Geology Reference
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X = realisations at time t 0
t 0
Time
Figure 2.1 Successive realisations of a stochastic process. The expected value of
a random variable at a specific time t 0 is found by averaging across an infinite
ensemble of such realisations.
Frequently, the stochastic process generating the time sequence will be station-
ary , or assumed to be approximately so. In this case, the statistical properties of the
process are independent of translations along the time axis. Then, the autocorrela-
tion is independent of the time index and we write it as
E f l f l k .
φ ff ( k )
=
(2.18)
The autocorrelation of stationary sequences is a Hermitian function of lag, for
E f l f l + k ,
φ ff (
k )
=
(2.19)
and, writing m for l
+
k ,wehave
E f m f m k = φ ff ( k ).
φ ff (
k )
=
(2.20)
For stationary sequences, averaging across an infinite ensemble of independent
realisations is equivalent to averaging along the time axis of a single record. This is
known as the ergodic hypothesis .For stationary power signals , the autocorrelation
can then be equivalently defined as
N
1
f l f l k .
φ ff ( k )
=
lim
N →∞
(2.21)
2 N
+
1
l =− N
 
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