Geoscience Reference
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z
D
z
.x/
(1.14)
z
.x
0
/
D
0
so that (
1.13
) is transformed into a linear system with a nonlinear output injection
z
D
A
z
C
.y/
y
D
C
(1.15)
z
C
2
R
p
n
. If this is the case, then we can easily
construct a Luenberger type of observer as follows.
A
2
R
n
n
and
for some matrices
z
D
A
z
C
.y/
C
G.y
C
z
/
(1.16)
Let
e
D
z
z
then the error dynamics is a linear system decoupled from
z
.t/
e
D
.A
GC/e
If
G
, the observer gain, is chosen so that the eigenvalues of
.A
GC/
are all in the
left half plane, then
t
!1
e.t/
D
0
Not all nonlinear systems can be transformed into a linear system with output
injection. The existence of the change of coordinates (
1.14
) can be determined
using Lie differentiation. Given a function
lim
h.x/
,let
dh
represents the 1-form, or
the gradient,
@h
@x
1
.x/
@h
@x
2
.x/
@h
dh.x/
D
@x
n
.x/
The Lie derivative is defined as follows
L
f
.h/
D
dh
f
L
f
.dh/
D
f
T
@
2
h
@x
C
dh
@f
@x
The following theorem was proved in
Krener and Isidori
(
1983
).
Theorem 1.1.
There exists a local change of coordinates (
1.14
) that trans-
forms (
1.13
) into a linear system with output inject (
1.15
) if and only if
f.x
0
/
D
0
h.x
0
/
D
0
L
f
.dh/
L
f
.dh/
and
is a linear combination of
for
k
D
0;1;
;n
1
.
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