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              Main Group Elements                                                                           3

              TABLE II Some Physical and Atomic Properties of Main Group Elements, Groups 13–16 (IIIA–VIA)
                                                                                 First      Relative
                                                                                ionization  abundance    ∆H ◦
                                                                                                           f
                      Density                    ∆H vap  Atomic                  energy   in crustal rock  hydride
                          3
              Symbol  (g/cm )  mp ( C)  bp ( C)  (kJ/mol)  radius ( ˚ A)  Electronegativity a  (kJ/mol)  (order in ranking) b  (kJ/mol)
                                           ◦
                                  ◦
               B        2.34     2180    3650    505      0.88        2.0         801         38          —
               Al       2.70      660    1467    291      1.43        1.5         578          3          —
               Ga       5.91      30     2403    270      1.22        1.6         579        33 (tie)     —
               In       7.31      157    2080    232      1.62        1.7         558         61          —
               Tl      11.85      304    1457    166      1.71        1.8         589         58          —
               C        2.25     3570    4830    715      0.77        2.5        1086         17         −74.9
               Si       2.33     1414    2680    383      1.18        1.8         786          2          34.3
               Ge       5.32      937    2830    328      1.22        1.8         761         53          —
               Sn       7.30      232    2270    296      1.41        1.8         708         48          —
               Pb      11.35      328    1750    178      1.46        1.9         715         36          —
               N     (1.25 g/liter)  −210  −196    2.8    0.70        3.0        1402        33 (tie)    −46.2
               P        1.83      44      280     12.4    1.10        2.1        1012         11           5.4
               As       5.73      800   Sublimes  32.4    1.21        2.0         947         51          66.4
               Sb       6.69      631    1580    194.8    1.41        1.9         834         62         145.1
               Bi       9.75      271    1564    178.5    1.46        1.9         703         69         277.8
               O     (1.43 g/liter)  −218  −183    3.4    0.66        3.5        1319          1        −286
               S        2.07      112     444     12.6    1.04        2.5        1004         16         −20.2
               Se       4.79      217     685     14.0    1.21        2.4         941         66          29.7
               Te       6.24      450     990     49.9    1.41        2.1         869        72 (tie)     99.6
               Po       9.32      254     962      —      1.65        2.0         813         —           —
                a  Pauling values.
                b  See Table III for more details.

                                                                                                        ◦
              nature. Like silicon, which it resembles in several respects,  erties is no easy matter. The melting point of 2180 C and
                                                                                    ◦
              it is essentially always found bonded to oxygen. Vast de-  the boiling point of 3650 C are approximate values com-
              posits of the three most important borate minerals, borax  monly listed in tables; they apply to the β-rhombohedral
              (Na 2 [B 4 O 5 (OH) 4 ] · 8H 2 O), kernite (Na 2 [B 4 O 6 (OH) 2 ] ·  form, the most stable modification. Pure crystalline boron
                                                                                                        3
              3H 2 O), and colemanite (Ca 2 [B 3 O 4 (OH) 3 ] 2 · 2H 2 O), are  is brittle, hard, low in density (2.35–2.45 g/cm ), and
              found in dry lake beds in California, Turkey, and  high in electrical resistance—clearly properties of a
              other arid regions. Borax and kernite are often shown  nonmetal.
              as Na 2 B 4 O 7 · 10H 2 O and Na 2 B 4 O 7 · 4H 2 O, respectively;  In most of its allotropic forms, elemental boron exists
              however, these are simplified representations of these two  in B 12 icosahedral structural units. An icosahedron has 12
                                                         −2
              important minerals, neither of which contains a B 4 O 7  vertices and 20 faces, each of which is a triangle. The man-
              ion. A good rule of thumb in boron chemistry is never to  ner in which the B 12 clusters are linked together to produce
              assume that things are as simple as they first appear.  a large three-dimensional network accounts for the high
                Boron of ∼95% purity can be prepared from the oxide  melting point and extreme hardness of this element.
              by reaction with powdered magnesium:

                        B 2 O 3 + 3Mg → 2B + 3MgO
                High-Purity boron (>99.9%) can be obtained by pass-
              ing a mixture of BCl 3 or BBr 3 and hydrogen over a heated
              tantalum filament:
                                                                  Because boron is the only nonmetal with just three va-
                                        ◦
                                 1000−1200 C
                 2BBr 3 (g) + 3H 2 (g) −−−−−−→ 2B (s) + 6HBr (g)  lence electrons at its disposal, it must resort to clever
                                                                stratagems in its bonding and structure. All the other
                Because elemental boron exists in so many allotropic  elements in Group 13 (Group IIIA) are metals; their
              modifications, the exact determination of physical prop-  chemistries are reasonably straightforward and relatively
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