Geoscience Reference
In-Depth Information
k is
fixed from the conditions of best approximation by (
2.71
). Then the Eq. (
2.69
)
is replaced by the approximate equation:
y
¼exp
ð
kx
Þ
X
m
a
i
x
i
L½
~
;
ð
2
:
72
Þ
i¼0
which can be easily solved. For the error
eð
x
Þ
¼y
ð
x
Þ~
y
ð
x
Þ
, we obtain an equation
from (
2.69
)to(
2.72
):
L½
e ðÞ
¼f
ðÞ
exp
kx
ð
Þ
P
m
ðÞ
R
m
ðÞ
ð
2
:
73
Þ
Solving Eq. (
2.73
), we have
1
n
þ
k
j
n
ð
b
a
Þ
M
k
j
eð
x
Þ
;
!
k
!
k¼0
where
s
Þ
¼
X
n
i
1
p
i
ð
x
s
Þ
M ¼
a
s
x
b
K
ð
x
max
j
;
s
Þ
j;
g
¼ max
½a
j
R
m
ð
x
Þ
j;
K
ð
x
;
ð
i
1
Þ!
;
b
i¼1
2.12.5.5 Re
nements of Approximate Solutions of Volterra Integral
Equations
Let us consider Volterra integral equation of the
first and of the second kind arising
in the remote monitoring problems:
Z
x
k
G
ð
x
;
y
Þuð
y
Þ
dy ¼ g
ð
x
Þ;
ð
2
:
74
Þ
a
Z
x
uð
x
Þk
K
ð
x
;
y
Þuð
y
Þ
dy ¼ f
ð
x
Þ;
ð
2
:
75
Þ
a
where x
∈
[a,b], the kernel K(x,y) and its derivatives K
x
ð
x
;
y
Þ
are continuous in the
region R{a
b}, f(x) is a continuously differentiable function in (a,b),
the kernek G(x,y) and g(x) are twice continuously differentiable functions of x,
G(x,x)
≤
y
≤
x
≤
≠
0. Then, as it is known, Eqs. (
2.74
) and (
2.75
) have unique solutions
ˆ
1
(x) and
ˆ
2
(x) respectively which are continuous and differentiable in [a,b] for any
ʻ
value of
. The case when G(x,x) = 0 for some point in the interval [a,b] or for the
entire interval needs special consideration. In our case, Eq. (
2.74
) is equivalent to
the equation of second kind
Search WWH ::
Custom Search