Structural Analysis
Structural Analysis
6th Edition
ISBN: 9781337630931
Author: KASSIMALI, Aslam.
Publisher: Cengage,
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Field applications of hydraulic conductivity
Hydraulic conductivity is one of the hydraulic properties of soil defined as a measurement of the ability of a porous medium to permit water movement or fluid flow through it. It is denoted by the letter K. It is influenced by the density and viscosity o…
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Hi! Question is shown in the picture. It is required to find absolute permeability.

The answer is: 1 Darcy

1. Absolute permeability of a core sample is being measured by water-flooding. The core sample is mounted in a transparent cylindrical tube, as shown in the figure below, and the air-water surface is monitored as function of time. The tube is placed in a vertical position and the water is assumed to flow through the whole core sample, evenly distributed over the surface. Calculate the absolute permeability of the sample when the air-water surface uses 400 seconds to move 18 cm. Water 100 cm 82 cm Core sample 2 cm q Additional data: Density of water is 1 g/cm³ Water viscosity is 1 cP Gravitational constant is 980 cm/s² Thickness of the core sample is 2 cm
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Transcribed Image Text:1. Absolute permeability of a core sample is being measured by water-flooding. The core sample is mounted in a transparent cylindrical tube, as shown in the figure below, and the air-water surface is monitored as function of time. The tube is placed in a vertical position and the water is assumed to flow through the whole core sample, evenly distributed over the surface. Calculate the absolute permeability of the sample when the air-water surface uses 400 seconds to move 18 cm. Water 100 cm 82 cm Core sample 2 cm q Additional data: Density of water is 1 g/cm³ Water viscosity is 1 cP Gravitational constant is 980 cm/s² Thickness of the core sample is 2 cm
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