492
CHAPTER
9.
STOCHASTIC
MODELING
Proof
It can be
observed
that
•
equation
(9.93)
is a
direct
consequence
of the
score-transform
theorem
(see
equation
(9.17))
and
definitions
(9.88)
and
(9.92).
•
equations
(9.94)
is a
straightforward
consequence
of the
approximation
(9.13)
and
properties
(9.91)
and
(9.89).
Let us now
assume
that
P(u,
o>)
is the
periodic
P-field
denned
in
section
(9.5.2)
and
that
F(u;
s)
is a
Gaussian cdf:
It can be
observed
that,
for any p G
[0,1],
Taking into account condition (9.73)
and
equations
(9.92)
or
(9.90),
it can be
deduced
that
where
Z(u,u;)
is the
GRFS used
to
build
P(U,UJ).
From this equation,
it can be
concluded
that
5(u,
a;)
is a
second-order
non-stationary
RF
honoring equations
(9.95).
9.6
Stochastic simulators
As
explained
in
section
(9.1),
the
main purpose
of
this chapter
is to
propose
simulation techniques capable
of
producing equiprobable solutions
to
inter-
polation problems. These solutions
are
called "simulations"
and are
defined
as
realizations
of
random functions called "stochastic simulators"
or,
more
simply,
"simulators." Many
different
techniques have been proposed
in the
literature
for
building simulators (e.g.,
see
[215,
58,
94]).
In
this section,
havin g
denned
the
notion
of
simulator, three examples
of
particularly simple
techniques
for
building simulators
are
given. Other techniques will
be
pre-
sented
later
on in
sections
(9.7.7),
(9.7.8), (9.9.1),
and
(9.8)
and in
chapter
10 .
9.6.1
The
interpolation versus simulation problem
As
suggested
in figure
(9.10),
let
z(u)
be an
unknown
scalar
function
defined
on
a
region
D of a
normed linear vector
space
36
8
(see
[141])
and
known only
o n
a finite
subset
D*
consisting
of N
sampling
points
{ui,...,
ujv}
belonging
toD:
36
For
example,
this
space
can be the
Euclidean
parametric
space
(x,
y,
z)
or a
curvilinear
parametric
space
(u,v,w)
corresponding
to a
stratigraphic
grid
(see
figure
(10.1)).