Upload
others
View
0
Download
0
Embed Size (px)
Citation preview
=e indicators mining ex- ? total rich- xxlziJ0ns. Mo- the analytic creasing the t they waild
? assessment Lysis taxied cal gLlidance great value
1ut progrr?ss logic judge-
'alse preci- %ions, pro- - resolution discwered
I sxnarios, =-4'- ef iciencies usefulness
Some Aspec ts o f M u l t i v a r i a t e A n a l y s i s
Dona ld E. Myers Department o f Mathematics U n i v e r s i t y o f Ar izond Tucson, A 2 85721 U.S.A.
ABSTRACT. C l a s s i c a l m u l t i v a r i a t e methods f o r a n a l y z i n g da ta t ab leaux
do n o t e x p l i c i t l y i n c o r p o r a t e s p a t i a l c o r r e l a t i o n . I n c o n t r a s t geo-
s t a t i s t i c a l t echn iques such as k r i g i n g , dua l k r i g i n g and c o k r i g i n g a r e
p r i m a r i l y e s t i m a t i o n methods. The m u l t i v a r i a t e f o r m a t i o n s o f dua l
k r i g i n g and d i s j u n c t i v e k r i g i n g , dua l c o k r i g i n g and c o - d i s j u n c t i v e
k r i g i n g , p r o v i d e methods which b r i d g e t h e gap between t h e two
approaches. B a s i c p r o p e r t i e s o f b o t h a r e p resented .
INTRODUCTION
The impor tance o f m u l t i v a r i a t e techn iques has been recogn i zed f o r a
number o f yea rs . I n p a r t i c u l a r , C l u s t e r A n a l y s i s . P r i n c i p a l
Components and D i s c r i m i n a n t Ana l ys i s have had widespread use.
However, t hese t o o l s wh i ch had t h e i r o r i g i n i n o t h e r d i s c i p l i n e s
o the r t h a n t h e geosciences do n o t f u l l y r e s p e c t some c h a r a c t e r i s t i c s
o f m u l t i v a r i a t e d a t a s e t s a r i s i n g o u t o f problems i n t h e geosciences,
m in ing , env i r onmen ta l m o n i t o r i n g , hyd ro logy and remote sensing. I n
P a r t i c u l a r t h e models u n d e r l y i n g t hese do n o t s p e c i f i c a l l y
I n c o r p o r a t e s p a t i a l c o r r e l a t i o n . The d icho tomy between t hese
techn iques and e s t i m a t i o n techn iques such as k r i g i n g can be seen i n
the c o n t e x t o f two p e r s p e c t i v e s o f a da ta t a b l e a u . Cons ider
( ' (.hun,q PI uI. I ~ d y . ) , Qu~lntlta(llive An(11ys~ of Mtnrrul rind Eticrpy Rt..wrrrrcs. 669.487 ' ' hh? 1). Rt,dcl Puhlrrhrng Company.
I n gene ra l m u l t i v a r i a t e techn iques i n t e r p r e t t h e t a b l e a u as a
( random?) sample o f s i z e n from a v e c t o r va l ued random v a r i a b l e
whereas g e o s t a t i s t i c s a l a Matheron wou ld model t h e t a b l e a u as a
non-random sample f r om one r e a l i z a t i o n o f a v e c t o r - v a l u e d random I
f u n c t i o n where t h e s p a t i a l c o r r e l a t i o n i s o f p r i n c i p a l i n t e r e s t . The I
above m u l t i v a r i a t e t echn iques do n o t r e q u i r e p o s i t i o n c o o r d i n a t e s and i
do n o t r e f l e c t t h e suppo r t o f t h e sample. I n gene ra l t h e y a r e n o t
e s t i m a t i o n , t echn iques b u t r a t h e r seek t o i d e n t i f y u n d e r l y i n g
phenomena o r d i s c e r n p a t t e r n s . The v a r i o u s forms o f k r i g i n g have
been deve loped and used f o r e s t i m a t i o n a lmos t e x c l u s i v e l y . There
have been a few i n s t a n c e s where a m u l t i v a r i a t e t e c h n i q u e such as
p r i n c i p a l components has been a p p l i e d i n c o n j u n c t i o n w i t h k r i g i n g ,
f o r example Borgman and Frahme (1976) , t lyers and Ca r r ( 1984 ) , Flyers
(1984) . Dav is and Greenes (1983) . I n each o f t hese t h e o b j e c t i v e was
t o s i m p l i f y o r t o a v o i d c o k r i g i n g . A d d i t i o n a l i n t e r e s t i n g
a p p l i c a t i o n s a r e g i v e n i n Bopp and B iggs (1981) o r Hopke e t a1 (1976)
n e i t h e r o f whom used g e o s t a t i s t i c s b u t s i m p l y con tou red t h e d e r i v e d
f a c t o r s t o i d e n t i f y p a t t e r n s . A l though p a t t e r n r e c o g n i t i o n i s a t o o l
much d e s i r e d i t i s as y e t n o t f u l l y developed.
The r e s u l t s p resen ted he re i n c o r p o r a t e some aspec t s o f c l a s s i c a l
mu1 t i v a r i a t e methods as w e l l as i n c o r p o r a t i n g s p a t i a l c o r r e l a t i o n and
a r e i n t e n d e d t o s t i m u l a t e f u r t h e r thought .
I. POSSIBLE GENERALIZATION
A . Cons ider a d a t a t a b l e a u w i t h an i n f i n i t e number o f rows,
i .e . one f o r each p o i n t i n a domain o f i n t e r e s t , i.e., each column i s
a f u n c t i o n , n o t j u s t a f i n i t e number o f p o i n t s and w h i c h i s w r i t t e n
s i m p l y as
For a f i n i t e number o f p o i n t s , i .e. a f i n i t e number o f l i n e s , a
u n i f o r m d i s t r i b u t i o n i s assumed, t h a t i s each l i n e i s e q u a l l y
weighted. For t h e i n f i n i t e case a p r o b a b i l i t y d i s t r i b u t i o n must be
assumed f o r each column. The ana logy t o choos ing a v e c t o r wh i ch
c a r r i e s t h e l a r g e s t amount o f v a r i a n c e i s t o choose a random v a r i a b l e
such t h a t t h e sum o f t h e squares o f t h e p r o j e c t i o n i s maximized. In
i a
! r i a b l e
u a s a
a ndom
re not
have
There
h a s
. ig ing,
, tlyers
c t i v e was
l ass ica l
t ion and
ows , )lumn Is - i t t e n
t h e f i n i t e version t h i s i s given as the inner product, f o r random
var iab les i t i s the conditionpl expectation. Let t h e conditional
expectat ion E ( Z i / U ) be wr i t t en in operator form DU Z i which
e a s i l y extends t o the vector Z = [Z1 , ... , Zm]. Writing the inner
product of two random var iables V , V as < V , W > = E ( V W ) , the
problem i s t o maximize
which i s a p o s i t i v e quadratic form. However, unl ike t h e f i n i t e
dimensional case where the b ivar ia te d e n s i t i e s a r e implied by the
d a t a , in t h i s case the operator D U i s character ized by b ivar ia te
d e n s i t i e s t h a t a r e unknown. One possible reso lu t ion of t h i s problem
i s t o assume t h a t each pa i r Zi, U i s b i v a r i a t e Gaussian and then i t
i s s u f f i c i e n t t o know t h e c o r r e l a t i o n f o r each pair . This i s
e s s e n t i a l l y t h e d i s junc t ive kr iging approach but r e c a s t in
mu1 t i v a r i a t e form, and will be discussed i n Sect ion IV.
6. Because the above formulation does not lead t o a numerical
solut ion without the use of s t rong d i s t r i b u t i o n a l assumptions i t i s
useful to ' r e -cons ider the problem from another perspect ive.
Principal components produces a representat ion of t h e data in t h e
following form
where FTF i s diagonal and the columns of F a r e ordered by percent
o f variance explained. One of the ob jec t ives of t h i s transformation
is t o remove i n t e r - v a r i a b l e c o r r e l a t i o n however t h i s method only
incorporates the i n t e r - v a r i a b l e c o r r e l a t i o n a t t h e same locat ion. I t
would be more appropria te t o remove s p a t i a l i n t e r - v a r i a b l e
correla t ion.
This suggests the following: i f
I S a vector of second order s t a t i o n a r y func t ions , f i n d
672
- Y ( x ) = [ Y 1 ( x ) , ..., Y ( x ) ] and C s u c h t h a t
P
- a n d t h e componen ts o f Y ( x ) a r e u n c o r r e l a t e d . W r i t t e n i n t e r m s o f
t h e v a r i o g r a m s a n d c r o s s - v a r i o g r a m s t h i s becomes
and 7 ( h ) i s t o be a d i a g o n a l m a t r i x . H e r e r Z ( h ) , Y y ( h ) d e n o t e Y
a n d
v Z ( h ) c o r r e s p o n d s t o a c o r r e l a t i o n mat r ix . , The r e p r e s e n t a t i o n
i s a n a l o g o u s t o t h e d i a g o n a l i z a t i o n o f t h e c o r r e l a t i o n m a t r i x as i n
P r i n c i p a l Components A n a l y s i s .
I f a l l o f t h e v a r i o g r a m s o f t h e componen ts o f Z ( x ) h a v e s i l l s t h e n
t h e t o t a l i n e r t i a o f i ( x ) i s t h e sum o f t h e s i l l s , i . e .
2 T r C Z ( - ) = I ( I C j k ) ~ y ( - ) k (9)
The c o l u m n s o f C c a n be n o r m a l i z e d b y r e q u i r i n g
t h e n t h e componen t o f P ( x ) w i t h t h e l a r g e s t p e r c e n t o f v a r i a n c e i s
t h e componen t o f Y o ( ) whose v a r i o g r a m h a s t h e l a r g e s t s i l l .
When t h e o b j e c t i v e i s p a t t e r n r e c o g n i t i o n a s o p p o s e d t o c o -
k r i g i n g , t h e n t h e s a m p l e v a r i o g r a m m a t r i x may s u b s t i t u t e f o r t h e t r u e
v a r i o g r a m m a t r i x . A f t e r t h e samp le v a r i o g r a m m a t r i x i s c o m p u t e d f o r
~ a r i c
each
s i n g ~
can t
and h
d e t e r - y ( x
d e c o ~
the c
Wac ke
Wacke
o f t h .
compo - Y ( x )
t h e v
r ange ' - r z ( h ) .
c o n s t !
i s mot
v a r i o l
11. I
t
t he fc
!jot or
i n t e r C
the s,
F
t e rms o f
(5
d e n o t e
( 7 )
i o n
(8)
I( as i n
1s t h e n
0-
he true ed f o r
\ a r i o u s l a g s a n d d i a g o n a l i z e d t o f i n d t h e e i g e n v a l u e s , t h e s i l l s f o r
each v a r i o g r a m a r e e s t i m a t e d by t h e e i g e n v a l u e s . When C i s non-
s i n g u l a r t h e e q u a t i o n
can be s o l v e d as
and hence a t l e a s t a t d a t a l o c a t i o n s t h e v a l u e s o f Y ( x ) a r e
d e t e r m i n e d . T h i s w o u l d p e r m i t s e p a r a t e k r i g i n g o f t h e components c f - - Y(x ) w i t h s u b s e q u e n t r e c o n s t r u c t i o n o f k r i g e d v a l u e s o f Z ( x ) . T h i s
d e c o m p o s i t i o n w o u l d a l s o a l l o w s i m u l a t i o n o f Z ( x ) by s i m u l a t i o n o f - t h e components o f Y ( x ) .
The model f o r m u l a t i o n g i v e n by ( 1 1 ) i s s i m i l a r t o t h a t used by
Wackernagel (1985) b u t t h e method o f a c h i e v i n g i t i s d i f f e r e n t . I n
Wackernagel t h e p r o c e d u r e i s t o model t h e v a r i o g r a m ( o r c o v a r i a n c e s )
o f t h e componen ts o f ? (x ) by n e s t e d models . It i s assumed t h a t t h e
components o f t h e s e n e s t e d mode ls r e p r e s e n t t h e components o f - Y ( x ) t h e n ' t h e c r o s s - v a r i o g r a m s a r e mode led as 1 i n e a r c o m b i n a t i o n s o f
t he v a r i o g r a m m o d e l s . I n p a r t i c u l a r i t i s o f t e n assumed t h a t t h e
p r i n c i p a l d i f f e r e n c e i n t h e v a r i o g r a m mode ls i s r e f l e c t e d i n t h e
ranges. The a p p r o a c h p r o p o s e d above a l l o w s a m o r e g e n e r a l model f o r - . iZ (h ) . N o t a l l s u c h m o d e l s c a n be d i a g o n a l i z e d whereas t h e
c o n s t r u c t i o n i n Wackernage l e n s u r e s a d i a g o n a l i z a b l e model and hence
i s more r e s t r i c t i v e i n p a r t i c u l a r i t assumes a l l v a r i o g r a m s and c r o s s
v a r i o g r a m s a r e p r o p o r t i o n a l t o t h e same model .
11. DUALITY - AN ALTERNATIVE
B e f o r e i n t r o d u c i n g a mu1 t i v a r i a t e v e r s i o n i t i s u s e f u l t o r e c a l l
t he f o r m u l a t i o n o f t h e u n i v a r i a t e k r i g i n g e s t i m a t i o n i n d u a l form.
' lot o n l y i s t h i s f o r m a n a l o g o u s t o t h e u s e o f s p l i n e s f o r
' " t e r p o l a t i o n b u t i t a l s o p r o v i d e s a me thod f o r r e m o v i n g o r r e d u c i n g
'he s p a t i a l c o r r e l a t i o n .
R e c a l l t h e e q u a t i o n s d e t e r m i n i n g t h e o r d i n a r y K r i g i n g
e s t i m a t o r . L e t xl, ..., xn be d a t a l o c a t i o n s w i t h d a t a Z ( x l ) ,
.. . . Z ( x n ) . Then t h e k r i g i n g e q u a t i o n s a r e w r i t t e n as
where
I n m a t r i x fo rm we have
wh ich we can w r i t e a s
where
f o r
a n c
i n t
not
t h e n
L e t
If u n i q u e neighborhood k r i g i n g i s used t h e n [ i b l T need o n l y be
computed once s i n c e a l l t h e i n f o r m a t i o n about t h e p o i n t t o be T
e s t i m a t e d i s c o n t a i n e d i n [ K O 11. Y i s a d a t a v e c t o r " d u a l " t o
Z. F i r s t i n t r o d u c e d by Matheron, Dubru le (1983) showed t h a t t h i s
f o r m u l a t i o n a l l owed f o r t h e use o f a un ique ne ighborhood i n c ross -
va l i d a t i o n and more r e c e n t l y Dubru le and Kostov (1986) have shown how
i t f a c i l i t a t e s t h e i n c o r p o r a t i o n o f i n e q u a l i t y c o n s t r a i n t s . Royer
and V i e i r a (1984). Ga l l i, M u r i l l o and Thomann (1984) have suggested
i n t e r p r e t a t i o n s o f Y.
Y , b have some p r o p e r t i e s wh ich have perhaps n o t been
noted. For example
A
YF = 0 and E(Y) = [O, 0,--0, 01
So t h a t Y i s cen te red i n two d i f f e r e n t senses.
I f E ( Z ( x ) ) = m t hen ~ ( i ) = m ~ ~ and E (b ) = m hence b i s
an unb iased e s t i m a t o r o f m. By w r i t i n g
then we o b t a i n
In a c r u d e sense Z i s r ep laced by new v e c t o r i n wh i ch each e n t r y i s - a l i n e a r c o m b i n a t i o n b u t t h e components o f Y a r e l e s s c o r r e l a t e d .
I f we compute
676
t h e n
w h i c h i s ana logous t o a c o r r e l a t i o n m a t r i x .
111. CO-DUALITY
A l t h o u g h d u a l k r i g i n g i s n o t q u i t e a m u l t i v a r i a t e t e c h n i q u e i t
sugges ts an e x t e n s i o n o f C o k r i g i n g t h a t can p r o p e r l y be c a l l e d m u l t i -
v a r i a t e .
R e c a l l f r o m Myers (1982, 1983, 1984) t h e g e n e r a l f o r m o f
c o k r i g i n g . As above xl, .. ., x n deno te sample l o c a t i o n s , - - Z(x l ) , ... , Z ( x n ) a r e t h e d a t a v e c t o r s where - Z ( x ) = [ Z 1 ( x ) , .. . , Z,(x)]. Then t h e c o k r i g i n g e s t i m a t o r i s g i v e n by
where
and
t h e n
- * U n l i k e t h e k r i g i n g e s t i m a t o r z t ( x 0 ) , Z ( x 0 ) i s n o t a s c a l a r and
hence i s n o t equa l t o i t ' s t r a n s p o s e b u t s i n c e
T T -*. L[~*(x,)I I = z ( x 0 ) (28)
Let
w i t h
we s h a l l work w i t h [ ? * ( x 0 ) l T u s i n g n o t a t i o n ana logous t o t h a t above
f o r d u a l k r i g i n g
Then
t h e n t h e c o k r i g i n g s y s t e m becomes
We h a v e t h e n
where
L e t
w i t h
A
Then 7 i s t h e " d u a l " t o 7 i n t h a t i t i s a v e c t o r o b t a i n e d f rom
b y i n c o r p o r a t i n g t h e s p a t i a l a n d i n t e r v a r i a c e c o r r e l a t i o n
q u a n t i f i e d by t h e v a r i o g r a m m a t r i x . We s e e i m m e d i a t e l y t h a t
and
o r a l t e r n a t i v e l y
The o r i g i n a l d a t a t a b l e a u i s t h e n g i v e n as a l i n e a r c o m b i n a t i o n o f
t h e e n t r i e s i n t h e new d a t a t a b l e a u . M o r e o v e r , B i s an e s t i m a t o r
o f E [ ~ ( X ) ] ~ when i(l;) i s second i y d e r s t a t i o n a r y and
T r a c e E[B - l ( i T ) ] [ B - E(? ' ) ] = T r [C(O) - K - ' F ( F ~ K - ~ F ) - ' ] ( 38 ) wh
6 . i s t h e sum o f t h e v a r i a n c e s o f t h e e s t i m a t i o n e r r o r s .
I V BIVARIATE GAUSSIAN MODEL o r . The f i r s t model p roposed t o g e n e r a l i z e p r i n c i p a l components
w o u l d r e q u i r e m i n i m i z i n g t h e q u a d r a t i c f o r m g i v e n b y e q u a t i o n ( 1 )
w h i c h i s d e t e r m i n e d by t h e c o n d i t i o n a l e x p e c t a t i o n o p e r a t o r . I n t u r n
t h i s w o u l d r e q u i r e knowledge o f ( a t l e a s t ) b i v a r i a t e d e n s i t i e s .
M a t h e r o n ( 1 9 7 6 ) e x t e n d e d t h e k r i g i n g e s t i m a t o r f r o m a l i n e a r t o a
n o n - l i n e a r f o r m by u t i l i z i n g a b i v a r i a t e Gauss ian d e n s i t y f u n c t i o n .
S p e c i f i c a l l y t h e d i s j u n c t i v e k r i g i n g e s t i m a t o r i s w r i t t e n i n t h e form
The f j l s a r e o b t a i n e d b y H e r m i t e p o l y n o m i a l e x p a n s i o n s w h i c h i n
t u r n a r e t h e e i g e n f u n c t i o n s o f t h e c o n d i t i o n a l e x p e c t a t i o n
O p e r a t o r . By u t i l i z i n g t h e g e n e r a l c o k r i g i n g f o r m u l a t i o n g i v e n i n
Eq. ( 2 6 ) , t h e DK e s t i m a t o r c a n b e f u l l y g e n e r a l i z e d .
A. P r e l i m i n a r i e s
2 L e t L . . d e n o t e t h e space o f f u n c t i o n s f , s u c h t h a t 1 J
f o r
t h e
f u n
i n
C.
r a n
d i s
i s
tha
for
f ( z i ( x j ) ) i s s q u a r e I n t e g r a b l e , i.e. E [ ~ ( z ~ ( x ~ ) ) ] ~ < -. Then f o r m arc
f o r
2 2 t h e sum L = L,,, wh ich i s n o t a d i r e c t sun s i n c e t h e
0 f
t o r
t u r n
n.
form
' i n
2 c o n s t a n t f u n c t i o n s a r e i n each Lij. I f I I ( I i i s t h e norm i n
2 m n 112-
Li t h e n [.I I I 1 i s a norm on L ~ . The non-1 i n e a r 1 = 1 * ~ = l
e s t i m a t o r f o r Z . ( x o ) i s t h e n t h e p r o j e c t i o n o f Z j (xo) o n t o t h e J
l i n e a r subspace o f L' genera ted by t h e e lements o f t h e L ? t h a t l k '
i s .
k 2 where f i j E L . l k ' 0 . The P r o j e c t i o n s
S i n c e Z * ( X ) i s a p r o j e c t i o n , t h e e r r o r s Z . ( x ) - Z * ( X ) a r e J 0 k J O j 0
or thogona l t o a l l t h e fi(zi ( x k ) ) and hence we have
* f o r a l l is J, k. S i n c e Z . ( x ) i s a 1 i n e a r combina t ion , each o f
J 0 these e x p e c t a t i o n s o n l y r e q u i r e s a b i v a r i a t e d e n s i t y . However t h e
k f unc t i ons fi a r e i n gene ra l unknown and t h e problem i s i n s o l u a b l e
i n t h i s g e n e r a l i t y .
C. T rans fo rma t i ons
As w i t h s i n g l e v a r i a b l e d i s j u n c t i v e k r i g i n g we assume t h a t each
random f u n c t i o n may be t r a n s f o r m e d t o one w i t h a Gaussian
d i s t r i b u t i o n . More s p e c i f i c a l l y we assume t h a t f o r each Zj t h e r e
i s a random f u n c t i o n Y j wh ich i s Gaussian and a f u n c t i o n 4 such j
t h a t Z . ( x ) = Q . ( Y . ( x ) ) f o r each j, x. Moreover , we assume t h a t J J J
f o r each i, j and each p a i r x, y
a r e b i v a r i a t e Gaussian. If i = j t h e n t h i s i s t h e usual assumpt ion
d i s j u n c t i v e k r i g i n g .
0. Hermi t i a n Expansions
I f Y(x) i s a Gaussian random f u n c t i o n and f i s a f u n c t i o n
such t h a t E [ f ( y ( x ) ) l Z < - then f may be rep resen ted by an k expans ion i n te rms o f H e r m i t e p o l y n o m i a l s . I n p a r t i c u l a r i f fij i s
a f u n c t i o n i n Li 2 t hen
k m
f . . [ Y ( x ) ) = 1 fk? H ( Y ( x ) ) 1 J p= 0 1J P
where f . . kP = E [ ~ ~ . ( Y ( ~ ) ] H ~ ( Y ( X ) ) ] 'J 1 J (431
T h i s p r o v i d e s a method f o r r e p r e s e n t i n g t h e unknown f u n c t i o n s k f . . Moreover t h e f u n c t i o n s . can be rep resen ted as 1 ~ ' J
E. B i v a r i a t e D e n s i t i e s
Under t h e assumpt ions t h a t each p a i r Yi(x) , Y j (y ) i s b i -
v a r i a t e Gaussian, t h e j o i n t d e n s i t i e s can be w r i t t e n i n t h e f o rm
where g ( x ) , y ( y ) a r e s tandard Gaussian d e n s i t i e s , pi: i s t h e
c o r r e l a t i o n c o e f f i c i e n t o f Yi(x), Y . (y ) . As w i t h u n i v a r i a t e J
d i s j u n c t i v e k r i g i n g we c o u l d a l s o cons ide r more gene ra l b i v a r i a t e
d e n s i t i e s such as t h e Hermitean models.
F. The O r t h o g o n a l i t y C o n d i t i o n s
Combining Eq. ( 4 1 ) , (42) we w i l l have
then \
where
f o r a l l j, E, r
U s i n g t h e t r a n s f o r m a t i o n s Z X ) = 4 . ( y . ) ) we o b t a i n J J
k S i n c e b o t h t h e $ .'I a n d t h e f i j l s a,re unknown we r e p l a c e k J k k f i j j j k b y s i m p l y f ( x k ) w h e r e o f c o u r s e t h e f . . I s
1 J J a r e n o t t h e o r i g i n a l ones a n d t h e n E q u a t i o n ( 4 0 ) becomes
1 J
If we write i t ( x ) = [ z * ( x ) , . .. , z:(x0)] and 0 1 0
t h e n we h a v e
where
Now i f we l e t F/ be w r i t t e n as
t h e n
and t h e e s t i m a t i o n v a r i a n c e i n ~2 i s g i v e n by
I = I Trace (tp) w C P
p= 0 P
- H
F s o l
Since t h e c P ' s a r e de te rm ined o n l y by t h e t r a n s f o r m a t i o n s t o
m i n i m i z e t h e e s t i m a t i o n v a r i a n c e i t i s s u f f i c i e n t t o m in im i ze , f o r
each p s e p a r a t e l y ,
f.loreover, f o r each p, i t i s s u f f i c i e n t t o c o n s i d e r
But m i n i m i z i n g
i s e x a c t l y t h e p rob lem o f c o k r i g i n g R (x ) u s i n g t h e d a t a - - P 0 H ( x ) . ... . H ( x ). Hence t h e m a t r i c e s BY. ... , B: a r e t h e
P 1 P n s o l u t i o n s o f t h e (simp1 e) c o k r i g i n g systems
a s f o rmu la ted i n Myers (1982)
For t h e b i v a r i a t e Gaussian case t h e e n t r i e s i n G~ a r e j k
i J. where p jk = c o r r e l a t i o n o f Y i ( x j ) YI(xk)
6 . The Undersampled' Case
~f f i s under-sampled, i .e . if f o r i and some k. Zi(xk) i s .k m i s s i n g t h e n i n e q u a t i o n (10) f o r a l l j, f . . E 0 and hence f o r a l l 1 J
k p p, f . . = 0. I n t h e c o n t e x t o f e q u a t i o n ( 2 7 ) t h i s i s e x a c t l y t h e 1 J
u n d e r - s a m p l e d f o r m u l a t i o n o f t h e c o k r i g i n g p r o b l e m a s g i v e n i n Myers
( 1 9 8 4 ) and i n C a r r . Myers and G lass (1985) hence t h e a l g o r i t h m
g i v e n t h e r e s t i l l s u f f i c e s .
V. DATA o r MODEL DRIVEN
P r i n c i p a l Components i s e s s e n t i a l l y a d a t a d r i v e n t e c h n i q u e ,
t h a t i s , n o p a r a m e t e r s need be s e p a r a t e l y f i t t e d n o r a r e t h e r e
a s s u m p t i o n s s u c h a s n o r m a l i t y o r s t a t i o n a r i t y . Some o f t h e
i n t e r p r e t a t i o n s o f t h e s e components and t h e i r e i g e n v a l u e s f o l l o w o n l y
frorn t h e g e o m e t r i c f o r m u l a t i o n w i t h o u t t h e u s e o f e x t e r n a l models.
C o k r i g i n g , d u a l k r i g i n g and c o k r i g i n g i n c o n t r a s t r e q u i r e f i t t i n g
v a r i o g r a r n s and c r o s s - v a r i o g r a r n s , t h e s e f i t t i n g t e c h n i q u e s a r e n o t on
c o m p l e t e l y s o l i d g r o u n d s t a t i s t i c a l l y and a l s o r e q u i r e i m p l i c i t
model 1 i ng o f t h e phenomena b y random f u n c t i o n s a n d t h e varograrns must
s a t i s f y c e r t a i n c o n d i t i o n s . The e x t e n s i o n f r o m l i n e a r t o n o n - l i n e a r
t e c h n i q u e s r e q u i r e v e r y s p e c i f i c s t a t i s t i c a l m o d e l s and assumpt ions
t h e s e a d d i t i o n a l c o n d i t i o n s a r e o f t e n u n t e s t a b l e . I t w o u l d appear , . t h a t m u l t i - v a r i a t e t e c h n i q u e s t h a t t r u l y i n c o r p o r a t e s p a t i a l
c o r r e l a t i o n a r e e i t h e r n o t p o s s i b l e o r a t l e a s t n o t a s y e t deve loped.
R e f e r e n c e s
A r m s t r o n g , M., ( 1 9 8 4 ) 'New Types o f D i s j u n c t i v e K r i g i n g ' , P a r t I, N-872 F o n t a i n e b l e a u
A r m s t r o n g , M. and Mathe ron . G. , (1985) ' I s o f a c t o r i a l m o d e l s f o r g r a n u l o - d e n s i m e t r i c d a t a ' , N-944 F o n t a i n e b l e a u
A r m s t r o n g , M. and Mathe ron . G., ( 1 9 8 5 ) 'New t y p e s o f D i s j u n c t i v e K r i g i n g ' , P a r t 11, N-943 F o n t a i n e b l e a u
Bopp, F. 111. a n d B i g g s , R. M e t a l s i n E s t u a r i n e Sed imen ts . F a c t o r A n a l y s i s a n d i t s E n v i r o n m e n t a l S i g n i f i c a n c e , S c i e n c e v 214, p 441-443
Borgman L. a n d Frahme, R. B . , ( 1 9 7 6 ) , 'Mu1 t i v a r i a t e P r o p e r t i e s o f B e n t o n i k i n N o r t h e a s t e r n Wyoming ' , i n Advanced G e o s t a t i s t i c s i n t h e M i n i n g I n d u s t r y , G u a r a s c i o , M. e t a1 ( e d s ) D. R e i d e l Pub1 i s h i n g , D o r d r e c h t
C a r r , J., M y e r s , D. E. and G l a s s , C., ( 1 9 8 5 ) ' C o - K r i g i n g : A Computer P r o g r a m ' , Computers and Geosc iences , 11, No 2 , p 111.
Ca rr, J. Co - C P 67
D a v i s , B d i s t r d a t a '
D u b r u l e , a n d C
D u b r u l e , i n t o Geo lo
G a l l i , A. p r o w f o r 1.ic m
Gupta, A. d i s t r i
Hopke, Ph. 0. J., J. Rad
Jackson , N b y d i s Colnpu t q m E o f f 4 i n
Kim. Y. C . : g e o s t a l DOE. Gr
L a n t u e j o u l , d e t e r m i
Marecha l , A K-304 F
M a r e c h a l , A g a u s s i e ~
M a r e c h a l , A. me thods Advancer Pub..
k i t h e r o n , G. Fon ta i ne
C a r r , J. and Flyers, D. E., 'COSIM: (1985) A FORTRAN I V Program f o r t h e
I Myers
:hm
IW o n l y
81 s.
n 9
o t on
; must
nea r
ons
a r ,
Co-Cond i t i ona l S i m u l a t i o n ' , Computers and Geosciences, 11, No. 6 P 675.
Dav i s , B. and Greenes, K., ( 1983 ) , ' E s t i m a t i o n u s i n g s p a t i a l l y d i s t r i b u t e d m u l t i - v a r i a t e Data; An example w i t h coa l q u a l i t y d a t a ' , iflath. Geology, 15, p. 287
Dubru le , 0.. (1983) . 'Two methods w i t h d i f f e r e n t ob . iec t i ves : s p l i n e s and k r i g i n g l , Math. Geology, 15, p 245
Dubrule, 0. and Kostov, C., (1986) 'An i n t e r p o l a t i o n method t a k i n g i n t o account i n e q u a l i t y c o n s t r a i n t s I. Methodology ' , Math. Geology, 18, No. 1, p 33
G a l l i , A . , H u r i l l o , E. and Thomann, J. , (1984 ) . 'Dual K r i g i n g . I t s p r o p e r t i e s and i t s uses i n d i r e c t c o n t o u r i n g ' , i n ~ e o s t a t i s t i c s f o r N a t u r a l Resource C h a r a c t e r i z a t i o n , G. Ve r l ey e t a1 (eds . ) , D.
R e i d e l Pub1 i s h i n g , Do rd rech t
Gupta, A. K., (1983) 'On t h e expans ion o f t h e b i - v a r i a t e gamma d i s t r i b u t i o n ' , Tech. Repor t , Bow l i ng Green S t . Univ.
Hopke, Ph., Rupper t , D.F., e l u t e , P. R., He tzger , W.J. and Crowley, 0. J., (176) 'Geochemical P r o f i l e o f Chautauqua Lake Sediments ,' J. R a d i o a n a l y t i c a l Chem. 29, p. 73.
Jackson, K. and Marechal , A., (1979) 'Recoverable r ese rves e s t i m a t o r b y d i s j u n c t i v e k r i g i n g ; a case s t u d y ' , i n 1 6 t h A p p l i c a t i o n o f Computers and Ope ra t i ons Research i n t h e M i n e r a l I n d u s t r y - m e m i n g Eng. o f American I n s t i t u t e o f K i n i n g and M e t t a l l u r g y , N.Y. 240-249
Kim, Y. C., t.lyers, D. E. and Knudsen, H. P., (1977) 'Advanced g e o s t a t i s t i c s i n o r e r e s e r v e e s t i m a t i o n and mine p l a n n i n g ' , U. S. DOE, Grand J u n c t i o n 237 p
Lan tue jou l , Ch. and R i v o i r a r d , J. , (1984) 'Une methode de d e t e r m i n a t i o n d 'anamorphose' N-916, Fon ta i neb leau
Marechal, A., (1974) ' G e n e r a l i t i e s s u r l e s f o n c t i o n s de t r a n s f e r t ' , K-3C4 Fon ta i neb l eau
Marechal , A. , ( 1 975) 'Ana l yse numer ique des anamorphoses gauss iennes ' , N-418 Fon ta i neb leau
Marechal, A., (1976) 'The p r a c t i c e o f t r a n s f e r f u n c t i o n s : Numer ica l methods and t h e i r a p p l i c a t i o n s ' . M. Guarascio e t a1 (eds) Advanced G e o s t a t i s t i c s i n t h e M i n i n g I n d u s t r y 253-206, D. R e i d e l Pub. Co., Do rd rech t -Ho l l and
Matheran, G. , (1973) 'Le K r i geage Di s j o n c t i f ' , N-360/N-432 Fonta i nebleau
Matheron , G., (1974) 'Les f o n c t i o n s d~ t r a n s f e r t des p e t i t s panneaux' N-395, F o n t a i n e b l eau Royer
G - Matheron , G. . (1975) 'Modeles i s o f a c t o r i e l s d i s c r e t s e t modele de a
Walsh ' . N-449, Fon ta i neb leau Wacke
Ra the ron , G., (1975) 'Modeles i s o f a c t o r i e l s pou r l ' e f f e t ze ro ' C c N-659, Fon ta i neb leau Sc -
Matheron , G. , (1 976) ' A simp1 e s u b s t i t u t e f o r c o n d i t i o n a l e x p e c t a t i o n : The d i s j u n c t i v e k r i g i n g ' , i n M. Guarascio e t a1 ( eds ) Advanced G e o s t a t i s t i c s i n t h e M i n i n g I n d u s t r y , D. Re ide l Pub. Co., Dordrech t -Ho l l a n d
Matheron , G. , (1976) ' F o r c a s t i n g b l o c k g rade d i s t r i b u t i o n s : The t r a n s f e r f u n c t i o n s ' M. Guarasc io e t a1 ( e d s ) Advanced G e o s t a t i s t i c s i n t h e M i n i n g I n d u s t r y , D. Re ide l Pub. Co., D o r d r e c h t - H o l l a n d 237-251
Matheron , G . , (1977) 'Peu t -on imposer des c o n d i t i o n s d ' u n i v e r s a l i t e au k r i g e a g e d i s j o n c t i f ' , N-539. Fon ta i neb leau
Matheron , G. , (1981) ' ~ u a t ' r e f a m i l l e s d i s c r e t e ' , N.-703, F o n t a i n e b l e a u
Matheron , G., (1982) 'Pour une a n a l y s e k r i g e a n t e des donnees r e g i n a l i s e e s ,' N-732, Fon ta i neb leau
Myers, D. E., (1982) , ' C o - K r i g i n g : The M a t r i x Form', Math. Geology - 14, No 3 p. 249
Myers , D. E., (1983) . ' E s t i m a t i o n o f L i n e a r Combina t ions and Co- K r i g i n g ' , Math Geology, 15 No. 5 p 633
Myers, D. E., (1984) , 'Co -K r i g i ng : New Developments ' , i n G e o s t a t i s t i c s f o r N a t u r a l Resource c h a r a c t e r i z a t i o n , G. Ve r l ey e t a1 ( eds ) , D. Re ide l P u b l i s h i n g Co, Do rd rech t
Myers, D. E. and Car r , J., ( 1984 ) . ' C o - k r i g i n s and P r i n c i p a l Components, B e n t o n i t e Data r e - v i s i t e d ' , Sc iences de l a Ter re , 21. p. 65
Mye rs , D. E., (1985) ' C o - k r i g i n g methods and A1 t e r n a t i v e s ' , i n t h e Ro le o f Data i n S c i e n t i f i c Progress, P. G laeser , ( d ) . E l s e v i e r Pub.
Rendu, Jean-Miche l , (1980) ' D i s j u n c t i v e K r i g i n g s : Comparison o f Theory w i t h a c t u a l r e s u l t s ' , Math. Geology, 12, No. 4, p. 305
R i v o i r a r d , J., (1985) 'Convergence des deve l oppements en polynome d ' Hermi t e ' , N-955, Fon ta i neb leau
R o y e r , J. J. and V i e i r a , P.C.. ( 1 9 8 4 ) ' D u a l Fo rma l i sm o f K r i a i n o ' i n G e o s t a t i s t i c s f o r ~ a t u r a l . ~ e s o u r c e C h a r a c t e r i z a t i o n , G. Veryy e t a l ( eds . ) , D. R e i d e l P u b l i s h i n g , D o r d r e c h t
Wacke rnage l , H. , ( 1 9 8 5 ) "'The i n f e r e n c e o f t h e l i n e a r model o f t h e C o r e g i o n a l i z a t i o n i n t h e c a s e o f a g e o c h e m i c a l d a t a s e t ,' S c i e n c e s d e l l a T e r r e , No. 24, p. 8 1