dynamic analysis of stacked rigid blocks
TRANSCRIPT
Dynamic analysis of stacked rigid blocks
Pol D. Spanos*, Panayiotis C. Roussis, Nikolaos P.A. Politis
Department of Civil Engineering, George R. Brown School of Engineering, Rice University, PO Box 1892, Mail Stop 318, 6100 Main Street, Houston,
TX 77005-1892, USA
Accepted 11 May 2001
Abstract
The dynamic behavior of a structural model of two stacked rigid blocks subjected to ground excitation is examined. Assuming no sliding,
the rocking response of the system standing free on a rigid foundation is investigated. The derivation of the equations of motion accounts for
the consecutive transition from one pattern of motion to another, each being governed by a set of highly nonlinear differential equations. The
system behavior is described in terms of four possible patterns of response and impact between either the two blocks or the base block and the
ground. The equations governing the rocking response of the system to horizontal and vertical ground accelerations are derived for each
pattern, and an impact model is developed by conservation of angular momentum considerations. Numerical results are obtained by
developing an ad hoc computational scheme that is capable of determining the response of the system under an arbitrary base excitation.
This feature is demonstrated by using accelerograms from the Northridge, CA, 1994, earthquake. It is hoped that the two-blocks model used
herein can facilitate the development of more sophisticated multi-block structural models. q 2001 Published by Elsevier Science Ltd.
Keywords: Dynamics; Stacked rigid blocks; Nonlinearity; Impact problem; Patterns of motion; Seismic response
1. Introduction
It is a common practice in structural engineering when
dealing with structures under dynamic excitation, to assume
deformable continuum behavior. For a number of structural
systems, however, rigid body motion may well be a credible
dynamic behavior model. In fact, the seismic behavior of
block-like structures standing free on their foundation, such
as ancient monuments, petroleum storage tanks, water
towers, nuclear reactors, concrete radiation shields, compu-
ter-type equipment, and various artifacts, has been the object
of numerous studies for over a century. The approaches on
the subject involve both deterministic and stochastic studies.
Housner's landmark study [1] has provided the basic
understanding on the rocking response of a rigid block and
sparked modern scienti®c interest. The response of a rigid
block subjected to horizontal and vertical ground accelera-
tions, with the option of elastic tie-down rods and the assump-
tion of no sliding has been examined by Aslam et al. [2].
Various patterns, free-¯ight pattern included, have been
analyzed by Ishiyama [3]. A study on the dynamic behavior
of a rocking rigid block supported by a ¯exible foundation
which permits up-lift has been performed by Psycharis and
Jennings [4]. Spanos and Koh [5] have investigated the rock-
ing response of a rigid block subject to harmonic ground
motion, assuming no sliding. The linear and nonlinear equa-
tions of motion have been solved numerically assuming zero
initial conditions to identify likely steady-state patterns of
response. Allen et al. [6] have studied the dynamic behavior
of an assembly of two-dimensional rigid prisms. Furthermore,
the rocking response has been investigated both analytically
and experimentally by Tso and Wong [7]. Hogan [8], adopt-
ing the model, the analysis, and the response classi®cation of
Spanos and Koh [5], has performed a complete investigation
of the existence and stability of single-impact subharmonic
responses (1, n) (with n $ 1), as a function of the restitution
coef®cient b . Psycharis [9] has also presented an analysis of
the dynamic behavior of systems consisting of two blocks.
Moreover, the impact problem has been approached by Sino-
poli [10] by adopting a unilateral constraint, `kinematic
approach'. The in¯uence of nonlinearities associated with
impact on the behavior of free-standing rigid objects
subjected to horizontal base excitations has been studied by
Yim and Lin [11]. Furthermore, a general, two-dimensional
formulation for the response of free-standing rigid bodies to
base excitation has been presented by Shenton and Jones
[12,13]. Also, Augusti and Sinopoli [14] have presented a
formulation of dynamics and impact problem for a single
rigid body freely supported on rigid foundation; a review of
Soil Dynamics and Earthquake Engineering 21 (2001) 559±578
0267-7261/01/$ - see front matter q 2001 Published by Elsevier Science Ltd.
PII: S0267-7261(01)00038-0
www.elsevier.com/locate/soildyn
* Corresponding author. Tel.: 11-713-527-4909; fax: 11-713-285-5191.
E-mail address: [email protected] (P.D. Spanos).
the numerous studies performed on this subject has also been
presented there. Allen and Duan [15] have examined the
reliability of linearizing the equations of motion of rocking
blocks. The rocking and the overturning of precariously
balanced rocks by earthquake have been examined by Shi et
al. [16]. The criteria for initiation of slide, rock, and slide-rock
rigid-body modes have been presented by Shenton [17].
Scalia and Sumbatyan [18] have examined the slide rotation
of rigid bodies subjected to a horizontal ground motion.
Moreover, Pombei et al. [19] have studied the dynamics of
a rigid block subjected to horizontal ground motion, towards
formulating criteria that separate the various patterns of the
motion. The rocking response of free-standing blocks under
cycloidal pulses has been examined by Zhang and Makris
[20]. Furthermore, Makris and Zhang [21] have studied the
rocking response and the overturning of anchored blocks
under pulse type motions. Kim et al. [22] have investigated
experimentally the vibration properties of a rigid body placed
on sand ground surface.
A probabilistic approach to the problem of rocking of
rigid blocks has been pursued by Yim et al. [23]; the rocking
behavior of rigid blocks subjected to horizontal and vertical
accelerations, assuming no sliding has been studied there.
Koh et al. [24] have studied the behavior of a rigid block
rocking on a ¯exible foundation. Modulated white noise has
been used as a model of horizontal acceleration of the foun-
dation. The statistics of the rocking response have been
found by an analytical procedure which involves a combina-
tion of static condensation and stochastic linearization. Koh
and Spanos [25] have also presented an analysis of block
random rocking. Furthermore, Giannini and Masiani [26]
have tackled the problem of the dynamic response of a
rigid block oscillator to a Gaussian white noise excitation
process. An investigation by Dimentberg et al. [27] has
focused on the toppling failure of a free standing and an
anchored rigid block due to horizontal and vertical base
excitations. Expressions for the statistical properties and
probability distribution of the random toppling time have
been obtained; the excitation has been idealized as a white
noise. Moreover, Cai et al. [28] have examined the toppling
of a rigid body under random excitation by modeling the
base acceleration as an evolutionary process with a broad-
band spectrum. More recently, Lin and Yim [29] have exam-
ined the rocking behavior of slender rigid objects subjected
to periodic excitations with and without noise disturbance for
a better understanding of their response and stability. In a
companion paper [30], Lin and Yim have also examined, in a
probabilistic context, the responses of fully nonlinear rocking
systems subjected to combined deterministic and stochastic
excitations. Furthermore, Giannini and Masiani [31] have
used a random vibration approach to study the response of
a slender rigid block to seismic excitation.
Clearly, the dynamic behavior of multi-block structures
has not, to date, been exhaustively studied. Even for the
simplest case of multi-block structures involving two-
block assemblies, the rocking problem becomes very
complex. Such a con®guration, in which one block is placed
over the other, can be thought of as the model of ancient
Greek and Roman type structures composed of large heavy
members of a piece of machinery or statue placed on top of a
block-like base.
This paper focuses on the dynamic behavior of structures
consisting of two rigid blocks; one serving as a base and
another one on top of the base. Assuming rigid foundation,
large friction to prevent sliding, and point contact during a
perfectly plastic impact, the only possible response mechan-
ism under base excitation is rocking about the corners of the
blocks. The analytical formulation of this nonlinear problem
is rather challenging. Its complexity is associated with tran-
sitions from one pattern of motion to another, each one
being governed by a set of highly nonlinear equations.
The paper presents a derivation of the exact (nonlinear)
equations of motion for the system considered undergoing
base excitation and a treatment of the impact problem by
deriving expressions for the post-impact angular velocities.
Furthermore, it contains numerical results from the devel-
opment and use of ad hoc computer program for determin-
ing free vibration and seismic response of the system.
2. Formulation
2.1. Possible patterns of rocking response
From the outset, it is noted that the term `pattern' is
chosen to describe the various con®gurations of the relative
positions to each other of the two blocks; the term `mode' is
discarded to prevent confusion stemming from its use in
standard structural dynamics of MDOF systems.
Here, the dynamic behavior of systems consists of two
symmetric rigid blocks as shown in Fig. 1. Assuming no
sliding, the rocking response of the system standing free
on a rigid foundation is investigated. The top block rests
symmetrically on the base block, and the latter rests on a
rigid horizontal surface. The blocks have masses mi, and
centroid moments of inertia IGi, where i is the block index
with i� 1 for the base block, and i� 2 for the top block.
The two blocks have bases Bi� 2bi and heights Hi� 2hi.
The bottom right points of the block are denoted by Oi and
the left are denoted by O 0i. The bottom right and left points
of the top block are related to the bottom right point of the
base block by the distances l and l 0, and the angles between
the right vertical of the base block and the segments O1O2
and O1O 02;b and b 0, respectively. Finally, the center of
mass for each block is denoted by Gi, and its location is
determined by the distance from the bottom right point ri,
and the angle between the right vertical of the block and the
distance radius uci.
The system possesses two degrees of freedom, namely, u 1
and u 2, denoting the angles of rotation of the two blocks
with respect to the vertical. When subjected to a base
excitation, the system may exhibit four possible patterns
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578560
of rocking motion. Fig. 2 illustrates the classi®cation of the
four possible patterns with respect to the angles of rotation
u 1 and u 2. Patterns 1 and 2 involve a 2-DOF system
response, and re¯ect rotations of the two blocks in the
same or opposite direction. Patterns 3 and 4 re¯ect a
SDOF system response; in particular, pattern 3 describes
the motion of the system rocking as one rigid structure,
and pattern 4 concerns the case where only the top block
experiences rotation. Furthermore, each of the afore-
mentioned patterns is subdivided into two subcases that
account for opposite angle signs.
2.2. Initiation of motion
Before dealing with the equations of motion, it is impor-
tant to derive appropriate criteria for the initiation of motion
of the system when subjected to a base excitation with hori-
zontal and vertical components �xg and �yg, respectively.
Speci®cally, as can be seen in Fig. 3, the system may be
set into rocking either in pattern 3 or in pattern 4 when the
overturning moment of the horizontal inertia force about
one edge exceeds the restoring moment due to the weight(s)
of the block(s) and the vertical inertia force.
The criteria for motion initiation follows.
Transition from rest to pattern 3a requires that
2h �xg 2 b1 �yg . b1g; �1�where
h � m1h1 1 m2�2h1 1 h2�m1 1 m2
�2�
is the distance of the center of mass of the system from the
base of the base block.
Transition from rest to pattern 3b requires that
h �xg 2 b1 �yg . b1g: �3�Transition from rest to pattern 4a requires that
2h2 �xg 2 b2 �yg . b2g: �4�Transition from rest to pattern 4b requires that
h2 �xg 2 b2 �yg . b2g: �5�
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578 561
Fig. 2. Classi®cation of rocking patterns for a system of two stacked rigid blocks with respect to the angles of rotation.
Fig. 1. Geometric model of two stacked rigid blocks.
2.3. Equations of motion
The equations of motion for the possible patterns and
their subcases are derived by means of Lagrange's method.
The kinetic energy of the system is
T � T1 1 T2 � 1
2
X2
i�1
�miv2Gi
1 IGi_u 2
i �; �6�
while its potential energy is given by
V � V1 1 V2 �X2
i�1
mihGig: �7�
In the above equations, vGidenotes the velocity of the i-th
center of mass and hGidenotes the distance of the i-th center
of mass from the base of the base block.
The equations of motion for all possible patterns and
subcases are presented below.
Pattern 1:
�IO11 m2l2� �u 1 1 m2lr2cos�g1� �u 2 1 m2lr2sin�g1� _u 2
2
2 mxlgr1sin�u1 2 Su1uc1�2 m2glsin�u1 2 Su1
b�� 2�m1r1cos�u1 2 Su1
uc1�1 m2lcos�u1 2 Su1
uc1�� �xg
1 �m1r1sin�u1 2 Su1uc1�1 m2lsin�u1 2 Su1
uc1�� �yg; �8�
and
m2lr2cos�g1�1 IO2�u 2 2 m2lr2sin�g1� _u 2
1 2 m2gr2sin�u2 2 Su1uc2�
� m2r2� �ygsin�u2 2 Su1uc2�2 �xgcos�u2 2 Su1
uc2��;
�9�where IOi
are the moments of inertia with respect to the
points Oi, and
g1 � u1 2 u2 1 Su1�uc2
2 b�: �10�
The signum function Su1accounts for the two subcases of
the pattern under consideration; this will also be the case for
patterns 2 and 3, while the signum function Su2will account
for the two subcases of pattern 4. It is de®ned as
Sui�
1 if ui . 0
0 if ui � 0
21 if ui , 0
8>><>>: : �11�
Pattern 2:
�IO11 m2l 02� �u 1 1 m2l 0r2cos�g2� �u 2 1 m2l 0r2sin�g2� _u 2
2
2 m1gr1sin�u1 2 Su1uc1�2 m2gl 0sin�u1 2 Su1
b 0�� 2�m1r1cos�u1 2 Su1
uc1�1 m2l 0cos�u1 2 Su1
b 0�� �xg
1 �m1r1sin�u1 2 Su1uc1�1 m2l 0sin�u1 2 Su1
b 0�� �yg;
�12�
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578562
Fig. 3. Initiation of motion.
and
m2l 0r2cos�g2� �u 1 1 IO2�u 2 2 m2l 0r2sin�g2� _u 2
1
2m2gr2sin�u2 1 Su1uc2�
� m2r2� �ygsin�u2 1 Su1uc2�1 �xgcos�u2 2 Su1
uc2��;
�13�
where
g2 � u1 2 u2 2 Su1�uc2
1 b 0�: �14�Pattern 3:
IO�u 1 2 MgRsin�u1 2 Su1
uc� � 2MR� �xgcos�u1 2 Su1uc�
2 �ygsin�u1 2 Su1uc��;
�15�and
u1 � u2; �16�where M is the total mass of the system (i.e. M �m1 1 m2�;R; uc; and IO are the distance of the center of
gravity of the system from any base corner of the base
block, the angle between the right vertical of the base
block and the distance radius of the center of gravity of
the system, and the mass moment of inertia with respect
to any base corner of the base block, respectively.
Pattern 4:
u1 � 0 �17�and
IO2�u 2 2 m2gr2sin�u2 2 Su2
uc2� � m2r2� �xgcos�u2 2 Su2
uc2�
2 �ygsin�u2 2 Su2uc2��:�18�
Note that the above equations of motion are valid only in the
absence of impact. The impact problem is addressed later.
Furthermore, note that for small angles u 1 and u 2 the preced-
ing equations can be simpli®ed as follows.
Pattern 1:
�IO11 m2l2� �u 1 1 m2lr2cos�g1L� �u 2 1 Su1
m1gr1sin�uc1�
1 Su1m2glsin�b�
� 2�m1r1cos�uc1�1 m2lcos�b�� �xg 2 Su1
�m1r1sin�uc1�
1 m2lsin�b�� �yg;
�19�and
m2lr2cos�g1L� �u 1 1 IO2�u 2 1 Su2
m2gr2sin�uc2�
� 2m2r2� �ygSu2sin�uc2
�1 �xgcos�uc2��; �20�
where
g1L � Su1�uc2
2 b�: �21�
Pattern 2:
�IO11 m2l 02� �u 1 1 m2l 0r2cos�g1L� �u 2 1 Su1
m1gr1sin�uc1�
1 Su1m2gl 0sin�b 0�
� 2�m1r1cos�uc1�1 m2l 0cos�b 0�� �xg 2 Su1
�m1r1sin�uc1�
1 m2l 0sin�b 0�� �yg;
�22�and
m2l 0r2cos�g2L� �u 1 1 IO2�u 2 1 Su1
m2gr2sin�uc2�
� 2m2r2� �ygSu1sin�uc2
�2 �xgcos�uc2��; �23�
where
g2L � Su1�uc2
1 b 0�: �24�Pattern 3:
IO�u 1 1 Su1
MgRsin�uc� � 2MR� �xgcos�uc�1 �ygSu1sin�uc��;
�25�and
u1 � u2: �26�Pattern 4:
u1 � 0; �27�and
IO2�u 2 1 Su2
m2gr2sin�uc2� � 2m2r2� �xgcos�uc2
�1 �ygSu2sin�uc2
��:�28�
2.4. Transition between patterns
After the system is set to motion, it switches from one
pattern to another due to either an impact or a sudden change
in ground excitation. Transition criteria in the absence of
impact are presented below; the impact problem is studied
in Sections 3 and 4. Once motion is initiated, transition can
occur from either pattern 3 or pattern 4; the conditions for
transition from one pattern to another are derived by consid-
ering the overturning and restoring moments. Transition
from pattern 3a to pattern 1a is illustrated in Fig. 4, and
requires that
2cos�uc22 u1� �xg 2 sin�uc2
2 u1� �yg
. gsin�uc22 u1�1 dcos�uc2
1 v� _u 21
1 dsin�uc21 v�1
IG2
m2r2
� ��u 1; �29�
where
d �����������������������2h1 1 h2�2 1 b2
1
q; �30�
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578 563
and
v � atan2h1 1 h2
b1
� �: �31�
Transition from pattern 3a to pattern 2a is illustrated in
Fig. 5, and requires that
cos�uc22 u1� �xg 2 sin�uc2
2 u1� �yg
. gsin�uc21 u1�1 dcos�2u1 1 uc2
1 v� _u 21
1 dsin�2u1 1 uc21 v�1
IG2
m2r2
� ��u 1: �32�
Transition from pattern 3b to pattern 1b is illustrated in
Fig. 6, and requires that
cos�uc21 u1� �xg 2 sin�uc2
1 u1� �yg
. gsin�uc21 u1�1 dsin�v 2 uc2
� _u 21
2 dcos�v 2 uc2�2
IG2
m2r2
� ��u 1: �33�
Transition from pattern 3b to pattern 2b is illustrated in
Fig. 7, and requires that
2cos�uc22 u1� �xg 2 sin�uc2
2 u1� �yg
. gsin�uc22 u1�2 dsin�v 1 uc2
� _u 21
1 dcos�v 1 uc2�2
IG2
m2r2
� ��u 1: �34�
Transition from pattern 4a to pattern 1a is illustrated in
Fig. 8, and requires that
2�m1 1 2m2�h1 �xg 2 �m1b1 1 m2j� �yg
. m2r2�jsin�uc22 u2�1 2h1cos�uc2
2 u2�� �u 2
1 m2r2�2h1sin�uc22 u2�2 jcos�uc2
2 u2�� _u 22 1 m1gb1;
�35�where
j � b1 2 b2: �36�Transition from pattern 4b to pattern 1b is illustrated in
Fig. 9, and requires that
�m1 1 2m2�h1 �xg 2 �m1b1 1 m2j� �yg
. 2m2r2�jsin�uc21 u2�1 2h1cos�uc2
1 u2�� �u 2
1 m2r2�2h1sin�uc21 u2�2 jcos�uc2
1 u2�� _u 22 1 m1gb1:
�37�
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578564
Fig. 5. Transition from pattern 3a to pattern 2a in the absence of impact.
Fig. 4. Transition from pattern 3a to pattern 1a in the absence of impact.
Transition from pattern 4b to pattern 2a is illustrated in
Fig. 10, and requires that
2�m1 1 2m2�h1 �xg 2 �m1b1 1 m2j0� �yg
. 2m2r2�j 0sin�uc21 u2�2 2h1cos�uc2
1 u2�� �u 2
2 m2r2�2h1sin�uc21 u2�1 j 0cos�uc2
1 u2�� _u 22
1 m1gb1; �38�
where
j 0 � 2b1 2 j: �39�
Finally, transition from pattern 4a to pattern 2b is illustrated
in Fig. 11, and requires that
�m1 1 2m2�h1 �xg 2 �m1b1 1 m2j0� �yg
. m2r2�j 0sin�uc22 u2�2 2h1cos�uc2
2 u2�� �u 2
2 m2r2�2h1sin�uc22 u2�1 j 0cos�uc2
2 u2�� _u 22
1 m1gb1: �40�
3. Accounting for impactÐpatterns 1 and 2
3.1. Preliminary remarks
In this section the impact problem is studied. During
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578 565
Fig. 6. Transition from pattern 3b to pattern 1b in the absence of impact.
Fig. 7. Transition from pattern 3b to pattern 2b in the absence of impact.
Fig. 8. Transition from pattern 4a to pattern 1a in the absence of impact.
vibration the system switches from one pattern to another,
and impact between the two blocks or between the base
block and the ground can occur. Under the assumption of
inelastic impact (no bouncing), the only possible response
mechanism is pure rocking about the corners of the two
blocks (point-impact). Furthermore, the duration of impact
is assumed to be in®nitesimal (impulsive motion), implying
negligible changes in position and orientation, and instanta-
neous changes in angular velocities. In this regard, the
impact is analyzed using the principle of impulse and
momentum.
3.2. Impact in pattern 1
3.2.1. Base block impact with the ground
First, assume that the system is rocking in pattern 1a.
When the angle of rotation of the base block becomes
zero, an impact occurs yielding a change of the rotation
pole from O1 to O 01, that is, a switch to pattern 2b, see
Fig. 12.
This induces an instantaneous change in the angular
velocities of the blocks, whose post-impact values, _u11
and _u12 , need to be determined. During impact, assum-
ing point-impact it can be argued that the only forces
that exert a moment about O 01 are the weights of the
blocks (the impulse forces pass through the point O 01).Furthermore, the angular impulse due to these ®nite
forces about O 01 is quite small since the time of impact
is negligible. Thus, the angular momentum of the
system about O 01 is conserved. The angular momentum
of the system about O 01 immediately before impact is
simply the sum of angular momenta of each block about
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578566
Fig. 10. Transition from pattern 4b to pattern 2a in the absence of impact.
Fig. 11. Transition from pattern 4a to pattern 2b in the absence of impact.
Fig. 9. Transition from pattern 4b to pattern 1b in the absence of impact.
the point under consideration. That is,
�h2O 0
1�system � �h2
O 01�base block 1 �h2
O 01�top block: �41�
The angular momentum of a rigid body about some
point A can be expressed in vector form as
hA � hG 1 rG=A £ mvG; �42�where vG is the velocity of the mass center G, rG/A is
the position vector of G relative to A, and hG is the
angular momentum of the body about its mass center.
The angular momentum is given by
hG � IGv; �43�with v being the angular velocity of the body, and IG
being the central mass moment of inertia of the body
about an axis perpendicular to the plane of motion. For
plane rigid body motion, the angular momentum vector
is always normal to the plane of motion so that Eq.(42)
can be rewritten as
hA � IGv 1 �mvG�d; �44�where d is the distance of the linear momentum vector
mvG from the point A. Eq. (44) is used to compute the
angular momentum of each block. Speci®cally, the
angular momentum of the base block is given by
�h2O 0
1�base block � IG1
_u21 1 �m1v2
G1�d; �45�
where IG1is the central mass movement of inertia of the
base block, _u21 and v2
G1are the angular velocity and
velocity of the mass center of the base block immedi-
ately before impact, respectively, and d is the distance
of the linear momentum vector m1v2G1
from the point
O 01.The angular momentum of each block, immediately
before and after impact, can be similarly determined.
Finally, the principle of conservation of angular momentum
for the system is expressed in the form
�h2O 0
1�system � �h1
O 01�system; �46�
where
�h2O 0
1�system � {IO1
2 2m1b21 1 m2l�r2cos�u2 2 uc2 1 b�
1 2h1cos�b�2 �2b1 2 j�sin�b��} _u 21 1 {IO2
1 m2r2�2h1cos�u2 2 uc2�1 �2b1 2 j�sin�u2
2 uc2��} _u22 ;
�47�and
�h1O 0
1�system � {IO1
1 m2l 0�r2cos�u2 2 uc2 2 b 0�1 2h1cos�b 0�
1 �2b1 2 j�sin�b 0��} _u 11 1 {IO2
1 m2r2�2h1cos�u2 2 uc2�1 �2b1 2 j�sin�u2
2 uc2��} _u12 :
�48�Eq. (46) involves the two unknown angular velocities, _u1
1
and _u12 , immediately after impact. A second equation may
be derived by considering the conservation of angular
momentum about O 02 for the top block alone. This is justi-
®ed by the fact that, since the top block point-contacts the
base block at O2, all impact forces are transmitted to the top
block through that point, so that the angular impulse of the
top block about O2 is zero (the angular impulse of a ®nite
force like the weight of the block can be neglected). Further-
more, since the motion is assumed impulsive, angular
impulse equals change in angular momentum, even about
the `moving' point O2. Therefore,
�h2O2�top block � �h1
O2�top block; �49�
where
�h2O2�top block � m2r2lcos�u2 2 uc2 1 b� _u2
1 1 IO2_u2
2 �50�and
�h1O2�top block � m2r2l 0cos�u2 2 uc2 2 b 0� _u1
1 1 IO2_u1
2 : �51�The system of Eqs. (46) and (49) is solved for the angular
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578 567
Fig. 12. Transition from pattern 1a to pattern 2b through impact.
velocities immediately after impact to yield
_u11 � A _u2
1 ; �52�and
_u12 � B _u2
1 1 _u22 ; �53�
where
A � IO2C1 2 C2C3
C4IO22 C2C5
; �54�
and
B � C5C1 2 C4C3
C2C5 2 C4IO2
; �55�
with
C1 � IO12 2m1b2
1 1 m2�r2cos�u2 2 uc2 1 b�1 2h1cos�b�2 �2b1 2 j�sin�b��;
�56�
C2 � IO21 m2r2�2h1cos�u2 2 uc2�1 �2b1 2 j�sin�u2
2 uc2��; �57�
C3 � m2r2lcos�u2 2 uc2 1 b�; �58�
C4 � IO11 m2l 0�r2cos�u2 2 uc2 2 b 0�1 2h1cos�b 0�1 �2b1
2 j�sin�b 0��; (59)
and
C5 � m2r2l 0cos�u2 2 uc2 2 b 0�: �60�Note that, by symmetry, the same analysis also holds for the
case of transition from pattern 1b to pattern 2a.
3.2.2. Impact between the two blocks
Next, consider the case where the system is rocking in
pattern 1a. When the angle of rotation of the top block
becomes equal to that of the base block, an impact between
the blocks occurs and the top block may either start rocking
about O 02 (pattern 2a), or remain in contact with the base block,
implying that the system rocks as one rigid-body about O1
(pattern 3a); the two possible transitions are illustrated in
Fig. 13.
Assume that the system switches from pattern 1a to
pattern 2a. The forces generated during impact are applied at
the point O1, so that the angular impulse of the system about
that point is zero. Consequently, the angular momentum of the
system about O1 is conserved during the time of impact. That
is,
�h2O1�system � �h1
O1�system; �61�
with
�h2O1�system � {IO1
1 m2l���������������������b2
1 1 �2h1 1 h2�2q
cos�z 2 b�} _u21
1 {IG21 m2r2
���������������������b2
1 1 �2h1 1 h2�2q
cos�u2 2 u1
2 uc2 1 z�} _u22 ;
�62�and
�h1O1�system � {IO1
1 m2l 0���������������������b2
1 1 �2h1 1 h2�2q
cos�z 2 b 0�} _u21
1 {IG21 m2r2
���������������������b2
1 1 �2h1 1 h2�2q
cos�u2 2 u1
1 uc2 1 z�} _u12 : (63)
A second equation may be derived by considering the conser-
vation of angular momentum about O 02, for the top block
alone. Since impact takes place at O 02, and neglecting the
angular impulse of the weight of the block, the angular impulse
of the top block about that point is zero. Furthermore, since the
motion is assumed is impulsive, the principle of conservation
of angular momentum is still valid about the `non-stationary'
point O 02. Therefore,
�h2O 0
2�top block � �h1
O 02�top block; �64�
with
�h2O 0
2�top block � m2r2lcos�u2 2 u1 1 uc2 1 b� _u2
1 1 IG2
1 m2r22cos�2uc2� _u2
2 ; �65�
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578568
Fig. 13. Transition from pattern 1a to either pattern 2a or pattern 3a through impact.
and
�h1O 0
2�top block � m2r2l 0cos�u2 2 u1 1 uc2 1 b 0� _u2
1 1 IO2_u2
2 : �66�Solving the system of Eqs. (61) and (64) for the angular
velocities immediately after impact yields
_u11 � A _u2
1 1 B _u22 ; �67�
and
_u12 � C _u2
1 1 D _u22 ; �68�
where
A � IO2E1 2 E2E3
E4IO22 E2E5
; �69�
B � IO2E6 2 E2E7
E4IO22 E2E5
; �70�
C � E5E1 2 E4E3
E2E5 2 E4IO2
; �71�
and
D � E5E6 2 E4E7
E2E5 2 E4IO2
; �72�
with
E1 � IO11 m2l
���������������������b2
1 1 �2h1 1 h2�2q
cos�z 2 b�; �73�
E2 � IG21 m2r2
���������������������b2
1 1 �2h1 1 h2�2q
cos�u2 2 u1 1 uc2 1 z�; �74�
E3 � m2r2lcos�u2 2 u1 1 uc2 1 b�; �75�
E4 � IO11 m2l 0
���������������������b2
1 1 �2h1 1 h2�2q
cos�z 2 b 0�; �76�
E5 � m2r2l 0cos�u2 2 u1 1 uc2 1 b 0�; �77�
E6 � IG21 m2r2
���������������������b2
1 1 �2h1 1 h2�2q
cos�u2 2 u1 2 uc2 1 z�;�78�
and
E7 � IG21 m2r2
2cos�2uc2�: �79�The preceding analysis was based on the assumption that, after
impact, the base and top blocks rock separately about O1 and
O 02, respectively (pattern 2a). If, however, _u12 . _u1
1 Ðwhich
is physically impossibleÐthen, after impact, the top block
remains in contact with the base block and the system rocks
as one rigid body about O1 (pattern 3a). In this case, _u12 � _u1
1 ,
and the proper value is derived by considering the conserva-
tion of angular momentum about O1 for the whole system.
That is,
�h2O1�system � �h1
O1�system; �80�
with
�h2O1�system � {IO1
1 m2l���������������������b2
1 1 �2h1 1 h2�2q
cos�z 2 b�} _u21
1 {IG21 m2r2
���������������������b2
1 1 �2h1 1 h2�2q
cos�u2 2 u1
2 uc2 1 z�} _u22 ;
�81�and
�h1O1�system � IO
_u11 ; �82�
where
IO � IO11 IG2
1 m2�b21 1 �2h1 1 h2�2� �83�
is the mass moment of inertia of the system about O1.
The ®nal relation is
_u11 � _u1
2 � B1
IO
_u21 1
B2
IO
_u22 ; �84�
where
B1 � IO11 m2l
���������������������b2
1 1 �2h1 1 h2�2q
cos�z 2 b�; �85�
and
B2 � IG21 m2r2
���������������������b2
1 1 �2h1 1 h2�2q
cos�u2 2 u1 2 uc2 1 z�:�86�
The same analysis also holds for the case of transition from
pattern 1b to pattern 2b or 3b.
3.3. Impact in pattern 2
3.3.1. Base block impact with the ground
First, note that if the system is rocking in pattern 2a when
the base block impacts the foundation, transition to pattern
1b occurs, see Fig. 14. In order to ®nd the angular velocities
after impact, conservation of angular momentum about O 01,for the system, and about O 02, for the top block, is ensured.
The equation concerning the conservation of angular
momentum about O 01 for the system is
�h2O 0
1�system � �h1
O 01�system; �87�
where
�h2O 0
1�system � {IO1
2 2m1b21 1 m2l 0�r2cos�u2 1 uc2 1 b 0�
1 2h1cos�b 0�2 jsin�b 0��} _u 21 1 {IO2
1 m2r2�2h1cos�u2 1 uc2�1 jsin�u2
1 uc2��} _u22 ;
�88�
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578 569
and
�h1O 0
1�system � {IO1
1 m2l�r2cos�u2 1 uc2 2 b�1 2h1cos�b�
1 jsin�b��} _u 11 1 {IO2
1 m2r2�2h1cos�u2
1 uc2�1 jsin�u2 1 uc2��} _u12 :
�89�Conservation of angular momentum about O 02 for the top
block requires that
�h2O 0
2�top block � �h1
O 02�top block; �90�
where
�h2O 0
2�top block � m2r2l 0cos�u2 1 uc2 1 b 0� _u2
1 1 IO2_u2
2 ; �91�and
�h1O 0
2�top block � m2r2lcos�u2 1 uc2 2 b� _u2
1 1 IO2_u2
2 : �92�Solving the system of Eqs. (87) and (90) for the angular
velocities immediately after impact yields
_u11 � A _u2
1 1 B _u22 ; �93�
and
_u12 � C _u2
1 1 D _u22 ; �94�
where
A � IO2E1 2 E2E3
E4IO22 E2E5
; �95�
B � IO2E6 2 E2IO2
E4IO22 E2E5
; �96�
C � E5E1 2 E4E3
E2E5 2 E4IO2
; �97�
and
D � E5E6 2 E4IO2
E2E5 2 E4IO2
; �98�
with
E1 � IO12 2m2b2
1 1 m2l 0�r2cos�u2 1 uc2 1 b 0�1 2h1cos�b 0�
2jsin�b 0��;�99�
E2 � IO21 m2r2�2h1cos�u2 1 uc2�1 jsin�u2 1 uc2��; �100�
E3 � m2r2l 0cos�u2 1 uc2 1 b 0�; �101�
E4 � IO11 m2l�r2cos�u2 1 uc2 2 b�1 2h1cos�b�1 jsin�b��; �102�
E5 � m2r2lcos�u2 1 uc2 2 b�; �103�
and
E6 � IO21 m2r2�2h1cos�u2 1 uc2�1 j�sin�u2 1 uc2�: �104�
The preceding analysis is also valid for transition from
pattern 2b to 1a.
3.3.2. Impact between the blocks
Next, assume that the system is rocking in pattern 2a. If
the angle of rotation of the top block becomes equal to that
of the base block, an impact between the blocks occurs and
the top block tends to start rocking about O2 (pattern 1a). It
is also possible, see Fig. 15, that after impact the two blocks
remain in full contact so that the system rocks as one rigid
body about O1 (pattern 3a).
Consider the case where the system switches from
pattern 2a to pattern 1a. To ®nd the angular velocities
after impact, conservation of angular momentum about O1
for the whole system, and about O2 for the top block is
invoked. Speci®cally,
�h2O1�system � �h1
O1�system; �105�
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578570
Fig. 14. Transition from pattern 2a to pattern 1b through impact.
where
�h2O1�system � {IO1
1 m2l 0���������������������b2
1 1 �2h1 1 h2�2q
sin�u1 1 z
2 b 0�} _u21 1 {IG2
1 m2r2
���������������������b2
1 1 �2h1 1 h2�2q
sin�u2 1 uc2
1 z�} _u22 ;
�106�
and
�h1O1�system � {IO1
1 m2l���������������������b2
1 1 �2h1 1 h2�2q
sin�u1 1 z
2 b�} _u21 1 IO2
_u12 : �107�
Similarly,
�h2O2�top block � �h1
O2�top block; �108�
where
�h2O2�top block � m2r2l 0cos�u1 2 u2 1 uc2 2 b 0� _u2
1 1 �IG2
1 m2r22cos�u1 1 u2 2 uc2 2 b 0�� _u2
2 ;
�109�
and
�h1O2�top block � m2r2lcos�u1 2 u2 1 uc2 2 b� _u2
1 1 IO2_u2
2 :
�110�
Solving the system of Eqs. (105) and (108) for the angular
velocities immediately after impact gives
_u11 � A _u2
1 1 B _u22 ; �111�
and
_u12 � C _u2
1 1 D _u22 ; �112�
where
A � IO2E1 2 IO2
E2
E3IO22 IO2
E4
; �113�
B � IO2E5 2 IO2
E6
E3IO22 IO2
E4
; �114�
C � E4E1 2 E3E2
IO2E4 2 E3IO2
; �115�
and
D � E4E5 2 E3E6
IO2E4 2 E3IO2
; �116�
with
E1 � IO11 m2l 0
���������������������b2
1 1 �2h1 1 h2�2q
sin�u1 1 z 2 b 0�; �117�
E2 � m2r2l 0cos�u1 2 u2 1 uc2 2 b 0�; �118�
E3 � IO11 m2l
���������������������b2
1 1 �2h1 1 h2�2q
sin�u1 1 z 2 b�; �119�
E4 � m2r2lcos�u1 2 u2 1 uc2 2 b�; �120�
E5 � IG21 m2r2
���������������������b2
1 1 �2h1 1 h2�2q
sin�u2 1 uc2 1 z� �121�and
E6 � IG21 m2r2
2cos�u1 1 u2 2 uc2 2 b 0�: �122�In the preceding analysis, it was assumed that, after impact,
the base and top blocks rock separately about O1 and O2,
respectively (pattern 1a). If this analysis leads to the physi-
cally impossible case where _u12 , _u1
1 , then, after impact,
the top block remains attached to the base block, and the
system rocks as one rigid body about O1 (pattern 3a). In this
case, _u12 � _u1
1 , and the associated value is derived by
ensuring the conservation of the angular momentum about
O1 for the system. Speci®cally,
�h2O1�system � �h1
O1�system; �123�
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578 571
Fig. 15. Transition from pattern 2a to either pattern 1a or pattern 3a through impact.
with
�h2O1�system � {IO1
1 m2l 0���������������������b2
1 1 �2h1 1 h2�2q
sin�u1 1 z
2 b 0�} _u21 1 {IG2
1 m2r2
���������������������b2
1 1 �2h1 1 h2�2q
sin�u2 1 uc2
1 z�} _u22 ;
�124�and
�h1O1�system � IO
_u11 ; �125�
with IO given by Eq. (83). The relation for the angular velo-
cities is the same as in Eq. (84), but here B1� E1 and
B2� E5, with E1� E5 given as above. This same analysis
also holds for the case of transition from pattern 2b to
pattern 1b or 3b.
4. Accounting for impactÐpatterns 3 and 4
4.1. Impact in pattern 3
Consider the case where the two blocks are rocking
together as one body about O1 (pattern 3a). When impact
with the foundation occurs, the pole of rotation switches to
O 01, and the top block may either start rocking indepen-
dently about O 02 (pattern 1b) or remain in contact with the
base block so that the system rocks as one rigid body
about O 01 (pattern 3b). The two possibilities are illustrated
in Fig. 16.
Consider the case where the system switches from pattern
3a to pattern 1b. The conservation of angular momentum for
the system is expressed as
�h2O 0
1�system � �h1
O 01�system; �126�
where
�h2O 0
1�system � �IO 2 2Mb2
1� _u21 ; �127�
and
�h1O 0
1�system � {IO1
1 m2l��2h1 1 h2�cos�b�1 bsin�b��} _u11
1 {IG11 m2r2�bsin�uc2�1 �2h1
1 h2�cos�uc2��} _u12 :
�128�Similarly,
�h2O 0
2�top block � �h1
O 02�top block; �129�
where
�h2O 0
2�top block � {IO1
1 m2l 0�h2cos�b�2 b2sin�b 0��} _u21 ;
�130�and
�h1O 0
2�top block � m2l�h2cos�b�1 b2sin�b��} _u1
1 1 IO2_u1
2 :
�131�Solving the system of Eqs. (126) and (129) for the angular
velocities immediately after impact yields
_u11 � A _u2
1 ; �132�and
_u12 � B _u2
1 ; �133�where
A � IO2C1 2 C2C3
C4IO22 C2C5
; �134�
and
B � C5C1 2 C4C3
C2C5 2 C4IO2
; �135�
with
C1 � IO 2 2Mb21; �136�
C2 � IG11 m2r2�b1sin�uc2�1 �2h1 1 h2�cos�uc2��; �137�
C3 � IO11 m2l 0�h2cos�b 0�2 b2sin�b 0��; �138�
C4 � IO11 m2l��2h1 1 h2�cos�b�1 b1sin�b��; �139�
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578572
Fig. 16. Transition from pattern 3a to either pattern 1b or pattern 3b through impact.
and
C5 � m2l�h2cos�b�1 b2sin�b��: �140�In the preceding analysis, it was assumed that after impact
the base and top blocks rock separately about O 01 and O 02,respectively (pattern 1b). If _u1
2 . _u11 ; after impact the top
block remains attached to the base block, and the system
rocks as one rigid body about O 01 (pattern 3b). In this case,_u1
2 � _u11 ; and the associated value is derived by ensuring
conservation of the angular momentum about O 01 for the
system. Speci®cally,
�h2O 0
1�system � �h1
O 01�system; �141�
with
�h2O 0
1�system � �IO 2 2Mb2
1� _u21 ; �142�
and
�h1O 0
1�system � IO
_u11 : �143�
Eq. (141) is solved for the common post-impact angular
velocity yielding
_u11 � _u1
2 � IO 2 2Mb21
IO
_u21 : �144�
The above relations also hold for transition from pattern 3b
to pattern 1a or 3a.
4.2. Impact on pattern 4
Assume that the system is rocking in pattern 4a. If the
angle of rotation of the top block becomes zero, an impact
with the base block occurs, and the pole of rotation of the
top block switches to O 02. Furthermore, the base block may
either start rocking about O 01 in pattern 1b, or remain still as
in pattern 4b, see Fig. 17.
Consider the case where the system switches from pattern
4a to pattern 1b. Conservation of angular momentum for the
system is expressed as
�h2O 0
1�system � �h1
O 01�system; �145�
where
�h2O 0
1�system � {IG2
1 m2r2��2h1 1 h2�cos�uc2�2 b1sin�uc2��} _u22 ;
�146�and
�h1O 0
1�system � {IO1
1 m2l��2h1 1 h2�cos�b�1 b1sin�b��} _u11
1 {IG21 m2r2��2h1 1 h2�cos�uc2�
1 b1sin�uc2��} _u12 :
�147�Similarly,
�h2O 0
2�top block � �h1
O 02�top block; �148�
where
�h2O 0
2�top block � �IO2
2 2m2b22� _u2
2 : �149�
and
�h1O 0
2�top block � m2l�h2cos�b�1 b2sin�b��u1
1 1 IO2_u1
2 : �150�
Solving the system of Eqs. (145) and (148) for the angular
velocities immediately after impact gives
_u11 � A _u2
2 ; �151�
and
_u12 � B _u2
2 ; �152�
where
A � IO2C1 2 C2C3
C4IO22 C2C5
; �153�
and
B � C5C1 2 C4C3
C2C5 2 C4IO2
; �154�
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578 573
Fig. 17. Transition from pattern 3a to either pattern 1b or pattern 4b through impact.
with
C1 � IG21 mx2r2��2h1 1 h2�cos�uc2�2 b1�; �155�
C2 � IG21 m2r2��2h1 1 h2�cos�uc2�1 b1sin�u2��; �156�
C3 � IO22 2m2b2
2; �157�
C4 � IO11 m2l��2h1 1 h2�cos�b�1 b1sin�b��; �158�
and
C5 � m2l�h2cos�b�1 b2sin�b��: �159�In the preceding analysis, it was assumed that after impact
the base and top blocks rock separately about O 01 and O 02,respectively (pattern 1b). If _u1
1 . 0, after impact the base
block remains still and only the top block continues rocking
(pattern 4b). In this case, _u12 is derived from
�h2O 0
2�top block � �h1
O 02�top block; �160�
with
�h2O 0
2�top block � �IO2
2 2m2b22� _u2
2 ; �161�and
�h1O 0
2�rtop block � IO2
_u12 : �162�
Eq. (160) is solved for the post impact angular velocity
yielding
_u12 �
IO22 2m2b2
2
IO2
_u22 : �163�
This relation holds for transition from pattern 4b to
pattern 1a or 4a.
5. Numerical applications
Due to the nonlinearity of the preceding equations of
motion, their numerical integration has been pursued by
using a four-order Runge±Kutta algorithm. The dynamic
response of the system for the case of free rocking and
ground excitation has been computed for various system
parameters.
First free rocking of the system is considered. It is
induced by rotating the system through an initial angular
displacement, say u10� u20
; releasing it, and letting it
rock back and forth about alternative corners until the
motion decays to rest.
In the following example, a system of two blocks having
slenderness ratios H1/B1� 1 and H2/B2� 2.5 with base
width B1� 1.25 m and B2� 1.0 m were used. The blocks
were assumed homogeneous of equal material densities
r 1� r 2� 2500 kg/m3. The time step for the Runge±Katta
method was 0.001 s.
Fig. 18 shows the results for u10� u20
� 0.15 rad, and
zero initial angular velocities. It can be seen that the angles
of rotation of the two blocks are decaying in an oscillatory
manner, with the one of the base block decreasing at a faster
rate.
The system starts rocking about point O1 (pattern 3a) and
remains in this pattern until an impact with the foundation
occurs. When such an impact takes place, the pole of
rotation switches to O 01, and the top block starts rocking
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578574
Fig. 18. Free vibration response of a two-block system.
independently about O 02 (pattern 1b). From this point on, the
system experiences a number of impacts before coming to
rest. Note that in free rocking impact is the only mechanism
for transition between patterns, with every impact being
accompanied by a pattern transition.
In this example, the base block comes temporarily to rest
very quickly, since the amplitude of the second cycle is
already quite small. This block experiences a few more
short periods of rocking, generally as a result of an impact
with the top block. For the cases where the base block can be
thought of as being still, the system may be assumed to rock
in pattern 4. However, the top block undergoes a number of
cycles before coming to rest, with decreasing amplitude in
each cycle, except for the second half cycle. At t� 1 s, the
angle of rotation reaches a value of 0.183 rad, exceeding the
initial value u20� 0.15 rad. This is not unreasonable, since
the angular velocity of the top block increases during the
®rst impact. Note also that, the period of vibration changes
signi®cantly in each cycle for both blocks.
The dynamics of the preceding system was also analyzed
by employing the linearized equations for small angles of
rotation. The results for both the linear and nonlinear formu-
lation are illustrated in Figs. 19 and 20 for the base and top
block, respectively. Examining these ®gures, it can be seen
that the linear formulation based results deviate signi®-
cantly, during non-negligible time segments from the results
obtained by integrating the nonlinear equations of motion.
As a second case, the response of the system to a hori-
zontal earthquake excitation was computed. Results are
presented here for an accelerogram recorded at Simi Valley
during the 1994 Northridge earthquake in California. This
accelerogram, shown in Fig. 21, exhibits a peak amplitude
of 0.71 g. The structural model described in the previous
example is considered again here. The system response is
shown in Fig. 22 for both the base and top blocks. It can be
seen that the response of the base block is, in general, much
less than that of the top block. In particular, the base block is
set into motion whenever a large peak on the excitation
occurs, or when it is hit by the top block, in which case
the system rocks as one rigid block (pattern 3a or 3b). Atten-
tion is also drawn to the fact that the maximum response of
the two blocks, which occur at different times, does not
follow immediately the peak amplitude of the ground accel-
eration. Furthermore, note that the rocking of the system
ceases before the end of the earthquake record.
6. Concluding remarks
The dynamic behavior of structures of two stacked rigid
blocks subjected to ground excitation has been examined.
Assuming no sliding, the rocking response of the system
standing free on a rigid foundation has been investigated.
The analytical formulation of this nonlinear problem has
proved challenging. Its complexity is associated with the
transition from one pattern of motion to another, each one
being governed by a set of highly nonlinear equations.
Furthermore, depending on the pattern, this transition can
happen either through impact, occurring between the
blocks or between the base block and the ground, or, in
the absence of impact, by an instantaneous separation of
the two blocks.
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578 575
Fig. 19. Rotation angle for the lower block; linear versus nonlinear formulation.
The exact (nonlinear) equations governing the rocking
response of the system to horizontal and vertical ground
acceleration have been derived for each pattern. The
nonlinear equations of motion have been integrated for
each pattern by developing an ad hoc computational method
involving a fourth-order Runge±Kutta scheme, and
accounting for the various patterns. Numerical results
for both free vibration and seismic response have been
derived.
The model used in this paper, besides demonstrating the
complexity of even a simple two-block system rocking on a
rigid foundation problem, can also be used to incorporate
some of the characteristics of a ¯exible foundation. For
example, by inserting an elastic layer between the base
block and the rigid ground, the complex impact problem
may be eliminated. Also, it is possible to undertake a
comprehensive numerical investigation of the system
response for the actual ground motions, utilizing the compu-
ter program developed in this work. In the same context,
using an ensemble of synthetic earthquake ground motions,
response statistics may be obtained for a range of system
parameters, from which possible systematic trends in the
system response may be identi®ed. Experimental investiga-
tion of the problem can also be expected in future work; this
attempt will be essential in validating the analytical results
for the nonlinear equations of motion. Finally, dynamic
analysis of multi-block structures, consisting of more than
two blocks, can be performed using a method analogous to
the one described in this work. This effort could perhaps
be expedited by incorporating in the analysis concepts of
the discrete elements technique as in the study of Azevedo
et al. [32].
P.D. Spanos et al. / Soil Dynamics and Earthquake Engineering 21 (2001) 559±578576
Fig. 20. Rotation angle for the upper block; linear versus nonlinear formulation.
Fig. 21. Accelerogram from the Northridge, CA, 1994, earthquake.
Acknowledgements
The support of this work by a grant from the National
Science Foundation is gratefully acknowledged. Further, the
assistance of Dr M. Kokolaras with the creation of an initial
electronic template for the paper is appreciated.
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