Question Bank • QB_IDE_ADV_062 MSQ • 2 Marks

Section 5: Irrigation and Drainage Engineering

Irrigation Water Conveyance and Application Methods

Subtopic: Design of irrigation channels and underground pipelines

Question Statement:

Which of the following equations represent Lacey's canonical regime equations for stable alluvial irrigation canals in true regime?

Options:

  • (A) Silt factor: $f = 1.76 \sqrt{d_{mm}}$, where $d_{mm}$ is mean sediment diameter in millimeters
  • (B) Regime flow velocity: $V = \left( \frac{Q f^2}{140} \right)^{1/6}$
  • (C) Wetted perimeter: $P = 4.75 \sqrt{Q}$
  • (D) Regime longitudinal bed slope: $S = \frac{f^{5/3}}{3340 Q^{1/6}}$

Answer Key:

A, B, C, D

Step-by-Step Solution & Explanation

All four relationships are Lacey's exact fundamental regime equations: - A: $f = 1.76 \sqrt{d_{mm}}$ defines the silt factor. - B: $V = [Q f^2 / 140]^{1/6}$ relates velocity, discharge, and silt factor. - C: $P = 4.75 \sqrt{Q}$ determines the semi-elliptical wetted perimeter. - D: $S = \frac{f^{5/3}}{3340 Q^{1/6}}$ defines the unique regime bed slope.
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