Environmental Engineering Reference
In-Depth Information
where L is the number of strata, a h are the relative areas of the strata (stratum
weights), and ¯
y h is the estimated mean of stratum h estimated by Eq. ( 4.3 ).
Provided all numbers of sampling locations are larger than 1, the sampling
variance of ¯
y STSI can be estimated by
V
y STSI
a h V
y h ,
L
¯
¯
=
(4.8)
h
=
1
y h is the estimated sampling variance of ¯
where V
¯
y h
V
y h
S h ( y )
n h
¯
=
,
(4.9)
with S h ( y )the spatial variance of y within stratum h , that can be estimated by
(compare with Eq. ( 4.5 ))
n h
y hi − ¯
y h 2
1
( n h
S 2 h ( y )
=
,
(4.10)
1)
i
=
1
and n h is the number of sampling locations in stratum h .
If only one location per stratum is selected, the sampling variance can be
approximated by the collapsed strata estimator (Cochran 1977 ).
The 100(1
α
)% confidence interval for
y is given by
¯
V
y STSI ,
t ( df )
1
¯
¯
y STSI ±
2 ·
(4.11)
α/
where t ( df )
1
2) quantile of the Student distribution with df degrees
of freedom. For df we can either take simply n
is the (1
α/
α/
2
L (Lohr 1999 , p. 101), or it can be
approximated by Sattherwaites method (Nanthakumar and Selvavel 2004 )
h = 1 a h S 2 h ( y )
2
n h
df
(4.12)
S 2 h ( y )
n h
2
h = 1 a h
1
n h
1
Random Grid Sampling
Similar to SI, for SY the spatial mean is estimated by the unweighted mean of the
measurements in the sample
n
1
n
¯
y SY =
y i .
(4.13)
i
=
1
 
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