Geoscience Reference
In-Depth Information
d
!
In our proofs we use the concept of level sets. For a function f
W
R
R
the
d
W
f.x/
g
(the
level set for a value
2
R
is given by L
.f;/
WD f
x
2
R
d
W
f.x/<
g
) and the level curve for a value
strict level set is L
<
.f;/
WDf
x
2
R
d
W
f.x/
D
g
: For a function f
i
.
/ we use
2
R
is given by L
D
.f;/
WDf
x
2
R
the notation
.f
i
/
WD
arg min
x2
R
f
i
.x/:
X
d
For two points x and y we denote the segment defined by x and y as
xy
.
In this chapter we focus on some fundamental results in the continuous,
network and discrete cases. We will describe in some detail a complete geometric
characterization for the planar 1-facility case, an optimal time algorithm for the
1-facility network problem as well as the computation of the entire set of Pareto-
optimal solutions of the discrete multicriteria p-median problem. Although we are
concentrating on the median case we will give some outlook to extensions.
9.2
1
-Facility Planar/Continuous Location Problems
In this section we study Problem (
9.1
)wheref
1
.
/;:::;f
Q
.
/ are convex, inf-
compact functions, defined in
2
, which represent different criteria or scenarios.
Recall that a real function f.
/ is said to be inf-compact if its lower level sets
f
x
2
R
d
W
f.x/
g
are compact for any
2
. The next result states a
useful characterization of the different solution sets defined in the previous section
using level sets and level curves which will be used later.
R
R
Theorem 9.1
The following characterizations hold :
Q
\
X
wPar
f
1
;:::;f
Q
,
L
<
.f
q
;f
q
.x//
D;
x
2
(9.2)
qD1
Q
Q
\
\
X
Par
f
1
;:::;f
Q
,
L
.f
q
;f
q
.x//
D
L
D
.f
q
;f
q
.x//
x
2
qD1
qD1
(9.3)
Q
\
X
sPar
f
1
;:::;f
Q
,
L
.f
q
;f
q
.x//
Df
x
g
:
x
2
(9.4)
qD1