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The Soil Profile
                118   Geotechnical Engineering

                                    5.6.6   Deciphering the Names
                                    Soil taxonomy names start with a prefix designating some key soil property used
                                    in classification, followed by more general names. For example, ‘‘Argalboll’’
                                    should be read as Arg-al-boll, for having a clay layer (arg), a white layer (alb),
                                    in a soft (Mollisoll soil order) soil. The taxonomic name therefore carries more
                                    information than the former name for this soil, which was ‘‘Planosol,’’ or flat soil.

                                    Soils are not isolated species, but form a continuum and are transitional one to
                                    another. Subgroup names are added in front to indicate whether a soil fits the
                                    central concept for that group, in which case it is called ‘‘Orthic.’’ If it represents
                                    an intergrade into another great group, that group will be indicated. This kind of
                                    detail is required to satisfy the sensibilities of soil scientists but ordinarily is of
                                    little concern in engineering.

                                    5.6.7   Important Soil Orders in Engineering

                                    The most critical soil orders for engineers are as follows:

                                    Histosol, because it designates peat that is weak, usually wet, highly compressible,
                                    and a nuisance in engineering.

                                    Vertisol, because it designates a considerable depth of highly expansive clay that
                                    can cause severe foundation and other problems.

                                    Aridosol, because it means desert conditions and may include highly expansive
                                    clay concentrated in shallow lakebeds or ‘‘playas,’’ and may include a layer
                                    cemented by secondary carbonates, ‘‘caliche.’’

                                    Mollisols and Alfisols, because they are likely to contain expansive clay B horizons
                                    (subsoils).

                                    Oxisols and Ultisols, because they are leached to such a low density that they may
                                    collapse under a foundation load, the clay mineral is not expansive but nevertheless
                                    can contribute to landslides, and there may be a surficial hard, laterite layer.


                                    5.6.8   Soil Database
                                    Identifications, descriptions, and engineering data for soil series are included in
                                    maps published by the USDA-NRCS. A soil series database is maintained at
                                    http://www.statlab.iastate.edu/soils/index/html/


                                    5.6.9   The Geotechnical Report
                                    Information, data, analyses, recommendations, and conclusions resulting from an
                                    investigation ordinarily are presented in a written report that is discussed in more

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