Geoscience Reference
In-Depth Information
The system (
2.66
) can be replaced by an equivalent system of m ¼ m
1
þþ
m
n
equations of the
first order, relative to the derivatives for all m unknown
functions. Then one of the standard software can be used to solve the last system.
Let the functions fi,
i
, i =1,
, n be continuous and differentiable with respect to
all arguments. Let us suppose that the solution of system (
2.66
) with the initial
conditions
…
y
i
ð
t
0
Þ
¼
ð
y
i
Þ
0
; ...;
y
ð
m
i
1
Þ
ð
t
0
Þ
¼
ð
y
ð
m
i
1
Þ
y
i
ð
t
0
Þ
¼
ð
y
i
Þ
0
;
Þ
0
i
i
exists and is unique in t
0
≤
≤
T.
Divide the interval [t0,T]
0
,T] into elementary intervals
t
k =[t
k
,t
k+1
] by a sequence of
points t
0
\
t
1
\
\
t
l
¼ T. On each such interval, let us search the solution of
system (
2.66
) in the form of a series:
ʔ
y
i
ð
t
k
Þþ
X
m
i
1
j
m
i
ð
t
t
k
Þ
y
ð
j
Þ
ð
t
k
Þþ
ð
t
t
k
Þ
ð
f
i
Þ
k
;
~
y
i
ð
t
Þ
¼
~
~
j
!
ð
m
i
Þ!
j¼1
ð
t
k
1
Þþ
X
m
i
j
1
s
ð
t
k
t
k
1
Þ
y
ð
j
Þ
i
ð
t
k
Þ
¼y
ð
j
Þ
i
y
ð
s
þ
j
Þ
i
ð
t
k
1
Þ
s
!
s¼1
m
i
j
þ
ð
t
k
t
k
1
Þ
ð
f
i
Þ
k
; ð
j ¼ 1
; ...;
m
i
1
Þ
ð
m
i
j
Þ!
The error of such a solution can be easily estimated, considering the exact
expansion of the functions y
i
(t) and y
ð
j
Þ
ð
t
Þ
in a Taylor series:
i
þ
M
i
j þ
X
m
i
1
h
k
j
!
h
m
i
þ
1
k
ð
m
i
þ
1
Þ!
ð
j
Þ
i
j
e
i
ð
t
k
þ
1
Þ
j e
i
ð
t
k
Þ
j
e
ð
t
k
Þ
j¼1
X
m
j
1
s¼0
e
X
h
m
i
k
ð
m
i
Þ!
n
ð
s
Þ
j
þ
M
i
ð
t
k
Þ
ð
2
:
67
Þ
j¼1
e
þ
X
m
i
j
1
h
k
1
s
ð
j
Þ
i
ð
j
Þ
i
ð
s
þ
j
Þ
i
e
ð
t
k
Þ
ð
t
k
1
Þ
e
ð
t
k
1
Þ
!
s¼1
!
X
m
j
1
s¼0
e
X
h
m
i
j
þ
1
k
ð
m
i
j
þ
1
Þ!
h
m
i
j
k
ð
m
i
j
Þ!
n
ð
s
Þ
j
þ
M
i
þ
ð
t
k
1
Þ
ð
2
:
68
Þ
j¼1
where
(
)
;
; ...;
@
f
i
@
t
f
i
@
y
1
@
@
f
i
M
i
¼
max
½t
0
;
T
y
ð
m
n
1
Þ
@
n
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