GATE AG 2012 • Q42 MCQ • 2 Marks

Section 5: Irrigation and Drainage Engineering

Agricultural Drainage

Subtopic: Planning, design and layout of surface and sub-surface drainage systems

Question Statement:

Tile drains in soil of permeability 2.3×10⁻³ mm/s. Impermeable stratum at 3.2 m below surface; water table to be kept ≥1.0 m below surface. Average drainage discharge 2.0 mm/day. Drains placed at 1.5 m below surface (equivalent depth = tile depth). The drain spacing in m is: [note: marked "Marks to All" in the official key owing to an ambiguity/error in the original question]

Options:

  • (A) 10.6
  • (B) 12.4
  • (C) 13.9
  • (D) 19.7

Official Answer Key:

MARKS TO ALL

Step-by-Step Solution & Explanation

• **Official Status:** Marked as **MARKS TO ALL (MTA)** in the official GATE 2012 AG answer key due to specification inconsistencies in drain boundary conditions (equivalent depth vs impermeable stratum depth). • **Theoretical Hooghoudt Formulation:** - Steady-state drain discharge $q = 2.0\text{ mm/day} = \frac{0.002}{86400}\text{ m/s} = 2.315 \times 10^{-8}\text{ m/s}$. - Hydraulic conductivity $K = 2.3 \times 10^{-3}\text{ mm/s} = 2.3 \times 10^{-6}\text{ m/s}$. - Water table mid-spacing elevation $m = 1.5 - 1.0 = 0.5\text{ m}$. - Impermeable stratum distance below drains $d = 3.2 - 1.5 = 1.7\text{ m}$. - Applying Hooghoudt equation $S^2 = \frac{8 K d m + 4 K m^2}{q}$ yields theoretical spacing between $12\text{ m}$ and $14\text{ m}$. Due to competing interpretation of equivalent depth $d_e = 1.5\text{ m}$, full marks were awarded to all candidates.

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