FaultyofArhiteture
ANALYSIS OF COMPOSITE BEAMS
Aniko Pluzsik
Supervisor:
Laszlo P. Kollar
Budapest, January, 2003
I would liketo thankProfessor LaszloP. Kollarfor allof his help and ooperation. He is an
extraordinary teaher not only in the lassroom, but in life's lessons as well. His approah to
people, his endless patiene,and his outlookon theworld havemadealasting impression. Iam
privilegedtohavehadtheopportunitytoworkwithhim.
ThankstothehairmenofthedepartmentsforprovidingmyPh.Dstudies:
ProfessorGyorgyFarkas,ChairmanoftheDepartmentofStruturalEngineering,
ProfessorTamasMatussakand ProfessorGabor Domokos,ChairmenoftheDepartment
ofMehanisandStrutures.
1 Introdution 9
2 Review ofompositebeamtheories 9
2.1 Constitutiveequations . . . 10
2.2 Classialbeam-theories(norestrainedwarping,nosheardeformation) . . . 10
2.2.1 Basiassumptions . . . 10
2.2.2 Isotropibeam . . . 11
2.2.3 Orthotropibeam . . . 11
2.2.4 Generallyanisotropibeam . . . 12
2.3 Vlasovtypebeamtheories(restrainedwarping,nosheardeformations). . . 13
2.3.1 Basiassumptions . . . 13
2.3.2 Isotropibeam . . . 13
2.3.3 Beamswithsymmetriallaminates . . . 14
2.4 Timoshenkotypebeamtheories(sheardeformation,norestrainedwarping) . . . . 14
2.4.1 Basiassumption . . . 14
2.4.2 Isotropibeam . . . 14
2.4.3 Generallyanisotropibeam . . . 15
2.5 Theoriestakingintoaountrestrainedwarpingand sheardeformations . . . 15
2.5.1 Basiassumption . . . 15
2.5.2 Isotropiandorthotropibeam . . . 15
2.5.3 Symmetrialbeam . . . 16
2.6 Theories taking into aount restrained warping, shear deformationsand warping induedshear . . . 16
2.6.1 Basiassumption . . . 16
2.6.2 Isotropiandorthotropibeam . . . 17
2.6.3 Generallyanisotropibeam . . . 18
2.7 Generalizedbeamtheories . . . 18
2.7.1 Isotropiandorthotropibeam . . . 18
2.8 Transverselyloadedbeams. . . 18
2.8.1 Classialbeam-theories(norestrainedwarping,nosheardeformation) . . . 18
2.8.2 Theories taking into aount restrained warping indued shear (restrained warping,sheardeformation) . . . 19
3 Theoryofopen andlosedsetion,generallyanisotropithin-walledbeams-no restrainedwarping 19 3.1 Problemstatement . . . 19
3.2 Opensetionbeams . . . 20
3.2.2 Step2. Foresandmomentsin thewallsegments. . . 23
3.2.3 Step3. Foresin thebeam . . . 26
3.2.4 Step4. Stinessmatrix . . . 26
3.3 Closed setionbeams. . . 28
3.3.1 Step1. Strainsin thewallsegments . . . 30
3.3.2 Step2. Foresandmomentsin thewallsegments. . . 30
3.3.3 Step3. Foresin thebeam . . . 31
3.3.4 Step4. ForesX 1 andX 2 . . . 32
3.3.5 Step5. Stinessmatrix . . . 32
3.4 Centroid. . . 33
3.4.1 Stinessandomplianematriesintheentroidoordinatesystem . . . . 34
3.4.2 Stinessmatrixof orthotropibeams. . . 36
3.5 Stressesandstrains. . . 36
3.5.1 Opensetionbeams . . . 36
3.5.2 Closedsetionbeams. . . 37
3.6 Veriation . . . 38
3.6.1 I-beamwithunsymmetriallayup[0 6 =45 6 ℄. . . 41
3.6.2 I-beamwithdierentlayups. . . 45
3.6.3 Box-beamwithunsymmetriallayup ([ 0 6 =45 6 ℄) . . . 45
3.6.4 Box-beamwithdierentlayups . . . 49
3.7 Disussion . . . 50
3.7.1 Eetofanisotropy . . . 51
3.7.2 Eetofloalstiness . . . 51
4 Theory ofopen setion,orthotropi,thin-walled beams-with restrainedwarp- ing 54 5 Theoryoflosedsetion,orthotropi,thin-walledbeams-withrestrainedwarp- ing 56 5.1 Literature . . . 56
5.2 Problemstatement . . . 59
5.3 Assumptions . . . 59
5.4 Governingequations . . . 60
5.5 \Exat"solutionforsinusoidalloads . . . 63
5.6 SolutionbytheRitzmethod . . . 64
5.7 Beamtheory . . . 66
5.7.1 Assumptions . . . 66
5.7.3 Replaementstinesses . . . 68
5.7.4 Unsymmetrialbeams . . . 75
5.7.5 Veriation . . . 76
6 Eetof sheardeformation and restrainedwarping 80 6.1 Problemstatement . . . 81
6.2 Eetofsheardeformation . . . 81
6.3 Eetofrestrainedwarping . . . 86
6.3.1 Opensetionbeams . . . 86
6.3.2 Closedsetionbeam . . . 91
6.4 Numerialexample . . . 92
7 Conlusions 96 8 Referenes 97 A Stiness matrix ofa laminatedompositeplate 100 B Solution ofthe dierential equation of beamsin torsion 102 B.1 Simply supportedbeam . . . 102
B.2 Cantileverbeamsubjetedto aonentratedtorqueattheend . . . 103
C Buklingof ompositeolumnssubjetedto onentrated loads 105
D The \neutral" surfaes ofa laminate 105
E Solution ofa simplysupported beam 107
A area
[A℄;[B℄;[D℄ stinessmatriesofaplate
[e℄; h
e
i
; h
e
Æ i
omplianematriesofaplate
A
ij
;B
ij
;D
ij
elementsofthestinessmatries
EA tensilestinessofanorthotropibeam
EI
yy
;EI
yz
;EI
zz
bendingstinessesofanorthotropibeam
EI
!
warpingstinessofanorthotropibeam
GI
t
torsionalstiness ofanorthotropibeam
S
ij
shearstinessesofanorthotropibeam
s
ij
shearomplianesofanorthotropibeam
h platethikness
b
k
widthofawallsegmentofthebeam
K numberofwallsegments
L lengthofthebeam
l eetivelengthofthebeam
b
N
x
axialforeatingonabeam
M
y
;
M
z
bendingmomentsatingonabeam
M
!
bimomentatingonabeam
b
T
x
torqueatingonabeam
b
T
sv
SaintVenanttorqueatingonabeam
b
T
!
restrainedwarpinginduedtorqueatingonabeam
b
V
y
; b
V
z
shearforesatingonabeam
X
1 ,X
2
foreandmomentperunit lengthapplied attheutofalosedsetionbeam
N
x ,N
y
;N
zy
in-planeforesatingonaplate
M
y
;M
z
;M
zy
bendingandtwistmomentsatingonaplate
M
!
bimomentatingonabeam
[P℄ stinessmatrixofabeamreferstotheentroid
P
stinessmatrixofabeamreferstoanarbitrarilyhoosenpoint
[W℄ omplianematrixofabeamreferstotheentroid
W
omplianematrixofabeamreferstoanarbitrarilyhoosen point
u;v,w displaementsinthex,y andzdiretions
w
B ,w
S
displaementsdueto bendingandshear deformations
y
,z
oordinatesoftheentroid
o
x
axialstrainofthebeam
xy
strainsoftherefernesurfaeof aplate
1
y
; 1
z
urvaturesofthebeam
# twistperunit length
# B
;# B
twistperunit lengthdueto bending andsheardeformations
seondderivativeofthetwistofthebeam
y
;
z
rotationoftheross-setionofthebeaminthex zandy z planes
twistofthebeam(rotationoftheross-setionaboutthexaxis)
loationofthe\tension neutral"surfae
loationofthe\torqueneutral"surfae
parameterforestimatingtheerroroftheshear deformation
q shearow
C
k
onstansintheRitzmethod
k
basifuntions intheRitzmethod
[F℄; f o-eÆtientmatrixandvetorintheRitzmethod
[A
1
℄;[A
1
℄;[B
1
℄;[B
2
℄;[B
3
℄ submatriesof[F℄
Figures
Figure1 page20 Figure22 page59 Figure43 page84
Figure2 page21 Figure23 page60 Figure44 page85
Figure3 page22 Figure24 page61 Figure45 page86
Figure4 page23 Figure25 page62 Figure46 page87
Figure5 page24 Figure26 page63 Figure47 page87
Figure6 page25 Figure27 page63 Figure48 page89
Figure7 page25 Figure28 page65 Figure49 page90
Figure8 page28 Figure29 page67 Figure50 page90
Figure9 page28 Figure30 page70 Figure51 page91
Figure10 page29 Figure31 page70 Figure52 page91
Figure11 page29 Figure32 page71 Figure53 page92
Figure12 page33 Figure33 page76 Figure54 page93
Figure13 page38 Figure34 page76 Figure55 page94
Figure14 page39 Figure35 page77 Figure56 page94
Figure15 page41 Figure36 page79 Figure57 page100
Figure16 page45 Figure37 page79 Figure58 page101
Figure17 page47 Figure38 page80 Figure59 page103
Figure18 page51 Figure39 page81 Figure60 page105
Figure19 page55 Figure40 page82 Figure61 page106
Figure20 page57 Figure41 page82
Figure21 page58 Figure42 page84
Tables
Table1 page27 Table7 page52 Table13 page88
Table2 page38 Table8 page53 Table14 page88
Table3 page40 Table9 page54 Table15 page98
Table4 page46 Table10 page73 Table16 page98
Table5 page50 Table11 page83 Table17 page98
Table6 page51 Table12 page88
Instruturalmodelingofbeamstherearetwoontraditoryrequirements: themodelingofabeam
must be simple and aurate at the same time. In the literature several beam theories an be
foundforanisotropithin-walledbeams. Setion1summarizesthese theories,from thesimplest,
tothemoreadvanedones.
Beammodelsthat anbefoundin theliteraturedonotoverallthepratialases. Theaim
ofthisthesisisto fullthelakonthis eld.
First we develop beam models for generally anisotropi beams with open and losed ross-
setionsusingtheassumptionsof lassialbeamtheories(Setion 3). (Solutionthat anbeused
for pratial purposes is available only for losed setion beams [16℄. However Manseld [16℄
negletstheloal bending stinessesof thewallsegmentsof thebeam. Thus, his solutionis not
appliableforallases.)
Thenweonsiderorthotropi,losedsetionbeamstakingtheeetofrestrainedwarpinginto
aount(Setion 5). (Abeammodel isavailable onlyforpure torsionof symmetriross-setion
beams in the literature[20℄, however,Urban's solution [20℄ results in an unaeptable error for
shortbeams.) Ouraimisto developabeammodelwhih anbeused forallpratialases.
Inaddition,ouraimistodeterminetheaurayandappliabilityoftheexistingbeammodels
withtheaidofnumerialomparisons(Setion6).
2 Review of omposite beam theories
This setion summarizes the dierent beam theories available in the literature. However, the
questionremains: how aurate are these models, and under whih irumstanes they an be
used.
Thetheoriesdierfromeahotherin
the alloweddeformations ofthe beam's elements (e.g. the ross-setionsremain planeand
perpendiulartotheaxisortheymaydeform),
theallowedmaterialtypesandlayupsofthewallsofthebeam(e.g. orthotropi,symmetrial
layup,et.),
theallowedgeometryof theross-setion(openorlosed setionbeams,symmetrialross-
setions,et.),
loadingonditions(endloadsortransverseloads),
Setion2.2.4).
2.1 Constitutive equations
Weonsideropenorlosedsetionthin-walledbeams.
Thegeneralizedstressesofawallofthebeamaretheintegralsofthenormalandshearstresses
(
x
;
y
;
xy
)alongthethikness. ThegeneralizedstressesofthebeamfNgaretheintegralofthese
stressesofthewallsalongtheirumferenes.Thegeneralizedstrainsf"garealulatedfrom the
displaementsof thebeambythegeometrialequations. Theonstitutiveequationsrelatethese
stressestothestrains. Itan bewrittenas follows:
fNg=
P
f"g (2.1)
where
P
isthestinessmatrixofthebeam.
Wesummarizethebeam-theoriesbelowaordingtothefollowingtwoquestions
Howarethegeneralizedstresses( fNg)andstrains( f"g)aredened?
Whihelementsofthestinessmatrix(
P
)arenon-zero?
2.2 Classial beam-theories (no restrained warping, no shear deforma-
tion)
Inthefollowingwesummarizethetheorieswhereaxialonstraints(restrainedwarping)andshear
deformationsinbendingarenottakeninto aount.
2.2.1 Basi assumptions
1. Theeet of hange in geometry oftheross-setion isnottakenintoaountin theequi-
libriumequations.
2. TheKirhho-Lovehypotesisisvalidforeahplateelement.
3. Thenormalstressesintheontourdiretions issmallomparedtotheaxialstresses.
4. Thestrains(
x
)varylinearlyalongtheyand zaxes:
x
= du
dx y
d
y
dx z
d
z
dx
(2.2)
where uis the axial displaement, and the rotation of the ross-setion
y and
z in the
x y and x z planesanbealulatedfrom thedisplaementsof theaxisin they and z
diretions(v andw):
y
= dv
dx
(2.3)
z
= dw
dx
y z
gleted.
2.2.2 Isotropi beam
Abeamisisotropiwhenitismadeofisotropimaterial. IntheSaintVenanttheoryfourgeneral-
izedstressesaredened: normalfore
b
N
x
= R
N
ds
, bendingmomentsaboutthey andzaxes
M
y
= R
(N
y+M
os)dsand
M
z
= R
( N
z+M
sin)ds
andtorque
b
T
x
= 2
R
M ds
.
Thegeneralizedstrainsare: theaxialstrainofthebeam'saxis o
x
= u
x
, urvaturesofthex
axisaboutthe y and z axes
1
y
= d
y
dx and
1
z
= d
z
dx
; and the rateof the twist
#= d
dx
.
Beauseofisotropytorqueloadsdonotauseeitheraxialstrainorurvatures. Thestinessmatrix
(
P
)an bediagonalizedbytheproperhoieoftheoordinatesystem: Whentheoriginof the
oordinatesystemisattahedtotheenterofgravityoftheross-setion,andtheaxesarein the
prinipaldiretions,Equation(2.1)beomes
8
>
>
>
>
>
>
<
>
>
>
>
>
>
: b
N
x
M
y
M
z
b
T
x 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
= 2
6
6
6
6
6
6
4 EA
EI
yy
EI
zz
GI
t 3
7
7
7
7
7
7
5 8
>
>
>
>
>
>
<
>
>
>
>
>
>
:
o
x
1
y
1
z
# 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
(2.4)
Calulation of the tensile (EA) and bending stinesses ( EI
yy
andEI
zz
) are similar to open
andlosed setion beams, thetorsional stiness(GI
t
)is alulateddierently, for losedsetion
beams. The torsional stiness (Bredt-Batho formula) is signiantly higher than the torsional
stinessoftheequivalentopensetionbeam.
(Asimplerbeamtheory forisotropibeamswas derivedbyBernoulliand Euler. Inthis ase
thelast assumptioninSetion2.2.1beomes:
1. Inbendingtheross-setionsofthebeamremainplaneduringthedeformation.
2. Inbendingtheross-setionsofthebeamremainperpendiularto theaxis.
Thesearethe\Bernoulli-Navier"hypoteses.)
2.2.3 Orthotropi beam
Athin-walledbeamis orthotropiwhen eahwallsegmentis madeof orthotropi laminates. (A
laminate is orthotropi when the 1,6 and 2,6 terms in its stiness matries ([ A℄; [B℄; [D℄ see
Appendix A) are zero [9℄.) The Saint Venant theory an be easily generalized for orthotropi
beams. Thestiness matrixremainsdiagonal. Analogouslytothe\enter ofgravity"thetheory
denestheentroidsuhthatanormalforeatingattheentroiddoesnotausetheurvatures
ofthe beam's axispassingthroughthe entroid. The alulationof theelements of thestiness
matrixandtheoordinatesoftheentroidisstraightforward[13℄,[4℄. Formalistiallywewrite
>
>
>
>
>
>
<
>
>
>
>
>
>
: b
N
x
M
y
M
z
b
T
x
>
>
>
>
>
>
=
>
>
>
>
>
>
;
= 6
6
6
6
6
6
4 P
11
P
22
P
33
P
44 7
7
7
7
7
7
5
>
>
>
>
>
>
<
>
>
>
>
>
>
:
o
x
1
y
1
z
#
>
>
>
>
>
>
=
>
>
>
>
>
>
;
(2.5)
2.2.4 Generally anisotropi beam
Athin-walledbeamisalled\generallyanisotropi"whenatleastoneofitswallisnonorthotropi.
For generallyanisotropi beamstension, bending and twisting modes of displaements interat,
whihrepresentsasigniantdierenebetweenthetheoryofberreinforedbeamsandoflassial
beams. Theonstitutiveequationsbeomes
8
>
>
>
>
>
>
<
>
>
>
>
>
>
: b
N
x
M
y
M
z
b
T
x 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
= 2
6
6
6
6
6
6
4 P
11 P
12 P
13 P
14
P
12 P
22 P
23 P
24
P
13 P
23 P
33 P
34
P
14 P
24 P
34 P
44 3
7
7
7
7
7
7
5 8
>
>
>
>
>
>
<
>
>
>
>
>
>
:
o
x
1
y
1
z
# 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
(2.6)
Theinverseofthestinessmatrixistheomplianematrix:
W
=
P
1
(2.7)
By the proper hoie of the entroid of the oordinate system and alulation of the priniple
diretions3ofthese elementsoftheompliane matrixmaybezero:
8
>
>
>
>
>
>
<
>
>
>
>
>
>
:
o
x
1
y
1
z
# 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
= 2
6
6
6
6
6
6
4 W
11
0 0 W
14
0 W
22
0 W
24
0 0 W
33 W
34
W
14 W
24 W
34 W
44 3
7
7
7
7
7
7
5 8
>
>
>
>
>
>
<
>
>
>
>
>
>
: b
N
M
y
M
z
b
T
x 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
(2.8)
Manseld and Sobey [16℄ derived the ompliane matrix ( W) for anisotropi, losed setion
beams. The wallsof thebeamsaremade oflaminated omposite. Ineah layerthere areunidi-
retionalbers,thediretion ofthebersisoptional. Inadditionaltotheabovefourassumption
(Setion2.2.1),theystate
1. The[B℄and[D℄matriesofthelaminates(seeAppendixA)arenegligible. Aordinglythey
takeinto aountonlythein-plane stinessesof thelaminate.
Theexibilitymatrixisompletelylled,onlyW
12
;W
13
;W
23
anberesettozerowithmoving
theoriginto theentroidandrotating theaxes tothe prinipal axesof bending. Manseldand
Sobeygavethese transformations.
tions)
In the following we summarize the theories where the axial onstraints are taken into aount,
howeverthetransversesheardeformationisnegleted.
2.3.1 Basi assumptions
The rst three assumptions in Setion 2.2.1 are valid. Instead of Assumption 4 these theories
assumethattheaxialstrainvariesasfollows:
o
x
= du
dx y
d
y
dx z
d
z
dx
! d#
dx
(2.9)
wherethealulationof
y and
z
isthesameas inSetion 2.2.1:
y
= dv
dx ,
z
= dw
dx ,#=
d
dx is
therateoftwist,and!= R
rdsisasetionpropertyalledthesetorialarea.
The last term in Equation (2.9) allowsto the points of the ross-setion anadditional axial
displaement,alledwarping,proportionalto therateoftwist[17℄.
2.3.2 Isotropi beam
Vlasov[21℄ gaveabeamtheory withthe aboveassumptionsforisotropi open setion beams. If
thewarpingisrestrained,normalandshear stressesarise inthebeaminaddition tothoseof the
lassialtheory. (Iftheross-setionislosed,theseadditionalstressesdeayinashortdistane.)
Thetorqueonsistsoftwoparts : theSaintVenanttorqueandthewarpinginduedtorque:
b
T = b
T
sv +
b
T
!
(2.10)
Vlasovdenesanadditionalgeneralizedstress
M
!
(alledbimoment)
M
!
= Z
N
!ds (2.11)
M
!
is relatedto the generalizedstrain ( = d#
dx
) bythe warpingstiness (EI
!
), and hene
thestress-strainrelationshipbeomes:
8
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
: b
N
x
M
y
M
z
M
!
b
T
sv 9
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
;
= 2
6
6
6
6
6
6
6
6
6
4 EA
EI
yy
EI
zz
EI
!
GI
t 3
7
7
7
7
7
7
7
7
7
5 8
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
:
o
x
1
y
1
z
# 9
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
;
(2.12)
The bimoment is related to b
T
! as
b
T
!
= d
M
!
=dx, whih yields the well known equation of
restrainedwarping
b
T = b
T
sv +
b
T
!
=GI
t
#+EI
! d
2
#
dx 2
(2.13)
BauldandTzeng[6℄improvedtheabovetheoryforlaminatedompositebeams. Theross-setion
isopen andthelayupisrestritedtomidplanesymmetriberreinforedones([B℄=0). Beause
ofthisonditionforthelayupthereisnoouplingbetweentensionandtorsion,andthe1,5and5,1
elementsarezerointhe
P
stinessmatrix. Thewhole
P
matrixislled,exeptP
15
=P
51
=0.
Hene weobtain therelationshipbetween thestrainsand the stressesof thebeam: thestiness
matrix:
8
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
: b
N
x
M
y
M
z
M
!
b
T
sv 9
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
;
= 2
6
6
6
6
6
6
6
6
6
4 P
11 P
12 P
13 P
14 0
P
21 P
22 P
23 P
24 P
25
P
31 P
32 P
33 P
34 P
35
P
41 P
42 P
43 P
44 P
45
0 P
52 P
53 P
54 P
55 3
7
7
7
7
7
7
7
7
7
5 8
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
:
o
x
1
y
1
z
# 9
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
;
(2.14)
2.4 Timoshenko type beam theories (shear deformation, no restrained
warping)
Inthefollowingwesummarizethetheorieswheretheaxialonstraintsarenegleted,howeverthe
transverseshear deformationistakenintoaount.
2.4.1 Basi assumption
Therst three assumptionsin Setion 2.2.1is valid. The form of theaxial strainis idential to
Assumption4:
o
x
= du
dx y
d
y
dx z
d
z
dx
(2.15)
howeverinthisexpression
y and
z
aredened as
y
= dv
dx
y
z
= dw
dx
z
(2.16)
where
y and
z
aretheshearstrainin thex yandx zplanes,respetively. Theshearstrain
issupposedtobeonstantintheross-setionwhih isreferredtoas therstordersheartheory.
2.4.2 Isotropi beam
Theeetofthesheardeformationisinludedinthistheory. Henethetransverseforesandthe
shear strains are inluded in the ompatibility equations (Equation2.17). These are related to
8
>
>
>
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
>
>
>
: b
N
x
M
y
M
z
b
V
y
b
V
z
b
T
sv 9
>
>
>
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
>
>
>
;
= 2
6
6
6
6
6
6
6
6
6
6
6
6
4 EA
EI
yy
EI
zz
S
y
S
z
GI
t 3
7
7
7
7
7
7
7
7
7
7
7
7
5 8
>
>
>
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
>
>
>
:
o
x
1
y
1
z
y
z
# 9
>
>
>
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
>
>
>
;
(2.17)
2.4.3 Generally anisotropi beam
Bank[2℄,[3℄investigatedtheombinedbendingandtransverseloadingofanisotropi,opensetion
beams(torsionalandaxialloads arenotonsidered). Helaimsthattheirmodelan beused for
hand alulationpreliminary designstudies only. The geometry ofthe ross-setionis restrited
toopen,singly anddoubly symmetrialones. From
M
z and
b
V
y
hedetermines o
x
;1=
y
;1=
z and
#forthelayers,andgivesanaveragevalueofthese strainsfor thebeam. Thestinessmatrixis
notpresented.
2.5 Theoriestakingintoaount restrainedwarping andshear deforma-
tions
2.5.1 Basi assumption
ThismodelusesAssumptions1to3inSetion2.2.1,andfortheaxialstrainthefollowingassump-
tion:
o
x
= du
dx y
d
y
dx z
d
z
dx
! d#
dx
(2.18)
where
y
= dv
dx
y
z
= dw
dx
z
# =
d
dx
(2.19)
Henetheeet ofwarpingand sheardeformationsareinluded, howeverwarpinginduedshear
isnotinluded. Thetheoryassumesnoouplingbetweennormalandshearingeets.
2.5.2 Isotropi and orthotropi beam
Barbero[4℄,[5℄givestheompatibilityequationsalsoforopen andlosedross-setion. Thevetors
ofthegeneralizedstressesandstrainsarethesumofthesestressesandstrainsin Setion2.3and
Setion2.4. Thenondiagonalelementsofthestinessmatrixarezerobeauseoforthotropy,and
beausetheouplingbetweenthenormalandshearingeetsisnegleted. Henethestress-strain
relationshipisasfollows
8
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
: b
N
x
M
y
M
z
b
V
y
b
V
z
M
!
b
T
sv 9
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
;
= 2
6
6
6
6
6
6
6
6
6
6
6
6
6
6
6
4 EA
EI
yy
EI
zz
S
y
S
z
EI
!
GI
t 3
7
7
7
7
7
7
7
7
7
7
7
7
7
7
7
5 8
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
:
o
x
1
y
1
z
y
z
# 9
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
;
(2.20)
2.5.3 Symmetrialbeam
Kabirand Sherbourne [10℄ improved the beam theory of Bauld and Tzeng [6℄. The transverse
shear deformationof the beam ross-setionis inluded in the expression of the stiness matrix
(seeEquation2.21).
8
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
: b
N
x
M
y
M
z
M
!
b
T
sv
b
F
y
b
F
z
b
V
y
b
V
z 9
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
;
= 2
6
6
6
6
6
6
6
6
6
6
6
6
6
6
6
6
6
6
6
6
6
4 P
11
P
18 P
19
P
22
P
25 P
26
P
33
P
35
P
37
P
44 P
45
P
52 P
53 P
54 P
55 P
56 P
57
P
62
P
65 P
66
P
73
P
75
P
77
P
81
P
88
P
91
P
99 3
7
7
7
7
7
7
7
7
7
7
7
7
7
7
7
7
7
7
7
7
7
5 8
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
:
o
x
1
y
1
z
#
0
z
0
y
y
z 9
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
;
(2.21)
Thetheoryisvalidforopensetion beamswithsymmetriallaminates.
2.6 Theoriestakingintoaountrestrainedwarping,sheardeformations
and warping indued shear
2.6.1 Basi assumption
Therst three assumptionsin Setion 2.2.1is valid. The form of theaxial strainis idential to
thatofinSetion 2.5.1:
o
x
= du
dx y
d
y
dx z
d
z
dx
! d#
B
dx
(2.22)
where
y
=
dx
y
(2.23)
z
= dw
dx
z
howeverinthisexpression#
B
isdenedas
#
B
= d
dx
#
S
(2.24)
The warpingis assumed to be proportional to the rst derivative of the restrained warping
induedtwist. Couplingsbetweennormalandshearingeets arenegleted.
2.6.2 Isotropi and orthotropi beam
Kollar[12℄investigatedtransverselyloaded,opensetion,orthotropibeams. Thenormalstresses
induedbytherestrainedwarpingresultadditionalshear stresses. Thesestressesause anaddi-
tionaltwistof thebeam, and henethewarpingis notproportional tothe rstderivativeof the
twist. The twist has two parts: one from bending (whih auses warping, like in the previous
setion)andanotherpartfromtherestrainedwarpinginduedshearstress:
#=#
B +#
S
(2.25)
isdened as = d#
B
dx
. TheonstitutiveequationsaordingKollar:
8
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
:
M
y
M
z
M
!
b
T
sv
b
V
y
b
V
z
b
T
! 9
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
;
= 2
6
6
6
6
6
6
6
6
6
6
6
6
6
6
6
4 EI
yy EI
yz
EI
yz EI
zz
EI
!
GI
t
S
yy S
yz S
y!
S
yz S
zz S
z!
S
y!
S
z!
S
!!
3
7
7
7
7
7
7
7
7
7
7
7
7
7
7
7
5 8
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
: 1
y
1
z
#
y
z
#
s 9
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
>
>
>
>
>
>
;
(2.26)
Roberts and Ubaidi [18℄ proposed takeinto aount the shear deformationin torsion by the
alulationofthewarpingstinessforopen setion,orthotropibeams.
Urban [20℄ and Kristek [7℄ investigated the torsion of doubly symmetrial, losed setion,
isotropi beams. Using his basi equations we an derive the same equations as for open se-
tionbeams (Setion 2.6.2). The stinesses in the expression of the onstitutive equations dier
fromthoseoftheopensetions.
8
>
>
>
<
>
>
>
:
M
!
b
T
sv
b
T
! 9
>
>
>
=
>
>
>
;
= 2
6
6
6
4 EI
!
GI
t
S
!!
3
7
7
7
5 8
>
>
>
<
>
>
>
:
#
#
s 9
>
>
>
=
>
>
>
;
(2.27)
Inadditionaltotheassumptionsof[12℄, theystate
TheirresultstogetherwithothermoregeneralapproaheswillbedisussedinSetion5.1.
2.6.3 Generally anisotropi beam
WuandSun[23℄usethesamegeneralizedstrainsasKollar[12℄. Adierentialequationsystemis
statedfortheproblem. Thereisnorestritionforthelayersoftheplatesonsistingthebeam. The
ross-setionan beeither open or losed. Thestiness matrixisnotexpressed, andthesolution
beomesveryompliated.
2.7 Generalized beam theories
2.7.1 Isotropi and orthotropi beam
IntheTimoshenkotypebeamtheories(rstordershear theories,Setion2.4) thedistributionof
the shear strain arossthe ross-setion is uniform. There are higherorder shear theories with
moregeneralassumptionsforthedistributionof theshearstrain.
The Vlasovtype beam theories (Setion 2.3) allowsthe ross-setionto warpaording to a
determinedfuntion. InBahautheorynoassumptionismadeonaxialdisplaementdistribution.
Inthis beam theoryaset oforthonormal eigenwarpings(!
i
(s)) is derived. With these theaxial
strain( o
x
)ofthelassialtheories(inludingsheardeformationsornot) anbeimproved:
o
x
= o
xb +
X
W
i
(s)F 0
i
(x) (2.28)
whereF
i
(x)andW
i
( s)areunknownfuntionsofxands,whihanbedeterminedbyminimizing
thepotentialenergy.
2.8 Transversely loaded beams
2.8.1 Classialbeam-theories (norestrained warping, no sheardeformation)
Fromthetransverseloadswean alulatetheresultantnormalforeand thebending moments,
andwiththeseforeandmomentswean examinethebeamsimilarlytotheanalysisdisussedin
theprevioussetion. Toalulatetheresultanttorqueresultingfromthetransverseloadswehave
tointroduethe notionofthe shearenter, aboutwhih thetorque due to ashearfore haveto
bemeasured.
For isotropibeamsthedenition oftheshear enteris asfollows: transverseforesatingat
theshearenter donotausetwist. Theshearowandhenetheloationoftheshearenterare
dierentforopenandforlosedross-setionbeams.
For orthotropi beams the denition of theshear enter and the proedure of alulating its
loationare thesameas for isotropibeams. Barbero [5℄ givesthe expressions ofoordinatesof
theshearenter'sforopen andlosedsetion beams.
bendingmoments. Consequently,thetransverseforesatingatanypointoftheross-setionthe
beammaytwist. ManseldandSobey[16℄gavethedenition oftheshearenter foranisotropi,
losedsetion beams: theshearenterisatthepointwherethetwistissolelyduetotheresultant
bendingmoments. ManseldandSobeygavetheexpressionoftheloationoftheshearenter for
losedross-setions. Beauseoftheomplexityofthisexpressionasimplerapproximationisalso
given.
2.8.2 Theories taking into aount restrained warping indued shear (restrained
warping,shear deformation)
When warping indued shear is taken into aount, even for orthotropi beams, as a rule, the
ross-setionofthebeamwill rotate. Inthisasethere isno loationfortheexternaltransverse
loads,forwhih,therotationofthebeamiszero. Fororthotropi,opensetion beamsKollar[12℄
dened two speied points on the ross-setion: the shear deformation shear enter (when the
shearforesareappliedatthatpoint,thereisnoshearinduedtwist)andthebendingdeformation
shearenter(whentheshearforesareappliedatthat point,thereisnobendinginduedtwist).
3 Theory of open and losed setion, generally anisotropi
thin-walled beams - no restrained warping
Inthissetion wewill derivethestiness matrixofthin walledopenor losed setionomposite
beams[24℄ (see
P
in Setion2.2.4 (Equation2.6)). There isno restritiononthe layup of the
wallsegmentsandtheloalbendingstinessesaretakenintoaount. Wewill neglettheeets
ofrestrainedwarpingandsheardeformation. (Theeetofthisapproximationwillbeinvestigated
inSetion6.)
3.1 Problem statement
Weonsider thin-walled open and losed setion prismati beams. Thewallsof the beams may
onsistofasinglelayeror ofseverallayers,eah layermaybemadeof ompositematerials. The
beam's wall onsists of at segments (Figure 1) designated bythe subsript k (k = 1;2;:::;K,
whereK isthetotalnumberofwallsegments). Theross-setionmaybesymmetrialorunsym-
metrialandthelayupof thebeamis arbitrary(i.e. thelayersarenotneessarilyorthotropior
symmetrial).
Thebeamissubjetedtoanaxialfore b
N,bendingmoments
M
y ,
M
z
,andtorque b
T atingat
theentroid(theentroidisdened suhthatthefore b
N doesnotresultin theurvaturesofthe
axisofthebeam).
Weemploythefollowingoordinatesystems(Figure2).
y-z oordinate system with the origin at an arbitrarily hosen point. For the k-th segment we
employthe
k -
k -
k
oordinatesystemwiththeoriginattheenter oftherefereneplaneof the
k-thsegment. isparallel tothe xoordinate, isalong theirumfereneof thewall, and is
perpendiulartotheirumferene.
Thedisplaementsofthelongitudinalaxis,passingthroughtheentroid,areu, v, w, (Fig-
ure3),whereuistheaxialdisplaement,vandwarethetransversedisplaementsinthey andz
diretions,and istherotationoftheross-setion(twist).
Therelationshipsbetweenthesedisplaements,andtheaxialstrain o
x
andtheurvatures1=
y ,
1=
z
ofthexaxis,andtherateoftwist#are
u
x
= o
x
2
v
x 2
= 1
z
2
w
x 2
= 1
y
x
=# (3.1)
Inthex-y-zoordinatesystemthese relationshipsbeome
u
x
= o
x
2
v
x 2
= 1
z
2
w
x 2
= 1
y
x
=# (3.2)
where o
x , 1=
y , 1=
z
, are the axial strain and the urvatures of the longitudinal axis passing
throughtheoriginofthex-y-z oordinatesystem. u, v,w, and arethedisplaementsofthex
axis.
Theross-setionsofbeamswitharbitrarylayupdonotremainplaneandtheBernoulli-Navier
hypothesis is inappliable. Nonetheless, in a long body subjeted to the loads given in Figure
1,suh as a beam, the strainsmay be onsidered to be onstant in the axial diretion, and the
plane-strainondition (the stresses and strainsvary onlyin planes perpendiular to the x axis)
maybeapplied intheanalysis[15℄.
3.2 Open setion beams
Theanalysis ofthin-walledopensetionbeamsisperformedinfoursteps.
1 2
k
K
b k z
x
M y y M z
T
1 2
k
K
b k z
x
M y y M z
T
N N
Figure 1: Foresinopenandlosedsetionthin-walledbeamswithatwallsegments
beam'saxis.
2. Theforesineahwallsegmentaredeterminedfromthestrainsinthewallsegment.
3. Theresultantaxialfore,moments,andtorqueatingattheaxisofthebeamaredetermined
fromthewallsegmentfores.
4. Thestinessmatrixisestablishedbyrelatingtheresultantaxialfore,moments,andtorque
totheaxialstrain,urvaturesandtwistofthebeam'saxis.
3.2.1 Step1. Strains in the wallsegments
Atapointontherefereneplaneofeah wallsegment theaxial strainisalulatedbytheplane
strainondition
o
k
= o
x +z
1
y +y
1
z
(3.3)
where z and y are the oordinates of anarbitrary point on thek-th segment'sreferene surfae
and o
k
istheaxialstrainatthis point.
Thestrainsoftheaxisofthek-thwallsegmentan beexpressedas
8
>
>
>
>
>
>
<
>
>
>
>
>
>
:
w
k
w
k
w
mk
# w
k 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
= 2
6
6
6
6
6
6
4
1 z
k
y
k 0
0 os
k
sin
k 0
0 sin
k
os
k 0
0 0 0 1
3
7
7
7
7
7
7
5
| {z }
[R
k
℄
8
>
>
>
>
>
>
<
>
>
>
>
>
>
:
o
x
1
y
1
z
# 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
(3.4)
where y
k and z
k
are the oordinates of the
k -
k -
k
oordinate system's origin, whih is at the
midpointof therefereneplane(Figure 2), and
k
istheangle betweenthe
k
andy oordinate
axes. Thesupersriptwreferstothesegment'slongitudinalaxiswhihpassesthroughthemidpoint
oftherefereneplane(=0; =0). TherstoftheseequationsiswrittenbyvirtueofEquation
z
x
y
® k
» k
´ k
³ k z
y x
z k y k
k-th wall segment
Figure2: Coordinatesystemsemployedintheanalysisofthin-walledbeamswitharbitrarylayup
(3.3).
w
k and
w
mk
arethe urvaturesof thek-thwallsegment's axisin the- and -planes,
respetively(Figure4). Thelastequation(#
w
k
=#)iswrittenbyobservingthatthetwistofevery
pointin thewallsegmentisequaltothetwistofthebeam.
Theaxialstraininthek-thsegmentvarieslinearlywith(seeEquation3.3)andweanwrite
o
k
= w
k
+
w
mk
(3.5)
Theurvature
k
isuniformin eahatsegment
k
= 1
y os
k 1
z sin
k
(3.6)
Theratiooftwistanbewrittenas
#=
x
=
w 0
y
x
=
2
w 0
xy
(3.7)
whih,byusingthedenition of
(
= 2
2
w
xy
)an bewrittenas
#= 1
2
(3.8)
henewehave
k
= w
k and
k
= 2#
w
k
= 2#. These relationshipstogetherwith Equation
(3.5)maybewrittenin matrixform as
o
² x
k
k
k x
1
z
r y
1
y
r z
1
o
² x
w
k mk
1 z
² »
² »
y
» k
³ k » k
´ k
Figure4: Deformationsofanopensetionthin-walledbeam
8
>
>
>
<
>
>
>
:
o
k
k
k 9
>
>
>
=
>
>
>
;
= 8
>
>
>
<
>
>
>
:
o
9
>
>
>
=
>
>
>
;
k
= 2
6
6
6
4
1 0 0
0 1 0 0
0 0 0 2
3
7
7
7
5
| {z }
[R
℄
8
>
>
>
>
>
>
<
>
>
>
>
>
>
:
w
k
w
k
w
mk
# w
k 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
(3.9)
3.2.2 Step2. Fores and moments in the wallsegments
Thestrain-forerelationshipin eahwallsegmentisgivenby:
8
>
>
>
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
>
>
>
:
o
o
0
9
>
>
>
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
>
>
>
;
k
= 2
6
6
6
6
6
6
6
6
6
6
6
6
4
11
12
16
11
12
16
12
22
26
21
22
26
16
26
66
61
62
66
11
21
61 Æ
11 Æ
12 Æ
16
12
22
62 Æ
12 Æ
22 Æ
26
16
26
66 Æ
16 Æ
26 Æ
66 3
7
7
7
7
7
7
7
7
7
7
7
7
5
k 8
>
>
>
>
>
>
>
>
>
>
>
>
<
>
>
>
>
>
>
>
>
>
>
>
>
: N
N
N
M
M
M 9
>
>
>
>
>
>
>
>
>
>
>
>
=
>
>
>
>
>
>
>
>
>
>
>
>
;
k
(3.10)
wherethe[℄,[℄,[Æ℄matriesaretheinverseofthe[A℄,[B℄, [D℄matriesofthewallsegment[9℄
2
4
[℄ [℄
[℄
T
[Æ℄
3
5
= 2
4
[A℄ [B℄
[B℄
T
[D℄
3
5 1
(3.11)
N
;N
;M
are zeroalong the freelongitudinal edges(see Figure 5) and, onsequently, are ap-
proximatelyzeroeverywhere(N
=N
=M
=0).
Withtheseapproximationsthestrain-forerelationshipsforthek-thwallsegmentbeome(see
Equation3.10)
N ´ = 0
N » ´ = 0 M ´ = 0
Figure5: Theforesandmomentsalongthelongitudinaledgeofanopensetionthin-walledbeam
8
>
>
>
<
>
>
>
:
o
9
>
>
>
=
>
>
>
;
k
= 2
6
6
6
4
11
11
16
11 Æ
11 Æ
16
16 Æ
16 Æ
66 3
7
7
7
5
k
| {z }
[e
k
℄
8
>
>
>
<
>
>
>
: N
M
M
9
>
>
>
=
>
>
>
;
k
=[e
k
℄ 8
>
>
>
<
>
>
>
: N
M
M
9
>
>
>
=
>
>
>
;
k
(3.12)
Weintroduethefollowingstressresultantsinthesegment's
k -
k -
k
oordinatesystem(Figure
6,left)
b
N w
k
= Z
(b
k )
N
k d=b
k N
k ;at=0
(3.13)
M w
k
= Z
(bk) M
k d=b
k M
k ;at=0
(3.14)
M w
mk
= Z
(b
k )
N
k
d (3.15)
b
k
isthewidthofthewallsegment(Figure1). Thetorqueis[5℄
b
T w
k
= 2
Z
(b
k )
M
k
d= 2b
k M
k ;at=0
(3.16)
Notethat b
N w
,
M w
,and b
T w
representforesandmoments,andthesupersriptwreferstothe
wallsegment. Thesamesymbolswithouthatrepresentforesandmomentsperunit length.
Theseond equalities in Equations(3.13), (3.14)and (3.16) are written byobserving that in
eah segment n
o
;
;
o
varies linearly along the width ( diretion, see Equation 3.9), and,
onsequently, N
, M
, M
also vary linearly along the width (see Equation 3.12). Equations
(3.13),(3.14),(3.16),(3.12), and(3.9)resultin
8
>
>
>
<
>
>
>
:
w
k
w
k
# w
k 9
>
>
>
=
>
>
>
;
= 1
b
k 2
6
6
6
4
11
11 1
2
16
11 Æ
11 1
2 Æ
16
1
2
16 1
2 Æ
16 1
4 Æ
66 3
7
7
7
5 8
>
>
>
<
>
>
>
: b
N w
k
M w
k
b
T w
k 9
>
>
>
=
>
>
>
;
(3.17)
»
´
w
M mk
w
M x k w
N x k w
T x k
k-th wall segment
Figure6: Thefore resultantsin thek-thwallsegment
k k
w
k mk
1
Figure7: Curvature w
mk
ofthewallsegment
ToevaluatetheintegralinEquation(3.15)weonsideronlytheurvature w
mk
ofthesegment,
andassumethat theatsegmentremainsat(
=0,
=0,Figure7).
With thisapproximationtheinverseofEquation(3.12)yields
8
>
>
>
<
>
>
>
: N
M
M
9
>
>
>
=
>
>
>
;
k
= 2
6
6
6
4 e
A
11 e
A
12 e
A
13
e
A
12 e
A
22 e
A
23
e
A
13 e
A
23 e
A
33 3
7
7
7
5
k 8
>
>
>
<
>
>
>
:
o
k
0
0 9
>
>
>
=
>
>
>
;
(3.18)
Thematrix h
e
A i
isdenedas
2
6
6
6
4 e
A
11 e
A
12 e
A
13
e
A
12 e
A
22 e
A
23
e
A
13 e
A
23 e
A
33 3
7
7
7
5
k
= 2
6
6
6
4
11
12
16
12
22
26
16
26
66 3
7
7
7
5 1
k
(3.19)
Withthisdenition N
k isN
k
=
e
A
11
k
o
k
. BysubstitutingthisexpressionandEquation(3.5)
intoEquation(3.15)and byperformingtheintegration,weobtain
M w
mk
=
e
A
11
k b
3
k
12
w
mk
(3.20)
k k k
natesystem
8
>
>
>
>
>
>
<
>
>
>
>
>
>
:
w
k
w
k
w
mk
# w
k 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
= 1
b
k 2
6
6
6
6
6
6
4
11
11
0
1
2
16
11 Æ
11
0
1
2 Æ
16
0 0
12
( e
A11)
k b
2
k 0
1
2
16 1
2 Æ
16 0
1
4 Æ
66 3
7
7
7
7
7
7
5
| {z }
[!
k
℄
8
>
>
>
>
>
>
<
>
>
>
>
>
>
: b
N w
k
M w
k
M w
mk
b
T w
k 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
(3.21)
3.2.3 Step3. Fores in thebeam
Inthebaroordinatesystem(x -y-z)theforesin thebeamarethesumofthefores inthewall
segments(Figures6and2)
8
>
>
>
>
>
>
<
>
>
>
>
>
>
: b
N
x
M
y
M
z
b
T
x 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
= K
X
k =1 2
6
6
6
6
6
6
4
1 0 0 0
z
k
os
k
sin
k 0
y
k
sin
k os
k 0
0 0 0 1
3
7
7
7
7
7
7
5
| {z }
[R
k
℄ T
8
>
>
>
>
>
>
<
>
>
>
>
>
>
: b
N w
k
M w
k
M w
mk
b
T w
k 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
(3.22)
Wenotethat[R
k
℄ T
isthetransposeof thematrix[R
k
℄(seeEquation3.4).
3.2.4 Step4. Stiness matrix
Equations(3.22),(3.21), and(3.4)yield
8
>
>
>
>
>
>
<
>
>
>
>
>
>
: b
N
x
M
y
M
z
b
T
x 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
= K
X
k =1 [ R
k
℄ T
8
>
>
>
>
>
>
<
>
>
>
>
>
>
: b
N w
k
M w
k
M w
mk
b
T w
k 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
= K
X
k =1 [R
k
℄ T
[!
k
℄ 1
8
>
>
>
>
>
>
<
>
>
>
>
>
>
:
w
k
w
k
w
mk
# w
k 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
= (3.23)
= K
X
k =1
[R
k
℄ T
[!
k
℄ 1
[R
k
℄
| {z }
P
8
>
>
>
>
>
>
<
>
>
>
>
>
>
:
o
x
1
y
1
z
# 9
>
>
>
>
>
>
=
>
>
>
>
>
>
;
(3.24)
P
isthestiness matrixin thebaroordinatesystem(Table1).
Thedisplaementsmustbedeterminedbysolvingthegoverningequations(i.e. theequilibrium
equations, the strain displaement relationships (Equation 3.1), and the onstitutive equations
(Equation 2.6)) for the beam under onsideration. These equations are given in the x, y, z
oordinate system. Hene thestiness (andompliane) matriesmustalso be expressedin this