JAWAHARLAL NEHRU TECHNOLOGICAL UNIVERSITY HYDERABAD
JAWAHARLAL NEHRU TECHNOLOGICAL UNIVERSITY HYDERABAD B.Tech II Year SURVEYING Previous Question Paper (March - 2022 - R15)
Answer any five questions
All questions carry equal marks
Main
Discuss in brief the different sources of errors in surveying.
Answer
Errors in surveying arise from various sources and are broadly classified into three categories:
- Instrumental Errors: These result from imperfections or faulty adjustments of the surveying equipment. Examples include a tape that is too long or short, a poorly adjusted level, or a compass needle that is not perfectly balanced. These can often be minimized by proper calibration and maintenance.
- Personal Errors: These are caused by the human element, such as limitations in human senses (sight, touch, hearing) or lack of skill. Examples include incorrect reading of a scale, improper leveling of the instrument, or mistakes in recording data. These can be reduced by careful observation and repeated measurements.
- Natural Errors: These arise from external environmental conditions such as temperature, humidity, wind, gravity, and refraction. For instance, the expansion or contraction of a steel tape due to temperature changes or the effect of atmospheric refraction on leveling. These are often corrected by applying mathematical corrections based on observed environmental conditions.
N 68° 15′ E is magnetic bearing of a line AB. The included angle ∠ABC measured 89° 20′. The point C is situated to the north of AB. Compute the bearing of BC. The deflection angle of CD is 25° 25′ to the right. Compute the bearing of CD.
Answer
Given:
Since point C is to the north of AB, the angle is measured clockwise from the line BA. The back bearing of AB is S 68° 15′ W, which is 248° 15′ in whole circle bearing (WCB). The bearing of BC is calculated as follows:
Converting back to quadrantal bearing:
The deflection angle of CD is 25° 25′ to the right. The bearing of CD is calculated by adding the deflection angle to the bearing of BC:
Since the result exceeds 360°, subtract 360°:
Therefore, the bearing of CD is N 3° 00′ E.
Find the length and Bearing of the side DA of the traverse ABCD from the following data:
| Line | Length (m) | Bearing |
|---|---|---|
| AB | 466.20 | 115° |
| BC | 378.50 | 38° |
| CD | 327.50 | 308° |
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What are the advantages and disadvantages of plane table surveying?
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What are the temporary adjustments of a leveling.
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What are the indirect methods of locating a contour? Write about any one method.
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The following staff readings were taken with a level which was shifted after 3rd, 8th and 10th readings: 1.875, 2.235, 3.310, 1.385, 0.930, 2.125, 1.125, 4.120, 1.875, 2.030 and 2.765. The first reading was taken with the staff held upon a benchmark of elevation 122.125. Enter the readings in the level book form apply the usual checks. Find also the difference in level between the first and last points.
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Derive an expression for trapezoidal formula for volume.
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A series of offsets were taken from a chain line to a curved boundary line at intervals of 15 meters in the following order: 0, 2.65, 3.80, 3.75, 4.65, 3.60, 4.95, 5.85 m. Compute the area between the chain line, the curved boundary and the end offsets by trapezoidal rule.
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Calculate the volume of earth work by Prismoidal formula in a road embankment with the following data: Formation level at chain age 0 is 202.30, top width is 0.6 m side slopes are 2:1. The longitudinal gradient of the embankment is 1 in 100 rising. The ground is assumed to be level all across the longitudinal section.
| Chainage (m) | 0 | 100 | 200 | 300 | 400 |
|---|---|---|---|---|---|
| Ground Levels (m) | 201.70 | 202.90 | 202.40 | 204.70 | 206.90 |
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How would you measure Horizontal angle by repetition with a Theodolite.
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Describe the various methods of traversing with Theodolite.
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Two horizontal distances of 40 m and 80 m were accurately measured, and the intercepts on the staff between the outer stadia wires were 0.626 and 0.926 respectively. Calculate the tachometric constants.
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Write the difference between simple curves and compound curves.
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