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<br />. <br /> <br />EM 1110-2-1913 <br />31 Mar 78 <br /> <br />. <br /> <br />Exploration from the ground surface will generally be adequate for levee <br />design purposes. Geophysical ground surface exploration can involve: <br />(1) seismic refraction and (2) electrical resistivity, Information ob- <br />tained from seismic refraction surveys includes material velocities, <br />delineation of interfaces between zones of differing velocities, and <br />the depths to these interfaces, The electrical resistivity survey is <br />used to locate and define zones of different electrical properties such <br />as pervious and impervious zones or zones of higher ionic activity such <br />as clayey strata, Both methods require distinct differences in prop- <br />erties of foundation strata materials in order to be effective, The <br />resistivity method requires a high resistivity contrast between mate- <br />rials being located, while the seismic method requires high contrast in <br />wave transmission velocities. Furthermore, the seismic method requires <br />that any underlying stratum transmit waves at a higher velocity than the <br />overlying stratum. Difficulties arise in the use of the seismic method <br />if the surface terrain and/or layer interfaces are steeply sloping or <br />irregular instead of relatively horizontal and smooth. Therefore, in <br />order to use these methods, one must be fully aware of what they can and <br />cannot do. EM 1110-2-1802 (ref. A-3a(3)) describes the use of both <br />seismic refraction and electrical resistivity. Dobrin (ref. A-5c) is a <br />valuable, general text on geophysical exploration, Applicable geophys- <br />ical exploration methods based on operation from the ground surface are <br />summarized in table 2-4. <br /> <br />c, Recent developments in the use of downhole logging devices have <br />shown that these tools can be used with success in correlating subsur- <br />face soil and rock stratification and in providing quantitative engineer- <br />ing parameters such as porosity, density, water content, and moduli, <br />They also provide valuable data for interpreting surface geophysical <br />data, The pUL~ose in using these methods is to allow cost sa\rings to <br />be made in the exploration program without lessening the quality of the <br />information obtained. This can be done by reducing the number of <br />borings required to determine subsurface stratification and by allowing <br />sampling to be done only in those zones where samples are necessary for <br />laboratory testing, thus reducing the number of undisturbed samples. <br /> <br />Section III, Field Testing <br /> <br />2-11. Preliminary Strength Estimates, It is often desirable to estimate <br />foundation strengths during Phase 1 of the exploration program, Various <br />methods of preliminary appraisal are listed in table 2-5. <br /> <br />2-12. Vane Shear Tests. Where undisturbed samples are not being ob- <br />tained or where samples of acceptable quality are difficult to obtain, <br />in situ vane shear tests may be utilized as a means of obtaining <br /> <br />2-9 <br /> <br />. <br /> <br />~. ~ ~: <br />