Stress/Strain Lecture 1 ME EN 372 Andrew Ning aning@byu.edu Outline Stress Strain Plane Stress and Plane Strain Materials
Stress 1D Stress P P σ = P A
3D Stress State σ yy τ yx τ yz τ xy σ xx τ xy τ xz τ zy σ = τ yx σ yy τ yz σ xx τ xz τ zx τ zy σ zz τ zx σ zz
Positive Sign Convention σ y τ xy (+) σ x Nominal vs true stress
Strain 1D Strain ∆ l l 0 ǫ = ∆ l l 0
u 1 u 0 x 0 x 1 ǫ x = u 1 − u 0 → ∂u x 1 − x 0 ∂x Normal strain can occur in all three directions. ǫ x = ∂u ∂x ǫ y = ∂v ∂y ǫ z = ∂w ∂z
Analogous to shear stress, there are three independent shear strain components. γ xy = θ 1 + θ 2 θ 2 θ 1 γ xy = γ yx = ∂v ∂x + ∂u ∂y γ yz = γ zy = ∂w ∂y + ∂v ∂z γ xz = γ zx = ∂u ∂z + ∂w ∂x
Plane Stress and Plane Strain Plane Stress σ yy σ y τ yx τ xy τ yz τ xy τ zy (+) σ x σ xx τ xz τ zx σ zz
Plane Strain Materials
Homogeneous: Isotropic: Linear Stress-Strain Relationships Most general material (in the elastic region): ǫ xx S 11 S 12 S 13 S 14 S 15 S 16 σ xx ǫ yy S 21 S 22 S 23 S 24 S 25 S 26 σ yy ǫ zz S 31 S 32 S 33 S 34 S 35 S 36 σ zz = γ xy S 41 S 42 S 43 S 44 S 45 S 46 τ xy γ xz S 51 S 52 S 53 S 54 S 55 S 56 τ xz γ yz S 61 S 62 S 63 S 64 S 65 S 66 τ yz
ǫ = Sσ S : compliance matrix Inverse: σ = Kǫ K : stiffness matrix. Orthotropic Materials Usually, a material contain certain symmetries. ǫ xx S 11 S 12 S 13 0 0 0 σ xx ǫ yy S 21 S 22 S 23 0 0 0 σ yy ǫ zz S 31 S 32 S 33 0 0 0 σ zz = γ xy 0 0 0 S 44 0 0 τ xy γ xz 0 0 0 0 S 55 0 τ xz γ yz 0 0 0 0 0 S 66 τ yz
Isotropic A special case of orthotropy is isotropy, in which the elastic properties are the same in every direction. ǫ x 1 − ν − ν 0 0 0 σ x 1 0 0 0 ǫ y − ν − ν σ y 1 0 0 0 ǫ z − ν − ν σ z = 1 E γ xy 0 0 0 2(1 + ν ) 0 0 τ xy γ xz 0 0 0 0 2(1 + ν ) 0 τ xz 0 0 0 0 0 2(1 + ν ) γ yz τ yz Inverse (stiffness matrix) σ x 1 − ν ν ν 0 0 0 ǫ x σ y ν 1 − ν ν 0 0 0 ǫ y 1 − ν 0 0 0 σ z ν ν ǫ z E = (1 + ν )(1 − 2 ν ) 1 − 2 ν 0 0 0 0 0 τ xy γ xy 2 1 − 2 ν τ xz 0 0 0 0 0 γ xz 2 1 − 2 ν τ yz 0 0 0 0 0 γ yz 2
E G = 2(1 + ν ) Strain in x-direction ǫ x = 1 E [ σ x − ν ( σ y + σ z )]
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