There is a capillary action that takes place above the groundwater table up to 2.3 m in height. Assume the unit weight of water is 10 kPa. Calculate the pore water pressure at the surface of the groundwater table. -13 kPa O 10 kPa 13 kPa 0 kPa

There is a capillary action that takes place above the groundwater table up to 2.3 m in height. Assume the unit weight of water is 10 kPa. Calculate the pore water pressure at the surface of the groundwater table. -13 kPa O 10 kPa 13 kPa 0 kPa

Fundamentals of Geotechnical Engineering (MindTap Course List)

5th Edition

ISBN:9781305635180

Author:Braja M. Das, Nagaratnam Sivakugan

Publisher:Braja M. Das, Nagaratnam Sivakugan

Chapter7: Seepage

Section: Chapter Questions

Problem 7.1P

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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.

Question

There is a capillary action that takes place above the groundwater table up
to 2.3 m in height. Assume the unit weight of water is 10 kPa. Calculate the
pore water pressure at the surface of the groundwater table.
-13 kPa
10 kPa
13 kPa
0 kPa

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