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31
In North Indian Plains, optimum depth of kor watering for wheat, is
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Answer & Solution
Answer: Option D
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32
The main cause of silting up a channel,
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Answer: Option D
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33
A fall which maintains its depth, is
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Answer & Solution
Answer: Option B
Solution:
A fall is a structure constructed across a canal to lower the water level and dissipate surplus energy caused by a difference in bed levels.

A low weir fall is specifically designed to maintain the depth of flow in the canal. It allows water to flow smoothly over a broad-crested weir while keeping the upstream depth nearly constant.

This type of fall helps in energy dissipation and prevents scouring and erosion downstream by stabilizing the flow conditions.

Trapezoidal notch fall and rectangular notch fall are primarily used for measuring discharge and controlling flow rather than maintaining depth.

Hence, among the given options, the fall that maintains its depth is the low weir fall.

Therefore, the correct answer as per exam and technical standards is Option B: A low weir fall.
34
Retrogression of the bed level of a river downstream a weir, occurs due to
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Answer: Option C
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35
The depth of the crest of a scouring sluice below the crest of a head regulator, is generally kept
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Answer: Option B
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36
For smooth entry of water in a canal, the angle between head regulator and water is generally kept
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Answer: Option C
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37
For a catchment area of 120 km2, the equilibrium discharge in m3/hour of an S-curve obtained by the summation of 6 hour unit hydrograph is
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Answer & Solution
Answer: Option A
Solution:
The correct answer is Option A: 0.2 x 106
The question involves understanding S-curve hydrographs and their relationship to unit hydrographs.
An S-curve hydrograph is created by summing an infinite series of unit hydrographs, each lagged by a duration equal to the unit hydrograph duration.
In this case, we have a 6-hour unit hydrograph.
The equilibrium discharge of the S-curve represents the constant rate of runoff when the rainfall continues indefinitely at a rate of 1 cm (or 1 unit) over the basin for the duration of the unit hydrograph.
The equilibrium discharge (Qeq) is calculated as:
Qeq = (Area of catchment x Rainfall depth) / Duration of Unit Hydrograph
Where, Area = 120 km2 = 120 x 106 m2
Rainfall depth = 1 cm = 0.01 m
Duration = 6 hours
Qeq = (120 x 106 m2 x 0.01 m) / 6 hours
Qeq = (1.2 x 106 m3) / 6 hours
Qeq = 0.2 x 106 m3/hour
Therefore, the equilibrium discharge of the S-curve is 0.2 x 106 m3/hour.
38
If the demand line drawn from a ridge in a flow mass curve does not intersect the curve again, it indicates that
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Answer: Option A
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39
The most suitable material for the central impervious core of a zoned embankment type dam is
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Answer: Option D
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40
The relation between probability (P) and recurrence interval (T) is given by
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Answer: Option A
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