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Phreatic line and discharge (crest 300 masl)

Short answer

Using Casagrande's method, y0 = 2.54 m, the phreatic line is y = sqrt(6.46+5.08x), and the exit lies 12.5 m along the downstream face. Specific discharge q = k·y0 = 1.271×10⁻⁵ m³/s per m.

A homogeneous earthen dam has the following data: dam crest level = 300.00 masl; deepest river bed level = 278.00 masl; HFL in the reservoir = 297.50 masl; dam crest width = 4.50 m; dam u/s slope = 3:1; dam d/s slope = 2:1 and coefficient of permeability of the dam material = 5×10−45 \times 10^{-4} cm/s. Determine the phreatic line of the dam section and the discharge passing through the dam.

Given data and assumptions: homogeneous dam on an impervious foundation, no drain, tail water neglected. Casagrande's basic parabola with focus at the d/s toe.

  • Dam height =300−278=22= 300-278 = 22 m; water head h=297.5−278=19.5h = 297.5-278 = 19.5 m; k=5×10−4k = 5\times10^{-4} cm/s =5×10−6=5\times10^{-6} m/s.

Step 1: Geometry

B=3(22)+4.5+2(22)=114.5 mb=3×19.5=58.5 m,0.3b=17.55 md=B−0.7b=114.5−40.95=73.55 m\begin{aligned} B &= 3(22)+4.5+2(22)=114.5\ \text{m}\\ b &= 3\times 19.5 = 58.5\ \text{m},\quad 0.3b=17.55\ \text{m}\\ d &= B-0.7b = 114.5-40.95 = 73.55\ \text{m} \end{aligned}

Step 2: Basic parabola

y0=h2+d2−d=19.52+73.552−73.55=2.54 my_0=\sqrt{h^2+d^2}-d=\sqrt{19.5^2+73.55^2}-73.55=2.54\ \text{m} y=y02+2y0x=6.46+5.08 xy=\sqrt{y_0^2+2y_0x}=\sqrt{6.46+5.08\,x}

Coordinates (xx from the d/s toe, yy above the base):

x from focus (m)y (m)
0.02.54
2.04.08
5.05.65
10.07.57
20.010.40
30.012.61
40.014.48
50.016.14
60.017.65
73.619.50

At x=dx=d, y=h=19.5y=h=19.5 m (corrected entry point A, located 0.3b=17.550.3b=17.55 m upstream of the point where the water line meets the u/s face).

Step 3: Corrections

  • Entry: the line starts at right angles to the u/s face and joins the parabola smoothly at A.
  • Exit: α=tan⁡−1(1/2)=26.57∘\alpha=\tan^{-1}(1/2)=26.57^\circ, so the parabola meets the d/s face at a+Δa=y01−cos⁡α=24.1a+\Delta a=\dfrac{y_0}{1-\cos\alpha}=24.1 m from the toe. Since α<30∘\alpha<30^\circ (outside Casagrande's chart), the exit point is found from Schaffernak's formula:
a=dcos⁡α−d2cos⁡2α−h2sin⁡2α=82.23−6,762−1,901=12.5 ma=\frac{d}{\cos\alpha}-\sqrt{\frac{d^2}{\cos^2\alpha}-\frac{h^2}{\sin^2\alpha}}=82.23-\sqrt{6,762-1,901}=12.5\ \text{m}

so the line leaves the d/s face about 12.5 m along the slope from the toe (about 5.6 m above the base). (Extrapolating Casagrande's factor 0.36 would give about 15.4 m.)

Step 4: Discharge

q=k y0=5×10−6×2.54=1.271×10−5 m3/s per mq=k\,y_0=5\times10^{-6}\times2.54=1.271 \times 10^{-5}\ \text{m}^3/\text{s per m}

(Schaffernak's q=k asin⁡αtan⁡α=5×10−6×12.5×0.447×0.5=1.40×10−5q=k\,a\sin\alpha\tan\alpha=5\times10^{-6}\times12.5\times0.447\times0.5=1.40\times10^{-5} m³/s per m is of the same order.)

Answer: y0=2.54y_0=2.54 m, phreatic line y=6.46+5.08 xy=\sqrt{6.46+5.08\,x}, exit point about 12.5 m up the d/s face; discharge q=1.271×10−5q=1.271 \times 10^{-5} m³/s per metre (≈1.098\approx1.098 m³/day per m).

✓ Answer checked by Claude Opus 5.5 (high effort)

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