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
uð
x
Þ
dx
dx
n
¼
uð
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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