Page 247 - Geotechnical Engineering Soil and Foundation Principles and Practice
P. 247

Pore Water Pressure, Capillary Water, and Frost Action
                242   Geotechnical Engineering

                                    is to place the structure on a raised gravel pad that has a relatively high thermal
                                    conductivity so that it cools from the outside. This and other arrangements are
                                    discussed by Phukan (1991).


                11.11    SUMMARY


                                    Positive pore water pressure weakens soil by reducing friction between soil grains.
                                    Pore pressure therefore is subtracted from total stress to obtain effective stress.

                                    Capillary action draws water up into a fine-grained soil, creating a capillary
                                    fringe. Soil in the capillary fringe may be saturated, so saturation is not a criterion
                                    for locating a groundwater table. A groundwater table is measured in an open
                                    boring where there is no capillary effect. Pore water pressures in a capillary fringe
                                    are negative relative to atmospheric pressure.

                                    Under static conditions, pore water pressure increases linearly with depth below a
                                    groundwater table, whereas soil weight-induced stresses increase with depth below
                                    the ground surface.

                                    Compressing saturated soil increases its pore water pressure. The increase over
                                    static groundwater conditions is excess pore water pressure, which like static pore
                                    water pressure acts to decrease effective stress and friction.

                                    Capillary action is a lead actor in frost heave.

                                    Permafrost conditions require special considerations and will become more
                                    prominent as mineral resources are developed in Arctic areas.


                                    Problems

                                     11.1. Why is the term ‘‘matric potential’’ now preferred over ‘‘capillary
                                          potential’’?
                                                                                                    3
                                     11.2. A soil unit weight above the groundwater table averages 115 lb/ft and
                                                                                 3
                                          below the groundwater table averages 112 lb/ft . The water table is 6 ft deep
                                          below the ground surface. Prepare a plot of total and effective stresses to
                                          a depth of 20 ft.
                                     11.3. Distinguish between artesian water pressure and excess pore water
                                          pressure.
                                     11.4. (a) Calculate the height of rise of pure water in a clean glass tube whose
                                          inside diameter is 0.15 mm, using T ¼ 7.75 mN/m. (b) What is the height of
                                          rise if the tube is sufficiently dirty to produce a wetting angle of 158?
                                     11.5. If the outside diameter of the tube in Problem 11.4 is 0.35 mm, what is the
                                          compressive stress in the walls of the tube in part (a) of that problem?

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