Fundamentals of Elasticity Theory Professor M. H. Sadd Reference: Elasticity Theory Applications and Numerics, M.H. Sadd, Elsevier/Academic Press, 2009 Theory of Elasticity Based Upon Principles of Continuum Mechanics, Elasticity Theory Formulates Stress Analysis Problem As Mathematical Boundary-Value Problem for Solution of Stress, Strain and Displacement Distribution in an Elastic Body. St Boundary Conditions Describe Physics on Boundary (Different For Each Problem) Su R Governing Field Equations Model Physics Inside Region (Same For All Problems) Value of Elasticity Theory - Develops “Exact” Analytical Solutions For Problems of Limited Complexity - Provides Framework for Understanding Limitations of Strength of Materials Models - Establishes Framework for Developing Linear Finite Element Modeling - Generates Solutions for Benchmark Comparisons with FEA Solutions Deformation and Strain Two-Dimensional Theory u dy y D' Strain Displacement Relations C' v(x,y+dy) y D C B' A' v dx x dy v(x,y) A u x v ey y ex dx B u(x+dx,y) 1 u v 1 exy xy 2 y x 2 u(x,y) x Three-Dimensional Theory ex e [e] e yx ezx exy ey ezy exz e yz ez Deformation and Strain Example Determinethecomponentsof strain for thefollowingdisplacement field u Axz , v B( x 2 y 2 ) , w Cxy , where A, B, C are const ants __________ __________ __________ __________ _ u ex Az x v ey 2 By y w ez 0 z 1 u v 1 exy 0 2 Bx Bx 2 y x 2 1 v w 1 1 0 Cx Cx e yz 2 z y 2 2 1 w u 1 ezx Cy Ax 2 x z 2 Rigid Body Motion Two-Dimensional Example z u y D C y dy z vo A dx v x B uo x General Form of Displacement Field u* uo z y v* vo z x Zero Strains! Strain Compatibility 1 2 3 4 y x Discretized Elastic Solid Undeformed Configuration 1 2 1 3 4 3 Deformed Configuration Continuous Displacements Compatibility Equation 2 4 Deformed Configuration Discontinuous Displacements 2 2exy 2ex ey 2 y 2 x 2 xy Strain Compatibility Example Check tosee if thefollowingstrain field ex Ay3 , e y Ax3 , exy Bxy( x y ) satisfies the two - dimensional compatibility equation __________ __________ __________ __________ __ 2 2 exy 2 ex e y 2 2 6 Ay 6 Ax 2 B(2 x 2 y ) 2 y x xy 2 6 A 4B A B 3 2 onlysatisfiesequation with A B 3 Body and Surface Forces Body Forces: F(x) Surface Forces: T(x) Cantilever Beam Under Self-Weight Loading S Sectioned Axially Loaded Beam Traction and Stress P3 P2 F n A p P1 (Sectioned Body) (Externally Loaded Body) Traction Vector F A0 A T n ( x, n) lim Note that ordinary elasticity theory does not include nor allow concentrated moments to exist at a continuum point Stress Components y T n ( x, n e1 ) x e1 xye2 xze3 yx yz xy zy y zx z x z T n ( x, n e2 ) yxe1 y e2 yze3 xz x T n ( x, n e3 ) zx e1 zy e2 z e3 x [ ] yx zx xy y zy xz yz z T n (σ x nx τ yx n y τ zx nz )e1 ( τ xy nx σ y n y τ zy nz )e 2 ( τ xz nx τ yz n y σ z nz )e 3 Stress Transformation x3 Three-Dimensional Transformation x3 x x l12 y m12 z n12 2( xy l1m1 yz m1n1 zx n1l1 ) x2 e3 e3 x2 e1 x1 z x l32 y m32 z n32 2( xy l3m3 yz m3n3 zx n3l3 ) xy x l1l2 y m1m2 z n1n2 xy (l1m2 m1l2 ) yz (m1n2 n1m2 ) zx (n1l2 l1n2 ) e2 e2 e1 y x l22 y m22 z n22 2( xy l2 m2 yz m2 n2 zx n2 l2 ) x1 l1 cos(xi, x j ) l2 l3 m1 m2 m3 yz x l2 l3 y m2 m3 z n2 n3 xy (l2 m3 m2 l3 ) yz (m2 n3 n2 m3 ) zx (n2 l3 l2 n3 ) zx x l3l1 y m3m1 z n3n1 xy (l3m1 m3l1 ) yz (m3n1 n3m1 ) zx (n3l1 l3n1 ) n1 n2 n3 y y' Two-Dimensional Transformation x x cos2 y sin 2 2 xy sin cos x' y x sin 2 y cos2 2 xy sin cos xy x sin cos y sin cos xy (cos2 sin 2 ) x Stress Transformation Example x x u x cos 2 x sin cos Dimensionless Stress 1 / x cos2 0.5 0 / x sin cos -0.5 0 10 20 30 40 50 (degrees) 60 70 80 90 Principal Stresses and Directions ( x ) xy xz n1 xy n1 ( y )n2 yz n3 0 xy ( y ) yz n2 0 xz xz n1 yz n2 ( z )n3 0 yz ( z ) n3 ( x )n1 xy n2 xz n2 0 Homogeneous System of Algebraic Equations,Non - T rivalSolution ( x ) xy xz xy ( y ) yz xz yz ( z ) 0 3 I12 I 2 I 3 0 Ii = Fundamental Invariants Roots of the characteristic equation are the principal stresses 1 2 3 Corresponding to each principal stress is a principal direction n1 n2 n3 that can be used to construct a principal coordinate system y 2 yx yz zx xz z x z (General Coordinate System) 1 n2 xy zy y 2 n1 x 3 n3 3 (Principal Coordinate System) 1 Equilibrium Equations y y y dy yx Fy x y dy xy Fx xy Body Forces yx xy x x dx x dx x yx y x yx Fx 0 x y xy y F 0 Fy 0 y x y Fx 0 M 0 xy yx Equilibrium Equation Example Assuming no body forces,show t hat t hefollowing st ressessat isfy t he equilibrium equat ions 3Pxy N 3P y2 x , y 0 , xy (1 2 ) 3 2c 2c 4c c __________ __________ __________ _________ x yx 3Py 3Py 0 3 3 0 a x y 2c 2c xy y 0 00 0 a x y Hooke’s Law x C11e x C12 e y C13 e z 2C14 e xy 2C15 e yz 2C16 e zx y C 21e x C 22 e y C 23 e z 2C 24 e xy 2C 25 e yz 2C 26 e zx z C31e x C32 e y C33 e z 2C34 e xy 2C35 e yz 2C36 e zx xy C 41e x C 42 e y C 43 e z 2C 44 e xy 2C 45 e yz 2C 46 e zx yz C51e x C52 e y C53 e z 2C54 e xy 2C55 e yz 2C56 e zx zx C61e x C62 e y C63 e z 2C64 e xy 2C65 e yz 2C66 e zx Isotropic Homogeneous Materials x ( e x e y e z ) 2e x y ( e x e y e z ) 2e y z ( e x e y e z ) 2e z xy 2e xy yz 2e yz zx 2e zx = Lamé’s constant = shear modulus or modulus of rigidity E = modulus of elasticity or Young’s modulus v = Poisson’s ratio 1 x ( y z ) E 1 e y y ( z x ) E 1 e z z ( x y ) E 1 1 e xy xy xy E 2 1 1 e yz yz yz E 2 1 1 e zx zx zx E 2 ex Orthotropic Materials (Three Planes of Material Symmetry) x y z yz zx xy 1 E 1 12 E1 13 E1 21 E2 1 E2 23 E2 31 E3 32 E3 1 E3 0 0 0 0 0 0 1 23 0 1 31 0 0 ex ey 0 ez 2e yz 0 2e zx 2 e 0 xy 1 12 Nine Independent Elastic Constants for 3-D Four Independent Elastic Constants for 2-D Physical Meaning of Elastic Constants p p p (Hydrostatic Compression) 0 p 0 ij 0 p 0 p ij 0 p 0 (Simple Tension) E 0 0 ij 0 0 0 eij 0 0 0 0 0 E / ex 0 0 E 0 E 0 (Pure Shear) 0 0 ij 0 0 0 0 0 / 2 0 0 eij / 2 0 0 0 0 0 / 2exy / xy 1 2 0 0 E p 1 2 eij 0 p 0 E 1 2 0 0 E p 3(1 2) p p k E E p k Bulk Modulus 3(1 2) ekk Relations Among Elastic Constants Typical Values of Elastic Constants Basic Formulation Fundamental Equations (15) - Strain-Displacement (6) - Compatibility (3) - Equilibrium (3) - Hooke’s Law (6) Fundamental Unknowns (15) - Displacements (3) - Strains (6) - Stresses (6) Typical Boundary Condtions T(n) S S R St R Su R u Traction Conditions Displacement Conditions Mixed Conditions Basic Problem Formulations Problem 1 (Traction Problem) Determine the distribution of displacements, strains and stresses in the interior of an elastic body in equilibrium when body forces are given and the distribution of the tractions are prescribed over the surface of the body. Problem 2 (Displacement Problem) Determine the distribution of displacements, strains and stresses in the interior of an elastic body in equilibrium when body forces are given and the distribution of the displacements are prescribed over the surface of the body. Problem 3 (Mixed Problem) Determine the distribution of displacements, strains and stresses in the interior of an elastic body in equilibrium when body forces are given and the distribution of the tractions are prescribed over the surface St and the distribution of the displacements are prescribed over the surface Su of the body. T(n) S S R St R Su R u Traction Conditions Displacement Conditions Mixed Conditions Basic Boundary Conditions Coordinate Boundary Examples r y=Ty xy=Tx r x r r y xy=Ty r x=Tx y x (Cartesian Coordinate Boundaries) (Polar Coordinate Boundaries) Non-Coordinate Boundary Example n = unit normal vector Ty( n) xynx y ny Fy ( x, y) Tx(n) x nx xyny Fx ( x, y) y x Boundary Condition Examples Fixed Condition Traction Condition Tx( n ) x S, Ty( n ) xy 0 u=v=0 y (n) x T Traction Condition xy 0, Ty( n ) y S S x b l S Tx( n) 0 Ty( n) 0 a x Traction Free Condition Tx( n ) xy 0, Ty( n ) y 0 (Coordinate Surface Boundaries) y Fixed Condition u=v=0 Traction Free Condition (Non-Coordinate Surface Boundary) Symmetry Boundary Conditions Rigid-Smooth Boundary Condition Symmetry Line u0 Ty( n ) 0 y x Example Solution – Beam Problem x x - Contours Saint-Venant’s Principle The Stress, Strain and Displacement Fields Due to Two Different Statically Equivalent Force Distributions on Parts of the Body Far Away From the Loading Points Are Approximately the Same. P/2 P/2 P x x y y xy xy x x y y Stresses Approximately Equal Strain Energy Strain Energy = Energy Stored Inside an Elastic Solid Due to the Applied Loadings One-Dimensional Case u y dy dz dx u x x u dx)dydz dudydz 0 0 x x x u d d ( )dxdydz dxdydz 0 0 x E 2x dxdydz 2E 2x Eex2 1 Strain Energy dU U x ex Volume dxdydz 2 E 2 2 x u dx x dU d (u z Three-Dimensional Case 1 1 ( x ex y e y z ez xy xy yz yz zx zx ) ij eij 2 2 1 1 1 1 (ex e y ez ) 2 (ex2 e y2 ez2 2xy 2yz 2zx ) 0 2 2 2 2 U Principle of Virtual Work The virtual displacement ui = {u, v, w} of a material point is a fictitious displacement such that the forces acting on the point remain unchanged. The work done by these forces during the virtual displacement is called the virtual work. U T Virtual Strain Energy ij eij dV V ( x ex y e y z ez xy xy yz yz zx zx )dV V W Virtual Work Done by Surface and Body Forces Ti n ui dS Fi ui dV St V Virtual Strain Energy = Virtual Work Done by Surface and Body Forces V ijeij dV Ti n ui dS Fi ui dV St V Change in Potential Energy (UT-W) During a Virtual Displacement from Equilibrium is Zero. U dV Ti n ui dS Fi ui dV U T W 0 St V V