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
6
þ
4
4
:
We set
y 1 þ
y 2
Δ
y
2
y 2
y 1
y m
,
2
2
to obtain
y m Δ
y
2
y m þ Δ
y
2
y 1
,
y 2
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
y 1 4
y 2 4
þ
,
2
one obtains:
,
y m 2
y 2
24R m 2 þ
y m 4
24R m 4
2R m 2 þ Δ
D
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
D
S
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
D
S
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
D
S
2R m 2 S
:
ð
6
:
74
Þ
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