INTERNATIONAL JOURNAL OF MATHEMATICS AND SCIENTIFIC COMPUTING (ISSN: 2231-5330), VOL. 3, NO. 2, 2013 17 Modified Adomian for Linear Partial Differential Equations Ruchi Nigam Abstract—In this paper we outline a strategy to use Adomian decomposition method properly for solving linear partial differential equation with homogeneous and inhomogeneous boundary. Our fundamental goal in this chapter is to present a further insight into partial solutions in the decomposition method, and the resolution of above cases by suitable transformation. The modifications are necessary in order to make the Adomian decomposition method efficient for boundary and initial value problems. The heat equation is chosen as an example and the cases where improper solution can be obtained are discussed. Index Terms—Adomian Laplace Transform. decomposition; Heat while the x equation obtained by inverting the Lx operator gives zero [1]. In a problem suggested by Professor Y. Cherrault [1], we use the same boundary conditions but choose u(x, 0) = x(ℓ − x). Again the x equation gives a zero result. However the t equation ∞ ∑ u = u(x, 0) + L−1 L un (2) x t n=0 equation; u0 = xℓ − x2 u1 = −2t MSC 2010 Codes – 44A10, 35K05 un≥2 = 0 yields u = xℓ − x + 2t which clearly does not satisfy the boundary conditions. The terms above, for m > 0, are I. I NTRODUCTION L 2 m um = [L−1 t Lx ] u(x, 0). ET us look at the possible difficulties in the heat equation ut = uxx , consequently, 0 < x < ℓ, t > 0, u(0, t) = 0, t > 0 u(ℓ, t) = 0, t > 0 u(x, 0) = sinx, 0 < x < ℓ u(x, t) = (1) n=0 u0 = sinx u2 = L−1 t Lx u3 = L−1 t Lx u4 = L−1 t Lx ∞ ∑ n=0 ∞ ∑ n=0 ∞ ∑ n=0 ∞ ∑ n=0 u0 = −tsinx u1 = t2 sinx 2! u2 = − u3 = ∞ ∑ m [L−1 t Lx ] f (x) (4) m=0 Thus, in the usual decomposition notation Lt u = Lx u or ∞ ∑ u = u(x, 0) + L−1 L un , x t u1 = L−1 t Lx (3) t3 sinx 3! t4 sinx 4! where u(x, 0) = f (x). In the case f (x) = x(ℓ − x), we see that the operation L−1 t Lx f (x) annihilates the series in a finite number of terms and the result does not satisfy the boundary conditions. This annihilation of the series was not the case with f (x) = sinx. The resolution of such cases was obtained by Adomian and Rach [1] by appropriate expansion of the initial term without making a priori assumptions about the solution. However, this technique failed to obtain exact solution in the case of initial-boundary value problems with inhomogeneous boundary conditions. A review of previous studies indicates that the difficulty arise while applying adomian decomposition method to partial differential equation with homogeneous and inhomogeneous boundary conditions. Hence we solve (1) using adomian with Laplace. For Adomian decomposition method one can refer to [1], [5], [6]. Applying Laplace both sides of equation (1) d2 u dx2 d2 u pu − x(ℓ − x) = ∞ ∑ dx2 t3 t4 t2 u(x, t) = un = (1 − t + − + − ....) = e−t sinx Solving by using adomian decomposition method 2! 3! 4! n=0 d2 u , Ru = pu, g = −x(ℓ − x), Lu = Ruchi Nigam was research scholar at Department of Mathematics, Indian 2 ∫dx ∫ Institute of Technology Roorkee, Roorkee-247667 and worked as assistant pu(x, p) − u(x, 0) .. . professor at IJCET, Tuticorin, India. Currently she is on child care leave. (E-mail: [email protected]) L−1 [.] x = (6) x1 = [.]dx2 dx1 0 (5) 0 (7) INTERNATIONAL JOURNAL OF MATHEMATICS AND SCIENTIFIC COMPUTING (ISSN: 2231-5330), VOL. 3, NO. 2, 2013 ∫ x ∫ x1 u0 = u(0, p) + xF (p) − x(ℓ − x)dx2 dx1 0 0 ) ( 3 x4 x ℓ = F (p)x − − 3! 3.4 ∫ x ∫ x1 u1 = pu0 dx2 dx1 0 0 ( 5 ) x3 x pℓ x6 p = p F (p) − − 3! 5! 3.4.5.6 ( 7 2 ) 5 x x p ℓ x6 p u2 = p2 F (p) − − 5! 7! 3.4.5.6.7.8 .. . Thus, ) ( p2 x5 px3 + ... u(x, p) = F (p) x + 3! 5! ( 3 ) x px5 p2 x7 − ℓ + + ..... 3! 5! 7! ( 4 ) 6 2 8 x px p x + 2 + + + .... 4! 6! 8! 18 Applying Laplace with adomian as stated above, we get ∫ x ∫ x1 u = u(0, p) + x.ux (0, p) − sin xdx2 dx1 0 0 ∫ x ∫ x1 + pudx2 dx1 (12) 0 0 u0 = F (p).x + sin x px3 − p sin x u1 = F (p) 3! p2 x5 + p2 sin x u2 = F (p) 5! p3 x7 u3 = F (p) − p3 sin x 7! (13) Thus, (8) The value of F (p) = ux (0, p) are found by applying the condition at x = ℓ. Substituting the value of F (p) in (8), we get a series ( 4 ) x px6 p2 x8 u(x, p) = + + .... 12 360 20160 ( 3 ) x px5 p2 x7 + − − − .... ℓ 6 120 5040 ) ( px3 p2 x5 x + + .... ℓ3 + 12 72 1440 ( ) −px p2 x3 p3 x5 + − − .... ℓ5 + ..... (9) 120 720 14400 in closed form above series can be written as √ 1 2 2 cosh{ p(2x − ℓ)/2} u(x, p) = x(ℓ − x) − 2 + 2 (10) √ p p p cosh( pℓ/2) ( ) px3 p2 x5 p3 x7 u(x, p) = F (p) x + + + ... 3! 5! 7! ( ) (14) + sin x 1 − p + p2 − p3 + ... The series is clearly of √ sinh px sin x u(x, p) = F (p) √ + p p+1 Applying boundary conditions at x = 1, we have √ sinh p sin 1 sin 1 F (p) √ + = ⇒ F (p) = 0 p p+1 p+1 (15) Solution in Laplace space is given by u(x, p) = sin x p+1 (16) Taking Laplace inverse, we get u(x, t) = sin xe−t (17) Although the above example can be solved by Adomian also because of the presence of the functions sinx and e−t . But the involvement of all the boundary conditions make laplace approach more reliable and efficient. Taking inverse Laplace Transform, we have Next consider (1) with boundary conditions u(x, 0) = [ 1 (2x − ℓ)2 ℓ2 16 ℓ2 T0 , ux (0, t) = 0, u(ℓ, t) = T1 . It is the case where it is u(x, t) = x(ℓ − x) − 2t + 2 { − } + t − 3 . ×difficult to obtain solution by decomposition method. Such 2 4 4 π 4 ] a problem can be easily solve by using Laplace approach to ∞ 2 2 n ∑ −(2n−1) π t (−1) (2n − 1)π(2x − ℓ)/2 2 /4) 4(ℓ decomposition method. Thus the solution is e cosh 3 (2n − 1) 2.(ℓ/2) n=1 d2 u (11) = pu − T0 dx2 ∫ x ∫ x1 x2 Consider equation (1) with inhomogeneous boundary u0 = − T0 dx2 dx1 + F (p) = −T0 + F (p) 2! conditions u(0, t) = T 1, u(ℓ, t) = T 2, and u(x, 0) = h(x). ( ) ∫ x 0∫ x10 x2 x4 T1 , T2 may be functions or numeric constants. In [1] steady u1 = pu0 dx2 dx1 = p F (p) − pT0 2! 4! state as well as transient solutions are obtained. However, for ( ) ∫0 x ∫0 x1 4 inhomogeneous boundary conditions the result obtained in [1] x x6 2 u = pu dx dx = p F (p) − T 0 2 1 2 1 does not satisfy the boundary conditions. And there was no 4! 6! ( ) ∫0 x ∫0 x1 consideration about the wrong result. We can deal with this dif6 8 x x u3 = pu2 dx2 dx1 = p3 F (p) − T0 ficulty by using Laplace with adomian. For example, consider 6! 8! 0 0 inhomogeneous conditions u(0, t) = 0, u(1, t) = sin 1e−t , and (18) u(x, 0) = sin x. INTERNATIONAL JOURNAL OF MATHEMATICS AND SCIENTIFIC COMPUTING (ISSN: 2231-5330), VOL. 3, NO. 2, 2013 ) ( x4 x6 x2 + p2 ... F (p) 1 + p + p2 2! 4! 6! ( 2 ) 4 6 x x x x8 − T0 + p. + p2 . + p3 . ... (19) 2! 4! 6! 8! u(x, t) = 19 a finite number of terms, we consider the Laplace Transform method. Thus, we have d2 u + L{g(x, t)} (29) dx2 The series is clearly of where L{g(x, t)} denotes the Laplace transform of the function g(x, t). T0 T0 √ √ cosh px + (20) Proceeding as stated above we may obtain the solution. u(x, p) = F (p) cosh px − p p In case of inhomogeneous heat equation with inhomoThe function F (p) has to be determined by applying the geneous boundary condition the equation can be reduced to condition at x = ℓ. Substituting the value, we have homogeneous boundary with the help of the transformation √ stated earlier and hence can be solve. cosh px T0 u(x, p) = (T0 − T1 ) (21) For example, consider the equation (24) where g(x, t) = 2x √ + p cosh pℓ p and boundary conditions u(0, t) = 0, u(1, t) = 0, u(x, 0) = Taking inverse Laplace x − x2 . In this case adomian method provides a solution u(x, t) = 2xt that does not satisfy the boundary conditions. ∞ 4(T1 − T0 ) ∑ (−1)n − (2n−1)22 π2 kt (2n − 1)πx 4t While using the Laplace approach we obtain the series u(x, t) = T1 + e cos ) of the ∑∞ ( n2 π 2 t π 2n − 1 2ℓ n=1 sin nπx. solution u(x, t) = x(1 − x) − π43 n=1 1−en3 (22) Another way of solving inhomogeneous boundary condition problem is by reducing the problem to homogeneous one by applying the transformation introduced in [7], [8]. Let pu = III. CONCLUSION hence with the technique stated above we can obtain the solution. The heat equations are solved Laplace approach to decomposition method. In cases where annihilation of the series is not the case, solution can be obtained by the usual decomposition method. In cases where Lm x operator annihilates the series in a finite number of terms improper solution may be obtained when consider the initial boundary value problems involving inhomogeneous boundary conditions. We overcome the difficulties by using the Laplace approach and the results are successfully obtained. The transformation used in this paper is a simple technique for special cases. However, the powerful Adomian decomposition method can be applied to much more complicated physical problems [2], [3], [4], [5] in comparison with other methods. The above examples are used for clarity and comparison, since they are obviously solvable by separation of variables. In general, the decomposition is more widely applicable. II. I NHOMOGENEOUS HEAT EQUATION R EFERENCES u(x, t) = υ(x, t) + g(x), f (x) = h(x) − g(x) (ℓ − x) x g(x) = T1 + T 2 ℓ ℓ substituting this in the problem yields υt = uxx , 0 < x < ℓ, t > 0, υ(0, t) = 0, t > 0 υ(ℓ, t) = 0, t > 0 υ(x, 0) = f (x), 0 < x < ℓ (23) Consider the inhomogeneous case ut = uxx + g(x, t) (24) u(x, 0) = u(ℓ, t) = u(0, t) = 0 (25) write t equation Lt = Lx + g(x, t) (26) According to adomian decomposition, we have u = u0 + L−1 t Lx ∞ ∑ un , (27) n=0 −1 with u0 = L−1 t g + u(x, 0) = Lt g, since initial condition is zero. m −1 um = (L−1 (28) t Lx ) Lt g are components of u. If annihilation of series is not the case the adomian method is sufficient to obtain the solution. In the cases where Lm x operator acting on g annihilates the series in [1] G. Adomian and R. Rach, “A further consideration of partial solutions in the decomposition method” Comput. Math. Appl. vol. 23, pp. 51–64, 1992. [2] G. Adomian, Nonlinear Stochastic Systems Theory and Applications to Physics, Kluwer, Dordrecht, Holland, 1989. [3] P. Vadasz and S. Olek, “Convergence and accuracy of Adomian’s decomposition method for the solution of Lorenz equations,” Int. J. of Heat and Mass Transfer, vol. 43, pp. 1715–1734, 2000. [4] P. Vadasz, “Local and global transitions to chaos and hysteresis in a porous layer heated from below,” Transport in Porous Media, vol. 37, no. 2, pp. 213–245, 1999. [5] R.C. Mittal and R. Nigam. “Solution of a class of singular boundary value problems,” Numerical Algorithms, vol. 47, pp. 169–179, 2008. [6] R.C. Mittal and R.Nigam. Solution of fractional integro-differential equations by adomian decomposition method, International Journal of Applied Mathematics and Mechanics, vol. 4, no. 2, pp. 87–94, 2008. [7] T. Myint-U, Partial Differential Equations of Mathematical Physics, North-Holland, New York, 1980. [8] R.B. Guenther and J.W. Lee, Partial Differential Equations of Mathematical Physics and Integral Equations, Dover, 1996.
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