Available at http://pvamu.edu/aam Appl. Appl. Math. ISSN: 1932-9466 Applications and Applied Mathematics: An International Journal (AAM) Vol. 05, Issue 2 (December 2010), pp. 585 – 604 (Previously, Vol. 05, Issue 10, pp. 1682 – 1701) Finite Element Analysis in Porous Media for Incompressible Flow of Contamination from Nuclear Waste Abbas Al-Bayati, Saad A. Manaa and Ekhlass S. Ahmed Department of Mathematics University of Mosul Mosul, Iraq profabbasalbayati@yahoo.com Received: March 19, 2010; Accepted: July 28, 2010 Abstract A non-linear parabolic system is used to describe incompressible nuclear waste disposal contamination in porous media, in which both molecular diffusion and dispersion are considered. The Galerkin method is applied for the pressure equation. For the brine, radionuclide and heat, a kind of partial upwind finite element scheme is constructed. Examples are included to demonstrate certain aspects of the theory and illustrate the capabilities of the kind of partial upwind finite element approach. Keywords: Finite element method; Galerkin method; incompressible flow; nuclear waste MSC (2000) No.: 65L60, 74S05, 82D75 1. Introduction The proposed disposal of high-level nuclear waste in underground repositories is an important environmental topic for many countries. Decisions on the feasibility and safety of the various sites and disposal methods is based, in part, on numerical models for describing the flow of contaminated brines and groundwater through porous or fractured media under severe thermal regimes caused by the radioactive contaminants. A fully discrete formulation is given in some detail to present key ideas that are essential in code development. The non-linear couplings between the unknowns are important in modeling the correct physics of flow. In this model one obtains a convection-diffusion equations which represent a mathematical model for a case of diffusion phenomena in which underlying flow is present; 585 586 A. Al-Bayati et al. w and bw correspond to the transport of w through the diffusion process and the convection effects, respectively, where and denoted respectively the gradient operator and the Laplacian operator in the spatial coordinates. The prediction of an accurate numerical solution for the convection dominated flow problem is one of the more difficult tasks in computational fluid dynamics. The central difference method and the conventional Galerkin method have consistently produced unphysical oscillatory solutions. One successful technique for solving such a problem is known as the upwind algorithm, which was originally devised for the finite difference method. In the finite element method, a popular technique known as the streamline upwind Petrov-Galerkin (SUPG) method is used. This method modifies the weighting functions by using the local velocity to dictate an upstream direction of these functions. Such modification eliminates the oscillatory behavior for some convection problems. For more details, see Wansophark and Pramote (2008). In this paper, we have considered the fluid flow in porous media using a Galerkin method for the pressure equation and a kind of partial upwind finite element scheme is constructed for the convection dominated saturation (or concentration) equation, the trace concentration of ith radionuclide and the heat equation. For more details of this subject see Douglas (2001, 2002), Huang (2000) and Chen et al. (2009). 2. Model Equations The model for incompressible flow and transport of contaminated brine in porous media can be described by a differential system that can be put into the following form, Gaohong and Cheng (1999). Fluid: (a) . u q Rs' , k ( x) (b) u (c) P a (c)P. (1) Brine: c u.c .( Ec c) g (c). t (2) Heat: d2 T c p u.T .( EH T ) Q(u, T , c, p ). t Radionuclide: c K i i u.ci .( Ec ci ) fi (c, c1 ,..., cN ), t (3) (4) AAM: Intern. J., Vol. 05, Issue 2 (December 2010) [Previously, Vol. 05, Issue 10, pp. 1682 – 1701] 587 with the boundary conditions ( a ) (b) (c ) ( d ) (e) u.n 0, ( Ec c cu ).n 0, on on ( Ec ci ci u ).n 0, on ( EH T c pTu ).n 0, on p 0, n (5) ( x, t ) (0, T ] and the initial conditions ( a ) (b) ( c ) (d ) p( x, 0) p0 ( x); x , c( x, 0) c0 ( x); x , ci ( x, 0) c0i ( x); x , T ( x, 0) T0 ; x , (6) where n is the unit outer normal to , x R 2 , t (0, T ] ; u is the Darcy velocity; P is 1 cw , q q( x, t ) is the production term; the pressure; Rs' Rs' (c) [c sK s f s /(1 cs )](1 c) is the salt dissolution term; k(x) is the permeability of the rock; (c) is the viscosity of the fluid, c dependent upon c , the concentration of the brine in the fluid and T is the temperature of the fluid, d 2 c p (1 ) R c pR , EH Dc pw K m' I , K m' km / 0 , D ( Dij ) (T u ij ( L T )ui u j / u ), and Q(u , T , c, p ) {[U 0 c p T0 ].u [U 0 c p (T T0 )) ( p / )][ q Rs' ]} qL qH qH . Ec D Dm I , and g(c) -c{[csK s f s /(1 c s )](1 c)} qc Rs' , c i is the trace concentration of the i-th radionuclide, and f i (c, c1 , c2 ,..., c N ) ci {q [csK s f s /(1 cs )](1 c)} qci qci qoi N k ij j K jc j i K ici . j 1 The reservoir will be taken to be of unit thickness and will be identified with a bounded domain in R 2 . We shall omit gravitational terms for simplicity of exposition, no significant mathematical questions arises the lower order terms are included. 588 A. Al-Bayati et al. We assume that: (A1) a (c), Rs' (c), g (c), f i (c, c1 ,....., c N ), Q(u , T , c, p ) C01 ( R ) , ( x), K i , d 2 H ' (), q L (0, T ; H 1 ()) 0 c0 a (c) , Rs' (c), g (c), ( x), f i (c, c1 ,..., cn ), K i , d 2 , Q(u , T , c, p ) c1 , c R, x Dm 0 , l t 0 (A2) The solution of the problem (1-6) are regular: C ( x, t ) L2 (0, T ; H 2 ()) L (0, T ; w' ()) Ci ( x, t ) L2 (0, T ; H 2 ()) L (0, T ; w' ()) P( x, t ) L (0, T ; H r 1 ()) , (r 2) ct , ctt , cttt L (0, T ; H 1 ()) ; pt , ptt L (0, T ; L ()) (A3) For any L () , the boundary values problem: , x x , 0, n 2 there exists unique solution H 2 () and a positive constant M such that 2 M [Manaa (2000)]. 3. Finite Element Spaces Consider a regular family {Th } of triangulation defined over , where h is the longest diameter of a triangular element with the triangular Th , we have a set of close triangles {ei }(1 i N e ) and a set of nodes {Pi }(1 i N P M P ) where Pi (1 i N P ) are interior nodes in and Pj ( N P 1 j N P M p ) are boundary nodes on . We put hs to be the maximum side length of triangles and k to be minimum perpendicular length of triangles for all e Th . Definition 3.1. A family Th constant of triangulations is of weakly acute type, if there exists a 0 0 independent of h such that, the internal angle of any triangle ei Th satisfies 0 2 . Definition 3.1.1. Let i ( p), (1 i M ), be the continuous function in s.t. i ( p), is linear on each e Th and i ( p j ) ij for any nodal point pj.. We denote Mh be the linear span of i , (1 i M ), i.e., a finite dimensional subspace of H 1 () and defined by: M h {z h | C (); z h is a linear function on e , e Th } . Also, define a subspace of H 01 () be: M 0 h {zh | zh M h ; zh ( Pk ) 0, k M 1,..., K } . AAM: Intern. J., Vol. 05, Issue 2 (December 2010) [Previously, Vol. 05, Issue 10, pp. 1682 – 1701] 589 We associate the index set { j i : Pj is adjacent to Pi } . Let Pi Pj Pk , be three vertices of triangular element e and i , j , k be barycentric coordinates. We have the following definitions [see Hu and Tian (1992)]. Definition 3.2. With each vertex Pi belonging to triangle e, the barycentric subdivision ie is given by: ie {P | P e ; i ( P) j ( P) , i ( P) k ( P), Pj e} , and the barycentric domain i associated with vertex Pi in is given by i ie , e Th . Definition 3.3. With the characteristic function i ( x) of barycentric domain i , the mass lumping operator : w C () wˆ L () is defined by wˆ ( p ) NP M P w( pi ) i ( p ) . i Using interpolation theory in Sobolev space [Ciarlet (1978)] and inverse inequality, with step-length hc , we have the relation between ŵ and w from the following lemma: Lemma 3.1. There exists a constant C such that: w wˆ o , p Chc w 1, p , wh 1 Mhc1 wh , w M h , p 1 (7) wh M 0 h . (8) Lemma 3.2. There exist constants C1 ,C2 0 such that: C1 w 0, p wˆ 0, p C2 w 0, p , w M h . (9) Definition 3.4. Let {M h } be a family of finite dimensional subspaces of C () , which is piecewise polynomial space of degree less or equal to r with step length hP and the P [1, ], r 2 , there exists a constant M such that for following property: for r 1 0 q 2 and wP () : inf x x{ M h } q, p Mh r 1q r 1, p . Similarly, we define {N h } be a family of finite-dimensional subspace of C () C () , which is piecewise polynomial space of degree less or equal to r-1 with the similar property as Mh and 0 q r 1. We also assume the families {M h } and {N h } satisfy inverse inequalities: L MhP1 , [Manaa (2000)]. L MhP1 , M h (10) 590 A. Al-Bayati et al. 4. Error Estimates Let 0 is time step and N T . We use a Galerkin finite element method for the pressure and velocity and partial upwind finite element scheme for brine, radionuclide, and heat. Let C 0 M h be a L2 () - projection of c 0 in M h : (c 0 C 0 , z h ) 0 z h M h . We can get P 0 Vh such that k ( x) P 0 , v) (q 0 , v) ( Rs' , v) , v Vh and U 0 Wh from 0 ) P dx 0 , ( (c 0 U0 k ( x) P 0 a (C 0 )P 0 0 (C ) If the approximate solution {P m ,U m , C m , Cim (i 1,2,..., N ), T m } Vh Wh M h M hN Rh is known, we want to find {P m1 ,U m1 , C m1 , Cim1 (i 1,2,..., N ),T m1} Vh Wh M h M hN Rh at t t m 1 , with five steps . Let (.,.) denote the inner product in L () 2 Step 1. Find Cm+1for m 0 ,1, ,N 1, such that (ˆD Cˆ m , zˆh ) ( Ec C m1 / 2 , z ) R (U m , C m1 / 2 , z h ) ( gˆ (C m1 / 2 ), zˆ h ) z h M h , (11) where D C m (C m1 C m ) / , C m1 / 2 (C m1 C m ) / 2 and with zi z h ( Pi ) , Cim 1 / 2 C m 1 / 2 ( Pi ) , and ijm U m .nij d , here nij is the unit outer normal to ij . ij The partial upwind coefficients should be required that [Hu and Tian (1992)]. (a ) ijm mji 1 (b) max{1/ 2,1 ij1} ij 1, if ij 0, max{1/ 2,1 ij1} ji 1, if ij 0. Step 2. Find Cim1 , for m 0 ,1, ,N 1 , such that: (12) AAM: Intern. J., Vol. 05, Issue 2 (December 2010) [Previously, Vol. 05, Issue 10, pp. 1682 – 1701] (ˆ Kˆ i D Cˆ im , zˆh ) ( Ec Cim 1 , z ) R(U m , Cim 1 , zh ) ( fˆi (C m 1/ 2 , C1m 1 ,..., CNm 1 ), zˆh ) zh M hN , where 591 (13) M R (U m , Cim 1 , zh ) zi ijm ( ijmCim 1/2 mji C mj 1/2 ) . i 1 ji Step 3. Find Tm+1 such that: (d 2 D Tˆ m , rˆh ) ( E H T m 1/2 , rh ) R (c pU m , T m 1/2 , rh ) (Qˆ (U m , T m , C m , P m ), rˆh ) (14) rh Rh , where M R(c pU m , T m1 / 2 , rh ) ri ijm ( ijmTi m1/ 2 mjiT jm1/ 2 ) . i 1 ji Step 4. Find Pm+1 such that: P m 1 dx 0 , ( k ( x) (C m1 ) P m1 , v) ( q m1 , v) ( Rs' , v) , v Vh . (15) Step 5. Find Um+1 as: U m 1 k ( x) P m 1 a (C m 1 )P m 1 . m 1 (C ) (16) Lemma 4.1. Let p Vh be the elliptic projection of p H 1 () into Vh defined by (a(c)p, v) (a(c)p, v) , v Vh . Then, there exists a constant k1 such that r 1 p p h p p p k1 p r 1 h p . Proof: See Quarteroni and Valli (1997). Some Important Remarks: 1. U m1.n 0 in . 2. If U l u l ChP (0 l m) , then U m1 u m1 ChP . (17) 592 A. Al-Bayati et al. and if U m u m ChP , then U m C1 . (18) 3. We will make the inductive assumption that if U l U m1 L L k * (0 l m) , then k* (19) 4. From Manaa (2000), if Th is regular triangulation of weakly acute type we have wh 1 6 / k wˆ h , wh M h (20) Theorem 4.1. C satisfies discrete mass conservation law ˆ D Cˆ m d gˆ m 1/2 (C )d , m 1, 2, , N . (21) Proof: In (10), let z h 1 , then ( EcC m1 / 2 , 1) 0 and M M R(U m , C m1 / 2 ,1) 1 ijmCijm1 / 2 i 1 j i eTh ( m ij Cijm1 / 2 ijmCijm1 / 2 ) 0 . pi , p je ,i ji Then (21) holds. Theorem 4.2. Ci satisfies discrete mass conservation law ˆKˆ D Cˆ i m i d f i m1 / 2 d , i 1,2,...., N Proof: Same as Theorem 4.1. Lemma 4.2. Let c :[0, t ] M h and ci :[0, t ] M hN , i 1,..., N such that ( Ecc c , z ) (c c , z ) 0, z M h , ( Ec(ci ci ), z ) ((ci ci ), z ) 0, z M hN , t J (22) AAM: Intern. J., Vol. 05, Issue 2 (December 2010) [Previously, Vol. 05, Issue 10, pp. 1682 – 1701] 593 and let c c , ci ci i , then, 1 Mhc , Mhc2 , t t i 1 Mhc , i Mhc2 , i t t Mhc 1 and Mhc . 1 Proof: See Ciarlet (1978). Lemma 4.3. For all zh M h and c c , c C , 2 ((u m .c m 1/2 ), zh ) R(U m , C m 1/2 , zh ) M (hc2 m 1/2 m 1/ 2 2 2 m 1/ 2 u m U m zh 2 2 2 ) z h , where 0 is arbitrary small constant. Proof: ((u m .c m 1/2 ), zh ) R(U m , C m 1/ 2 , zh ) ((u m U m ).c m 1/2 , zh ) (U m(c m 1/2 C m 1/2 ), zh ) (U m .C m 1/2 , zh zˆh ) [(U m .C m 1/2 , zˆh ) R (U m , C m 1/2 , zh )] J 1 J 2 J 3 J 4. With (A1) and (A2) we have: J 1 ((u m U m ).c m 1/2 , zh ) M u m U m . zh 2 2 M ( u m U m zh ). Using (A1), (19), (20) and (9) we have: (23) 594 A. Al-Bayati et al. J 2 (U m .(c m 1/2 C m 1/2 ), zh ) M [ (c m 1/2 c m 1/2 ) (c m 1/2 C m 1/2 ) ]. zh M [ m 1/2 m 1/ 2 ]. zh M[ 6 m 1/2 2 6 m 1/2 2 ] M zh ˆ k k 2 2 2 2 M ( m 1/ 2 m 1/2 zh ). From (A2), (19), (20), (7) and (8) we have J 3 (U mC m 1/2 , zh zˆh ) M U m C m 1/2 . zh zˆh M m 1/2 zh zˆh M m 1/2 zh zˆh M c m 1/ 2 zh zˆh k1 k2 k3 2 2 k1 M [hc2 m 1/2 ] zh 2 2 k2 M [hc2 m 1/2 zh ] 2 k3 M [hc2 zh ] 2 2 2 2 J 3 M [hc2 m 1/2 m 1/2 zh ] zh . Using (11), (9), (18) and (19) implies J4 M z (C m 1 / 2 i i 1 Cijm1/ 2 )U m .nij d C m1 / 2 .U m zˆh . ji ij Since Cijm1/ 2 ijm Cim1/ 2 mji C mj1/ 2 , J4 eTh P Pje ,i j ( zi z j ) (C m1 / 2 Cijm1 / 2 )U m .nij d ije M C m1 / 2 c m1 / 2 c m1 / 2 c m1 / 2 c m1 / 2 zˆh M h e ( z h e ) eTh (C m 1 / 2 Cijm1 / 2 )d PiPj e ,i j e ij M [ m1 / 2 m1 / 2 c m1 / 2 ] z h and in element e we have C m1/ 2 Cijm1/ 2 2 (C m1/ 2 e) he , then J 4 3M 2 he3 ( zh e) . (C m 1/2 e) M [ m 1/2 m 1/2 c m 1/2 ] zh eTh AAM: Intern. J., Vol. 05, Issue 2 (December 2010) [Previously, Vol. 05, Issue 10, pp. 1682 – 1701] M (hc2 m1 / 2 2 m 1 / 2 2 m 1 / 2 2 2 595 2 z h ) z h / Hence, J1+J2+J3+J4 Implies (23). Lemma 4.4. For all z h M h and i ci ci , i ci Ci , 2 ((u m .ci m 1/2 ), zh ) R(U m , Ci m 1/ 2 , zh ) M (hc2 i m 1/2 i m 1/2 2 2 i m 1/2 u m U m zh 2 2 2 ) z h , (24) where 0 is arbitrary small constant. Proof: ((u m .ci m 1/2 ), zh ) R (U m , Ci m 1/2 , zh ) ((u m U m ).ci m 1/ 2 , zh ) (U m(ci m 1/2 Ci m 1/2 ), zh ) (U m .Ci m 1/2 , zh zˆh ) [(U m .Ci m 1/2 , zˆh ) R(U m , Ci m 1/2 , zh )] J 1 J 2 J 3 J 4. Same as Lemma 4.3. Lemma 4.5. There exists a positive constant k2 such that: P m1 P m1 k 2 C m1 c m1 (25) Proof: We have (a (C m 1 )P m 1 , ) ( q m 1/ 2 , v) ( Rs' (C m 1 ), v), (26) (a(c m 1 )p m 1 , ) (q m1/2 , v) ( Rs' (c m1 ), v). (27) subtracting (27) from (26), we get (a (C m 1 )( P m 1 P m 1 ), ) ([a(C m 1 ) a(c m 1 )]P m 1 , ) ( Rs' (C m 1 ) ( Rs' (c m 1 ), v) Let P m1 P m1 Vh , then 2 ( P m 1 P m 1 ) (a (C m 1 )( P m 1 P m 1 ), ( P m 1 P m 1 )) ([a (c m 1 ) a (C m 1 )]P m 1 , ( P m 1 P m 1 )) ( Rs' (C m 1 ) ( Rs (c m 1 ), P m 1 P m 1 ) . 596 A. Al-Bayati et al. Using (A1), we have M P m 1 C m 1 c m 1 ( P m 1 P m 1 ) C m 1 c m 1 P m 1 P m 1 with lemma 4.1 and (A2) if hP >0 is sufficiently small P m1 P m1 k1 P r 1 hPr M , so we have (25). Lemma 4.6. There exists a positive constant k3 such that U m1 u m1 k3 ( C m1 c m1 hPr ) (28) Proof: U m1 u m1 a (C m1 )P m1 a (c m1 )P m1 a (C m1 )( P m1 p m1 ) a (C m1 ) a (c m1 ) p m1 . From (A1) and (A2) , we have const. P m1 p m1 C m1 c m1 p m1 L we have P m1 p m1 P m1 p m1 P m1 p m1 . Using Lemma 4.1 and Lemma 4.5, we get P m1 p m1 k 2 C m1 c m1 k1 P m1 r 1 h pr , from (A2), (28) holds. Theorem 4.3. For all m l N if 0 , then c l 1 C l 1 M ( hc hPr ) , where M independent of and hc . Proof: Multiply (2) by zh and integrating by parts to obtain t (m 1 / 2) . Let wm1/ 2 w(., (m 1 / 2) ) and wm1/ 2 ( wm1 wm ) / 2 . Then, AAM: Intern. J., Vol. 05, Issue 2 (December 2010) [Previously, Vol. 05, Issue 10, pp. 1682 – 1701] 597 ( D c m , zh ) ( Ecc m 1/2 , zh ) (u m c m 1/2 , zh ) c m 1/ 2 ), z h ) t (( Ecc m 1/2 Eccm 1/2 ), zh ) ( (u m c m 1/2 u m1/2 cm 1/ 2 ), zh ). ( g (c m 1/2 ), zh ) ( ( D c m (29) Let e c C (c c ) (C c ) . Subtract (10) from (29), to obtain: (ˆ D eˆ m , zˆh ) ( Ecem 1/2 , zh ) ( R (U m , C m 1/2 , zh ) (u mc m 1/2 , zh )) ((ˆ D cˆ m , zˆh ) ( D c m , zh )) c m 1/2 ) , zh ) t (( Ecc m 1/2 Eccm 1/2 ), zh ) ( (u mc m 1/2 u m1/2 cm 1/2 ), zh ). (( g (c m 1/2 ), zh ) ( gˆ (C m 1/2 ), zˆh )) ( ( D c m Hence, (ˆ D ˆ m , zˆh ) ( Ec m 1/ 2 , zh ) (ˆ D ˆ m , zˆh ) ( Ec m 1/2 , zh ) ((u mc m 1/2 , zh ) R (U m , C m 1/2 , zh )) (( g (c m 1/ 2 ), zh ) ( gˆ (C m 1/2 ), zˆh )) ( ( D c m , zh ) (ˆ D cˆ m , zˆh )) (( ( D c m c t m 1/ 2 ) , zh ) (( Ecc m 1/2 Eccm 1/2 ), zh ) ( (u mc m 1/2 u m1/2 cm 1/2 ), zh ) I1 I 2 I 3 I 4 I 5 I 6. In (30) , let zh m1 / 2 M h , and using (A1) the Left Hand Side (LHS) is 2 ˆ ˆ m1 ˆ m 2 2 2 c0 m1 / 2 . From (A1), we have: I1 (ˆD ˆ m , zˆh ) M ( D ˆ m 2 2 ˆ m1 / 2 . Using (7) and (8), we have D ˆ m D m D m D ˆ m D m Mhc D m . 1 From (9) we have ˆ m1 / 2 M m1 / 2 M ( m1 m ) 2 I1 M ( m1 m 2 D m 2 2 hc2 D m ) . 1 (30) 598 A. Al-Bayati et al. 2 2 Using (A1), we have I 2 M m 1 / 2 m 1 / 2 . From Lemma 4.3, 2 I 3 M (hc2 m 1/2 m 1/2 2 2 2 2 m 1/ 2 u m U m ) m 1/2 . Let c m1 c m Girault (1979))] ( c t m1/ 2 1 / 24 3c t 3 2 ) . Using (A1), (A2) we get [Raviart and I 4 Mhc (1 2 ) z h 1 Mhc (1 2 ) z h Mhc z h Mhc z h 1 Mhc 2 z h Mhc 2 z h 1 2 M (hc2 hc2 4 ) m1/ 2 2 2 2 I 5 M (hc2 m1 / 2 m1 / 2 ) m1 / 2 . Let I6=K1+K2+K3. So, 2 2 K1 M ( 4 m 1 m ), 2 K 2 M 2 m 1/2 , 2 2 K 3 M ( 2 m 1 m ). Then, we get I 6 M ( 2 m1 2 m 2 ) m1 / 2 . Relation (30) can be written now as 2 ˆ ˆ m 1 ˆ m 2 2 2 2 2 2 c0 m 1/2 M ( m 1 m D m hc2 D m m 1 1 2 2 2 2 m 1/2 m 1/2 u m U m hc2 2 ) m 1/2 . Take the summation from 0 to l, where m l N , and C 0 c 0 so 0 0 2 AAM: Intern. J., Vol. 05, Issue 2 (December 2010) [Previously, Vol. 05, Issue 10, pp. 1682 – 1701] l 1 2 ˆ ˆ l 1 M 1 m M 2 D 2 2 L2 ( L2 ) M 2 hc2 D 2 m 0 l 599 l L2 ( H 1 ) M 2 1 M 2 (hc2 2 ) M 3 u m U m 2 m 0 2 m 0 Where w 2 L2 ( x ) N wm . 2 m 0 x Using (7) and (A1), we get 6 ˆ l 1 l 1 ˆ l 1 Mhc l 1 ˆ l 1 Mhc M ˆ l 1 k 1 ˆ ˆ l 1 M 0 ˆ l 1 , so l 1 2 l l 1 M 1 m M 3 u m U m M 2 ( D 2 2 m0 m 0 2 L2 ( L2 ) hc2 D 2 L2 ( H 1) 2 L2 ( H 1 ) (31) h ). 2 c 2 From Lemma 4.6, we have l m 0 2 l u m U m M ( m 2 2 L2 ( L2 ) h p2 r ) m0 From (31) and (32), we have l 1 l 1 M 1 m M 2 (hc2 2 h p2 r ) . 2 2 m 0 From Gronwall inequality, we get: l 1 M (hc hPr ) . It is c l 1 C l 1 M (hc hPr ) . Theorem 4.4. For all m l N if 0 , then ci l 1 Ci l 1 M ( hc hPr ) , where M independent of and hc . (32) 600 A. Al-Bayati et al. Proof: Multiply (4) by zh and integrate by parts to obtain t (m 1 / 2) . Let wm1/ 2 w(., (m 1 / 2) ) and w m1/ 2 ( w m1 w m ) / 2 . Then ( K i D ci m , zh ) ( Ecci m 1/2 , zh ) (u m ci m 1/2 , zh ) ( fi (c m 1/2 , c1m 1/2 ,..., cNm 1/ 2 ), zh ) ( Ki ( D ci m ci t m 1/ 2 (33) ), zh ) (( Ecci m 1/2 Ecci ,m 1/2 ), zh ) ( (u m ci m 1/ 2 u m1/2 ci ,m 1/2 ), zh ). Let e ci Ci (ci ci ) (ci Ci ) i i . Subtract (10) from (33) to obtain: (ˆ Ki D eˆi m , zˆh ) ( Ecei m 1/2 , zh ) ( R(U m , Ci m 1/2 , zh ) (u m ci m 1/ 2 , zh )) ((ˆ D cˆi m , zˆh ) ( D ci m , zh )) ( ( fi (c m 1/2 , c1m 1/2 ,..., cNm 1/2 ), zh ) ( f i (C m 1/ 2 , C1m 1/2 ,..., C Nm 1/2 ), zˆh )) ( Ki ( D ci m ci t (( Ecci m 1/ 2 Ecci ,m 1/2 ), zh ) ( (u mci m 1/2 u m1/2 ci ,m 1/2 ), zh ). Hence, (ˆ Kˆ i D ˆi m , zˆh ) ( Eci m 1/2 , zh ) (ˆ Kˆ i D ˆi m , zˆh ) ( Ec i m 1/2 , zh ) ((u mc m 1/2 , z ) R (U m , C m 1/2 , z )) (( fˆ (C m 1/2 , C m 1/2 ,..., C m 1/2 ), zˆ ) i h i h i 1 N h ( f i (c m 1/2 , c1m 1/2 ,..., cNm 1/2 ), zh )) ( K i D ci m , zh ) (ˆ K i D cˆi m , zˆh )) ci m 1/2 Ecci ,m 1/2 ), zh ) m 1/2 ) , z h ) (( Ecci t ( (u m ci m 1/ 2 u m1/2 ci ,m 1/2 ), zh ) I1 I 2 I 3 I 4 I 5 I 6. (( ( D ci m The rest of the proof is the same as in Theorem 4.3. Theorem 4.5. With the assumption (A1)~ (A3), if hc O(hP ), O(hP ) , then cC L ( l 2 ) u U L ( l 2 ) M ( hc hPr ) . Proof: We will prove, first the inductive assumption (19). We have (34) m 1/2 ), zh ) AAM: Intern. J., Vol. 05, Issue 2 (December 2010) [Previously, Vol. 05, Issue 10, pp. 1682 – 1701] U m1 L a (C m ) L P m1 L k 4 P m1 L 601 . But, P m 1 L P m 1 P m 1 L P m 1 When hc o(hP ) , o(hP ) (r 2) , L MhP1 P m 1 P m 1 k5 2k5 . P m1 L k *, U m1 u m1 k 3 ( C m1 c m1 hPr ) , m 0,1,..., N (35) and from Theorem 4.3, c m1 C m1 M (hc hPr ) , m 0,1,..., N . (36) Equations (35) and (36) implies c m1 C m1 u m1 U m1 M ( hPr hc ) , m 0,1,..., N . This will complete the proof. 5. Numerical Applications Example 5.1. A two dimensional diffusion-convection problem of interest is concerned with a description of sediment transport in channels. The governing differential equation is [Smith et al. (1973)]: dx c c c 2c 2c d ux uy y 2 2 x y t x y , where c is the sediment concentration, dx and dy are the sediment diffusion coefficients ,ux and uy are the fluid velocity component in the x and y directions. The boundary conditions of the problem are c u y c M 1c, y d y c u y M2 y d y (M 1 is constant), at y 0, (M 2 is constant), at y -56.0. We use a Kind of upwind finite element method to solve this problem with the mesh as triangular element with 82 nodes and take the values ux=1. E-6, uy=0.49 , dx=0, dy=0.0135, 602 A. Al-Bayati et al. we take the time step τ=300 and the number of time steps Nτ =30 for θ =1 ,the time step τ=100 and the number of steps Nτ =90 for θ = 1/2 , and also the time step τ=300 and the number of steps Nτ =30 for θ = 2/3 . In figure (5.1) we show that we can solve this problem by decreasing the time step τ and increasing the number of time steps Nτ for a kind of partial upwind finite element method. Example 5.2. In this example, we solve a purely convective problem in one dimension [Smith et al. (1973)]: u y c c , y t where c is the concentration in the region 2 y 0 , subject to the boundary conditions c 1, y 0, 0 t 0.2, c 0, c 0, y y 0, t 0.2, y 2, for all t. We discretized this region into 200 triangular elements with 202 nodes and with the same distance between any two nodes is 0.02 in both directions x and y, and take uy =1.0, the time step τ=0.04 and the number of time steps Nτ =25 for θ =0.5. Figure (5.2) shows the computed solution after one second and it draws between the concentration and coordinate y, we can see that while y convergence to zero the value of concentration convergence oscillation to solution. 1.00 Y=-56 =1, 0.80 =0.5, Concentration =2/3, =300, =30 =100, =90 =300, =30 0.60 =0.5, =300, =30 Y=-28 0.40 0.20 Y 0 0.00 0.00 40.00 80.00 120.00 160.00 Time (minutes) Figure 5.1. A kind of partial upwind F.E.M. for triangular element at Different values of θ in Example 5.1. AAM: Intern. J., Vol. 05, Issue 2 (December 2010) [Previously, Vol. 05, Issue 10, pp. 1682 – 1701] 1.20 Exact solution at t=1 second 603 A kind of partial upwind FEM Galerkin method for triangular element 0.80 Concentration Galerkin method for quadrilateral element 0.40 0.00 -0.40 -2.00 -1.60 -1.20 -0.80 -0.40 0.00 Coordinate Y Figure 5.2. Solutions in Example 5.2 after one second for θ =0.5, τ =0.04 , Nτ =25 6. Conclusions We used the system with large coupled of strongly non-linear partial differential equations arising from the contamination of nuclear waste in a porous media. For the incompressible case the method satisfied the discrete mass conservation law for approximate C , Ci and ~ derived the error estimates in L (0, T , L2 ()) . The two examples included clearly demonstrate certain aspects of the theory and illustrate the capabilities of a kind of partial upwind F.E.M. Acknowledgement The author would like to thank the editor and, especially, the reviewers for their valuable comments. 604 A. Al-Bayati et al. REFERENCES Ciarlet, P.G. (1978). The finite Element Method for Elliptic Problems. North-Holland, Amsterdam, New York. Chen, M.-C.; Hsieh, P. W.; Li, C.T.; Wang, Y.T. and Suh-Yuh Y. (2009). On two iterative leastsquares finite element schemes for the incompressible Navier-Stokes problem. Numerical Functional Analysis and Optimization, 30, 436-461. Gaohong, W. and Cheng A. 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