Laminar and Turbulent Flow of Water Through Sand

by M. Anandakrishnan,
G. H. Varadarajulu,


Serial Information: Journal of the Soil Mechanics and Foundations Division, 1963, Vol. 89, Issue 5, Pg. 1-16


Document Type: Journal Paper

Discussion: (See full record)
Discussion: (See full record)
Discussion: (See full record)

Abstract: The flow of water through sands during turbulence is represented by vn=k'i in which v is the velocity of flow; i the hydraulic gradient; k', a coefficient of turbulence; and n, a turbulence exponent. Values of n and k' are obtained from a plot of constant head permeability tests on four sands, shown as log-log plot of velocity versus hydraulic gradient. For truly laminar flow, n equals 1. For sands with d10 > 0.03 cms, the value of n is greater than 1, indicating turbulent flow. The value of n varies with grain size and hydraulic gradient. A plot of Reynold's number versus Friction Factor shows turbulent flow in one case of sand (d10 = 0.03 cm) with Reynold's number substantially less than 1. A method is shown for conducting variable head tests for turbulent flow. The quantity of seepage through sand during turbulent flow can be calculated using the appropriate values of k' and n determined in the laboratory by the procedures outlined herein.

Subject Headings: Turbulent flow | Sandy soils | Water flow | Turbulence | Hydraulic gradients | Soil water | Sand (hydraulic) | Fluid velocity

Services: Buy this book/Buy this article

 

Return to search