THE LIMIT VALUES AND THE DISTIBUTION OF THREE-DIMENSIONAL PASSIVE EARTH PRESSURES STANISLAV ŠKRABL About the author Stanislav Škrabl University of Maribor, Faculty of Civil Engineering Smetanova ulica 17, 2000 Maribor, Slovenia E-mail : stanislav.skrabl@uni-mb.si Abstract This paper presents a novel approach to the determination of the critical distribution and limit values of three-dimensional passive soil pressures acting on flexible walls following the upper-bound method within the framework of the limit-analysis theory. The method of limit analysis with a set of three-dimensional kinematically admissible hyperbolic translational failure mechanisms is used to determine the critical distribution of the passive pressures along the retaining structure's height. The intensity of the passive pressures is gradually determined with the mentioned translational failure mechanisms in the top-down direction. Thus, the critical distribution, the trust point and the resultant of the passive pressures that can be activated at the limit state for the chosen kinematic model are obtained. The results of the analyses show that the total sum of passive pressures, considering the critical distribution, is lower than the comparable values published in the literature. Furthermore, the trust point of the passive pressure resultant is independent of the friction between the retaining structures and the soil. Keywords limit analysis, earth pressure, passive pressure, failure surface, soil-structure interaction 1 INTRODUCTION In geotechnical practice, the results of three-dimensional analyses of passive earth pressures are used to design some anchor systems, to ensure the stability of the foundations of arching and bridging structures, to design embedded caissons and other retaining structures with spaced out vertical supporting elements, etc. It is only logical that research into passive earth pressures is frequently presented in the literature. The major part of the research deals with 2D stability analyses, while much less attention is paid to 3D analyses. The magnitudes of the earth pressures for the active and passive limit states can be determined by different methods: the limit-equilibrium method (Terzaghi 1943), the slip-line method (Sokolovski 1965) and the limit-analysis method (Chen 1975). In the limit-equilibrium and slip-line methods the static equilibrium and failure conditions are considered, while the expected movements of the retaining structures are not directly considered in the analysis. Generally, a limit analysis serves for determining the upper and lower bounds of the true collapse load by taking into account the supposed movements. The results of the analyses can differ essentially, because they depend on the chosen failure mechanism or the kinematic model of the limit state. Irrespective of the chosen procedure and the method used, the considered static or kinematic model should be in equilibrium when the limit state is reached. Researchers have used many different methods to determine earth pressures, among them Coulomb (1776), Brinch Hansen (1953), Janbu (1957), Lee and Herington (1972), Shields and Tolunay (1973), Kerisel and Absi (1990), Kumar and Subba Rao (1997), Soubra and Regenass (2000), Soubra (2000), Skrabl and Macuh (2005) and Vrecl-Kojc and Skrabl (2007). The above-cited, published research mainly considers the 2D problem of passive earth pressures. The results of 3D analyses have been presented only by Blum (1932), ACTA GeOTeCHNICA SLOVENICA, 2008/i 37. S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE ËflRTH PRESSURES and to a restricted extent. Extensive 3D analyses were treated by Ovesen (1964), who presented the procedure for determining the bearing capacity of different anchor plates based on 2D solutions of passive earth pressures and the results of several experimental studies in 3D conditions. presented geomechanical analysis is based on the following suppositions and limitations: - the structure discussed is a vertical, flexible wall with an area of bh (b = width; h = height) and a horizontal backfill, Soubra and Regenass (2000) published the results of an analysis for determining the 3D passive pressure according to the limit-state analysis using the upper-bound theorem for the translational kinematic admissible multi-block failure mechanism. Duncan and Mokwa (2001) treated the procedures for determining the bearing capacities for anchor plates and presented the results of several experimental studies. Skrabl and Macuh (2005) presented the procedure for a spatial passive pressure analysis based on the hyperbolic kinematic admissible failure mechanism and the upper-bound theorem. The authors of all the above-mentioned works considered the presumed distribution of passive pressure along the retaining wall height (a triangular distribution for the determination of the self-weight contribution, y , and a rectangular distribution for the determination of the surcharge contribution, q). This paper considers the distribution of passive earth pressures along the retaining structure height. The passive pressures distribution is determined numerically with simultaneous analyses of twenty different kinemati-cally admissible translational spatial failure mechanisms. The results of the analyses show that the resultants of the passive pressures obtained by the presented, proposed procedure give values, lower than those published in the literature for almost all cases; only for the case when S = 0° and 0 < 30° are the differences minimal, where the values are a little lower or equal to the values presented by Soubra and Regenass (2000), and Skrabl and Macuh (2005). The application of the upper-bound theorem ensures that the actual values of the passive soil pressures cannot be higher than the values presented in the continuation of this paper. the distribution of the passive pressures (pp) along the wall height is defined by: pp = ePy ■ y-{y - yo )+epq ■ q+< (1) where factors ePY , epq and epc define the distribution p> pq pc of the passive pressures along the height of the vertical wall, andy andy0 are the coordinates (see Fig. 1), the resulting value of the passive earth pressure is defined by: h2 * * • 7—b + Kpc • c h-b + Kpq • q -h-b (2) Pp = K Py 2 where KpY, Kpc and Kpq are comparative coefficients of the passive earth pressure due to the soil-weight influence, the cohesion influence, and the surcharge influence, respectively, for a standard, assumed passive pressure distribution, the value of the factor epy at the top of the wall (y=y0) is equal to 0, its appurtenant values epq and epc are determined with a two-dimensional model (b/h = œ) considering the boundary condition for the 3D kinematic admissible failure mechanism, the discussed translational failure mechanism is bounded by the log spiral in the region of the retaining wall, and by the hyperbolic surfaces defined by the envelope of the connected hyperbolic half-cones at the lateral sides, the lateral surfaces coincide with the margins of the considered retaining wall, the backfill is homogenous, the soil is isotropic and considered as a Coulomb material with the associative flow rule obeying Hill's maximal work principle. 2 ASSUMPTIONS AND LIMITATIONS It is a characteristic of passive earth pressures under 3D conditions that they increase as the width of the wall decreases. The value depends on the ground properties and the height/width relationship of the wall. It can be several times higher than the value for 2D cases. The 3 THE UPPER- AND LOWER-BOUND THEOREMS The upper-bound theorem ensures that the rate of the work due to the external forces of the kinematic systems in equilibrium is smaller than, or equal to, the rate of dissipated internal energy for all kinematically 22. ACTA GEOTECHNICA SLOVENICfl, 2008/l S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE GARTH PRESSURE admissible velocity fields. The kinematically admissible velocity fields obey strain-velocity compatibility conditions and velocity boundary conditions, as well as the flow rule of the considered materials. The lower-bound theorem for rigid-plastic material using the associative flow rule enables an evaluation of the lower-bound theorem of the true passive earth pressures for each statically admissible stress field that satisfies the equilibrium and stress boundary conditions, and does not violate the yield criteria anywhere. The true value of the failure load is bracketed between both limit values with the expected deviations, which are usually acceptable in geotechnical design. The presented research considers only the upper-bound theorem of the limit analysis to determine the 3D passive earth pressures using the kinematically admissible velocity field. The solution of the 3D passive earth pressure problem according to the kinematic approach is equivalent to the solution of the limit-equilibrium approach (Mroz and Drescher 1969; Michalowski 1989; Salençon 1990; Drescher and Detournary 1993). The aim of the presented research is to improve on the known lowest values of the upper-bound solutions presented in the literature (Soubra and Regenass 2000, Skrabl and Macuh 2005) using a more exacting passive pressure distribution. 4 TRANSLATIONAL 3D FAILURE MECHANISM The applied 3D translational failure mechanism represents an extension of the plane slip surface in the shape of a log spiral (see Fig. 1). A very similar 'friction cone' mechanism in the upper-bound analysis of a 3D bearing-capacity problem was used by Michalowski (2001). Every point along the retaining wall height (1-0, see Fig. 1) is given an exactly defined and kinematically admissible hyperbolic friction cone. The flexionally curved axis and the cross-section of the shaft surface with the plane r-9 (see Fig. 1) are: r°o = r- cosh(($ - )tan^>) (3) r = r ■ e (0—0, )tan $ r = r ■ e -(0—0,)tan $ (4) (5). The radius and the centre of the arbitrary half cone in the r-z plane are: R* = r* ■ sinh[($ — $*)tan$] (6) where R* , r* and 9* denote the cone diameter in the cross-section of the plane 9-z, and the polar coordinates of the apex of the hyperbolic half-cone. Figure 1. Cross-section of the failure mechanism. ACTA GEOTECHNICA SLOVENICA, 2008/i 33. S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE ËflRTH PRESSURES Figure 2. The scheme of the spatial failure mechanism. All hyperbolic half-cones whose infinite set represents the lateral surface of the failure mechanism are also kinematically admissible when the additional geometry condition is satisfied: Vr >- -A r < r ; §0 < [t/2 — (7) which ensures that there exists no half-cone with its apex on the vertical wall (1-0, see Fig. 2) that could intersect the vertical wall under point (r0,$0). Since all the hyperbolic half-cones are kinematically admissible, then using the additional condition (7) the lateral surface, which is the envelope of the infinite set of all half-cones defined by expressions (8), (9) and (10), is also kinematically admissible. r& = r,cosh[($ — $„)tan 0] — r,sinh[($ — $„)tan 0]sin(e.) (8), zs = r,sinh[(§ — §,)tan 4 ]cos(e„) (9), tanh [( § — & )tan 4] + tan 4 tan s, = arcsin(dR, /dr) = arcsin 1 + tanh [(§ — §,)tan0]tan0 tan (10). Considering r* = r1 and = , expressions (8), (9) and (10) define the coordinates of the envelope on the leading half-cone. The coordinate zf of the lateral failure surface can be expressed: 1 sin § zf = zs, = r,sinh[(§ — §,)tan 4 ]cos(e») (11) Vr > rs A r < r1e (§—§1)tan 4 (12) Zf = z(r, §) = ^2rr1 cosh[(§ — §1)tan0 ] — r2 — r12 5 WORK EQUATION The considered failure mechanism on the width b is limited on the left by a vertical wall, on the right by a curved surface in the shape of a log spiral, and above by an even surface on which the surcharge can act. Both lateral surfaces are defined by the curved surfaces of the leading half-cone and the envelope of all the other hyperbolic half-cones (see Fig. 2). At each point on the so-formed failure surface the normal vector of the surface encloses with the plane r-z shear angle 0 and also defines the direction of the normal stress to the surface (see Fig. 3). dN = a dA, dT0 = dN tan0, dQ0 = ^dN2 + dT2 (13) where a and A denote the normal stress and the area of the lateral surface, and N and T^ denote the resultant x 0 22. ACTA GEOTECHNICA SLOVENICfl, 2008/l S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE GARTH PRESSURE 9o ru Figure 3. The forces on the failure surface. values of the normal and the shear-stress components on the spatially formed failure surface. The shear cones on the failure surface define all the real or admissible directions of the forces dT^ and dQ^ (see Fig. 3). According to the upper-bound theorem the analyses should consider those directions of shear-strength activation that are kinematically admissible and ensure the highest possible value of the passive pressure for the chosen failure mechanism. The considered spatially formed failure body is certainly symmetrical in the symmetry plane r-9 that runs through the centre of the rectangular wall surface, and should be in equilibrium, considering all the forces that act on it. Certainly, all the forces dQ^ act in the plane r-z, and so they do not cause any momentum around the z axis, which runs through the coordinate system's origin. Like in the 2D analyses, the equilibrium condition of all the momentums around the z axis is chosen for the work equation. From Fig. 3 it is evident that the maximum possible passive pressures arise when the shear force dT^ acts at each point of the failure surface in a direction that is defined by the cross-section of the normal plane through the centre of the hyperbolic half-cone and the tangent plane to the failure plane through the considered point. The coefficients of the individual parts of the passive pressure epy and epq (let us call them the coefficients of passive pressure distribution) in the 3D problem are not constant along the wall height h. Certainly, they increase non-linearly with increased ratios of b/h. If y ^ 0, 0 # 0, S # 0 and q = c = 0 the work equation can be given in the following integral form: f ( x0 )(Cos£ cos $ sin£ tan $ tan $„ sin3 $ sin2 $ 2 '1" f f (1 + 2zf / b)sin $ r2drd$ = 0 $o yo/cos$ 01 )d$ -f f (1 + 2zf / b)sin $ r 2drd$- (14) $ $ xn / sin $ 10 ACTA GEOTECHNICA SLOVENICA, 2008/i 33. S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE ËflRTH PRESSURES And when y = 0, 0 # 0, S # 0, q # 0, and c = 0 it can be given in the following integral form: J cosC cos $ sinC )d$ -j (1 + 2zf /tyyl-^^Ldd = 0 (15) J 1 cos3 $ sin3 $ sin2 $ At point y = y0 and when b/h = the factor of the passive pressure distribution is epy = 0, and the appurtenant value of the factor of the passive pressure distribution epq is determined with a 2D model considering the geometry condition (7). The unknown functions e^y = e (0, S, b/h) and epq = epq (0, S, b/h), which are the minimal possible solutions of the integral expressions (14) and (15) for all real ratios b/h, define the distribution of the passive pressures along the wall height. The minimum values of and e can be determined numerically for an individual in advance for known ratios of b/h. The geometry model (height h = 1, unit weight y = 1 and ratio b/h) and the soil characteristics (shear angle 0 and the friction between the soil and the wall S) were used in our analysis. 6 NUMERICAL ANALYSIS AND RESULTS The values of the passive pressure distribution factors epy and epq are determined gradually from the top of the wall downwards for different ratios of b/h (b/h = 100, 75, 50, 25, 20, 16 down to 0.25), as can be seen in Fig. 4. It is assumed in the analysis that the passive pressures increase linearly between the individual calculation points upwards of the wall height. For each calculating point along the wall height there is an exactly determined spatial failure surface, which ensures the smallest possible value of the factors of the passive pressure distribution, ePY and epq , for the chosen ratio b/h. py pq In step m of the passive pressure determination, the minimum values of the factors e° to e'"1 and ePq to e"*-1 p ! p ! pq pq are known from the preceding steps. The appurtenant known momentums can be determined with the expres- The numerical resolving of the integral equations (14) and (15) is performed by dividing the analysed region in the x-y plane into an arbitrary number of triangular and rectangular finite elements. These are suitable for Gauss's numerical integration as well as for the calculation of the integral over the area of the plane y = y0 , where one-dimensional Gauss's numerical integration elements (see Fig. 4) are used. fm-1 m- , , ^¡+1- yi-1) c (y- + y, + y,+1) ■ c U, =£ep-,(y,-y0)-±-n—cosC-r—+— x0sinC (16), /T1 = e Pq (^) [cos C ^^ - x0 sin C1 + ' pq m— 1 £ • ¡=1 pq (y,+1 - y,-1) pq Ay,-1 + yt + y,+1) . , cosC--x„ sin c (17), Figure 4. Passive pressure distribution and the scheme of the numerical integration. $ $ $ 22. ACTA GEOTECHNICA SLOVENICfl, 2008/l S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE GARTH PRESSURE /■m _ Py = /•m _ pq = ( ym y m—l) Pi 2 ( ym ym—1) 2 cos S(ym—1 + 2 ym) — x0 sinS cosS(ym—1 + 2ym) — v sinS (18), (19), where fm 1 and fm 1 define the momentums of the J py J pq already known values of the passive pressures, and fPY and fm , the momentums of the passive pressures for em^f = 1 and ¿m^ = 1, according to the origin of the coordinate system x-y-z. The appurtenant momentum of the unit weight of the ground (y = 1) and the surcharge (q = 1), above the failure surface are determined using expressions (20) and (21). gr< = —EEKwk (1 + 2zf /b)rjk sin (20) j=1 k=1 where A'yy denotes the area of the triangular or rectangular element j in the plane x-y (see Fig. 4), Wjk is the weight coefficient for Gauss's integration point k, zf is the coordinate z on the envelope of the hyperbolic half-cones, rjk is the radius of the integration point k on element j in the plane x-y, and $jk is the appurtenant angle of the radius rjk. In the numerical integration of the considered problem in plane x-y, 514 rectangular and 42 triangular elements with 9 and 6 Gauss's integration points were used (see Fig. 4). P r gpq = —EELxyWk (1 + 2zf /b)rlk sinVlk (21), i=1 k=1 where denotes the length of a one-dimensional integration element l on the ground surface y = y0 in the plane x-y (see Fig. 4), wlk is the weight coefficient for Gauss's integration point k, zlfk is the coordinate z of the integration point on the envelope of the hyperbolic half-cones in the plane y = y0 , rlk is the radius of the integration point k on element l in the plane x-y, and $lk ACTA GEOTECHNICA SLOVENICA, 2008/i 33. S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE ËflRTH PRESSURES is the appurtenant angle of the radius rlk. In the numerical integration of the considered problem in the plane, 42 one-dimensional integration elements with 3 Gauss's integration points were used. The unknown values of the passive pressure distribution factors are determined using: em — Py g - f &PY J t P ft em — pq g - f &pq J t pq Py ft (22), pq In the numerical procedure determining the minimal value of the passive pressure distribution factors e^ and em , the starting failure surface in the optimization procedure is determined with the initial values of the parameters and $2, which should satisfy the following boundary conditions: > 0, y0 > 0, > (n/2) -< (23). Mathematical optimization was used to determine the unknown parameters and §2 of the critical failure surface, which defines, in the considered calculation step, the minimal value of the unknown factor of the passive pressure distribution, e^ the wall. and em , at the toe of pq The Solver Optimization Tool (Microsoft Excel) with the generalized-reduced-gradient method was used in the minimization process. The result of the gradual determination of the passive pressure distribution factors from the top of the wall downwards are the numerical values of the factors epY and epq, and a set of spatial failure surfaces that are presented in Fig. 5 for the case when $ = 40° and 8/$ = 1. The values of the factors of the passive pressure distribution, epy and e^ , for different values of $ , 5/$ and b/h are presented in Figs. 6 and 7. The values of the comparative passive pressure coefficients, K*ri and K, and the distances of the handling points of the resultants, ay , and a.q , from the surface of the backfill soil are presented in Tables 1 and 2. The values of the handling points are given for individual shear angles and given ratios b/h, where the numerically obtained results for different shear ratios 8/$ do not deviate by more than 0.5% from their average value. The appurtenant values of the substitutive coefficient and the distances of the resultants from the surface of the backfill soil are determined with the expressions (24) to (27). m m 1000 q 100 : 10 :\0>=45° 5/0=1 ------ 1000 0.25 0.5 1 2 b/h 5 10 25 1000 100 10 : 8/ 0=1/3 ^^0=45" .____ --- 0.25 0.5 1 2 b/h 5 10 25 1000 100 10 : 8/0=0 0.25 0.5 1 2 b/h 5 10 25 Figure 6. The factors of passive pressure distribution epy for different values of $ , 8/$ and b/h. 22. ACTA GEOTECHNICA SLOVENICfl, 2008/l S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THREE-DIMENSIONAL PASSIVE eflRTH PRESSURE m—1 Ky = E(en (y.— yo)(y,+i— y—)+em (y„— yo)(ym — ym—ù (24) i=1 m—1 = ^(e'p-f (y — yo)( y.+i— y.—i)(y.—1 + y. + y.+1—3 yo)/3) + ¡=1 ePY ( y m—yo)( ym—y m—1)( ym—1 +2 ym— 3 yo)/3 (25) m—1 K = e0q ( y1 — yo)/2 + £ (ep, ( y.+1 — y.—1 )/2 + emH ( ym — ym—1 ) /2 (26) .=1 m—1 = elq ( y1— yo)( y1— yo)/6+^(eM( y.+1— y.—1)( y.—1 + y. + y.+1— 3 yo)/6) + .=1 C( ym—ym—1)( ym—1 +2 ym—3 y o)/6 (27) In the analyses of the spatial stability problems the theorem of corresponding states (Caquot and Kérisel 1948, Soubra and Regenass 2ooo) is still valid. The comparative coefficient of the passive earth pressure due to cohesion ( K ) can be determined by using the comparative coefficient of passive earth pressure due to the surcharge ( K'pq ). K = KM — 1/cos(^) pc tan(^) (28) The values of c for the purely cohesive soil (c > 0 and 0 = 0) with different ratios of ca/c and with a centre of gravity of epc the pressures measured from the top of the wall are given in Table 3. 1000 g 100 10 ; ^0=45° 5/0=1 ^—v. —--- 1000 3 0.25 0.5 1 2 ^5 10 25 1000 1000 q 100 10 8/$=o 0.25 0.5 1 2 ^5 10 25 Figure 7. The factors of passive pressure distribution e pq for different values of 0 , S/0 and b/h. acta geotechnica slovenica, 2008/l 2Ç. S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE ËflRTH PRESSURES Table 1. Values of K*py for different values of the parameters f, 8 and b/h with the centre of gravity of the epy pressures measured from the top of the wall f 8/f center of b/h_(deg) 0 1/3 1/2 1/3 1 gravity 15 3.6279 4.1527 4.3864 4.6365 5.1458 0.712 20 5.3933 6.4350 7.0004 7.5984 8.8877 0.712 25 7.9261 10.0117 11.2456 12.6106 15.7108 0.725 0.25 30 11.8711 15.9410 18.5946 21.7237 29.5912 0.730 35 20.0486 27.6728 33.3372 40.5337 60.4985 0.734 40 43.0671 57.3693 69.2222 85.9233 139.1175 0.738 45 116.4677 149.3839 177.6761 220.0038 375.5334 0.741 15 2.6711 3.0260 3.2012 3.3775 3.7313 0.699 20 3.7238 4.4311 4.8126 5.2130 6.0592 0.706 25 5.2089 6.5721 7.3711 8.2474 10.2079 0.712 0.5 30 7.4363 9.9335 11.6437 13.5710 18.3323 0.718 35 11.9863 16.5711 19.9663 24.2567 36.0095 0.724 40 24.6495 32.8951 39.7426 49.3782 79.7705 0.729 45 64.2513 82.5392 98.8063 121.9540 208.4111 0.734 15 2.1892 2.4647 2.6014 2.7383 3.0092 0.687 20 2.8862 3.4211 3.7071 4.0047 4.6270 0.693 25 3.8439 4.8396 5.4156 6.0425 7.4308 0.698 1 30 5.8439 7.0201 8.1663 9.4902 12.6793 0.704 35 7.9191 11.0232 13.2817 16.1123 23.6998 0.710 40 15.4367 20.6573 25.0023 31.1047 50.0679 0.716 45 38.1335 49.1298 58.6535 72.9298 124.8263 0.723 15 1.8479 2.1801 2.2961 2.4114 2.6380 0.678 20 2.4651 2.9099 3.1455 3.3890 3.8937 0.683 25 3.1579 3.9637 4.4240 4.9214 6.0131 0.687 2 30 4.1095 5.5370 6.4305 7.4462 9.8331 0.691 35 5.9395 8.2498 9.9397 12.0356 17.5319 0.696 40 10.8269 14.5378 17.6323 21.9686 35.1861 0.702 45 25.0634 32.4150 38.8084 48.4179 83.0027 0.707 15 1.7980 2.0064 2.1091 2.2105 2.4084 0.672 20 2.2106 2.5986 2.8021 3.0112 3.4411 0.674 25 2.7423 3.4307 3.8182 4.2341 5.1395 0.676 5 30 3.4441 4.6399 5.3717 6.1970 8.1113 0.679 35 4.7302 6.5872 7.9347 9.5873 13.8072 0.682 40 8.0584 10.8652 13.2127 16.4877 26.2246 0.686 45 17.2046 22.3721 26.8925 33.7108 57.8700 0.691 15 1.7483 1.9478 2.0456 2.1422 2.3290 0.670 20 2.1253 2.4935 2.6857 2.8827 3.2865 0.671 25 2.6034 3.2508 3.6129 4.0005 4.8411 0.672 10 30 3.2223 4.3370 5.0128 5.7721 7.5262 0.673 35 4.3270 6.0335 7.2664 8.7689 12.5571 0.675 40 7.1344 9.6407 11.7401 14.6610 23.2244 0.677 45 14.5765 19.0171 22.9160 28.8085 49.4740 0.681 15 1.6984 1.8886 1.9817 2.0736 2.2518 0.667 20 2.0396 2.3876 2.5686 2.7541 3.1334 0.667 25 2.4644 3.0696 3.4067 3.7670 4.5479 0.667 2D 30 3.0000 4.0321 4.6525 5.3492 6.9591 0.667 35 3.6901 5.4448 6.5993 7.9724 11.3870 0.667 40 4.5989 7.6224 9.8346 12.6613 20.3076 0.667 45 5.8284 11.1974 15.6822 21.9144 40.6109 0.667 22. ACTA GEOTECHNICA SLOVENICfl, 2008/l S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE GARTH PRESSURE Table 2. Values of K*pq for different values of the parameters f, 8 and b/h with the centre of gravity of the epq pressures measured from the top of the wall f 8/f center of b/h (deg) 0 1/3 1/2 2/3 1 gravity 15 4.5768 5.2900 5.6081 5.9280 6.5309 0.609 20 7.0283 8.4840 9.2341 9.9907 11.5050 0.621 25 10.7112 13.5556 15.1308 16.8518 20.5128 0.630 0.25 30 16.2767 21.6076 25.0415 28.8780 37.6802 0.637 35 26.9519 36.2461 42.7186 51.2493 72.8142 0.642 40 52.6835 68.3932 81.3285 98.5627 151.3097 0.646 45 116.5809 149.1632 176.9264 217.2506 349.3207 0.650 15 3.1488 3.5825 3.8054 4.0025 4.4002 0.582 20 4.5447 5.4631 5.9108 6.3815 7.3299 0.596 25 6.5956 8.3312 9.2904 10.3297 12.5242 0.608 0.5 30 9.6385 12.8412 14.8706 17.1286 22.2471 0.618 35 15.4244 20.8022 24.6109 29.5968 41.8059 0.625 40 29.1399 37.9850 45.2969 55.1065 84.9392 0.632 45 62.8494 88.6238 95.8063 118.0501 191.9431 0.638 15 2.4316 2.7450 2.9041 3.0424 3.3246 0.555 20 3.3004 3.9297 4.2434 4.5715 5.2181 0.569 25 4.5344 5.7128 6.3552 7.0497 8.4886 0.581 1 30 6.3194 8.4512 9.7630 11.2191 14.4578 0.592 35 9.6528 13.0803 15.5514 18.7062 26.1839 0.601 40 17.3562 22.7883 27.2809 33.3902 51.4902 0.610 45 35.9646 46.3732 55.2288 68.4366 112.5270 0.619 15 2.0703 2.3184 2.4440 2.5563 2.7758 0.534 20 2.6753 3.1633 3.4047 3.6552 4.1404 0.545 25 3.5038 4.3975 4.8749 5.3812 6.4281 0.555 2 30 4.6598 6.2408 7.1807 8.2196 10.4893 0.565 35 6.7730 9.2194 11.0219 13.1920 18.2517 0.575 40 11.4902 15.1828 18.2730 22.5430 34.4973 0.585 45 22.5171 29.1956 34.9820 43.6475 72.5151 0.598 15 1.8513 2.0600 2.1639 2.2564 2.4323 0.516 20 2.2974 2.6965 2.8917 3.0896 3.4692 0.522 25 2.8854 3.5970 3.9688 4.3579 5.1504 0.529 5 30 3.6641 4.9014 5.6070 6.3809 8.0320 0.536 35 5.0419 6.9032 8.2543 9.7985 13.3404 0.543 40 7.9825 10.6136 12.8683 16.0172 23.9640 0.551 45 14.4186 18.8594 22.8019 28.7468 47.8074 0.560 15 1.7775 1.9726 2.0678 2.1531 2.3132 0.509 20 2.1705 2.5382 2.7169 2.8958 3.2362 0.512 25 2.6793 3.3254 3.6605 4.0075 4.7070 0.516 10 30 3.3322 4.4441 5.0746 5.7474 7.1781 0.521 35 4.4630 3.1341 7.3062 8.6307 11.6245 0.526 40 6.7878 9.0886 11.0668 13.7561 20.3108 0.531 45 11.7060 15.4077 18.7082 23.7798 39.2151 0.538 15 1.6984 1.8836 1.9685 2.0050 2.1969 0.500 20 2.0369 2.3770 2.5400 2.7022 3.0107 0.500 25 2.4644 3.0468 3.3495 3.6573 4.2786 0.500 2D 30 3.0000 3.9871 4.5357 5.1180 6.3569 0.500 35 3.6903 5.3540 6.3516 7.4707 9.9784 0.500 40 4.5990 7.4305 9.3077 11.5115 16.7775 0.500 45 5.8284 10.7914 14.4498 19.0443 30.7851 0.500 ACTA GEOTECHNICA SLOVENICA, 2008/i 33. S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE ËflRTH PRESSURES Table 3. Values of K*pc for f = 0° and different values b/h and cjc with center of gravity of epc pressures measured from the top of the wall. b/h K* ^ PC center of Ca/C = 0 c/c = 1/3 c/c = 1/2 c/c = 1/3 c/c = 1 gravity 0.25 6.9282 7.4720 7.7231 7.9631 8.4156 0.6051 0.50 4.5691 5.0257 5.2356 5.4287 5.7541 0.5854 1.00 3.3302 3.7248 3.8942 4.0439 4.2737 0.5611 2.00 2.6822 3.0314 3.1760 3.3024 3.4925 0.5391 5.00 2.2783 2.5938 2.7217 2.8321 2.9997 0.5192 10.00 2.1402 2.4427 2.5646 2.6693 2.8249 0.5104 Table 4. Comparison of K*py and K*pq with KpY and Kpq for different values f, S/f and b/h. ■ pq ■py pq K (Soubra and Regenass 2000) K (Skrabl and Macuh 2005) K*py (proposed) $ ( ) 81$ b/h=0.5 b/h=1.0 b/h=10.0 b/h=0.5 b/h=1.0 b/h=10.0 b/h=0.5 b/h=1.0 b/h=10.0 20 0.5 5.04 3.85 2.75 4.92 3.76 2.69 4.81 3.71 2.69 1.0 6.99 5.14 3.35 6.35 4.77 3.30 6.06 4.63 3.29 40 0.5 53.74 31.22 14.75 41.55 25.92 11.85 39.74 25.00 11.74 1.0 131.75 77.02 26.42 90.36 55.48 23.93 79.77 50.07 23.22 $ C) 8/$ Kpq (Soubra and Regenass 2000) Kpq (Skrabl and Macuh 2005) K*pq (proposed) b/h=0.5 b/h=1.0 b/h=10.0 b/h=0.5 b/h=1.0 b/h=10.0 b/h=0.5 b/h=1.0 b/h=10.0 20 0.5 6.22 4.45 2.75 6.10 4.35 2.73 5.91 4.24 2.72 1.0 8.06 5.54 3.17 7.79 5.44 3.27 7.33 5.22 3.24 40 0.5 74.26 43.48 12.82 49.68 29.50 11.33 45.30 27.28 11.07 1.0 130.19 73.35 21.22 104.80 61.07 21.36 84.94 51.49 20.31 7 COMPARISON WITH EXISTING SOLUTIONS In the literature only 2D analyses of the soil-pressure-limit values using different approaches are presented, while the research results for 3D cases are very limited. The research results of 3D passive pressure analyses according to the theorem of the upper-bound value have been presented in Soubra and Regenass (2000), and Skrabl and Macuh (2005). A comparison of the results for the coefficients K*py and K*pq for 8/$ = 0.5 and 1, $ = 20° and 40°, b/h = 0.5,1, 10 is presented in Table 4. A comparison of the results indicates that, particularly at greater shear angles and greater ratios of 8/$, the differences between the values of passive-earth-pressure coefficients for the compared failure mechanisms are the greatest. The coefficient Kpy for the proposed trans-lational failure mechanism is up to 11.72% smaller than the same coefficient for the failure mechanism (Skrabl and Macuh, 2005) when b/h = 0.5, while the coefficient Kpq is up to 18.95% smaller for the same b/h = 0.5. For higher ratios of b/h the difference gradually decreases, and when b/h > 20 the solutions are almost equal. 8 CONCLUSIONS This paper presents a procedure for determining 3D passive earth pressures according to the kinematic method of limit analysis. The set of three-dimensional kinematically admissible hyperbolic translational failure mechanisms with lateral surfaces bounded by the envelope of the hyperbolic half-cones is used to determine the critical distribution of passive pressure along a flexible retaining structure's height. The intensity of the passive pressures is gradually determined with the previously mentioned translational failure mechanisms from above, downwards. Thus, the critical distribution, the trust point and the resultant of the passive pressures that can be activated at the limit state for the chosen kinematic model are obtained. 22. ACTA GEOTECHNICA SLOVENICfl, 2008/l S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE GARTH PRESSURE Using the diagrams presented in Figs. 6 and 7 it is possible to determine the actual critical distribution of the passive pressure limit values for any arbitrary practical case (within the frame of given assumptions) that is applicable in geotechnical design. The results of the numerical analyses indicate that, when considering the upper-bound theorem and the set of three-dimensional kinematically admissible hyperbolic translational failure mechanisms, the passive-earth-pressure coefficients are lower than in the case of the hyperbolic translational failure mechanism and the translational mechanisms published in the literature for b/h < 10. The upper-bound values of the comparative passive-earth-pressure coefficients with a calculated pressure distribution are lower than the existing solutions with an assumed pressure distribution obtained using the upper-bound method within the framework of the limit analysis. This means that the classically presumed passive-earth-pressure distribution in 3D analyses is not acceptable, because it can actually not be activated. Furthermore, the trust point of the passive pressures resultant is independent of the friction between the retaining structures and the soil. Therefore, the presented results are applicable in geotechnical practice. ji length of one dimensional integration element I on the ground surface; N resultant value of normal stress component on spatial formed failure surface; q resultant value of stress on spatial formed failure surface; R* cone diameter; r polar co-ordinate; r* polar co-ordinate of the apex of the curved cone; co-ordinate appurtenant to gradient angle of the E* envelope; T resultant value of shear stress component on spatial $ formed failure surface; Wjk wkk weight coefficients for Gauss's integration point k; co-ordinate appurtenant to gradient angle of the E* envelope; co-ordinate of the section of the envelope and the Cl leading cone shaft in plane r-$; y unit weight of the soil; 8 friction angle at the soil-structure interface; £1 gradient of the envelope in point rEl which is defined in an arbitrary plane r-z; $ angle of internal friction of the soil; $ polar co-ordinate; $* polar co-ordinate of the apex of the curved cone. LIST OF SYMBOLS REFERENCES b c Ca epc epY epq /'m py cm J pq gq h K * K area of triangular or rectangular element j in plane x-y; width of the retaining wall; cohesion; adhesion along the soil-structure interface; factor of passive earth pressure distribution of the cohesion influence; factor of passive earth pressure distribution of the soil weight influence; factor of passive earth pressure distribution of the surcharge influence; fm momentums of passive pressures for e^ = 1 fpq momentums of passive pressures for e"q = 1 momentums due to unit weight of the ground; pi K pq momentums due to surcharge loading on the backfill surface; height of the retaining structure; comparative coefficient of passive earth pressure of the cohesion influence; comparative coefficients of passive earth pressure of the soil weight influence; comparative coefficient of passive earth pressure of the surcharge influence; [1] Blum, H. (1932). Wirtschaftliche Dalbenformen und deren Berechnung. Bautechnik, 10(5): 122-135 (in German). [2] Brinch Hansen, J. (1953). Earth Pressure Calculation, Danish Technical Press, Copenhagen. [3] Caquot, A., and Kérisel, J. 1948. Tables for the calculation of passive pressure, active pressure and bearing capacity of foundations, Gauthier-Villars, Paris. [4] Chen, W. F. (1975). Limit analysis and soil plasticity. Elsevier Scientific Publishing Company, Amsterdam, The Netherlands. [5] Coulomb, C. A. (1776). Essai sur une application des règles de maximis et minimis à quelques problèmes de statique relatifs à l'architecture. Mémoire présenté à l'académie Royale des Sciences, Paris, Vol. 7, 343-382 (in French). [6] Drescher, A., and Detournay, E. (1993). Limit load in translational failure mechanisms for associative and non-associative materials. Géotechnique, London, 43(3): 443-456. [7] Duncan, J. M. and Mokwa, R. L. (2001). Passive earth pressures: Theories and tests. Journal of ACTA GEOTECHNICA SLOVENICA, 2008/i 33. S. SKRABL: THE LIMIT VALUES AND THE DISTRIBUTION OF THRËË-DIMËNSIONflL PASSIVE ËflRTH PRESSURES Geotechnical and Geoenvironmental Engineering Division, ASCE, 127(3): 248-257. [8] Janbu, N. (1957). Earth pressure and bearing capacity calculations by generalised procedure of slices. In Proceedings of the 4th International Conference, International Society of Soil Mechanics and Foundation Engineering 207-213. [9] Lee, I. K., and Herington, J. R. (1972). A theoretical study of the pressures acting on a rigid wall by a sloping earth on rockfill. Géotechnique, London, 22(1): 1-26. [10] Kérisel, J., and Absi, E. (1990). Tables for the calculation of passive pressure, active pressure and bearing capacity of foundations. Gauthier-Villard, Paris, France. [11] Kumar, J., and Subba Rao, K. S. (1997). Passive pressure coefficients, critical failure surface and its kinematic admissibility. Géotechnique, London, England, 47(1): 185-192. [12] Michalowski, R. L. (1989). Three-dimensional analysis of locally loaded slopes. Géotechnique, The Institution of Civil Engineering, London, England, 39(1): 27-38. [13] Michalowski, R. L. (2001). Upper-bound load estimates on square and rectangular footings. Géotechnique, The Institution of Civil Engineering, London, England, 51(9): 787-798. [14] Mroz, Z., and Drescher, A. (1969). Limit plasticity approach to some cases of flow of bulk solids. Journal of Engineering for Industry, Transactions of the ASME, 91: 357-364. [15] Ovesen, N. K. (1964). Anchor slabs, calculation methods, and model tests. Bull. No. 16, Danish Geotechnical Institute, Copenhagen: 5-39. [16] Salençon, J. (1990). An introduction to the yield design theory and its applications to soil mechanics. European Journal of Mechanics - A/Solids, Paris, 9(5): 477-500. [17] Shields, D. H., and Tolunay, A. Z. (1973). Passive pressure coefficients by method of slices. Journal of the Soil Mechanics and Foundation Division, ASCE, 99(12): 1043-1053. [18] Skrabl, S., and Macuh, B. (2005). Upper-bound solutions of three-dimensional passive earth pressures. Canadian Geotechnical Journal, Ottawa, 42: 1449-1460. [19] Sokolovski, V. V. (1965). Static of granular media. Pergamon Press, New York. [20] Soubra, A. H. (2000). Static and seismic earth pressure coefficients on rigid retaining structures. Canadian Geotechnical Journal, Ottawa, 37: 463-478. [21] Soubra, A. H., and Regenass, P. (2000). Three-dimensional passive earth pressure by kinematical approach. Journal of Geotechnical and Geoenvi- ronmental Engineering Division, ASCE, 126(11): 969-978. [22] Terzaghi, K. (1943). Theoretical soil mechanics. Wiley, New York. [23] Vrecl-Kojc, H., and Skrabl, S. (2007). Determination of passive earth pressure using three-dimensional failure mechanism. Acta Geotechnica Slovenica, 4(1): 10-23. 22. ACTA GEOTECHNICA SLOVENICfl, 2008/l