Difficulty: Easy
Correct Answer: All of the above
Explanation:
Introduction / Context:Differential levelling establishes elevations by reading a staff from a fixed instrument set-up. Knowing how the line of collimation and staff readings relate to the horizontal reference surface prevents conceptual errors in field notes and computations.
Given Data / Assumptions:
Concept / Approach:With the instrument clamped, the BS and FS share the same line of collimation (horizontal plane). A staff reading is effectively the vertical distance between this plane and the staff zero at the observed point. In geometric levelling, we treat the horizontal reference as a level surface passing through the telescope axis for the small area around the instrument.
Step-by-Step Solution:
BS and FS from one set-up share the same horizontal line of sight.Staff reading concept: reading = HI − RL_point, i.e., vertical drop from the plane of collimation to the ground point.Local level surface approximation: coincides with the horizontal reference through the instrument axis.Therefore, all three statements are mutually consistent and correct.Verification / Alternative check:Field-book checks (sum BS − sum FS = last RL − first RL) rely on the common horizontal plane assumption for each set-up and confirm consistency when arithmetic balances.
Why Other Options Are Wrong:
Common Pitfalls:Confusing the reference plane when the instrument is moved; ignoring curvature/refraction over long sights (where refined corrections may be required); mixing instrument height with staff readings.
Final Answer:All of the above
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