MCQ Surveying
Topics: Principles & classifications · Mapping & projections · Distance & directions · Leveling · Theodolite traversing · Plane table · Errors & adjustments · Curves
Q1. The primary objective of surveying is to:
Q2. The fundamental principle of surveying is to work from:
Q3. Geodetic surveying takes into account:
Q4. Plane surveying assumes the Earth's surface to be:
Q5. A map scale of 1:50,000 means 1 cm on the map represents:
Q6. Contour lines join points of equal:
Q7. UTM is an example of a:
Q8. Which map projection preserves angles (conformal)?
Q9. Gunter's chain has a length of:
Q10. The correction for slope when measuring distance L along a slope of angle θ is approximately:
Q11. True bearing is measured from:
Q12. Magnetic declination is the angle between:
Q13. Whole-circle bearing of a line is 120°. Its reduced bearing is:
Q14. The line of collimation of a dumpy level is:
Q15. Height of collimation method is preferred when:
Q16. A backsight (BS) in leveling is a reading on:
Q17. Reciprocal leveling is used to eliminate errors due to:
Q18. A theodolite is primarily used to measure:
Q19. In a closed traverse, the algebraic sum of latitudes should be:
Q20. Bowditch's rule distributes closing error in proportion to:
Q21. The deflection angle method is commonly used for:
Q22. Plane table surveying is a method of:
Q23. The two-point problem in plane tabling is used to:
Q24. Systematic errors are:
Q25. Accidental (random) errors tend to:
Q26. Least squares adjustment is used to:
Q27. The degree of a circular curve is the angle subtended at the centre by:
Q28. Transition curves are provided to:
Q29. Length of a simple circular curve of radius R and deflection angle Δ (radians) is:
Q30. Summit and valley curves on highways are examples of:
Surveying – Theory & Formulae
Surveying establishes relative positions of points for maps, engineering design, property boundaries and construction layout.
- Work from whole to part – establish primary control first, then densify; localises errors.
- Plane surveying – small areas; Earth treated as plane.
- Geodetic surveying – large areas; Earth curvature and spheroidal shape considered.
- Classifications by purpose (topographic, cadastral, engineering, route, hydrographic) and by instruments/methods.
Scale: representative fraction (e.g. 1:50,000). Large scale = more detail.
Contours: lines of equal elevation; spacing indicates slope.
Coordinate systems: geographic (φ, λ); projected grid (E, N) e.g. UTM, State systems.
Map projections transform the curved Earth to a plane. Types: conformal (preserve angles – Mercator, Transverse Mercator), equal-area, equidistant. Choice depends on region and purpose.
Distance measurement: chaining/taping, EDM, total station, GPS. Corrections: slope, temperature, tension, sag, absolute length.
$$ D_{\text{horizontal}} = L \cos\theta \approx L - L(1-\cos\theta) $$
Bearings
- Whole-circle bearing (WCB): 0°–360° from north.
- Reduced (quadrantal) bearing: N/S acute angle E/W.
- True, magnetic and grid bearings; magnetic declination converts magnetic ↔ true.
$$ \text{True bearing} = \text{Magnetic bearing} \pm \text{Declination} $$
Determines elevation differences. Instruments: dumpy, tilting, automatic, digital levels; leveling staff.
$$ HI = RL_{\text{BS}} + BS,\quad RL_{\text{point}} = HI - FS\text{ (or IS)} $$
- Height of collimation (HI) method – convenient for many intermediate sights.
- Rise and fall method – checks arithmetic; good for change points.
- Curvature and refraction corrections for long sights; reciprocal leveling eliminates collimation error when the instrument cannot be placed midway.
Theodolite measures horizontal and vertical angles. Traverse: series of connected lines with measured lengths and angles/bearings.
$$ \text{Latitude} = L\cos\theta,\quad \text{Departure} = L\sin\theta $$
Closed traverse: \(\sum Lat = 0\), \(\sum Dep = 0\) ideally. Closing error adjusted by:
- Bowditch (compass) rule – corrections proportional to side lengths.
- Transit rule – corrections proportional to latitude/departure of the side.
Graphical method: map is drawn in the field as observations are made. Methods: radiation, intersection, traversing, resection.
- Three-point problem – orient and locate station using three known points (Bessel, tracing-paper, trial-and-error methods).
- Two-point problem – when only two points are available (more involved).
Advantages: immediate check of work; suitable for small areas. Disadvantages: weather-sensitive; lower precision than instrumental surveying for large control networks.
- Blunders – mistakes; must be eliminated by checks.
- Systematic (cumulative) – follow a pattern (e.g. tape too short); correct by calibration/formulae.
- Random (accidental) – small, compensating; treated by least squares / probability.
Least squares adjustment minimises \(\sum v^2\) to obtain most probable values of unknowns under linear (or linearised) observation equations.
Horizontal circular curve
$$ T = R\tan\frac{\Delta}{2},\quad L = R\Delta\ (\Delta\text{ in rad}) = \frac{\pi R\Delta^\circ}{180},\quad E = R\left(\sec\frac{\Delta}{2}-1\right),\quad C = 2R\sin\frac{\Delta}{2} $$
where \(T\) = tangent length, \(L\) = arc length, \(E\) = external distance, \(C\) = long chord, \(\Delta\) = deflection angle, \(R\) = radius.
Degree of curve: central angle subtended by a standard chord (or arc), e.g. 30 m.
Transition (spiral) curves: curvature increases linearly with length; used to introduce super-elevation and centrifugal acceleration gradually.
Vertical curves: usually equal-tangent parabolas connecting grades \(n_1\) and \(n_2\); length designed for sight distance and comfort (summit and valley curves).
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