Body and Surface Forces Body Forces: F(x) Surface Forces: T(x) (a) Cantilever Beam Under Self-Weight Loading S (b) Sectioned Axially Loaded Beam Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island Traction Vector P3 P2 F n A p P1 (Externally Loaded Body) F A0 A T n ( x, n) lim Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island (Sectioned Body) T n ( x, n e1 ) x e1 xy e 2 xz e3 T n ( x, n e 2 ) yx e1 y e 2 yz e3 T n ( x, n e3 ) zx e1 zy e 2 z e3 Stress Tensor y yx yz zy y xy x zx xz z x [ ] yx zx xy y zy xz yz z x z y n Traction on an Oblique Plane Tn T n ( x n x yx n y zx n z )e1 ( xy n x y n y zy n z )e 2 x z Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island ( xz n x yz n y z n z )e3 Ti n ji n j Stress Transformation ij QipQ jq pq l1 Qij l2 l3 m1 m2 m3 n1 n2 n3 x x l12 y m12 z n12 2( xy l1m1 yz m1n1 zx n1l1 ) y x l22 y m22 z n22 2( xy l2 m2 yz m2 n2 zx n2 l2 ) 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 ) 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 ) Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island Two-Dimensional Stress Transformation y y' cos sin 0 Qij sin cos 0 0 1 0 x' x x x cos 2 y sin 2 2 xy sin cos y x sin 2 y cos 2 2 xy sin cos xy x sin cos y sin cos xy (cos 2 sin 2 ) Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island x y xy x y 2 x y 2 y x 2 x y 2 x y 2 cos 2 xy sin 2 cos 2 xy sin 2 sin 2 xy cos 2 Principal Stresses & Directions 1 , 2 , 3 det[ ij ij ] 3 I12 I 2 I 3 0 y 2 2 yx yz zy y 1 xy 1 x zx xz z 3 x 3 z (General Coordinate System) Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island (Principal Coordinate System) Traction Vector Components N A N Tn n n Tn S (| T n | N 2 )1/ 2 S S S 2 ( N 2 )( N 3 ) 0 Admissible N and S values lie in the shaded area S 2 ( N 2 )( N 3 ) 0 S ( N 3 )( N 1 ) 0 2 N 3 2 1 S 2 ( N 1 )( N 2 ) 0 S 2 ( N 1 )( N 2 ) 0 S 2 ( N 3 )( N 1 ) 0 Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island Mohr’s Circles of Stress Example 3-1 Stress Transformation For the given state of stress below, determine the principal stresses and directions and find the traction vector on a plane with unit normal n = (0,1,1)/2. 3 ij 1 1 1 0 2 1 2 0 The principal stress problem is started by calculating the three invariants, giving the result I1 = 3, I2 = -6, I3 = -8. This yields the following characteristic equation 3 3 2 6 8 0 The roots of this equation are found to be = 4, 1, -2. Back-substituting the first root into the fundamental system (1.6.1) gives n1(1) n 2(1) n3(1) 0 n1(1) 4n 2(1) 2n3(1) 0 n1(1) 2n2(1) 4n3(1) 0 Solving this system, the normalized principal direction is found to be n(1) = (2, 1, 1)/6. In similar fashion the other two principal directions are n(2) = (-1, 1, 1)/3, n(3) = (0, -1, 1)/2. The traction vector on the specified plane is calculated using the relation Ti n Elasticity 3 1 1 Theory, Applications and Numerics M.H. Sadd , University of Rhode Island 1 0 2 1 0 2 / 2 1 / 2 2 / 0 1 / 2 2 / 2 2 2 Spherical, Deviatoric, Octahedral and von Mises Stresses ~ ˆ ij ij ij ~ 1 . . . Spherical Stress Tensor ij kk ij 3 1 ˆ ij ij kk ij . . . Deviatoric Stress Tensor 3 1 1 1 oct (1 2 3 ) kk I1 . . . Octahedral Normal 3 3 3 and Shear Stresses 1/ 2 1 1 2 2 2 2 1/ 2 oct [(1 2 ) ( 2 3 ) ( 3 1 ) ] 2 I1 6 I 2 3 3 e vonMises Elasticity 3 1 ˆ ij ˆ ij [( x y ) 2 ( y z ) 2 ( z x ) 2 6( 2xy 2yz 2zx )]1 / 2 2 2 1 [(1 2 ) 2 ( 2 3 ) 2 ( 3 1 ) 2 ]1 / 2 2 Theory, Applications and Numerics M.H. Sadd , University of Rhode Island . . . von Mises Stress Stress Distribution Visualization Using 2-D or 3-D Plots of Particular Contour Lines • • • • • Particular Stress Components Principal Stress Components Maximum Shear Stress von Mises Stress Isochromatics (lines of principal stress difference = constant; same as max shear stress) • Isoclinics (lines along which principal stresses have constant orientation) • Isopachic lines (sum of principal stresses = constant) • Isostatic lines (tangent oriented along a particular principal stress; sometimes called stress trajectories) Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island Example Stress Contour Distribution Plots Disk Under Diametrical Compression P P (a) Disk Problem Maximum Shearing Stress Contours - Isochromatics (b) Max Shear Stress Contours (Isochromatic Lines) von Mises Stress Contours Sum of Principal Stress Contours - Isopachics (d) Sum of Principal Stress Contours (Isopachic Lines) Elasticity (e) von Mises Stress Contours Theory, Applications and Numerics M.H. Sadd , University of Rhode Island Maximum Principal Stress Contours (c) Max Principal Stress Contours Stress Trajectories for Disk (f) Stress Trajectories (Isostatic Lines) Equilibrium Equations Tn S F F 0 T S i n V dS Fi dV 0 V xy yx r F 0 ij ji yz zy zx xz Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island x yx zx Fx 0 x y z xy y zy Fy 0 x y z xz yz z Fz 0 x y z Stress & Traction Components in Cylindrical Coordinates x3 z z z rz r σ r rz r x2 r x1 d T r e r e z e z Tz rz e r z e z e z dr Equilibrium Equations r 1 r rz 1 ( r ) Fr 0 r r z r r 1 z 2 r F 0 r r z r rz 1 z z 1 rz Fz 0 r r z r Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island z rz z z Tr r e r r e rz e z r r Stress & Traction Components in Spherical Coordinates x3 R R σ R R R R R R TR R e R R e R e x2 R T R e R e e T R e R e e x1 Equilibrium Equations R 1 R 1 R 1 (2 R R cot ) FR 0 R R R sin R r 1 1 1 [( ) cot 3 R ] F 0 R R R sin R r 1 1 1 ( 2 cot 3 R ) F 0 R R R sin R Elasticity Theory, Applications and Numerics M.H. Sadd , University of Rhode Island