Reciprocal Levelling
Let the level difference among stations A and B is required to be measured precisely, and it is not probable to set up instrument midway among A and B (Figure 8). At first, instrument is set up and levelled extremely near to A and staff is held at A and B and readings recorded correspondingly. The instrument is then shifted to a position O2 very near to station B, and staff readings once again taken for station A and B correspondingly.
Let a1 and b1 be the readings from position O1, while a2 and b2 are readings along with instrument at O2. If there is no collimation error, the line of collimation should coincide along with horizontal line. If there is no error due to curvature and refraction etc., the level line should merge within horizontal line. Therefore, in an error free environment there shall be a single line in place of three, both in instrument position at O1 (Figure 8(a)) and at O2 (Figure (b)).
Figure : Reciprocal Levelling
Since instrument position O1 is extremely near to or exactly at A, there will be practically no deviation in staff reading at A (i.e. reading a1 is correct) although the true reading (level difference among A and B) would be
d = (b1 - e) - a1 . . . (4.2)
Similarly for instrument position extremely near to or exactly at B, the true level difference would be
d = b2 - a2 + e . . . (4.3)
Adding Eqs. (4.2) and (4.3), we get
2d = (b1 - a1) + (b2 - a2) or d = 1/2 {(b1 - a1) + (b2 - a2)} . . . (4.4)
Eq. (4.4) does not have a "e" term hence is error free. The magnitude of error e is acquired through subtracting Eq. (4.3) from Eq. (4.2).
i.e. e = 1/2 {(b1 - a1) - ( b2 - a2)}
This procedure of reciprocal levelling eliminates errors because of collimation and curvature. The refraction error might not be fully eliminated as there is a possibility that refraction of the air might change during shifting of instrument from O1 to O2. Therefore for more accurate results and to eliminate any probable refraction error, two independent instruments are set at stations O1 and O2 concurrently and readings a1, a2, b1 and b2 recorded at the similar instant.