{finish spatial power of tractions} Example 1 A Compressible Neo-Hookean Material undergoing Homogeneous Stretch and Rotation Motion Consider the deformation of a cubic block of material, with sides of length 1, initially occupying the region 0 X 1 , X 2 , X 3 1 . The subsequent motion of the material is given by f (X, t ) x X 1 tX 2 e1 tX 1 X 2 e 2 X 3e 3 This is a two-dimensional motion, with the material stretching and rotating about the X 3 axis, as illustrated. t 0 t2 t 1 The spatial description of the motion is obtained by inverting these equations: f 1 (x, t ) X x1 tx2 tx x e1 1 2 2 e 2 x3e 3 2 1 t 1 t Deformation The deformation gradient is 1 t 0 x F t 1 0 , X 0 0 1 F 1 1 1 t 2 t 2 1 t 0 t 1 t2 1 1 t2 0 0 0 1 This deformation is homogeneous, meaning that the deformation is the same for all points (F is independent of position). The Jacobian determinant is J dv det F 1 t 2 dV The right Cauchy-Green tensor is 1 t 2 0 T C F F 0 1 t2 0 0 0 0 1 For example, the stretch for a line element (in the reference configuration) in the direction dX e1 is given by 2 e1 C e1 C11 1 t 2 . In this simple case of a homogeneous deformation, this stretch for line elements in the direction e1 is the same for all points in the material. The left Cauchy-Green tensor is b F F T and equals C is this example. It follows that the stretch of a line element (in the current configuration) in the direction dx is given by 1 t 2 0 1 dx 0 1 t2 2 dx 0 0 0 dx 0 dx 1 For example, in the direction dx e1 2e 2 at t 2 , the stretch is 5. The deformation can be decomposed into stretch tensors through F R U or F v R , where U and v are, respectively, the right (material) and left (spatial) stretch tensors. Since C is diagonal, 1 t2 U C 0 0 and 0 1 t2 0 0 0 1 R FU 1 1 2 1 t t 1 t2 0 0 0 1 t 1 t 1 2 1 t2 0 which is proper orthogonal, R R T I, det R 1. The deformation can thus be decomposed into a pure stretch along the principal (material) axes, which here are just the axes e1 , e 2 , e 3 , and then followed by a rotation about the X 3 axis. For example, at t 1 , the rotation is 45 o clockwise. The left stretch tensor is now obtained from v F R T and it turns out to be the same as U (and b v 2 ). Thus the deformation can also be decomposed into, first, a rigidbody rotation, followed by a pure stretch to the subsequent configuration. For example, considering the configuration at t 1 (see figure above), first rotate clockwise by 45 o ; then the rotated line elements dx (1) (1 / 2 )e1 1 / 2 e 2 , dx ( 2) 2e1 map to the final positions v dx (1) e1 e 2 and v dx ( 2) 2e1 . Nanson’s formula, nds JF T NdS , relates unit normals in the reference and current configurations. Each of the six sides of the block has surface area dS 1 and ds 1 t 2 . For example, the unit normal N e 2 is mapped to the unit normal n te1 e 2 / 1 t 2 through n1 n 2 n3 N e2 n t 1 t2 1 1 t2 t 1 t 2 1 t 2 2 1 t 0 e1 1 1 t2 t 1 t2 1 1 t2 0 0 0 0 1 1 0 e2 Rates of Deformation The velocity is (in the material description – the material coordinates are constant) V ( X, t ) dx d X 1 tX 2 e1 tX 1 X 2 e 2 X 3 e 3 X 2 e1 X 1e 2 dt dt The velocity in the spatial description can be obtained by substituting into the above expression the motion X f 1 (x, t ) , to get v(x, t ) tx1 x2 x tx e1 1 2 2 e 2 2 1 t 1 t These two velocities are the same, they are the velocities of material particles in the material, expressed in two different ways. The acceleration is zero, A( X, t ) dV / dt 0 . The acceleration can also be obtained directly from the spatial velocity using the material time derivative, a(x, t ) dv(x, t ) v(x, t ) grad v v dt t which turns out to be zero. The spatial velocity gradient is now t 1 t2 1 l grad v 2 1 t 0 1 1 t2 t 1 t2 0 0 0 0 This can be decomposed into its symmetric and skew-symmetric parts: the rate of deformation d t 1 t 2 0 0 0 1 2 1 t 0 1 l lT 2 0 t 1 t2 0 0 0 0 and the spin w 1 l lT 2 1 1 t2 0 0 0 0 0 The skew-symmetric spin can be written in the form of a vector, the angular velocity, ω w23e1 w13e 2 w12e 3 1 e3 1 t 2 which clearly corresponds to a clockwise rotation of material particles about the e 3 axis. Note also that div v v1 v2 v3 2t x1 x2 x3 1 t 2 so that the rate of change of the volume ratio dv / dV is J Jdiv v 2t Stress Suppose now that the Cauchy stress is 1 2 / 3 2 t 0 0 ln J 3 J 1 σ J 1 0 ln J J 2 / 3t 2 0 3 2 2 / 3 2 0 0 ln J J t 3 The Equations of Motion The equations of motion in the spatial description are div σ b v and it can be seen that the Cauchy stress is uniform throughout the material at any time instant, div σ ij / x j o . There are also no accelerations and so there are no body forces. The PK1 stress is P Jσ F T 1 2 / 3 2 t ln J 3 J 1 t2 ln J 1 J 2 / 3 t 2 3 t 1 t2 0 1 3 t 1 t2 1 ln J J 2 / 3t 2 3 1 t2 ln J J 2 / 3t 2 0 0 0 2 ln J J 2 / 3t 2 3 The equations of motion in the material description are Div P B 0 A and these three terms are also zero. Balance of Mechanical Energy Material Description The PK2 stress is S JF 1 σ F T 1 2 / 3 2 t ln J 3 J 1 t2 0 0 0 1 3 1 t2 ln J J 2 / 3t 2 0 0 0 2 ln J J 2 / 3t 2 3 Also, t 0 0 E F T d F 0 t 0 0 0 0 and then the stress power is 2t S:E 1 t2 1 2 / 3 2 t ln J 3 J The same result can be obtained by using the alternative stress power expression, P : F . The stress power is independent of position within the material, and the volume in the undeformed configuration V is unity so the total stress power is 2t 1 ln J J 2 / 3t 2 2 3 S : E dV S : E 1 t V Look now at the power of the power of the surface tractions: T VdS . The velocity dS is zero over the front and back faces (the sides with unit normals e 3 ), and is nonzero over the other four sides (with normals in the reference configuration e1 , e 2 ). The PK1 traction is given by T P N and is shown in the figure for these four faces, and given below (the PK1 stress is uniform throughout the material). T( 2) P e 2 P12 e1 P22 e 2 T(3) P (e1 ) T(1) T(1) P e1 P11e1 P21e 2 T( 4) P (e 2 ) T( 2) 1 2 / 3 2 t e1 te 2 , ln J 3 J 1 1 ln J J 2 / 3t 2 te1 e 2 , 2 3 1 t T(1) T( 2 ) 1 1 t2 Substituting in the velocity V X 2 e1 X 1e 2 now leads to T(3) T(1) T( 4 ) T( 2 ) T VdS T X (1) dS e e 2 dS (1) T e 2 1 dS(1) ( 2) 1 X 1e 2 dS ( 2 ) dS( 2 ) T X e dS ( 3) 2 1 ( 3) dS( 3 ) T X e dS ( 4) 1 2 ( 4) dS( 4 ) 1 1 1 1 T(1) X 2 e1 e 2 dX 2 dX 3 T( 2 ) e1 X 1e 2 dX 1 dX 3 0 0 0 0 1 1 1 1 0 0 0 0 T(1) X 2 e1 dX 2 dX 3 T( 2 ) X 1e 2 dX 1 dX 3 1 1 1 1 T(1) e1 e 2 T( 2 ) e1 e 2 T(1) e1 T( 2 ) e 2 2 2 2 2 2t 1 ln J J 2 / 3t 2 2 3 1 t which equals the stress power, and so the mechanical energy is balanced: dV T V dS B V dV S : E dV V dt S V V dV V Spatial Description In the spatial description, the stress power is σ : d J 1 2t 1 t2 1 2 / 3 2 ln J J t 3 The total stress power in the material, with dv JdV , is then 2t 1 ln J J 2 / 3t 2 2 3 σ : ddv σ : d dv Jσ : d 1 t v v In the spatial description, the power of the surface forces is t v ds . Again, we only s need to look at four sides, since the velocity is zero over the front and back. The unit normals to these four faces are shown in the figure. n (3) n (1) 1 n ( 2) 1 t 2 te1 e 2 n ( 4 ) n ( 2 ) 1 n (1) 1 t 2 e1 te 2 The tractions acting over these surfaces are then obtained from Cauchy’s law, t σ n . Examining the first surface, the velocities of particles there are those for particles with material coordinates X 1 1 , so, eliminating x1 , X1 tx x x1 tx2 1 t 2 , v (1) 1 2 2 e1 e 2 t x2 e1 e 2 1 t X1 1 x1 tx2 1 1 t 2 The integration over 1 1 dX dx 1 is straightforward. The integration over dX in the reference configuration corresponds to the integration dl in the current configuration. With 3 0 0 3 1 2 0 dl dx2 dx1 dl (dx1 ) 2 (dx 2 ) 2 1 t 2 dx 2 over this surface, we have dl 1t 1 t 2 dx 2 t The double integral in the reference confuguration to the integral f (x) J dx dx 2 3 J 23 f (X)dX 2 dX 3 can be converted where J is the Jacobian for the change of variable: X 2 / x2 X 2 / x3 X 3 / x2 X 3 / x3 1 1 t 2 The limits of integration are obtained Thus the complete expression of the power of the tractions is t v ds s 1 1t 1 1 t v (1) dx 2 dx3 2 (1) 1 t 0 t 1 t2 1 1 t2 1 1 t t ( 2) v ( 2 ) dx1 dx3 0 t 1 1 t (3) v (3) dx2 dx3 0 0 1 1 t2 1 1 t ( 4) 0 0 v ( 4 ) dx1 dx3 The integral over the first surface is then t (1) v (1) ds s 1 1 t2 1 1 t t J 1 (1 t 2 ) 3 / 2 (1) v (1) dx 2 dx3 0 t J 1 (1 t 2 ) 3 / 2 1 1t e te 2 t x 2 e1 e 2 dx 2 dx3 1 0 t 1 1t 2t x dx dx 2 2 3 0 t J 1 t 1 / 2 (1 t 2 ) 3 / 2 where ln J J 2 / 3t 2 / 3 . 1 1 t2 1 1 t t 0 t (1) 1 1 t2 1 1 t J 1 v (1) dx1 dx3 (1 t 2 ) 3 / 2 1 1 t (3) v (3) dx2 dx3 0 0 te 1 e 2 e1 x1 t e 2 dx1 dx3 0 t 1 1 t J 1 (1 t 2 ) 3 / 2 2t x dx dx 1 1 3 0 t J 1 t 1 / 2 (1 t 2 ) 3 / 2 J 1 (1 t 2 ) 3 / 2 e J 1 (1 t 2 ) 3 / 2 1 1 1 1 1 te 2 x 2 e1 dx 2 dx3 0 0 x dx dx 2 2 3 0 0 J 1 1 / 2 (1 t 2 ) 3 / 2 1 1 t2 1 1 t 0 0 ( 4) J 1 v ( 4 ) dx1 dx3 (1 t 2 ) 3 / 2 J 1 (1 t 2 ) 3 / 2 1 1 te 1 e 2 x1e 2 dx1 dx3 0 0 1 1 x dx dx 1 0 0 J 1 1 / 2 (1 t 2 ) 3 / 2 1 3 and the total is t v ds J s 1 2t ln J J 2 / 3t 2 / 3 2 3/ 2 (1 t ) and so the mechanical energy is balanced in the spatial description: dv t v ds b v dv σ : ddv v dt dv s v v v Strain Energy and Conservative Force System The above Cauchy and PK2 stresses were actually derived from the strain energy function 1 1 2 W ln J J 2 / 3 I b 3 2 2 This is the strain energy of a compressible Neo-Hookean material. It is a hyperelastic model (since the stress is obtained from a strain energy function) of an isotropic material (since the Cauchy stress is a function of the left Cauchy-Green strain b only). Here, J det F . We write this in terms of the third invariant of b, III b det b : III b J 2 . Differentiating W now gives J / III b III b / III b 1 / 2 J , so W W W W 2 σ 2 J 1 III b I 2 J 1 I b b 2 J 1 b III b I b II b II b W J 2 W 2 J 1 J I 2 J 1 b J III I b b 1 J 1 ln J I J 2 / 3 b trb I 3 The PK2 stress can also be obtained directly through W W W W S 2 I b I 2 C2 III b C 1 II b III b I b II b 1 ln JC 1 J 2 / 3 I trC C 1 3 leading to the PK2 stress given earlier. 1 1 2 Explicitly, from W ln J J 2 / 3 I b 3 , the time derivative of the strain 2 2 energy is 1 d 1 W J 1 J ln J J 2 / 3 trb J 2 / 3 trb 3 dt 2 Now J Jdiv v so J 1 J div v 2t 1 t2 and trb 3 2t 2 d trb 4t dt so 2t W 1 t2 1 2 / 3 2 t ln J 3 J It can be seen that this time derivative of the strain energy is precisely the stress power, as expected for a hyperelastic material: W 1 U Jσ : d S : E 0 Here, U is a strain energy per unit mass, whereas W is the strain energy per unit (reference) volume.