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CESIUM                                                                141

            Cesium

              Cesium is the heaviest alkali metal and also the rarest, with an abundance
            of  about 7  x    wt.% in the earth’s crust (Fleischer, 1962). It has an ionic
            radius  of  1.69 8, which  is  distinctly  larger than  potassium,  and it cannot
            replace potassium in minerals as easily as rubidium; probably because of  this,
            it forms its own minerals. It is leached from igneous and metamorphic rocks
            by  water  during weathering,  and is adsorbed by  hydrolysate  sediments and
            soils more  readily  than rubidium or potassium.  Its low ionization  potential
            indicates  that  it  has  the greatest  chemical  reactivity  of  the alkali metals.
            Cesium and rubidium were discovered in  1860 by  Robert Bunsen by use of
            spectral analysis, a method which he and Kirchhoff invented.
              Cesium  concentrates primarily like rubidium,  in marine argillaceous sedi-
            ments.  Some shales contain about 15 ppm; deep-sea red  clays, 20 ppm; and
            glauconite,  15 ppm  of  cesium  (Goldschmidt,  1958). Sea  water  contains
            5 x      mg/l of  cesium, and some subsurface brines contain up to 1 mg/l.

            Beryllium
              Beryllium is a member of  the alkaline earth group in the periodic chart of
            the  elements,  but  few  of  its  properties  are similar to the  more  abundant
            members,  such  as  magnesium,  calcium,  and  strontium.  Beryllium,  like
            lithium,  is a light element with  an atomic weight of  9.012  (Table 5.111;  see
            also Moeller, 1954), and like lithium,  it is an exception to the rule that light
            elements are more abundant than heavy elements. The earth’s crust contains
            about 6 x      wt.% of beryllium (Fleischer, 1962).
              In sedimentary rocks, beryllium is restricted primarily to hydrolysates and
            especially  to  bauxites  enriched  in  aluminum  (Goldschmidt,  1958). Shales
            contain  about  6 ppm,  and  some  coal  ashes  contain  up  to 8,000 ppm,  al-
            though  generally  only about 4 ppm.  The concentration  of  beryllium  in sea



            TABLE 5.111

            Properties of the alkaline earth metals
            Property      Beryllium  Magnesium   Calcium    Strontium   Barium

            Atomic number  4        12          20          38          56
            Ionic radius
            (A 1          0.31       0.65        0.99        1.13        1.35
            Outer electronic
            configuration   1s’ 2s’   2s’ 2p6 3s’   3s2 3p6 4s2   4s’ 4p6 5s2   5s2 5p6 6s’
            Atomic weight   9.012   24.31       40.08       87.62      137.34
            Ionization
            potential (V)   9.320    7.644       6.111       5.692       5.210
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