Geoscience Reference
In-Depth Information
10
9
8
7
6
5
4
3
2
1
0
0
10
20
30
40
50
60
Distance
Fig. 11.10 Theoretical form of multifractal semivariogram in comparison with three experimen-
tal semivariograms based on 128 rows in patterns similar to the one shown in Fig. 10.22 .
Deviations between experimental semivariograms and continuous curve are relatively large, but
there is probably no significant bias (Source: Agterberg 2001 , Fig. 5)
adjoining blocks along a line. Experimentally, their semivariogram resembles
Matheron's semivariogram for infinitesimally small blocks. Extrapolation of their
spatial covariance function to infinitesimally small blocks would yield infinitely
large variance when h approaches zero.
Figure 11.17 shows three experimental semivariograms each based on 128 rows
of 128 numbers in patterns similar to the 2-D multifractal previously shown in
Fig. 10.22 . The theoretical semivariogram satisfies:
n
i
1
2
Þ ˄ ðÞþ 1
Þ ˄ ðÞþ 1
2 k ˄ ðÞþ 1
ʳ k
ðÞ ¼ ʾ 2
ðÞ
1
ð
k
þ
1
þ
ð
k
1
g
where k
represents distance between successive cells measured in
multiples of E , ʾ 2 ( E ) is the non-centered second-order moment obtained by
dividing the mass-partition function for q
¼
1, 2,
...
(2) is
the second-order mass exponent. The two parameters used for the theoretical
curve in Fig. 11.10 were in accordance with the results for q
¼
2 by number of cells, and
˄
2shownin
Figs. 11.4 and 11.5 . The experimental semivariograms are each based on 128 2
individual values. They deviate markedly from the theoretical curve although
on the average they are closer to it. Problems associated with lack of precision
of
¼
experimental
semivariograms
are well-known in spatial
statistics
( cf . Cressie 1991 ).
Search WWH ::




Custom Search