Next: Regionalized Variables
Up: Some Theoretical Distributions
Previous: The Normal Distribution N()
  Contents
The Lognormal Distribution
Applied work shows that values of ore samples do usually not follow the
normal distribution, however, the logarithm of the values might much
better be approximated by a normal distribution.
This can be observed especially frequently in ore deposits with low
grades, or when investigating geochemical data (trace elements). The distribution is
right skewed (skewness is positive), and a typical histogram of samples
from a gold mine is presented in Figure 2.9.
Figure 2.9:
Histogram of Samples from a Gold Mine.
 |
The density function
is defined by
The transformed variable
is normally distributed as
. After the transformation
of the
data, the parameters
and
may be estimated as in case of
the normal distribution, namely as
Using the original data,
can also be found via the
geometric mean:
or
An equivalent estimator of
also is the median of the
untransformed data.
Example
2.5: In the following two tables (Koch and Link, 1970-71[13]) we
see frequencies of grades of samples of gold. One can immediately see
the difficulties for the estimation of
.
Frequency Distribution of 1536 Gold Samples (in dwt) from the
City Deep Mine, South Africa.
Interval |
|
Cumulative |
Rel. Cumulative |
|
[dwt/short ton] |
Frequ. |
Frequ. |
Frequ. [%] |
|
0 |
- | 5 |
910 |
910 |
59.24 |
5 |
- | 10 |
208 |
1118 |
72.79 |
10 |
- | 15 |
118 |
1236 |
80.47 |
15 |
- | 20 |
80 |
1316 |
85.68 |
20 |
- | 25 |
54 |
1370 |
89.19 |
25 |
- | 30 |
33 |
1403 |
91.34 |
30 |
- | 35 |
24 |
1427 |
92.90 |
35 |
- | 40 |
13 |
1440 |
93.75 |
40 |
- | 45 |
14 |
1454 |
94.66 |
45 |
- | 50 |
8 |
1462 |
95.18 |
50 |
- | 55 |
8 |
1470 |
95.71 |
55 |
- | 60 |
10 |
1480 |
96.36 |
60 |
- | 65 |
4 |
1484 |
96.62 |
65 |
- | 70 |
4 |
1488 |
96.88 |
70 |
- | 75 |
3 |
1491 |
97.07 |
75 |
- | 80 |
1 |
1492 |
97.14 |
80 |
- | 85 |
1 |
1493 |
97.20 |
85 |
- | 90 |
4 |
1497 |
97.46 |
90 |
- | 95 |
1 |
1498 |
97.53 |
95 |
- | 100 |
7 |
1505 |
97.99 |
100 |
- | 105 |
3 |
1508 |
98.18 |
105 |
- | 110 |
2 |
1510 |
98.31 |
110 |
- | 115 |
3 |
1513 |
98.51 |
120 |
- | 125 |
2 |
1515 |
98.63 |
125 |
- | 130 |
1 |
1516 |
98.70 |
130 |
- | 135 |
5 |
1521 |
99.03 |
145 |
- | 150 |
1 |
1522 |
99.09 |
150 |
- | 155 |
1 |
1523 |
99.16 |
155 |
- | 160 |
3 |
1526 |
99.35 |
180 |
- | 185 |
1 |
1527 |
99.42 |
190 |
- | 195 |
2 |
1529 |
99.56 |
205 |
- | 210 |
2 |
1531 |
99.68 |
215 |
- | 220 |
1 |
1532 |
99.72 |
245 |
- | 250 |
1 |
1533 |
99.81 |
305 |
- | 310 |
1 |
1534 |
99.87 |
420 |
- | 425 |
1 |
1535 |
99.93 |
620 |
- | 625 |
1 |
1536 |
100.00
|
|
Frequency Distributions of Means of Samples of Different Size. The
samples were selected randomly from a set of 900 gold samples from the
Homestake Mine.
Interval |
Sample Size |
|
[ppm Au] |
1 |
5 |
25 |
100 |
|
0 |
- | 1 |
439 |
175 |
0 |
0 |
1 |
- | 2 |
120 |
121 |
3 |
0 |
2 |
- | 3 |
67 |
105 |
36 |
1 |
3 |
- | 4 |
44 |
88 |
82 |
5 |
4 |
- | 5 |
35 |
69 |
124 |
38 |
5 |
- | 6 |
26 |
66 |
131 |
149 |
6 |
- | 7 |
23 |
57 |
146 |
222 |
7 |
- | 8 |
14 |
40 |
114 |
201 |
8 |
- | 9 |
23 |
45 |
83 |
198 |
9 |
- | 10 |
14 |
35 |
73 |
98 |
10 |
- | 11 |
16 |
31 |
56 |
49 |
11 |
- | 12 |
13 |
16 |
38 |
22 |
12 |
- | 13 |
13 |
12 |
25 |
10 |
13 |
- | 14 |
13 |
23 |
34 |
5 |
14 |
- | 15 |
9 |
15 |
15 |
2 |
15 |
- | 16 |
10 |
19 |
15 |
|
16 |
- | 17 |
8 |
11 |
7 |
|
17 |
- | 18 |
7 |
5 |
5 |
|
18 |
- | 19 |
9 |
4 |
7 |
|
19 |
- | 20 |
1 |
1 |
1 |
|
20 |
- | 21 |
6 |
5 |
0 |
|
21 |
- | 22 |
7 |
7 |
4 |
|
22 |
- | 23 |
1 |
5 |
2 |
|
23 |
- | 24 |
6 |
7 |
0 |
|
24 |
- | 25 |
1 |
1 |
0 |
|
25 |
- | 26 |
3 |
4 |
0 |
|
26 |
- | 27 |
3 |
5 |
0 |
|
27 |
- | 28 |
4 |
1 |
0 |
|
28 |
- | 29 |
2 |
3 |
0 |
|
29 |
- | 30 |
6 |
6 |
1 |
|
30 |
- | 31 |
2 |
4 |
|
|
31 |
- | 32 |
6 |
1 |
|
|
32 |
- | 33 |
7 |
0 |
|
|
33 |
- | 34 |
1 |
1 |
|
|
34 |
- | 35 |
0 |
1 |
|
|
35 |
- | 49 |
14 |
7 |
|
|
50 |
- | 99 |
21 |
3 |
|
|
100 |
- | |
8 |
|
|
|
|
Next: Regionalized Variables
Up: Some Theoretical Distributions
Previous: The Normal Distribution N()
  Contents
Rudolf Dutter
2003-03-13