Flow of ground water through porous medium is governed by well-known Darcy’s law which states that the rate of flow, Q through a saturated porous medium is: (i) Proportional to the difference in hydraulic head Ah between the two flow sections, (ii) Proportional to the area of flow cross-section A, and (iii) Inversely proportional to […]
Darcy’s Law (With Equations) | Well Irrigation
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