COMPUTATIONAL METHODS IN ENGINEERING AND SCIENCE EPMESC X, Aug. 21-23, 2006, Sanya, Hainan, China ©2006 Tsinghua University Press & Springer New FDM for Plane Elasticity in Polar Coordinates B. Q. Zhu 1*, J. S. Zhuo 2, J. F. Zhou 1 1 2 College of Mechanical & Electrical Engineering, Hohai University, Changzhou, 213022 China College of Civil Engineering, Hohai University, Nanjing, 210098 China Email: [email protected] Abstract Circular sector domain is the typical area of plane elasticity in polar coordinates for solution. It can be changed to rectangle area with suitable variable substitution. With radial coordinate or circumferential coordinate treated as “time” and dual variables introduced, two symplectic systems of different forms can be established for plane elasticity in polar coordinates by using Hellinger-Reissner generalized variational principle. In this paper, FDM is introduced into radial symplectic system of elasticity. The idea of FDM in Lagrange system is adopted. After meshes and nodes being set, the surrounding area of each node is used as integrating area. From Hamilton’s dual equations, difference equations for each node are established by using integral interpolation method. Combining the difference equations of all nodes, whole difference format is constructed. The problems of thick-walled cylinder and curved beam are calculated by programming. The numerical results show that the proposed FDM is effective. Another numerical method is provided for plane elasticity in polar coordinates. Elasticity problems are always solved with one kind of variables in Lagrange system. Traditional FDM includes stress difference method and displacement difference method. These difference methods have some particular limits because they are restricted by the system itself. With dual variables for solution, the new FDM can treat complex boundary conditions better. Displacements and stresses can be obtained directly. The format of FDM with stress boundary condition is discussed in this paper. The problem with displacement boundary condition can be treated similarly. Key words: elasticity, plane problem in polar coordinates, radial symplectic system, integral interpolation method, new FDM INTRODUCTION Plane problems in polar coordinates are always solved with one kind of variables in Lagrange system. Traditional FDM includes stress difference method and displacement difference method. These methods have some particular limits because they are restricted by the system itself. With radial coordinate or circumferential coordinate treated as “time” and dual variables introduced, two symplectic systems of different forms can be established for plane elasticity in polar coordinates by using Hellinger-Reissner generalized variational principle[1-4]. An analytical method is given to plane elasticity in circular sector domain. The method is applied to the problems of elastic curved beam, elastic wedge, stress singularity of fracture mechanics, etc. [3-8], and its superiority is shown to that in Lagrange system. In circumferential symplectic system, a new solution of elasticity in polar coordinates is obtained [9]. By installing analytical element into FEM program system, semi-analytical FEM is introduced into symplectic system, and it can be used for stress intensity factor solution of plane crack, etc [10-13]. In this paper, the FDM is introduced into radial symplectic system. A new difference format is constructed, and another numerical method is provided for plane elasticity in polar coordinates. HAMILTON’S DUAL EQUATIONS IN RADIAL SYMPLECTIC SYSTEM Circular sector domain shown in Fig.1 is the typical area of plane elasticity in polar coordinates for solution. With the variable substitution ξ = ln ρ (i.e. ρ = eξ ), it can be changed to the rectangle area as shown in Fig.2, in which ξ 1 = ln R1 , ξ 2 = ln R2 . Via new variables ( S ρ = ρσ ρ , Sϕ = ρσ ϕ , S ρϕ = ρτ ρϕ ) introduced and radial coordinate ξ ⎯ 696 ⎯ treated as “time”, Hellinger-Reissner generalized variational principle can be expressed as follows [2]: α2 ξ2 − 1 δ∫ α ∫ξ ∂uϕ ∂u ρ ⎧ 1 2 ⎫ ) + S ρϕ (u&ϕ − uϕ + )− [ S ρ2 + Sϕ2 − 2ν S ρ Sϕ + 2(1 + ν ) S ρϕ ]⎬ d ξ d ϕ = 0 ⎨ S ρ u& ρ + Sϕ (u ρ + 2E ∂ϕ ∂ϕ ⎩ ⎭ (1) in which, the dot represents the derivative of a variable about ξ . R1 O =0 R2 Figure 1: Circular sector domain in polar coordinates 2 1 Figure 2: Rectangle area after variable substitution Performing variation of Eq. (1) to S ϕ , it follows that S ϕ = E (u ρ + ∂uϕ ∂ϕ ) + νS ρ (2) Substituting Eq. (2) into Eq. (1), Hamiltonian mixed energy variational principle is given ∂uϕ 2 ∂u ρ ∂uϕ 1 ) − u ϕ ) + E (u ρ + S ρ u& ρ + S ρϕ u&ϕ + νS ρ (u ρ + ) + S ρϕ ( ⎨ − ∂ϕ 2 ∂ϕ ∂ϕ 1 ⎩ 1 2 ⎫ − [(1 − ν 2 ) S ρ2 + 2(1 + ν ) S ρϕ ]⎬ d ξ d ϕ = 0 2E ⎭ α δ∫ ξ2 ⎧ α ∫ξ (3) Expanding Eq. (3), Hamilton’s dual equations in radial symplectic system are obtained u& ρ = − ν u ρ − ν u& ϕ = − ∂u ρ ∂ϕ S& ρ = Eu ρ ∂uϕ ∂ϕ + 1−ν E 2 Sρ 2 (1 + ν ) S ρϕ E ∂uϕ ∂ S ρϕ + E + νS ρ − ∂ϕ ∂ϕ + uϕ + ∂ 2uϕ ∂S ρ ∂u ρ − S ρϕ − E −ν S& ρϕ = − E 2 ∂ϕ ∂ϕ ∂ϕ ⎫ ⎪ ⎪ ⎪ ⎪ ⎪ ⎬ ⎪ ⎪ ⎪ ⎪ ⎪ ⎭ (4) FORMAT OF NEW FDM The basic idea of the new FDM in radial symplectic system is similar to that in Lagrange system. After meshes and nodes being set in the area for solution, the surrounding area of each node is used as integrating area. Difference ⎯ 697 ⎯ equations for each node are established by using integral interpolation method. The following discussion is focused on the problem with stress boundary condition. 1. Difference equations for inner node Uniform meshes are set in rectangle area ( ξ1 ≤ ξ ≤ ξ 2 , ϕ1 ≤ ϕ ≤ ϕ 2 ). For convenience, the inner node is marked P0. Its adjacent nodes are P1, P2, P3, and P4. hξ and hϕ are, respectively, the steps in direction ξ and direction ϕ (as shown in Fig.3). The surrounding area (hatched part in Fig.3) of P0 is used as integrating area D. 2 2 3 3 3 2 0 4 1 1 1 4 4 Figure 3: Internal node and its surrounding area By integrating Eq. (4) over the area D and using Green’s formula, it follows that ⎫ ⎪ ⎪ D D ∂D ∂D ⎪ 2(1 + ν ) ⎪ S ρϕ d ξ d ϕ = 0 − uϕ d ϕ + u ρ d ξ − uϕ d ξ d ϕ − E ⎪ D D ∂D ∂D ⎬ − S ρ d ϕ − Eu ρ d ξ d ϕ − Eu ϕ d ξ − νS ρ d ξ d ϕ + S ρϕ d ξ = 0 ⎪ ⎪ D D ∂D ∂D ∂D ⎪ ∂u ϕ ⎪ d ξ + νS ρ d ξ + S ρϕ d ξ d ϕ = 0 ⎪ − S ρϕ d ϕ + Eu ρ d ξ + E ϕ ∂ D ∂D ∂D ∂D ∂D ⎭ ∫ − uρ d ϕ + ∫∫νu ρ d ξ d ϕ + ∫ νuϕ d ξ − ∫∫ ∫ ∫ ∫∫ ∫ ∫∫ ∫ ∫ 1 −ν 2 Sρ dξ dϕ = 0 E ∫∫ ∫ ∫∫ ∫ ∫ ∫ (5) ∫∫ Considering a general function g (ϕ , ξ ) and with g i representing the function value at Pi (i = 0,1,L 4) , following expressions are deduced from integral midpoint formula and difference formula − ∫ g dϕ ≈ (g N2 − g N 4 ) hϕ ≈ ∂D ∫∫ g2 − g4 hϕ , 2 ∫ g dξ ≈ (g N1 − g N3 )hξ ≈ ∂D g1 − g 3 hξ 2 ⎡ g − g0 g0 − g3 ⎤ hξ ⎡ ∂g ⎤ ∂g ∂g d ξ ≈ ⎢( ) N1 − ( ) N3 ⎥ hξ ≈ ⎢ 1 − ⎥ hξ = [ g1 + g 3 − 2 g 0 ] hϕ ⎥⎦ hϕ ∂ϕ ∂ϕ ⎦ ⎢⎣ hϕ ⎣ ∂ϕ ∂D ∫ g d ξ d ϕ ≈ g 0 hξ hϕ , D Substituting these into Eq. (5) and simplifying them, the difference equations for inner node are established uρ2 − uρ4 2hξ uϕ 2 − uϕ 4 2hξ Sρ2 − Sρ4 2hξ + νu ρ 0 + ν + u ρ1 − u ρ 3 2hϕ − Eu ρ 0 − E S ρϕ 2 − S ρϕ 4 2hξ uϕ1 − uϕ 3 +E − 2hϕ − uϕ 0 − 2(1 + ν ) S ρϕ 0 = 0 E uϕ 1 − uϕ 3 2hϕ u ρ1 − u ρ 3 2hϕ 1 −ν 2 Sρ0 = 0 E +E − νS ρ 0 + S ρϕ 1 − S ρϕ 3 2hϕ uϕ 1 + uϕ 3 − 2uϕ 0 2 hϕ +ν =0 S ρ1 − S ρ 3 2hϕ + S ρϕ 0 ⎯ 698 ⎯ ⎫ ⎪ ⎪ ⎪ ⎪ ⎪⎪ ⎬ ⎪ ⎪ ⎪ ⎪ = 0⎪ ⎪⎭ (6) 2. Difference equations for the node on boundaries ϕ = ±α On boundaries ϕ = ±α , the node and its surrounding area are shown in Fig. 4. 2 2 2 3 0 1 1 4 2 3 2 3 1 2 0 3 4 4 4 4 1 4 (a) ϕ = −α (b) ϕ = α Figure 4: Node on boundaries ϕ = ±α and its surrounding area On boundary ϕ = −α , the integrals of general function g (ϕ , ξ ) are − ∫ g d ϕ ≈ ( g N2 − g N4 ) hϕ ∂D ∫ g dξ ≈ (g N 2 g2 − g4 hϕ 4 g1 − g 0 hξ 2 − g 0 )hξ ≈ 1 ≈ ∂D 1 ∫∫ g d ξ d ϕ ≈ 2 g 0 hξ hθ D Since the stress boundary condition is under discussion, therefore ∫ S ρϕ d ξ ≈ (S ρϕ ) − N1 hξ ∂D ∫ Eu ρ d ξ + ∂D ∫ E ∂D ≈ ( Eu ρ + E ≈ (E ∂uϕ 2 C3 C4 S ρϕ |ϕ = −α d ξ ≈ +E S ρϕ 1 + S ρϕ 0 2 hξ − ∫ C3 C4 S ρϕ |ϕ =−α d ξ ∫ d ξ + νS ρ d ξ ∂ϕ ∂D ∫ + νS ρ ) N1 hξ − ∂ϕ u ρ1 + u ρ 0 ∂uϕ ∫ u ϕ 1 − uϕ 0 hϕ C3 C4 +ν ( Eu ρ + E S ρ1 + S ρ 0 2 ∂uϕ + νS ρ ) |ϕ =−α d ξ ∂ϕ )hξ − ∫ C3 C4 Sϕ |ϕ =−α d ξ Substituting these into Eq. (5) and simplifying them, the difference equations for the node on boundary ϕ = −α take the final form uρ 2 − uρ 4 2hξ uϕ 2 − u ϕ 4 2hξ Sρ2 − Sρ4 2hξ + νu ρ 0 + ν + u ρ1 − u ρ 0 hϕ +E − hϕ − uϕ 0 − − Eu ρ 0 − E S ρϕ 2 − S ρϕ 4 2hξ uϕ 1 − uϕ 0 hϕ 2(1 + ν ) S ρϕ 0 = 0 E uϕ 1 − uϕ 0 hϕ u ρ1 + u ρ 0 1 −ν 2 Sρ0 = 0 E +E − νS ρ 0 + S ρϕ1 + S ρϕ 0 2(uϕ1 − uϕ 0 ) 2 hϕ hϕ +ν 2 − hϕ hξ S ρ1 + S ρ 0 hϕ − C3 ∫C S ρϕ |ϕ =−α d ξ = 0 4 2 hϕ hξ ⎯ 699 ⎯ C3 ∫C Sϕ |ϕ =−α d ξ + S ρϕ 0 4 ⎫ ⎪ ⎪ ⎪ ⎪ ⎪⎪ ⎬ ⎪ ⎪ ⎪ ⎪ = 0⎪ ⎪⎭ (7) For that on boundary ϕ = α , the difference equations take the similar form as follows. uρ 2 − uρ 4 2hξ uϕ 2 − uϕ 4 2hξ Sρ2 − Sρ4 2hξ uϕ 0 − uϕ 3 + νu ρ 0 + ν + hϕ u ρ1 − u ρ 3 2hϕ − uϕ 0 − 2hξ hϕ uρ 0 + uρ 3 −E hϕ 1 −ν 2 Sρ0 = 0 E 2(1 + ν ) S ρϕ 0 = 0 E uϕ 0 − uϕ 3 − Eu ρ 0 − E S ρϕ 2 − S ρϕ 4 − −E − νS ρ 0 − S ρϕ 0 + S ρϕ 3 hϕ 2(uϕ 0 − uϕ 3 ) 2 hϕ 2 + hϕ hξ S ρ1 + S ρ 0 −ν + hϕ C2 ∫C S ρϕ |ϕ =α d ξ = 0 1 2 hϕ hξ C2 ∫C Sϕ |ϕ =α d ξ + S ρϕ 0 1 ⎫ ⎪ ⎪ ⎪ ⎪ ⎪⎪ ⎬ ⎪ ⎪ ⎪ ⎪ = 0⎪ ⎪⎭ (8) 3. Difference equations for the node on boundaries ξ = ξ1 , ξ 2 On boundaries ξ = ξ1 , ξ 2 , the node and its surrounding area are shown in Fig. 5. 3 2 2 3 3 3 2 3 1 4 1 1 0 1 1 4 1 4 2 0 3 4 (a) ξ = ξ1 (b) ξ = ξ 2 Figure 5: Node on boundaries ξ = ξ 1 , ξ 2 and its surrounding area On boundary ϕ = −α , the integrals of general function g (ϕ , ξ ) are ∫ g dϕ ≈ ( g N − 2 − g 0 ) hϕ ≈ ∂D ⎡ ∂g ∂g ∫ ∂ϕ d ξ ≈ ⎢⎣( ∂ϕ ) N 1 −( ∂D g2 − g0 hϕ 2 ∫ g dξ ≈ (g N 1 − g N3 ) ∂D hξ 2 ≈ g1 − g 3 hξ 4 1 ∫∫ g d ξ d ϕ ≈ 2 g 0 hξ hϕ D hξ ⎤ hξ ⎡ g1 − g 0 g 0 − g 3 ⎤ hξ ∂g ≈⎢ − = [ g1 + g 3 − 2 g 0 ] ) N3 ⎥ ⎥ ∂ϕ ⎦ 2 ⎢⎣ hϕ hϕ ⎦⎥ 2 2hϕ But C1 C1 Sρ0 + Sρ2 C4 C4 2 − ∫ S ρ d ϕ ≈ − ∫ S ρ |ξ =ξ1 d ϕ + ( S ρ ) N 2 hϕ = − ∫ S ρ |ξ =ξ1 d ϕ + ∂D C1 C1 S ρϕ 0 + S ρϕ 2 C4 C4 2 − ∫ S ρϕ d ϕ ≈ − ∫ S ρϕ |ξ =ξ1 d ϕ + ( S ρϕ ) N 2 hϕ = − ∫ S ρϕ |ξ =ξ1 d ϕ + ∂D hϕ hϕ So the difference equations for the node on boundary ξ = ξ1 are uρ2 − uρ0 hξ uϕ 2 − uϕ 0 hξ Sρ0 + Sρ2 hξ + νu ρ 0 + ν + u ρ1 − u ρ 3 2hϕ − Eu ρ 0 − E S ρϕ 0 + S ρϕ 2 hξ uϕ 1 − u ϕ 3 +E − 2hϕ − uϕ 0 − 2(1 + ν ) S ρϕ 0 = 0 E u ϕ 1 − uϕ 3 2hϕ u ρ1 − u ρ 3 2hϕ 1 −ν 2 Sρ0 = 0 E +E − νS ρ 0 + S ρϕ1 − S ρϕ 3 2hϕ 2 − hϕ hξ C1 ∫C S ρ |ξ =ξ 4 1 dϕ = 0 S ρ1 − S ρ 3 1 2 + S ρϕ 0 − (uϕ1 + uϕ 3 − 2uϕ 0 ) + ν 2 2hϕ hξ hϕ hϕ ⎯ 700 ⎯ C1 ∫C S ρϕ |ξ =ξ 4 1 ⎫ ⎪ ⎪ ⎪ ⎪ ⎪⎪ ⎬ ⎪ ⎪ ⎪ ⎪ d ϕ = 0⎪ ⎪⎭ (9) Similarly, difference equations for that on boundary ξ = ξ 2 are uρ0 − uρ 4 hξ uϕ 0 − uϕ 4 hξ + νu ρ 0 + ν + S ρϕ 0 + S ρϕ 4 − uϕ 1 − uϕ 3 − Eu ρ 0 − E hξ 2hϕ u ρ1 − u ρ 3 +E +E 2hϕ ⎫ ⎪ ⎪ ⎪ ⎪ ⎪⎪ ⎬ ⎪ ⎪ ⎪ ⎪ d ϕ = 0⎪ ⎪⎭ 1 −ν 2 Sρ0 = 0 E 2(1 + ν ) S ρϕ 0 = 0 E − uϕ 0 − 2hϕ hξ − 2hϕ u ρ1 − u ρ 3 Sρ0 + Sρ4 − uϕ1 − uϕ 3 S ρϕ1 − S ρϕ 3 − νS ρ 0 + 2 + hϕ hξ 2hϕ C2 ∫C 3 S ρ |ξ =ξ 2 d ϕ = 0 S ρ1 − S ρ 3 1 2 (uϕ1 + uϕ 3 − 2uϕ 0 ) + ν + S ρϕ 0 + 2 2hϕ hξ hϕ hϕ C2 ∫C 3 S ρϕ |ξ =ξ 2 (10) 4. Difference equations for the node at corners At four corners, the node and its surrounding area are shown in Fig. 6. 0 ( 3) 22 2 2 3 3 44 (a) ϕ = −α , ξ = ξ1 3 3 1 4 4 00 ( 11) 44 1 2 3 11 33 1 1 4 22 33 1 0 ( 4) 22 33 2 2 3 1 4 4 N2 (b) ϕ = α , ξ = ξ1 − g N4 ) hϕ hξ ≈ ∂D ∫ g dξ ≈ (g − g N3 ) N1 2 ∂D 1 ∫∫ g d ξ d ϕ ≈ 4 g 2 ≈ (c) ϕ = −α , ξ = ξ 2 (d) ϕ = α , ξ = ξ 2 g2 − g0 hϕ 4 g1 − g 0 hξ 4 0 hξ hϕ D But − ∫ S ρ d ϕ ≈ (S ρ ) N2 ∂D hϕ 2 hϕ − ∫ S ρϕ d ϕ ≈ ( S ρϕ ) N 2 2 ∂D hξ ∫ S ρϕ d ξ ≈ (S ρϕ ) N 2 1 ∂D C1 Sρ0 + Sρ2 C4 4 − ∫ S ρ |ξ =ξ1 d ϕ = C4 C1 S ρϕ 0 + S ρϕ 2 4 S ρϕ 1 + S ρϕ 0 C4 4 ∂uϕ ∂uϕ ≈ (E ∂D u ρ1 + u ρ 0 4 ∂D +E uϕ1 − uϕ 0 2hϕ +ν S ρ1 + S ρ 0 4 C1 hϕ − ∫ S ρϕ |ξ =ξ1 d ϕ C4 C3 − ∫ S ρϕ |ϕ =−α d ξ = ∫ Eu ρ d ξ + ∫ E ∂ϕ d ξ + ∫νS ρ d ξ ≈ ( Eu ρ + E ∂ϕ ∂D C1 hϕ − ∫ S ρ |ξ =ξ1 d ϕ C4 − ∫ S ρϕ |ξ =ξ1 d ϕ = C3 hξ − ∫ S ρϕ |ϕ =−α d ξ C4 + νS ρ ) N1 hξ 2 1 4 For the node at ϕ = −α , ξ = ξ1 , the integrals of general function g (ϕ , ξ ) are ∫ g dϕ ≈ (g 0 ( 2) 1 4 Figure 6: Node at corners and its surrounding area − 2 C3 ∂uϕ C4 ∂ϕ − ∫ ( Eu ρ + E C3 )hξ − ∫ Sϕ |ϕ =−α d ξ C4 So the difference equations for the node are ⎯ 701 ⎯ + νS ρ ) |ϕ =−α d ξ uρ 2 − uρ 0 hξ uϕ 2 − uϕ 0 hξ Sρ 2 + Sρ 0 hξ +ν uρ 0 +ν + hϕ uρ1 − uρ 0 − uϕ 0 − hϕ − Euρ 0 − E S ρϕ 2 + S ρϕ 0 hξ uϕ1 − uϕ 0 +E 1 −ν 2 Sρ 0 = 0 E 2(1 + ν ) S ρϕ 0 = 0 E uϕ1 − uϕ 0 uρ1 + uρ 0 hϕ − hϕ +E −ν S ρ 0 + S ρϕ1 + S ρϕ 0 hϕ 4 − hξ hϕ (∫ C3 C4 ) C1 S ρϕ |ϕ =−α d ξ + ∫ S ρ |ξ =ξ1 d ϕ = 0 C4 Sρ1 + Sρ 0 2 4 (uϕ1 − uϕ 0 ) + ν + S ρϕ 0 − 2 hϕ hξ hϕ hϕ (∫ C3 C4 C1 Sϕ |ϕ =−α d ξ + ∫ S ρϕ |ξ =ξ1 C4 ⎫ ⎪ ⎪ ⎪ ⎪ ⎪ ⎪ ⎬ ⎪ ⎪ ⎪ ⎪ d ϕ = 0⎪ ⎪⎭ (11) ) The equations for other corners can be established similarly and won’t be listed here anymore. Combining the difference equations of all nodes, whole difference format is constructed. The numerical solution can be obtained for the problem of circular sector domain in polar coordinates. EXAMPLES To verify the effectiveness of the new FDM, calculations are implemented by programming. Two Examples are given here. 1. Example 1 Thick-walled cylinder subjected to inner pressure p=120MPa (Fig. 7). The inner radius is a=50mm, and external radius b=100mm. The properties of materials are E=200GPa, and ν = 0.3 . a p b Figure 7: Thick-walled cylinder subjected to inner pressure This is an Axis-symmetric problem. Taken out from the cylinder by two radial sections whose angle is equal to 10º, a block can be used for calculation. 10 meshes are set here in direction ξ , i.e. hξ = 0.06931 . The numerical results of calculation are listed in Table 1. Table 1 The numerical results of calculation for thick-walled cylinder problem ρ , mm Analytical solution u ρ , mm σ ρ , MPa σ ϕ , MPa u ρ , mm New FDM σ ρ , MPa σ ϕ , MPa 50 0.0590 −120 200 0.0590 −119.53 200.26 53.59 0.0560 −99.29 179.29 0.0559 −99.45 178.85 57.43 0.0533 −81.26 161.26 0.0533 −80.92 161.47 61.56 0.0509 −65.56 145.56 0.0508 −65.69 145.23 65.98 0.0486 −51.90 131.90 0.0487 −51.66 132.07 70.71 0.0467 −40.00 120 0.0466 −40.11 119.75 75.79 0.0449 −29.64 109.64 0.0450 −29.48 109.79 81.23 0.0434 −20.63 100.63 0.0433 −20.72 100.44 87.06 0.0421 −12.78 92.78 0.0421 −12.67 92.90 93.30 0.0409 −5.948 85.95 0.0409 −6.02 85.80 100 0.0400 0 80 0.0400 0.06 80.09 ⎯ 702 ⎯ a b 2. Example 2 Curved beam subjected to equal and opposite forces at two ends (Fig. 8). The inner radius is a=150mm, and external radius b=200mm. The magnitude of the force F =1 kN. The properties of materials are E=200GPa, and ν = 0.3 . O F F Figure 8: Curved beam subjected equal and opposite forces at two ends Taking symmetry into consideration, only the right half of the beam is calculated. 18 meshes are set in direction ϕ and 16 in direction ξ , i.e. hϕ = 0.08727 and hξ = 0.01798 . Assuming u ρ |ϕ =90°, ρ =a = 0 , the calculations for displacements on section ϕ = 0 are listed in Table 2 and the calculations for stresses on section ϕ = 90° in Table 3. Table 2 The calculations of displacements on section ϕ = 0 Analytical solution New FDM ρ , mm u ρ , mm uϕ , mm u ρ , mm uϕ , mm 150 2.0448 0.9372 1.9807 0.9028 155.49 2.0448 1.0187 1.9807 0.9821 161.19 2.0448 1.1023 1.9807 1.0635 167.09 2.0448 1.1885 1.9808 1.1473 173.21 2.0448 1.2774 1.9810 1.2340 179.55 2.0448 1.3697 1.9812 1.3238 186.12 2.0448 1.4655 1.9815 1.4172 192.94 2.0448 1.5654 1.9818 1.5148 200 2.0448 1.6697 1.9823 1.6170 Table 3 The calculations of stresses on section ϕ = 90° Analytical solution New FDM ρ , mm σ ρ , MPa σ ϕ , MPa σ ρ , MPa σ ϕ , MPa 150 0 485.98 0. 34 459.65 155.49 14.71 364.21 14.35 343.43 161.19 24.27 248.08 23.50 232.50 167.09 29.23 136.90 28.27 126.27 173.21 30.06 30.06 29.10 24.16 179.55 27.20 -73.00 26.39 −74.33 186.12 21.02 -172.81 20.51 −169.68 192.94 11.85 -269.82 11.74 −262.32 200 0 -364.48 0.38 −352.63 The numerical results of the examples above show that the new FDM is effective. ⎯ 703 ⎯ CONCLUSIONS A new FDM is introduced into radial symplectic system of elasticity. The format of FDM is constructed, and a new numerical method is provided for plane elasticity in polar coordinates. With dual variables for solution, the new FDM can treat complex boundary conditions better. Displacements and stresses can be obtained directly. The format of new FDM with stress boundary condition is discussed in this paper. The problem with displacement boundary condition can be treated similarly. In the process of constructing the format with integral interpolation method, uniform meshes are chosen and rectangle area is used as the surrounding area of each node. If varied meshes are chosen or polygon area is used, different format of FDM can be constructed. Whether this kind of format has any conservative property needs to be studied further, and its well-posedness should be proved later. REFERENCES 1. Yao Weian, Zhong Wanxie. Symplectic Elasticity. Higher Education Press, Beijing, China, 2002 (in Chinese). 2. Zhong Wanxie. New Solution System of Elasticity. Dalian University of Technology Press, Dalian, China, 1995 (in Chinese). 3. Zhong WX, Xu XS, Zhang HW. On a direct method for the problem of elastic curved beams. Engineering Mechanics, 1996; 13: 1-8 (in Chinese). 4. Zhong Wanxie. Plane elasticity in sectorial domain and the Hamiltonian system. Applied Mathematics and Mechanics (English Edition), 1994; 15: 1113-1123. 5. Yao Weian. Jordan solutions for polar coordinate Hamiltonian system and solutions of paradoxes in elastic wedge. Acta Mechanica Sinica, 2001; 33: 79-86 (in Chinese). 6. Zhang Hongwu, Li Yunpeng, Zhong Wanxie. Stress singularities near corner of wedged dissimilar materials. Journal of Dalian university of technology, 1995; 35: 776-782 (in Chinese). 7. Zhang Hongwu, Zhong Wanxie, Li Yunpeng. The interface crack singularity analysis of the bi-material body based on Hamilton principle. Acta Mechanica Solida Sinica, 1996; 17: 19-30 (in Chinese). 8. Sun Yan, Liu zhengxin, Zhong Wanxie. Analysis and calculation of stress singularity at crack tip of Hamiltonian system. Chinese Quarterly of Mechanics, 2001; 22: 18-23 (in Chinese). 9. Zhou Jianfang, Zhuo Jiashou. A new solution of elasticity in polar coordinate. Acta Mechanica Sinica, 2001; 33: 839-846 (in Chinese). 10. Wang Chenqiang, Zheng Changliang. Semi-analytical finite element method for fictitious crack model in fracture mechanics of concrete. Applied Mathematics and Mechanics (English Edition), 2004; 25: 1265-1270. 11. Wang Chenqiang, Yao Weian. Application of the Hamilton system to Dugdale model in fracture mechanics. Chinese Journal of Applied Mechanics, 2003; 20: 151-155 (in Chinese). 12. Wang Chenqiang, Zheng Changliang. Semi-analytical finite element method for calculation of SIF and CTOD of model II crack. Journal of Dalian University of Technology, 2004; 44: 478-481 (in Chinese). 13. Wang Chenqiang, Zheng Changliang. Analytical formulas for plane crack elements and semi-analytical element method for model I and model II Dugdale models. Engineering Mechanics, 2005; 22: 33-37 (in Chinese). ⎯ 704 ⎯
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