2001, W. E. Haisler 19 Chapter 3: Conservation of Linear Momentum Although the conservation of linear momentum equations may be left in terms of tractions, it is more convenient and customary to put the tractions in terms of stresses. For this purpose, consider a two dimensional planar body as shown below: F2 F1 b = thickness f y x z Make two free bodies by passing a plane with unit normal n through the body as shown below: 2001, W. E. Haisler 20 Chapter 3: Conservation of Linear Momentum F2 F1 b f y x z Original Body F2 F1 t ( n ) t (n ) -n n R1 R2 Free Body #1 R3 Free Body #2 f 2001, W. E. Haisler 21 Chapter 3: Conservation of Linear Momentum On the cut edge of each free body, we must place equal and opposite forces. Since these forces act over some area, we write these forces in terms of the traction t(n ) as shown on the figure. Now consider a smaller free body taken from FB #2 above by passing horizontal and vertical cutting planes as shown below: j t (n ) t ( j) f A ( j) A (n ) n y x n Freebody #2 t (n ) A(i ) t (i ) i The inclined side of the wedge has a unit outward normal n , a surface area A( n ) and the traction is t( n ) . The normal makes an 2001, W. E. Haisler 22 Chapter 3: Conservation of Linear Momentum angle with the x-axis as shown (positive is CCW from the xaxis) and the unit normal is given by: n nx i ny j (cos )i + (sin ) j = [cos( + )]i +[sin( + )]j = -(cos )i - (sin ) j . On the i and j surfaces, the area is A( i ) and A( j ) , respectively, and the tractions are t( i ) and t( j ) , respectively. Each traction vector may be resolved into its x and y components as shown below: 2001, W. E. Haisler 23 Chapter 3: Conservation of Linear Momentum t( n ) t ( n ) x i t ( n ) j t ( j) y y t( i ) t ( i ) x i t ( i ) j t ( j) x A (n ) t (n ) x y y A ( j) A(i) x t (i ) x t( j ) t ( j ) x i t ( j ) j y n nx i n y j n t (i ) y t (n ) y (cos ) i + (sin ) j A ( i ) A ( n ) cos , A ( j) A ( n ) sin We now apply conservation of liner momentum for the tractions, 0 Fext , to obtain: 2001, W. E. Haisler 24 Chapter 3: Conservation of Linear Momentum x-component: 0 t (n ) x (A (n ) ) t ( i ) A ( i ) t ( j) A ( j) x x y-component: 0 t (n ) y (A (n ) ) t ( i ) A ( i ) t ( j) A ( j) y y Substituting the area relations into the above gives: x-component: 0 t (n ) x (A (n ) ) t ( i ) A (n ) cos t ( j) A (n ) sin x x y-component: 0 t (n ) y (A ( n ) ) t ( i ) A ( n ) cos t ( j) A ( n ) sin y y Canceling the area gives: t (n ) x t ( i ) cos t ( j) sin x x t (n ) y t ( i ) cos t ( j) sin y y Note that the normal vector has components of nx cos cos ; ny sin sin 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum 25 Hence the traction on the normal face can be written as t ( n ) x nx t ( i ) +n y t ( j) x x t ( n ) y nx t ( i ) +n y t ( j) y y This last set of equations is called Cauchy's formula. It provides the relationship between the traction components that act on a surface with unit outward normal n and the x and y components of tractions required to keep the free-body in equilibrium, i.e., satisfy conservation of linear momentum. It is useful to write to write the tractions on the x and y faces in terms of Cauchy stresses as follows: 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum xx t ( i ) x , yx t ( j) x , xy t ( i ) y , yy t ( j) y Note the following notation: xx is the traction on the x face acting in the x direction, xy is the traction on the x face acting in the y direction, yx is the traction on the y face acting in the x direction, etc. 1st subscript = face acting on; 2nd = direction of traction. With this notation, Cauchy's formula becomes: t (n ) x nx xx ny yx t (n ) y nx xy ny yy 26 2001, W. E. Haisler 27 Chapter 3: Conservation of Linear Momentum Recall: traction and normal vectors are given by t(n ) t (n ) x i t (n ) j y and n nx i n y j = (cos ) i + (sin ) j . In matrix notation: t (n ) t (n ) x t ( n ) , n nx y n y And the Cauchy stress tensor is given by xx xy t ( i ) x yy yx t ( j) x t (i) y t ( j) y Thus, Cauchy formula in vector and matrix notation is given by: t (n ) n or t n (n ) 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum 28 Once again, Cauchy’s formula is nothing more than Conservation of Linear Momentum applied to an element of material as shown below and which is subjected to stress components on each face as shown. In order for the element to be in static equilibrium (satisfy COLM), the stresses (and tractions) must satisfy Cauchy’s formula t(n ) n . yy t ( j) y yx t ( j) x xy t ( i ) y xx t ( i ) x n y x z t( n ) 2001, W. E. Haisler 29 Chapter 3: Conservation of Linear Momentum Suppose the element is chosen at a boundary where the outward unit normal is n an external traction t(n ) is applied. Then we can use Cauchy's formula to determine the internal stress state. yy yx external surface xy n y t( n ) x z body xx 2001, W. E. Haisler 30 Chapter 3: Conservation of Linear Momentum Consider a material point in the planar body at some point (x,y,z). At this point, we observe an internal stress state given by the stress tensor [] as shown below: yy yx F2 F1 b = thickness f xx xy y x z yx yy xy xx 2001, W. E. Haisler 31 Chapter 3: Conservation of Linear Momentum In 2-D, a complete picture of the Cauchy stress tensor and Cauchy's formula is: yy yx xx xy yx y x z yy xy yy yx xy t( n ) xx xx xy yx n n yy xx t( n ) Note: 1) on opposite faces of the normal plane, the normal vector and traction are opposite. 2) On opposite faces of the square, stresses are in opposite directions. On the +x face, xy is positive in + y direction; on the -x face, xy is positive in the -y direction. 2001, W. E. Haisler 32 Chapter 3: Conservation of Linear Momentum For a 3-dimensional state of stress, Cauchy's formula becomes t ( n ) σ xx nx σ yx n y σ zx nz x t ( n ) σ xy nx σ yy ny σ zy nz y t ( n ) σ xz nx σ yz n y σ zz nz z and the Cauchy stress tensor is given by: xx yx zx xy yy zy xz t ( i ) x yz t ( j) x zz t (k ) x t (i ) y t ( j) y t (k ) y t (i) z t ( j) z t (k ) z In chapter 4, conservation of angular momentum, we will shown that the stress tensor must be symmetric so that xy yx , etc. 2001, W. E. Haisler 33 Chapter 3: Conservation of Linear Momentum y yy t(j) yx xy yz zy 0 t(k) k xx j x z i zx zz z x t(i) 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum 34 We want to replace the traction terms ( t , etc.) on the right (i) side of conservation of linear momentum by equivalent stress terms (xx, etc). In dyadic notation (a special vector notation), the stress matrix can be written as ii ji ki xx yx zx ij jj kj xy yy zy ik jk kk xz yz zz Thus, we can write the tractions in terms of stresses as 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum 35 , t j , t i i j k j i xx xy xz t k k Thus, we can write the traction terms in linear momentum as: ti t j tk (i ) ( j ) (k ) x y z x y z i j k y z x 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum 36 Conservation of linear momentum becomes v (v )v g t Note that the “dot product” results in a vector (not a scalar since is a matrix), and is given by xx yx zx ( )i x y z xy yy zy ( )j x y z xz yz zz ( )k x y z 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum 37 Conservation of Linear Momentum has 3 components: xx yx zx vx vx vx vx x comp : ( vx vy vz ) gx x y z t x y z xy yy zy vy vy vy vy y comp : ( vx vy vz ) gy x y z t x y z xz yz zz vz vz vz vz z comp : ( vx vy vz ) gz x y z t x y z 2001, W. E. Haisler 38 Chapter 3: Conservation of Linear Momentum At a given point, the nine components of a stress tensor (three stresses each acting on the three x, y, z faces of a cube) can always be resolved into vector components acting on a face having a different orientation relative to the x,y,z axes. Consider a unit normal vector n nxi ny j nzk representing the unit normal to a surface. The dot product n will give the projection of onto the plane defined by the unit normal vector n , and yields the traction (stress) vector t n acting on the surface with normal n . n NOTE: tn is not a vector normal to the plane but a vector that acts on the plane with a unit normal n. 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum z t (n) t(-j) -i n -j -k x t (-k) 39 For a surface described by f(x,y,z)=0, the gradient of f, f , gives the normal to the surface. The unit normal is then given t(-i) f n nx i n y j nz k . f y Also, nx cos x , n y cos y , and nz cos z where x is the angle between n and x-axis ( i ), y is angle between n and y-axis ( j ), and z is angle between n and z-axis ( k ). t t i j k i i xx xy xz 2001, W. E. Haisler 40 Chapter 3: Conservation of Linear Momentum t n (n i n j n k ) n x y z (n i n j n k ) (ii ij ik x y z xx xy xz ji ki yx zx jj kj yy zy in jn kn x xx x xy x xz in jn kn y yx y yy y yz in jn kn z zx z zy z zz jk kk yz zz ) 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum 41 Thus, we have tn n i (nx xx n y yx nz zx ) j (nx xy n y yy nz zy ) k (nx xz n y yz nz zz ) Note that the traction vector t has components on the normal n face which are in the x,y,z directions. This is an equilibrium statement of forces in x, y and z directions. Often referred to as the Cauchy tetrahedron. 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum 42 The Conservation of Linear Momentum is often defined in terms of the deviatoric (or extra) stress tensor S. S 1 ( xx yy zz)I PI 3 where P 1 ( xx yy zz) 3 P is the average normal (or hydrostatic) compressive stress. the identity matrix. I is 2001, W. E. Haisler 43 Chapter 3: Conservation of Linear Momentum xx P S xx S xy S xz S yx S yy S yz yx S zx S zy S zz zx xy xz yy P yz zy zz P Note: the sum of the diagonal terms of [S] = 0. The above can be written as [] = [S] - P [I] where [I] = identity matrix. Hence, Conservation of Linear Momentum becomes: [ v (v )v] g S P t 2001, W. E. Haisler Chapter 3: Conservation of Linear Momentum 44 Conservation of Linear Momentum has 3 components: xx yx zx vx vx vx vx x comp : ( vx vy vz ) gx x y z t x y z xy yy zy vy vy vy vy y comp : ( vx vy vz ) gy x y z t x y z xz yz zz vz vz vz vz z comp : ( vx vy vz ) gz x y z t x y z Sxx S yx Szx P vx vx vx vx ( vx vy vz ) gx x y z x t x y z Sxy S yy Szy vy vy vy vy ( vx vy vz ) gy P x y z y t x y z Sxz S yz Szz P vz vz vz vz ( vx vy vz ) gz x y z z t x y z