Geoscience Reference
In-Depth Information
The general solution of Eq. ( 2.53 ) is known:
c ð k Þ
1
c ð k Þ
2
c ð k Þ
n
~
y ¼ ~
y ð x
;
;
; ...;
Þ;
ð 2
:
57 Þ
where the constants are determined from the initial conditions at the beginning of
each interval [x k , x k+1 ]. The calculations are carried out successively beginning with
the interval (k = 0).
Let us estimate the error in solution of Eq. ( 2.49 ). Let y(x) and
~
y ð x Þ by the exact
and the approximate solutions respectively. Let us denote
y ð m i Þ
k
f k ¼ f ð x k ; ~
P ik ¼ P i ð x k ; ~
y 0 k ; ...; ~
y k ; ~
Þ;
y k Þ;
ð 2
:
58 Þ
e k ¼ y ð x k Þ~
y ð x k Þ
Let us integrate times Eqs. ( 2.49 ) and ( 2.53 ) from x k to x, and consider the
final
results for x = x k+1 . For the sake of convenience and brevity let us denote
Z
Z
Z
Z
x k þ 1
x
x
x k þ 1
x Þ dx dx
n
¼
x Þ dx
;
x k
x k
x k
x k
n
n
we have
Z
x k þ 1
y k þ 1 ¼ y k þ y k h k þ h k X
X
n 1
n
h s 2
k
s
y ð s Þ
k
P i y ð n i Þ dx
!
s¼2
i¼1
x k
n
ð 2
:
59 Þ
Z
x k þ 1
Z
x k þ 1
f ð x
;
y Þ dx þ k
W½y dx
x k
x k
n
n
Z
x k þ 1
y k þ 1 ¼y k þ y 0 k h k þ h k X
X
n 1
s¼2 y ð s Þ
n
h s 2
k
s
P ik y ð n i Þ dx
k
!
i¼1
x k
n
ð 2
:
60 Þ
Z
Z
x k þ 1
x k þ 1
f k dx þ k
W k ½y dx
þ
x k
n
x k
n
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