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CHAPTER 2


                                                Corrosion Basics









                 2.1  Why Metals Corrode
                      The driving force that causes metals to corrode is a natural consequence
                      of  their  temporary  existence  in  metallic  form.  In  order  to  produce
                      metals  starting  from  naturally  occurring  minerals  and  ores,  it  is
                      necessary to provide a certain amount of energy. It is therefore only
                      natural that when these metals are exposed to their environments they
                      would  revert  back  to  the  original  state  in  which  they  were  found.
                      A typical cycle is illustrated by iron. The primary corrosion product of
                      iron, for example, is Fe(OH)  (or more likely FeO·nH O), but the action
                                             2
                                                                 2
                      of oxygen and water can yield other products having different colors:
                          •  Fe O ·H O  or  hydrous  ferrous  oxide,  sometimes  written  as
                               2
                                   2
                                 3
                             Fe(OH) , is the principal component of red-brown rust. It can
                                   3
                             form a mineral called hematite, the most common iron ore.
                          •  Fe O ·H O  or  hydrated  magnetite,  also  called  ferrous  ferrite
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                               3
                                   2
                             (Fe O ·FeO), is most often green but can be deep blue in the
                                 3
                               2
                             presence of organic complexants.
                          •  Fe O  or magnetite is black.
                               3  4
                         The energy required to convert iron ore to metallic iron is returned
                      when  the  iron  corrodes  to  form  the  original  compound.  Table  2.1
                      describes  the  results  of  x-ray  diffraction  of  products  found  on
                      specimens exposed to real environments where it can be seen that the
                      metals often revert to naturally occurring mineral forms during the
                      corrosion process [1]. The amount of energy required and stored in a
                      metal or that is freed by its corrosion varies from metal to metal. It is
                      relatively high for metals such as magnesium, aluminum, and iron,
                      and relatively low for metals such as copper, silver, and gold. Table 2.2
                      lists a few metals in order of diminishing amounts of energy required
                      to convert them from their oxides to metal.
                         The high reactivity of magnesium and aluminum expressed as
                      energy  in  Table  2.2  is  paralleled  by  the  special  efforts  that  were
                      historically required to transform these metals from their respective
                      ores. The industrial process to produce aluminum metal on a large
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