Page 110 - Geotechnical Engineering Soil and Foundation Principles and Practice
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The Soil Profile
                                                                                          The Soil Profile  105

                  Y       accumulation of gypsum
                  Z       accumulation of soluble salts, for example in dried lakebeds

                  Many of these substripts have important implications in engineering and in
                  geology. For example, an A b horizon is a buried topsoil, and buried topsoils can
                  be conducive to landslides.


                  Question: Which other subscripts can have engineering significance?


                  5.3   FACTORS INFLUENCING A SOIL PROFILE


                  5.3.1  Climate
                  Climate, in particular the patterns of temperature and precipitation, exerts
                  a major influence on weathering. For example, soils in the humid tropics are far
                  more deeply and severely weathered than those in arctic or desert conditions.

                  Weathering Stages of a Soil
                  Climate strongly affects clay mineralogy because of selective leaching and
                  reconstitution of mineral ingredients. A guide to intensity of weathering is the
                  weathering stages for the fine-clay size fraction by M. L. Jackson and his
                  associates at the University of Wisconsin (Table 5.1).

                  As might be expected, gypsum and its occasional companion, halite or rock
                  salt, are relatively soluble and leach out first, so a soil containing gypsum is not
                  highly weathered unless the gypsum came in later as a secondary mineral.



                  Stage          Mineral                     Formula or common occurrence  Table 5.1
                  1              Gypsum                      CaSO 4  .  2H 2 O, an evaporite  Jackson-Sherman
                  2              Calcite                     CaCO 3 , limestone            (1953) sequence
                  3              Hornblende etc.             Dark minerals in granite, basalt  indicated by minerals
                  4              Biotite                     Black mica in granite         remaining in the
                  5              Feldspars                   Dominant in granite, basalt   fine-clay fraction.
                  6              Quartz                      SiO 2 abundant in granite     Arrows indicate
                  7              Muscovite                   K-rich white mica, granite    progressive removal
                  8              Illite, vermiculite, chorite  Mica clay mineral, shale    of potassium (K) in
                  9                                          Expansive clay mineral, soil  the series muscovite
                                !
                  10             Kaolinite                   Nonexpansive China clay       to smectite, and of
                  11             Gibbsite                    Al(OH) 3 , aluminum ore       silica (SiO 2 ) in the
                                 Smectite   !
                  12             Hematite                    Fe 2 O 3 , red iron oxide     series smectite to
                  13             Anatase                     TiO 2 , soil                  gibbsite


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