Estimate the ratio of equivalent hydraulic conductivity (a) A layered soil is given in Figure Q2(a), Given thatH = 1 mH2 = 1.5 mH3 = 2 mk1 = 10-4 cm/seck2 = 3.2 X 10-2 cm/seck3 = 4.1 X 10-5 cm/seckH(eq)ky(eq)Estimate the ratio of equivalent hydraulic conductivity,kiH2H3Figure Q2 (a)

Hydraulic conductivity is the ability of a material to conduct fluid from the porous space. It is…

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Engineering

Civil Engineering

Estimate the ratio of equivalent hydraulic conductivity

Structural Analysis

6th Edition

ISBN:9781337630931

Author:KASSIMALI, Aslam.

Publisher:KASSIMALI, Aslam.

Chapter2: Loads On Structures

Section: Chapter Questions

Problem 1P

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Concept explainers

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 of the fluid. It is also called permeability. Hydraulic conductivity is defined as the ratio of velocity to the hydraulic gradient. The different methods used to determine the hydraulic conductivity are laboratory methods (constant head permeability tests and falling head tests), in-situ field methods (pumping in and pumping out tests), small scale field tests (infiltration tests and slug tests), and indirect methods such as estimation from grain size, consolidation test data, and horizontal capillary test. The pedotransfer function (PTF) method is a specific empirical estimating approach employed in the soil sciences is also used to determine the hydraulic conductivity of the soil.

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Estimate the ratio of equivalent hydraulic conductivity

(a) A layered soil is given in Figure Q2(a), Given that
H = 1 m
H2 = 1.5 m
H3 = 2 m
k1 = 10-4 cm/sec
k2 = 3.2 X 10-2 cm/sec
k3 = 4.1 X 10-5 cm/sec
kH(eq)
ky(eq)
Estimate the ratio of equivalent hydraulic conductivity,
ki
H2
H3
Figure Q2 (a)

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