Page 212 - Geotechnical Engineering Soil and Foundation Principles and Practice
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Soil Water
                                                                                             Soil Water  207

                   10.3. Prepare a table outlining a classification of soil water and state the basis
                        for each class.
                   10.4. How can one distinguish by means of a single boring between a main
                        water table and a perched water table?
                   10.5. Name two ways in which a soil can be saturated above the water table.
                   10.6. Name two natural processes by which the elevation of a water table may
                        be lowered.
                   10.7. How may a water table be lowered artificially?
                   10.8. What causes a water table to rise? Explain.
                   10.9. What clues would you look for to indicate former high elevations of a
                        water table?
                  10.10. What happens when a dispersed clay dries out? Explain in terms of
                        double-layer theory.
                  10.11. A soil is dispersed for particle size analysis by adding a small amount of a
                        sodium salt. Explain how this works using double-layer theory.
                  10.12. A landslide in wet clay soil is taking the back yard of a multimillion-dollar
                        home owned by your favorite movie star, and if it keeps on raining the
                        house will be next to go. Wells will not drain the smectite clay and it is not
                        practical to move the house. Two possibilities are suggested, electrical
                        drainage, or boring holes in the clay and filling the holes with quicklime.
                        Tell how each method will operate.
                  10.13. How will calcium carbonate, CaCO 3 , affect the pH of water? Compare its
                        effectiveness with hydrated lime for chemical soil stabilization.
                  10.14. What is the difference between a water dipole and hydrogen-bonded
                        water? Which occurs where?
                  10.15. What is the zeta potential?
                  10.16. DNA fragments carry a negative charge and are separated using
                        electrophoresis because smaller pieces move faster. Suggest a reason why
                        they move faster.

                  Further Reading

                  Baver, L. D., Gardner, W. H., and Gardner, W. R. (1972). Soil Physics, 4th ed. John Wiley
                     & Sons, New York.
                  Bjerrum, L., Moum, J., and Eide, O. (1967). ‘‘Application of Electro-osmosis to a
                     Foundation Problem in a Norwegian Quick Clay.’’ Geotechnique 17, 214–235.
                  Grim, R. E. (1968). Clay Mineralogy, 2d ed. McGraw-Hill, New York.
                  Ho, Clara, and Handy, R. L. (1963). ‘‘Characteristics of Lime Retention by
                     Montmorillonitic Clays.’’ Highway Research Record 29, 55–69.
                  Mitchell, J. K. (1993). Fundamentals of Soil Behavior, 2nd ed. John Wiley & Sons,
                     New York.




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