ElasticitySummary.pdf
-
Upload
jack-rasal -
Category
Documents
-
view
2 -
download
0
Transcript of ElasticitySummary.pdf
-
CVEN4304 Structural Analysis & Finite ElementsCVEN9820 Computational Structural Mechanics
Summary of Elasticity Theory
Chongmin Song
School of Civil and Environmental EngineeringUniversity of New South Wales
1
-
Course Materials
Lecture notes
Section 3.1 of Cook
Appendix C of Logan
2
-
Strain-Displacement Relationship (Plane Strain)
Displacements in x-, y -directions: {u} = [ u v ]TStrains ({} = []{u})
xyxy
{}
=
uxvy
uy
+vx
=
x0
0
y
y
x
[]
{uv
} {u}
3
-
Stress State and Equilibrium Equations
Equilibrium in plane strain and in plane stress
x tdy xy tdx+(x +x ,x dx)tdy +(xy + xy ,y dy)tdx+Fx tdxdy = 0xx
+xyy
+ Fx = 0
xyx
+yy
+ Fy = 0
In matrix form: []T{}+ {F} = 0
x0
y
0
y
x
[]T
xyxy
{}
+
{FxFy
} {F}
= 0
Note that the differential operator [] is the same as instrain-displacement relationship.
4
-
Stress-Strain Relationship: Normal stresses andstrains
xx
y
y
z
z
Hookes law (E : Youngs modulus)
x =xE
y =yE
z =zE
Poissons effect (: Poissons ratio)
y = xE x = yE
x = zE
z = xE z = yE
y = zE5
-
Stress-Strain Relationship: Normal stresses andstrains
Superposition
x =xE y
E z
E
y = xE +yE z
E
z = xE yE+zE
Conversely
x =E
(1+ )(1 2) ((1 )x + y + z)
y =E
(1+ )(1 2) (x + (1 )y + z)
y =E
(1+ )(1 2) (x + y + (1 )z)
6
-
Stress-Strain Relationship: Shear stresses and strains
Hookes law (G : shear modulus)
=
G
In stress components:
xy =xyG
; yz =yzG
; xz =xzG
or conversely
xy = Gxy ; yz = Gyz ; xz = Gxz
Shear modulus is not independent of E and
G =E
2(1+ )
7
-
Stress-Strain Relationship (3D)
In matrix form ({} = [E ]{} with elasticity (constitutive) matrix [E ])
xyzxyyzxz
=
2G1 2
1 0 0 0 1 0 0 0 1 0 0 00 0 0 122 0 00 0 0 0 122 00 0 0 0 0 122
xyzxyyzxz
Conversely ({} = [E ]1{})
xyzxyyzxz
=
1E
1 0 0 0 1 0 0 0 1 0 0 00 0 0 2(1+ ) 0 00 0 0 0 2(1+ ) 00 0 0 0 0 2(1+ )
xyzxyyzxz
8
-
Plane Strain Condition
One dimension (z) is much larger than the other two (x and y )
In-plane forces do not vary along the largest dimension z.
Dam Pipeline
z
9
-
Plane Strain Condition
No displacement occurs along the largest dimension z
w = 0; z = wz
= 0
Inplane displacements u and v are independent of z
u = u(x , y)v = v(x , y)
; xz =
uz
+wx
= 0
yz=vz
+wy
= 010
-
Plane Strain Condition: Stress-Strain Relationship
Considering z = yz = zx = 0
xyzxy00
=
2G1 2
1 0 0 0 1 0 0 0 1 0 0 00 0 0 122 0 00 0 0 0 122 00 0 0 0 0 122
xy0xy00
Elasticity matrix for plane strain condition:
[E ] =2G
1 2
1 0 1 00 0
1 22
Normal stress along the largest dimension z
z = xE yE+zE
= 0; z = (x + y )
11
-
Plane Stress Condition
One dimension (z) is much smaller than the other two (x and y )
zz = yz = xz = 0
12
-
Plane Stress Condition: Stress-Strain Relationship
xyzxy00
=
1E
1 0 0 0 1 0 0 0 1 0 0 0
0 0 0 2(1+ ) 0 00 0 0 0 2(1+ ) 00 0 0 0 0 2(1+ )
xy0xy00
Elasticity matrix for plane stress condition ({} = [E ]{}):
[E ]1 = 1E
1 0 1 00 0 2(1+ )
; [E ] = E1 2
1 0 1 00 0 12
Normal strain along the largest dimension z
z = E (x + y )
13
-
Boundary Conditions
Enforced displacements
u = u; v = v ; w = w
For example, fixed boundary:
u = v = w = 0
14
-
Boundary Conditions
Prescribed tractions
Unit outward normal (l, m) onboundary.
Equilibrium on boundary AB withlength ds
Boundary conditions
x = lx +mxyy = lxy +my
Written in matrix form{xy
}=
[l 0 m0 m l
]
[L]T
xyxy
= [L]T{}15
-
Boundary Conditions
Similarity with differential operator in equations of equilibrium
[L] =
l 00 mm l
; compare with [] =
x0
0
y
y
x
[L] is in the same form as [] with l , m replacing
x,
y.
16
-
Pure Bending of a Beam
Displacement solution
u = Cxyv = 0.5C(x2 + y2)
Note that planes remain planes(u varies linearly in y and u = 0at neutral axis y = 0)
Strains
x =ux
= Cy
y =vy
= Cy
xy =vx
+uy
= Cx Cx = 017
-
Pure Bending of a Beam (conted)
Stresses (Plane stress condition)
x =E
1 2 (x + y ) =E
1 2 (Cy + C2y)
= CEy (Linear variation over cross section)y =
E1 2 (y + x ) =
E1 2 (Cy Cy)
= 0
xy = Gxy = 0
Equilibrium (body force Fx = Fy = 0)
xx
+xyy
= 0+ 0 = 0
xyx
+yy
= 0+ 0 = 0
18
-
Pure Bending of a Beam (conted)
Boundary conditions
Left side: outward normal (1, 0)x = lx +mxy = CEyy = lxy +my = 0
Right side: outward normal (1, 0)
x = lx +mxy = CEyy = lxy +my = 0
x
y
hn=(1,0)n=(-1,0)
Bending moment (b: thickness of beam)
M =12(CE h
2
) h
2(
23h2
) b 2 = CE bh
3
12
Constant C for a applied bending moment M
C =MEI
(I : Moment of inertia)
19
-
Common Civil Engineering Problems
Mathematical model in form of
[]T {}+ {F} = 0; {} = [E ]{}; {} = []{u}; {} = [L]T {}
Quantity Solid mechanics Heat conduction Seepage flow
Function Displacements {u} Temperature T Hydraulic head hField gradient Strains: {T} = []T {h} = []h
{} = []{u} where [] =[
x
y
z
]TConstitutive law Elasticity [E ] Conductivity [] Permeability []
Induced field Stresses: Fluxes: Velocities:
{} = [E ]{} {f} = []{T} {v} = []{h}Surface load Tractions: Normal flux: Normal velocity:
{} = [L]T {} fn = [L]T {f} vn = [L]T {v}Internal load Body forces: {F} Source: Q Source QEquilibrium []T {}+ {F} = 0 []T {T} Q = 0 []T {h} Q = 0
20