Geoscience Reference
In-Depth Information
Inserting into (
6.70
) and replacing
R
1
2
and
1
R
2
2
with
1
R
m
2
produces:
1
y
1
2
2R
m
2
þ
y
m
2
2R
m
2
þ
y
2
2
2R
m
2
þ
y
1
4
24R
m
4
þ
y
m
4
24R
m
4
þ
y
2
4
24R
m
4
S
6
D
ᄐ
6
þ
4
4
:
We set
y
1
þ
y
2
Δ
y
2
ᄐ
y
2
y
1
y
m
ᄐ
,
2
2
to obtain
y
m
Δ
y
2
y
m
þ
Δ
y
2
y
1
ᄐ
,
y
2
ᄐ
y
2
2
:
Since the term containing y
4
is minute, and hence replaced by y
m
4
þ
ʔ
and y
1
2
y
2
2
2y
m
2
þ
ᄐ
y
1
4
y
2
4
þ
ᄐ
,
2
one obtains:
,
y
m
2
y
2
24R
m
2
þ
y
m
4
24R
m
4
2R
m
2
þ
Δ
D
ᄐ
S 1
þ
ð
6
:
71
Þ
and the resulting equation:
y
m
2
y
2
24R
m
2
þ
y
m
4
24R
m
4
2R
m
2
þ
Δ
Δ
S
ᄐ
D
S
ᄐ
S
:
ð
6
:
72
Þ
The above is the formula for the distance correction of the Gauss projection.
When S
350 km, the equation has an accuracy of 0.001 m, or
better. Therefore, this formula is applicable to computations of the first-order
triangulation.
For the second-order triangulation (accurate to 0.01 m), we can leave out the last
term in the above equation, namely:
<
70 km and y
m
<
y
m
2
y
2
24R
m
2
2R
m
2
þ
Δ
Δ
S
ᄐ
D
S
ᄐ
S
:
ð
6
:
73
Þ
For the third-order triangulation (accurate to 0.1 m), one has only to consider the
first term:
y
m
2
Δ
S
ᄐ
D
S
ᄐ
2R
m
2
S
:
ð
6
:
74
Þ
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