Finite Dynamic Model for Infinite Media: Engineering Mechanics Research

6719
August,
1969
EM
4
Journal of the
ENGINEERING MECHANICS DIVISION
Proceedings of the American Society of Civil Engineers
FINITE
DYNAMIC
MODEL
FOR
INFINITE
MEDIA
By
John
Lysmer,
1 M.
ASCE,
and
Roger
L.
Kuhlemeyer,2
A.
M.
ASCE
INTRODUCTION
The
rational
approach
to
analytical
studies
of
sonic
flaw
detection
meth-
ods,
blast
effects,
foundation
vibrationsi
and
numerous
other
dynamic
prob-
lems
is
to
consider
them
as
"-'ave
propagation
problems
in
an
infinite
solid.
This
approach
has
two
major
advantages:
(1) The
radiation
of
energy
from
the
excited
zone
to
the
far
field
is
properly
accounted
for;
and (2) the
·concept
of
infinity
is
mathematically
convenient
when the
aim
is
to find
closed
form
analytical
solutions
for
simple
homogeneous
systems.
For
most
of
the
complicated
geometrics
encountered
in
practice
it
is
not
possible
to
find
closed
form
solutions
and,
therefore,
it
is
necessary
to
re-
sort
to
numerical
methods
of
the
finite
difference
or
discrete
mass
type.
With
these
methods
only a
finite
number
of
nodal
points
can
be
considered;
thus
the
numerical
methods
are
not
directly
applicable
to
infinite
systems.
A
gen-
eral
method
through
which
an
infinite
system
may
be
approximated
by a
finite
system
with a
special
viscous
boundary
condition
is
described
herein.
The
resulting
model
may
be
analyzed
by
ordinary
numerical
methods
but
is
han-
dled
with
particular
ease
by
the
finite
element
method.
Examples
utilizing
the
finite
model
for
analysis
of
steady
state
foundation
vibration
problems
are
presented
herein.
The
results
clearly
demonstrate:
(1)
The
near
equivalence
between
an
infinite
half
space
and the
proposed
finite
model;
and
(2) the
power
of
the
method
to
analyze
previously
unsolvable
problems.
Note.-
Discussion
open
until
January
1, 1970.
To
extend
the
closing
date
one
month,
a
written
request
must
be
filed
with
the
Executive
Secretary,
ASCE.
This
paper
is
part
of
the
copyrighted
Journal
of
the
Engineering
:Vlechanics
Division,
Proceedings
of
the
American
Society
of
Civil
Engineers,
Vol.
95,
No.
EI'l14,
August,
1969.
:\1anuscript
was
submitted
for
review
for
possible
publication
on
August
1, 1968.
1
Asst.
Prof.
of
Civ.
Engrg.,
Univ. of
Calif.,
Berkeley,
Calif.
2
Grad.
Student,
Dept.
of
Civ.
Engrg.,
Cniv.
of
Calif.,
Berkeley,
Calif.,
and
Staff
Engr.,
Dames
and
:rvloore, San
Francisco,
Calif.
(on
leave
of
absence).
859
860
August,
1969
PROPOSED
MODEL
Fig.
1
show_s
a
typical
example
of
an
infinite
system.
Consider
an
imagj,
nary
convex
boundary
enclosing
all
sources
of
disturbance
and
all
irregular
geometrical
features.
Propagation
of
energy
will
occur
only
from
the
interior
to the
exterior
region
and
all
energy
arriving
at
the
boundary
will
pass
int()
the
exterior
region.
The
effect
of the
exterior
region
on the
interior
region
is
therefore
identical
to
that
of
an
energy
absorbing
or
nonreflecting
boundary,
This
observation
leads
directly
to the
idea
of
determining
the
dynamic
re.
sponse
of the
interior
region
from
a
finite
model
consisting
of
the
interior
region
subjected
to a
boundary
condition which
ensures
that
all
energy
arriv.
ing
at
the lxiundary
is
absorbed.
The
writers
have
investigated
different
pas.
-/
'>;;;;>>
I
,n>7~77,
7T7n?:
111
»n~"T>n>'7'>~
~
>>v»»»
J
I
J
I
I
I
exterior
region
\ I
\ ,~
\ I'!
\ I "
\
1.8
I I
\ I
if
\
I~
\
18
',,
interior /1
, region
,,,.
/
................
.,....,,,...
---.-
FIG.
1.-TYPICAL
INFINITE
SYSTE.I\-1
sibilities
for
expressing
this
boundary
condition
analytically
and
have found
that
the
most
promising
way
is
to
express
it
by
the
conditions
a
=a
p
Vp
W
T = b p
Vs
ti
111
(2)
in
which a
and
T
ar~
the
normal
and
shear
stress,
respectively;
W and U
are
the
normal
and
tangential
velocities
respectively;
p
is
the
mass'
density;
v5
and
Vp
are
the
velocities
of
S-waves
and
P-waves,
respectively;
and
a
and
b
are
dimensionless
parameters.
The
_propos'ed
boundary
condition
corresponds
to a
situation
in
which
the convex
boundary
is
supported
on
infinit€simal
dash-
pots
oriented
normal
and
tangential
to
the
boundary.
·
REFLECTION
AT
VISCOUS BOUNDARY
It
is
necessary
to
study
the
reflection
of
elastic
waves
at
the
viscous
boundary
defined
in
Eqs.
1
and
2
in
order
to
deter~ine
appropriate
param-
eters
a
and
b.
The
phenomena
may
be
studied
by a technique
similar
to the
EM 4 INF1NJTE
MEDIA
861
one
used
by
Ewing,
Jardetzky,
and
Press
(2)3
for
the
reflection
and
refraction
of
elastic
waves
at
an
interface
between
two
media.
Incident
P-Wave.-The
situation
for
the
case
of
an
incident
P-wave
is
shown
in
Fig.
2. The
x-axis
represents
the
viscous
boundary
and
the
elastic
medium
is
located
in
the
lower
half
plane.
The
incident
wave
generates
two
reflected
waves,
an
S-wave
which
travels
with
the
velocity
Vs
=
1¥,
...................................... (3)
and, a
P-wave
which
propagates
with
the
velocity
1
Vp
= - Vs
s . . . . . . . . . . . . . . . .
(4)
In the
previous
equations
G
is
the
shear
modulus
ands
is
an
elastic
constant
defined
by
s2
= 1 - 2 µ
2
(!
-
µ)
in which µ
is
Poisson's
ratio.
••....•••.••••.•••.••••••..••
(5)
z
FIG.
2.-INCIDENT
P-\11.'AVE
AT
'\lISCOUS BOUNDARY
The
directions
of the
incident
and
reflected
waves
are
related
through
Snell1s Law
Cos
ZJ
=
s.
cos
e
.................................
(6)
and the
velocity
of the wave
front
along
the
x-axis
is
c = V p
sec
e ,
...
,
......•......................
(7)
The
horizontal
and
vertical
displacements
may
be
written
in
terms
of
displ~c~ment
potentials
cb
and
lfJ
as
'3
Numerals
in
parentheses'
refer
to
corresponding
items
in
the
Appendix
I.-
References
.
862
u =
.!!.!£..
ax
a~
az
W =
a$
+
a~
oz
ax
August,
1969
(8)
••.••••.••.••.•.•.•.••••..•••••.•.•.
(9)
in
which ¢ =
1Jlz
,z
,t)
and
1.Ji
= lj;(x ,z
,t)
represent
the
displacements
due to
P-
waves
and
S-waves,
respectively.
Since
the wave
fronts
of the
three
waves
in
Fig.
2
must
travel
along the
x-axis
at
same
velocity
c,
it
can
be
shown that
the
displacement
potentials
for
harmonic
waves of
frequency
w
must
have
the
form
~=exp
[ik(ct
+ z tan e -x)]
+A
exp
[ik(ct
-z tan e -x)]
(JO)
~
incident
P-wave
reflected
P-wave
and
~
= B
exp
[i
k(c
t -z tan v -x)] . . . (J ! I
reflected
S-wave
in
which
k
is
the
wave
number
defined
by
k =
~
. • • • . . . (J2)
c
and
A
and
B
are
the unknown
amplitudes
of the
reflected
waves.
These
ampli-
s s
z
FIG.
3.-INCIDENT
S-WAVE
AT
VISCOUS BOUNDARY
tudes
may
be
determined
by the
stress
boundary
conditions
defined
in
Eqs.
1
and
2
which
may
be
expressed
in
terms
of
displacement
potentials
as
follows:
1 - 2 s2
s'
'
(~
ft)
__ a
(~
a,P)
v
<b
+ 2
oz
2 + aioz -s
Vs
az
+
ax
· · · · · · · · (IS)
INFINITE
MEDIA
863
=
:s
(:£
-
:~)
(14)
Substitution of
Eqs.
10
and
11
into
Eqs.
13
and 14
yields
the
two
linear
equations
(1
- 2 s2
cos
2(]
+a
sin
e)A
+(sin
211
+a
cos
B)B
==
2 s2
cos
2 e -1 + a
sin
e . . . . . . . . . I
15
l
(b
cos
v + s2
sin
28)A
+
(cos
2v
-b
sin
v)B
= s2
sin
2e
-b
cos
v
...................•.........
(16)
from which the
amplitudes
A
and
B
may
be
determined
as
functions of the
incident
angle
e.
1--'
---l
i/'
FIG.
4.-INCIDENT
P-\VAVE
Incident
S-Wave.-The
case
of an
incident
S-wave
shown
in
Fig.
3
may
be
solved
in
a
similar
fashion.
Eqs.
6
to
9
and
Eqs.
12
to
14
are
valid
for
this
case
but
Eqs.
10 and 11
must
be
replaced
by
¢=A
exp [ i
k(c
t -z tan e -
x)]
.....................
117)
reflected
P-wave
~
exp
[ik(c
t + z
tan
v -
x)]
+ B exp
[ik(c
t -z
tan
v -x)] (18)
~
incident
S-wave
reflected
S-wave
Thus the
linear
equations
applicable
to
define A and B for
the
case
of
an
incident S-wave
are
as
follows:
(s
2
sin
28
+ b
cos
v)A
+(cos
2v -b
sin
v)B
= -
cos
2v -b
sin
v (19)
(-cos
2v
+a
sin
&)A
+(sin
2v
+a
cos
e)B =
sin
2v
-a
cos
8
{20)
A
special
case
occurs
when the
incident
angle
v
becomes
smaller
than
the
critical
angle
Ver
defined
by
1 / 19 100%
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