Geoscience Reference
In-Depth Information
Fig. 3.1 Classical Neyman-
Pearson decision-making
procedure to choose between
the two hypotheses H 0 and H 1
true. In this case, the parameter a of the real density f a can be equal to neither a 0
or a 1 .
Errors of the
first kind,
a
, and the second kind,
b
, satisfy the following formulas
respectively:
5 E a1 n E a0 nÞð D a0 1 = 2
2 n ;
a exp½ 0
:
g
ð 3
:
2 Þ
b exp½ 0 : 5 E a1 n E a0 nÞð D a1 1 = 2
2 n ;
g
ð 3 : 3 Þ
where
Z 1
E a n ¼
ln f a1 ð x Þ=
½
f a0 ð x Þ
f a ð x Þ dx
ð 3
:
4 Þ
1
Z 1
2 f a ð x Þ dx E a ðÞ
2
D a n ¼
f ln f a1 ð x Þ=
½
f a0 ð x Þ
g
ð 3
:
5 Þ
1
Neyman-Pearson theory focuses on testing a statistical hypothesis provided that
the volume of observations allows the calculation of basic statistical characteristics
including the empirical distribution function. In this case, theoretical probability
density function f a (x) is assessed on the base of
2 -criterion. Unfortunately,
empirical results of environmental monitoring usually do not satisfy this condition.
In this case a sequential procedure is used where the sample size is not
ˇ
fixed in
advance. Instead, data are evaluated as they are collected, and further sampling is
stopped in accordance with a pre-de
cant results
are observed. Thus, a conclusion may sometimes be reached at a much earlier stage
ned stopping rule as soon as signi
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