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A STUDY OF SIMPLIFIED SHALLOW WATER WAVES: ASSESSMENT OF ADOMIAN’S DECOMPOSITION METHOD<br />
FOR THE ANALYTICAL SOLUTION<br />
Mehdi Safari<br />
The operat<strong>in</strong>g with the operator<br />
1<br />
0<br />
(()()())<br />
1<br />
L on both sides of Eq. (18) we have<br />
u f L g t R u F u , (20)<br />
where f<br />
0<br />
is the solution of homogeneous equation<br />
Lu 0 , (21)<br />
<strong>in</strong>volv<strong>in</strong>g the constants of <strong>in</strong>tegration. The <strong>in</strong>tegration constants<br />
<strong>in</strong>volved <strong>in</strong> the solution of homogeneous equation ( 21) are to be<br />
determ<strong>in</strong>ed by the <strong>in</strong>itial or boundary condition accord<strong>in</strong>g as the<br />
problem is <strong>in</strong>itial-value problem or boundary-value problem.<br />
The ADM assumes that the unknown function u ( x ,) t can be<br />
expressed by an <strong>in</strong>f<strong>in</strong>ite series of the <strong>form</strong><br />
<br />
u ( x ,)( t ,) u<br />
n<br />
x t , (22)<br />
n 0<br />
and the nonl<strong>in</strong>ear operator F () u can be decomposed by an <strong>in</strong>f<strong>in</strong>ite<br />
series of polynomials given by<br />
<br />
F () u An<br />
, (23)<br />
n 0<br />
where u<br />
n<br />
( x ,) t will be determ<strong>in</strong>ed recurrently, and An<br />
are the socalled<br />
polynomials of u<br />
0, u1,..., u<br />
n<br />
def<strong>in</strong>ed by<br />
n<br />
1 d <br />
An F () , u 0,1, n2...<br />
<br />
n<br />
n ! d <br />
<br />
<br />
<br />
i<br />
<br />
i <br />
n 0 <br />
0<br />
(24)<br />
ADM IMPLEMENT FOR FIRST MODEL OF SHALLOW<br />
WATER WAVE EQUATION<br />
We first consider the application of ADM to first model of shallow<br />
water wave equation. If Eq. (2) is dealt with this method, it is <strong>form</strong>ed as<br />
L u L u 4uL u 2L u L udx L u,<br />
(25)<br />
t<br />
where<br />
xxt<br />
t<br />
3<br />
<br />
<br />
L t<br />
, L x<br />
, L xxt<br />
,<br />
2<br />
t x x<br />
t<br />
If the <strong>in</strong>vertible operator<br />
L<br />
1<br />
t<br />
x<br />
t<br />
x<br />
t<br />
dt<br />
0<br />
x<br />
(26)<br />
is applied to Eq. 25, then<br />
L L u L<br />
1<br />
t<br />
t<br />
1<br />
t<br />
( L<br />
is obta<strong>in</strong>ed. By this<br />
xxt<br />
u(<br />
x,<br />
t)<br />
u(<br />
x,0)<br />
L<br />
u 4uL u 2L u<br />
1<br />
t<br />
( L<br />
xxt<br />
t<br />
x<br />
<br />
x<br />
u 4uL u 2L u<br />
t<br />
x<br />
L udx L u),<br />
<br />
x<br />
t<br />
x<br />
L udx L u),<br />
t<br />
x<br />
(27)<br />
(28)<br />
is found. Here the ma<strong>in</strong> po<strong>in</strong>t is that the solution of the decomposition<br />
method is <strong>in</strong> the <strong>form</strong> of<br />
u ( x,<br />
t)<br />
un<br />
( x,<br />
t)<br />
, (29)<br />
n0<br />
Substitut<strong>in</strong>g from Eq. 29 <strong>in</strong> 28, we f<strong>in</strong>d<br />
<br />
<br />
n0<br />
<br />
<br />
<br />
<br />
L ( , ) 4 ( , ) ( , )<br />
1<br />
0<br />
0<br />
0<br />
( , ) ( ,0)<br />
<br />
<br />
<br />
xxt <br />
un<br />
x t <br />
un<br />
x t Lt<br />
<br />
un<br />
x t <br />
n<br />
n<br />
n<br />
<br />
u<br />
n<br />
x t u x Lt<br />
<br />
, (30)<br />
<br />
x<br />
<br />
<br />
<br />
2 ( , )<br />
( , )<br />
( , ) <br />
Lx<br />
<br />
un<br />
x t <br />
Lt<br />
<br />
un<br />
x t dx<br />
Lx<br />
<br />
un<br />
x t <br />
n0<br />
n0<br />
n0<br />
<br />
is found.<br />
Accord<strong>in</strong>g to Eq.19 approximate solution can be obta<strong>in</strong>ed as follows:<br />
<br />
2 1 c 1<br />
<br />
( c 1)sech<br />
x<br />
2 c<br />
u0<br />
( x,<br />
t)<br />
<br />
<br />
,<br />
2c<br />
1 c 1<br />
c 1<br />
( c 1)s<strong>in</strong>h<br />
<br />
x<br />
2<br />
t<br />
1(<br />
, )<br />
c c<br />
x t <br />
,<br />
<br />
3 1 c 1<br />
<br />
2c<br />
cosh <br />
x<br />
2<br />
c <br />
(31)<br />
u (32)<br />
t<br />
<br />
(33)<br />
u2( x,<br />
t)<br />
( Lxxtu1<br />
4u1Lt<br />
u1<br />
2Lxu1<br />
Lt<br />
u1dx<br />
Lxu1<br />
) dt,<br />
0<br />
Thus the approximate solution for first model of shallow water wave<br />
equation is obta<strong>in</strong>ed as<br />
u x,<br />
t)<br />
u ( x,<br />
t)<br />
u ( x,<br />
t)<br />
u ( x,<br />
) , (34)<br />
(<br />
0 1<br />
2<br />
t<br />
The terms u0 ( x,<br />
t),<br />
u1(<br />
x,<br />
t),<br />
u2<br />
( x,<br />
t)<br />
<strong>in</strong> Eq.34, obta<strong>in</strong>ed from<br />
Eqs.31, 32, 33. In Fig.1 the first model of shallow water wave equation<br />
with the first <strong>in</strong>itial condition (31) of Eq. (2) when c=2 has been shown.<br />
ADM IMPLEMENT FOR SECOND MODEL OF SHALLOW<br />
WATER WAVE EQUATION<br />
Now we consider the application of ADM to second model of shallow<br />
water wave equation. If Eq. (3) is dealt with this method, it is <strong>form</strong>ed as<br />
x<br />
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