theory anisotropic thick plates
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FTD-HT-
2 3-600-69
EDITED
RANSLATION
THEORY
OF
ANISOTROPIC
THICK
PLATES
By:.
G .Lekhnitskiy
English
pages:
Source:N
SSSR.
Izvestiya.
ekhanika
iMashinostroyeniye(Academy
of
Sciences
of
the
USSR.
*ws.
Mechanics
and
MachineBuilding))
No.2 ,1959,pp.
142-1H5.
Translated
by:
.
Koolbeck/TDBRS-3
TH IS
TRANSLAT ION
S
A
Rt
NDIT IONO F
TH R
ORIGI -
NAL
P0USI6N
TIXT
WTHGUT
ANY
ANALYTICAL
O R
EDITORIAL
OMM I N T .
TATEMENTSOR
THRORIIS
ADVOCATED ORIMPLIED ARE THOS E
O P
TH E
SOW
AND 00NO TNECESSAR I LYREFLECT
TNI
POSIT ION
O RPINION
PIC
ORS IONICHNOLOOY
I-
VIS ION.
PREPAREDBY.
TRANSLAT ION
DIVISION
FORE IGN
T E CMNOLO SV DIVIKON
IP-APt,
OH I O .
FTD-
H T
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3- 6oo -69
Date21
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19
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THEORYOP
ANISOTROPIC
THICK
PLATES
S .G.
Lekhnitskiy
(Saratov)
The
goaloftheseremarks
is
to
show
how
the
classicaltheory
of
thick
plates
isgeneralized
to
thecase
ofa
plate
possessing
anisotropyofa
particular
type,
thatis,
a platemanufactured
from
transversallyIsotropie
materialandconsequently
possessing
five
independent
elasticconstants.
1 .
Generalinformation
. In
the
classical
statement,
the
problem
of
equilibrium
ofan
Isotropie
thick
plateisreduced
to
thedeterminationof six
componentstresseso
a
...,
T nd
x y
xy
threoprojections
of
displacement-
u ,
v ,
w which
strictly
satisfy
allequations
of
elasticity
theoryand
also
theboundary
conditionsonthe
flat
surfaces(faces). Theconditionson
the
lateral
surface,i.e.,
on
the
edge
of
the
plate,
are
satisfied
approximately,"ontheaverage,"a sinthetheoryOfthe
generalized
planestressstateorinthetheoryof
bending
of
thick
plates.
If
the
platei s
deformed
only
by
aload
distributedalong
the
edge,twobasiccasesofequilibrium
aredistinguished:
a )
the
plane
stress
state,and
b )
bending. Each
case
reduces
tothe
determination
inthe
region
of
the
plate
of
a
single
biharmonic
function
of
thevariables
x ,
y
( a
function
of
stresses
or,
correspondingly,of
thedeflectionof
themiddleplane),
satisfying
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V
theboundaryconditionsonthe
contour;thecorresponding
solutions
are
called
homogeneous
([1],
page
200).
Iftheflatsurfaces
are
alsoloaded
the
solution
is
obtained
by
superimposing
the
homogeneous
solutions
and
thesolution
for
an
infiniteelastic
layer
bounded
bytwo
parallel
planesover
which
given
forces
are
distributed.
he
homogeneous
solutions
foran
Isotropie
plate
are
determined
by
simpleformulas
which
connect
stresses
and
displacements
with
thebiharmonicfunction.
Iti s
easyto
show
that
in
the
caseof
a
transversally
Isotropie
platethehomogeneous
solutions
alsohavea
very
simplestructureandalsoconnect
stresses
and
displacementswiththe
biharmonic
function.
Let
there
be
a
plate
which
is
cutout
of
transversally
Isotropiematerial
in
sucha
way
that
in
it
theplane
ofisotropy
is
parallel
tothemiddlesurface.e
will
take
the
latter
as
plane
xy
and
designate
thethickness
oftheplate
as
h . The
equations
of
the
generalizedHookelaw
are
writtenasfollows
([2],page
28):
T^
+ V
+
A
l
1
(1.1)
2 1 - f v )
xi
Here
Eand
E ,
are
theYoung
moduli
for
tension-compression
indirectionsparallelandperpendicularto
themiddle
plane;
vi s
the
Poissoncoefficient,
characterizing
the
contractioninthe
plane
of
isotropy
during
tension
inthesame
plane;v ,
i sthesame
parameter
for
stretching
in
the
transverse
direction
z ;v
?
i s
the
Poissoncoefficient
which
characterizes
contractioni n
the
directionwhichi s
normal
tothemiddlesurfaceduringtension
in
planes
whichareparallelto
the
middle
surface;
G=E/2(l+
v);
and
G ,i stheshearmodulus
for
planes
whichareparallel
and
normal
to
the
middlesurface, in
all
there
arefive
different
constants,sinceE v ,=E,v
?
.
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~r
Ten
unknown
functions
must
satisfy
thebasic
systemof
equations
of
equilibrium
for
a
transversallyIsotropie
body;
we
will
obtainthis
system
by
adding
to(1.1)three
equations
of
equilibrium
of
a
continuous
medium:
d ,
4
dt
i> F fh * \* .
d * F
h*
\
*
,
\
V-Vi
0
(2.1)
(2.2)
(2.3)
Here
F
i s
a
function
of
Airystresses,
satisfyingthe
equation
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W-? ( V - - J 5 T
+
^-)
2 . 4 )
Thefirst
terms
of
the
expressions
-
u ,v ,
o
o and
T
x
y
x y
will
be
the
average
over
the
thickness
of
the
values
of
displacements
andstresses
andare
connected
by
the
equations
of
theplane
problem
i
a/
(2.5)
a
ii
2< 1
+
v .
* F
B y t r diy
Th e
second
terms,
depending
on
z ,
are
correctionmembers
which
takeinto
account
the
change
inthe
displacements
and
stresses
over
the
thickness.
I n
order
to
obtain
the
distribution
of
stresses
in
athickplate
i t
i s
necessary
firsttosolvetheplaneproblem,
i.e.,
t o
findF ,
u ,
andv .
Inthe
case
ofan
isotropic
material,v~
=
v ;a
e
v/2(l
+
v).
3 .
Bending
,
If
the
plate
is
deformed
by
abending
load
distributed
only
along
the
edge,displacementsand
stresses
are
expressed
through
a
biharmonic
function
a s
follows:
.__
..
,
^...-^v*.
( 3 . 1 )
E
o*n
3 V , \
( *
-
,\*
%h
fop,
z ?
f t \
9
,
Here
*-*+T*I T- **
p-i-i?
3.3)
Stresses
o
ando leadto
bending
momentsM
nd
M
T
leads
x y
x
y
x y
t o
the
torsion
moment
H, :
t ,
T
ead
; o
shearing
forces. The
x y
X i , z
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7
The
formulas
for
displacements,
stresses,
and
oments
are
obtainedfrom(3.1),(3.2),and
(3.1)
by
adding
toheirright
sides,
respectively,
the
expressions
'-IF*' -ir*
*--*+
^8=5^+
3 . 8 )
v-v-v-
3.9)
The
normal
stress
on
areas
which
are
parallel
to
themiddle
plane
i s
different
from
zero:
kK
| i
- T + i r ) + - f . l T - T r )
3 . 1 0 )
4 .
ending
of
a
round
plate
.
e
shall
consider
in
greater
detail
thecase
of
around
platewithradiusa,
supported
along
the
entire
edge
and
bentbyuniformly
distributed
load
q;
the
weight
of theplatei s
ignored.
Wewill
obtain
theexpressions
fordisplacements
u u
Q
and
r
stresses
c o_,and
T
Q
in
cylindricalcoordinates
from
the
r
re
t f
corresponding
expressionsof
the
theory
ofthin
plates;
wewill
replacew
Q
in
the
latter
by
the
quantity
w.,
whichdepends
on
z ,
and
we
will
add
to
the
right
sides
the
functions
2T
IE
tH ( 3 1 4 i \
(4.1)
I norder
tofindthe
moments
M M andH
n
,i ti s
necessary
r U r
6
to
takethe
formulas
ofthetheory
of
thinplates,to
replacew
Q
in
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them
b ythe
e x p re s s i on
w ,andtoad dthem o me n t scorresponding
8 '
o
o'
and
o,
i.e.,
(4.2)
It
isclearthatw
n
isafunctiononlyof
di s p e rs i on
r :
0
* W
A
+
D ,%
(4.3)
(termswhich
give
asingularity
in
the
centerarediscarded).
Theboundary
conditions
have
the
form
- 0 ,
/
f
-
o
hen
r
a
(4.4)
Weshall
i n t ro d u ce
the
finalformulasf or
di s p l a ce me n t
wat
anypoint
and
forthestresses:
-*J6(i-v)i>(T+T
a
-TV+ "
v - * [ c ^ * - *
+
-
* - J r ) l
= - 4 F [ 3
+
v ) _ 3 v
,
rfm(
T
-
J
3 * 4 :
N
f r
/
A
(4.5)
(4.6)
Here
the
following
designations
areused:
-r=vfrflr-*S'JBJECTAREA
15, 20
TOPIC
TAGS
modulusof
elasticity,
anisotropic
medium,
elasticity
theory,
circular
plate,Isotropie
property
AUTHOR
CC-AUTHORS
LEKHNITSKIY.
S.
G .
10-OATE
OFNFO
5 9
SOURCE
ANSSSR.IZVESTIYA.MEKHANIKA
I
MASHINOSTROYENIYE
RUSSIAN)
FTT>
6-DOCUMENT
NO.
HT-23-6QO-6Q
PROJECT
NO .
72?01-7fi
7-HEADERCLASN
SECURITYAND
DOWNGRADING
NFORMATION
UMCL.
0
7>-SUPERSEDES
7*-CHANCS
6A-CONTP.OLMARKING
NONE
UNCL
76-
REEL/
FRAME
NO.
1891
785
CONTRACT
NO.
XRE FACC .
NO .
65-
AO-GEOGRAPHICAL
AREA
NO .O FPASES
U
PUBLISHING
OATE
4-
TYPE
PRODUCT
TRANSLATION
REVISION
REQ
NONE
STEP
NO .
02-UR/OI79/59/OOO/OO2/OI42/OI45
ABSTRACT
( )
The
material
ofthe
plate
is
assumed
to
be
transversely
Isotropie,withthe
planes
ofisotropy
parallel
tothemiddle
surface,andthe
material
therefore
possessesfive
independent
elasticconstants.
quationsare
given
without
detailedderi-
vation
forthe
displacements
and
stressescorresponding
to
a
state
of
plane
stress,
and
for
the
displacements,
stressesand
moments
in abentplate,
bothfor
thegeneralcase,andforthe
particularcaseofa
plate
bent b ya
uniformly
distributed
pressureinadditiontoitsownweight.or
a
simply
supported
circular
plate
subjected
to
a
uniformly
distrubuted
pressure
the
equations
for
displacements,
stressesand
moments
are
given,
neglecting
theweight
of
theplate.
or
the
particular
cases
considered,
the
errors
of
thethinplate
approximationare
negligible
if
the
materialisIsotropie,but
areappreciable
ifthematerial
isanisotropic.
the
errorsbecominglargerthe
smaller
the
ratio.here
are
4
Sovietreferences.
AF$C IfoTii F TDOVER PR IN T D EC
8)
AFc lum