Civil Engineering - Water Resources Engineering
Exercise : Water Resources Engineering - Section 3
- Water Resources Engineering - Section 1
- Water Resources Engineering - Section 2
- Water Resources Engineering - Section 3
41.
Isopiastic lines are the contours
42.
The coefficients of permeability of soils of an unconfined aquifer and another confined aquifer were determined by pumping water from the wells and observing the effect of water table in two test wells at equal distances was found to be equal. The total height of confined aquifer H is given by
43.
The radius of influence is
44.
When a constant discharge 2.91 litres/sec. was obtained in a pumping test, the draw downs in the test wells at 3 m and 6.184 m were 2.6 m and 0.3 m respectively. If over-all depth of the pumping well was 16 m, the permeability of the soil, is
45.
If ω is unit weight of water, Q the discharge in cumecs, H the total head lift and η, the efficiency of the pump, the H.P. of the motor is
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