Correct Answer - Option 1 : 10
4/3
Concept:
Determination of seepage discharge when the medium is isotropic:
Seepage discharge per meter length is given by, \(q = kh\frac{{{N_f}}}{{{N_d}}}\)
Where, h = Hydraulic head or head difference between upstream and downstream level or head loss through the soil
Nf = Total number of flow channels
Nd = Total number of equipotential drops
k = Coefficient of permeability
Calculation:
Permeability of sand, Ksand = 3 × 10-3 cm/sec
Permeability of clay, Kclay = 9 × 10-7 cm/sec
h, Nf and Nd are same for both the soil (given in the question)
∵ \(q = kh\frac{{{N_f}}}{{{N_d}}}\)
⇒ q ∝ K
\(\frac{{{q_{sand}}}}{{{q_{clay}}}} = \frac{{{K_{sand}}}}{{{K_{clay}}}}\)
⇒ \(\frac{{{q_{sand}}}}{{{q_{clay}}}} = \frac{{3 \times {{10}^{ - 3}}}}{{9 \times {{10}^{ - 7}}}} = \frac{1}{3} \times {10^4}\)