations in ensuring the safe performance of the supported structure. The procedures generally followed to estimate settlement of foundations due seismic load are available in literature and are reviewed below. Fig.1. Failures of Shallow Foundations in Adapazari [4] Fig.2 Failure of apartment buildings at Kawagishi-Cho, Niigata, due to liquefaction of the soil during the 1964 (M=7.5) Niigata Earthquake Settlement of Shallow Foundations on Non-liquefiable Soil Most shallow foundations for earthquake loads are designed by following the psuedo-static approach. The settlement and tilt of the foundation is also commonly obtained by using same procedures as for a foundation subjected to static vertical loads and moments. The following

Fig. 3. Failure due sliding and tilting of houses due to liquefaction in the Turnagain Height area of Anchorage during the 1964 Alaska Earthquake ( M= 8.6) methods can be conveniently used in this case. Prakash and Saran [5] Method A procedure to determine the settlement and tilt of foundations subjected vertical load and moment was developed by Prakash and Saran [5] which uses Eqs. (1and 2). =1.0 1.63 2.63 + 5.83 (1) =1.0 2.31 22.61 + 31.54 (2) Where, S o = settlement at the center of the foundation for vertical load only S e = settlement at the center of the eccentrically loaded foundation (combined action of vertical load and moment) S m = maximum settlement of the eccentrically loaded foundation B = width of the foundation E = eccentricity given by e =, Q = vertical load and M = moment. The tilt of the foundation t may then be obtained from the following equation: = + sin (3) S e, S m and t can thus be obtained if S o can be determined. Prakash and Saran [5] have suggested the use of plate load test to determine S o. The value of S o can also be obtained by any other procedure commonly used for determination of immediate or elastic settlement of foundations. The method can be used to make a preliminary estimate of settlement and tilt. Richards et al, [6] Method (Richards et. Al;[6] suggested the use of the following equation to estimate the seismic settlement of a strip footing using equation (4).

2 4 V k S ( m ) 0.174 h * Eq tan α AE Ag A = (4) Where, S Eq = seismic settlement (in meters), V = peak velocity for the design earthquake (m/sec), A = acceleration coefficient for the design earthquake, g = acceleration due to gravity (9.81 m/sec 2 ). The value of tan α AE in Eq (4) depends on φ and k h *. Figure 4 shows the variation of tan α AE with k h * for φ values from 15-40. Figure 4. Variation of tan α AE with k h * and φ [6] Several other researchers have also suggested procedures for determining the settlement and tilt of the foundations subjected to static vertical loads and moments. Settlement of Foundations in Liquefying Soil Simplified Procedures for the Evaluation of Settlements of Structures During Earthquakes Ishihra and Tokimatsu [7] A procedure to determine earthquake induced settlements of structures on saturated sand deposits due to pore water pressure generation was developed by Ishihara and Tokimatsu [7]. To investigate the effectiveness of the proposed method, the observed values of settlement of structures were also compared with the values obtained from the proposed method. The total settlement of the structure due to earthquake shaking (S st ) is given as: S st = S v + S e (5) where, S v = settlement due to volumetric strain caused by earthquake shaking S e = immediate settlement due to change in soil modulus.

Knowing the value of the cyclic stress ratio developed in the soil during earthquakes and normalized (N 1 ) 60 value, the volumetric strain can be determined from Fig. 5 below. Fig 5 Cyclic Stress ratio, (N1)60 vs. Volumetric Strain [8]. The relationship shown in Fig. 5 was proposed earlier by Tokimatsu and Seed [8] which is based on the controlling factors like maximum pore pressure generated before initial liquefaction and the maximum shear strain after liquefaction. The cyclic stress ratio developed in the soil during earthquakes is given as:. = 0.65 r m (6) where,. = Equivalent Shear Stress Ratio induced by the earthquake shaking of M = 7.5 a max = maximum horizontal acceleration at the ground surface σ o = total overburden pressure at the depth considered. r d = Stress reduction factor that varies with depth. r m = Scaling factor for a stress ratio concerning the magnitude of earthquake By integrating the volumetric strains for different depths, the settlement of the structure can be computed. For values of M other than 7.5, magnitude scaling factors may be used. Ishihara and Tokimatsu [7] suggested that the immediate settlement caused by the change in soil modulus can be computed as: S e = q.b.i p (7) Where, q = contact pressure of the structure B = width of the structure I p = coefficient concerning the dimension of the structure, thickness of soil layer and Poisson s ratio of soil.

E 1 and E 2 = Young s Moduli of soil before and during earthquake shaking respectively. The reduction in the shear modulus of soil during earthquake shaking can be computed based on the effective shear strain (γ eff ) induced in the soil as given in Eq. (8) below: γ eff = 0.65.. σ o.r d. (8) Fig. 6 Determination of induced Shear Strain [8]. Fig 7: Scaling factor vs. width ratio where, G max = Shear modulus at low shear strain level G eff = effective shear modulus at induced shear strain level a max = maximum horizontal acceleration at the ground surface σ o = total overburden pressure at the depth considered. Using the computed value of γ eff in graph in Fig. (6), the value of corresponding effective

shear strain (γ eff ) is obtained and G eff can be calculated. They have further emphasized that the change in effective stress due to pore pressure generation as well as the shear strain level developed in the soil are highly influenced when there is liquefaction and therefore, do not recommend to use Eq. (7) to compute the settlement of structure. In such condition, the settlement of the structure is affected due to the shear deformation of the soil strata and thus young s modulus can t be accurately determined. Accordingly, they have estimated an approximate relationship based on the field observations as given in Eq. (9). S st = S v.r b (9) Where, r b = scaling factor concerning the shear deformation which may be obtained from figure 7. Based on the studies of Niigata earthquake (1964) done by Ishihara and Tokimatsu [7], the importance of large width of the structure (compared to the thickness of the liquefied layer) on reducing the liquefaction induced settlement can be noted very clearly from figure 7. It can be seen from Fig. (7) that appreciable settlement occurred where the width ratio was less than 2 whereas the settlement was small and constant where the width ratio exceeds 2 or 3. Ishihara and Tokimatsu [7] developed parameter r b that is equal to the settlement ratio normalized by the settlement ratio at width ratio equal to 3. They found the computed values generally consistent with the observed values, and proposed that this simplified method of computation can be used as a first approximation to predict earthquake induced settlement of structures. Ishihara and Yoshmine [9] Ishihara and Yoshmine [9] have provided a chart to estimate the post-liquefaction volumetric strain of clean sand as function of factor of safety against liquefaction. This chart is shown in figure 8. This chart can be easily used if any of the corrected SPT values, cone resistance at the site or the maximum cyclic shear strain induced by the earthquake are known. The chart in Fig. 8 is convenient to use. The factor of safety against liquefaction failure is calculated and then the volumetric strain is determined using value of relative density of the deposit or its the corrected standard penetration resistance or cone penetration resistance. The settlement of the deposit may then be calculated as : = (10) where, S= settlement H= thickness of the deposit, and = volumetric strain. For deposits consisting of various layers of saturated sand, the settlement for each layer may be calculated and the total settlement obtained as the sum of the settlements of each layer. Additional Comments on Foundation Performance on Liquefied Soil Gazetas et. al; [10] studied tilting of buildings in it1999 Turkey earthquake. Detailed scrutiny of the Adapazari failures showed that significant tilting and toppling were observed only in relatively slender buildings (with aspect ratio: H / B > 2), provided they were laterally free from

2.0 1.8 1.6 1.4 FS L 1.2 1.0 0.8 0.6 0.4 0.2 3 % 3.5 % 4 % 6 % D r= 70 8 % [(N 1) 60=20, q =110] c1 D r=80 max = 10 % [(N 1) 60=25, q c1=147] D r = 90% 2 [(N 1) 60=30, q c1=200kg/cm ] D r= 40 D r= 30 D r= 50 (N ) =6 (N 160 160 ) =3 D r= 60 (N ) =10 160 q =45 q =33 c1 c1 (N q =60 1) 60=14 c1 q =80 c1 0 10 20 30 40 50 Post Liquefaction Volumetric Strain, v(%) Fig. 8. Chart for Post Liquefaction Volumetric Strain [9]. other buildings on one of their sides. Wider and/or contiguous buildings suffered small if any rotation. For the prevailing soil conditions and type of seismic shaking; most buildings with H / B > 1.8 overturned, whereas building with H / B < 0.8 essentially only settled vertically, with no visible tilting. Figure 9 shows a plot of H/B to tilt angle of building. Soil profiles based on three SPT and three CPT tests, performed in front of each building of interest, reveal the presence of a number of alternating sandy-silt and silty-sand layers, from the surface down to a depth of at least 15 m with values of point resistance q c (0.4 5.0) MPa. Seismo cone measurements revealed wave velocities Vs less than 60 m/s for depths down to 15 m, indicative of extremely soft soil layers. Ground acceleration was not recorded in Tigcilar. Using in 1-D wave propagation analysis, the EW component of the Sakarya accelerogram (recorded on soft rock outcrop, in the hilly outskirts of the city) leads to acceleration values between 0.20 g -0.30 g, with several significant cycles of motion, with dominant period in excess of 2 seconds. Even such relatively small levels of acceleration would have liquefied at least the upper-most loose sandy silt layers of a total thickness 1 2 m, and would have produced excess pore-water pressures in the lower layers. Discussion Evaluation of foundation settlement for a wide range of soil, foundation and earthquake parametersis complicated. The empirical charts and relationships developed are based on the several assumptions and are limited to some specific conditions which cannot be generalized to other combinations of foundation load and diameter, density and thickness of the liquefiable sand layer and intensity and duration of shaking.

Fig.9. The angle of permanent tilting as a unique function of the slenderness ratio H/B (Gazetas et. al;[10]. The present practice of estimating liquefaction induced settlement based on post-liquefaction reconsolidation settlements under free field conditions might misrepresent and largely underestimate the consequences of liquefaction (Andrianopoulos et al; [11], Dashti et. Al; [12], and Liu and Dobry [13].This practice ignores the deviatoric deformation (settlements due to the cyclic inertial forces acting on the structures within the liquefiable soil under a building s foundation as well as volumetric deformations due to localized drainage during shaking. Presently, well calibrated analytical tools and design procedures that identify, evaluate and mitigate the most critical mechanisms of liquefaction induced settlement are wanting. Due to the discontinuousness of soil skeleton and large amount of lost pore water and continued loss in soil stiffness, it is very difficult to exactly reflect the actual performance of buildings in liquefying soils (Liu, [14]. Duku et. al;[15]) have investigated the use cyclic simple shear tests to estimate the volumetric compression in clean sand. They also identified the significant parameters affecting volumetric compression under cyclic loading conditions. Cone penetration approach has also been used to estimate liquefaction induced settlements [16]. Conclusions Considerable research effort has been devoted to the determination of seismic settlement of foundations. Experimental, and analytical procedure have been used to study the settlement of foundations. Use of SPT and CPT tests provides simple solutions for estimating seismic settlements. There is need for simple but reliable methods for estimating foundation settlement. References 1. Mendoza, M.J. and Avunit,G. (1988) The Mexico Earthquake of September 19,1985-Behavior of Building Foundations in Mexico City, Earthquake Spectra, 4(4): 835-853. 2. Karaca, G. (2001), An Investigation into Large Vertical Displacement Experienced by the Structures in Adapazari during 17 August 1999 Earthquake, MS thesis, Middle East Technical University, Ankara, Turkey. 3. Bakir, B.S., Sucuoglu, H. and Yilmaz, T. (2002), An Overview of Local Site Effects and the Associated Building Damage during 17 August 1999 Izmit Earthquake, Bulletin of seismological Society of America, 92(1): 509-526, 2002. 4. Yılmaz, M. T., Pekcan, O., Bakır B. S. 2004. Undrained cyclic shear and deformation behavior of silt-clay

mixtures of Adapazarı, Turkey. Soil Dynamics and Earthquake Engineering, Vol. 24(7), 497-507. 5. Prakash, S. and Saran, S.(1977), Settlement and Tilt of Eccentrically Loaded Footings, Journal Structural Engineering, Roorkee, Vol. 4, No. 4, pp. 166-176. 6. Richards, R., Elms, D.G. and Budhu, M. (1993), Seismic Bearing Capacity and Settlement of Foundations, Journal of Geotechnical Engineering Division, ASCE, Vol. 119, No. 4, April, pp 662-674. 7. Ishihara, K and Tokimatsu, K. (1988). Simplified Procedures for the evaluation of settlements of structures during earthquakes, Proceedings of Ninth World Conference on Earthquake Engineering, Tokyo-Kyoto, Japan, 3, 95-100. 8. Tokimatsu, K. and Seed, H.B. (1987). Evaluation of Settlements in Sand Due to Earthquake Shaking. J. of Geotechnical Engineering, ASCE. Vol. 113(8): 861-878. 9. Ishihara, K. and Yoshimine, Y., (1992), Settlement of buildings on saturated sand during earthquakes, Soils and Foundations, Vol. 17, No. 1, pp. 23-38. 10. Gazetas, G., Apostou, M. and Anasta- Sopoular, J.(2004), Seismic Bearing Capacity Failure and Overturning of Terveler Building in Adapazari 1999, Proc. Fifth Inter.Conf on Case histories in Geotechnical Engineering. New York CD ROM SOAP11(1-51), 2004. 11. Andrianopoulos, K.I., Bouckovalas, G.D., Karamitros, D.K., & Papadimitriou, A.G. (2006). Effective Stress Analysis for the Seismic Response of Shallow foundations on Liquefiable Sand, Numerical Methods in Geotechnical Engineering, Proceedings of the 6th European Conference on Numerical Methods in Geotechnical Engineering. 12. Dashti, S., Bray, J.D., Pestana, J.M., Riemer, M. & Wilson, D. (2010 b). Centrifuge testing to evaluate and mitigate liquefaction induced building settlement mechanisms, J. Geotech. Geoenviron. Engng., ASCE, 136(7), 918-929. 13. Liu, L., Dobry, R., (1997). Seismic Response of Shallow Foundation on Liquefiable Sand. J. Geotech. Geoenviron.Engng.,ASCE, 123(6), 557-567. 14. Liu, H. (1995). An Empirical Formula for the Evaluation of Building Settlements due to Earthquake Liquefaction. Proc. 3 rd Inter. Conf. Rec. Adv. Geotech. EQ Engrg. & Soil Dyn., Vol. 1, 289-293. 15. Duku, P.M., Stewert, J.P., Whang, D.H. and Yee, E.(2008), Volumeteric Strains of Clean Sands Subjected to Cyclic Loads, Journal of Geotechnical and geo-environmental Engineering, ASCE, Vol. 134, No. 8,.1073-1085. 16. Zhang, G., Robertson, P.K. and Brachman R.W.I.,(2002), Estimating Liquefaction Induced Ground Settlements from CPT for Level Ground Conditions, Can. Geotech. Journal, No. 39, pp 1168-1180.