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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