Page 48 - Corrosion Engineering Principles and Practice
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28   C h a p t e r   2                                     C o r r o s i o n   B a s i c s    29


                      water can increase its conductivity or change other properties of the
                      liquid,  but  does  not  increase  or  decrease  its  acidity.  For  instance,
                                              +
                      whether a given amount of H  ion is produced in water by introducing
                      hydrochloric (HCl), sulfuric (H SO ), or any other acid is immaterial.
                                                   4
                                                2
                      The  pH  of  the  solution  will  be  the  same  for  the  same  number  of
                      dissolved hydrogen atoms.
                         The pH may be measured with a meter or calculated if certain
                      parameters are established. Water itself dissociates to a small extent
                                                            −
                                                   +
                      to  produce  equal  quantities  of  H   and  OH   ions  displayed  in  the
                      following equilibrium:
                                                  +
                                          H O   H +  OH −                  (2.3)
                                           2

                      pH,  originally  defined  by  Danish  biochemist  Søren  Peter  Lauritz
                      Sørensen in 1909, is a measure of the concentration of hydrogen ions.
                      The term pH was derived from the manner in which the hydrogen
                      ion  concentration  is  calculated;  it  is  the  negative  logarithm  of  the
                      hydrogen ion (H ) concentration:
                                    +
                                          pH = −  log (a H +                (2.4)
                                                       )
                                                   10

                      where log  is a base-10 logarithm and a  is the activity (related to
                                                        H+
                               10
                      concentration) of hydrogen ions. The “p” in Eq. (2.4) stands for the
                      German word for power, potenz, so pH is an abbreviation for power
                      of hydrogen.
                         A higher pH means there are fewer free hydrogen ions, and that a
                      change of one pH unit reflects a tenfold change in the concentrations of
                      the hydrogen ion. For example, there are 10 times as many hydrogen
                      ions available at pH 7 than at pH 8. The pH scale commonly quoted
                      ranges from 0 to 14 with a pH of 7 considered to be neutral.
                         Substances with a pH less that 7 are considered to be acidic, and
                      substances with a pH equal to or greater than 7 are considered to be basic
                      or alkaline. Thus, a pH of 2 is very acidic and a pH of 12 very alkaline.
                      However, it is technically possible to have very acidic solutions with a
                      pH lower than zero and concentrated caustic solutions with a pH greater
                      than 14. Such solutions are in fact typical of many ore extracting processes
                      that require the digestive power of caustics and acids.
                         Low-pH acid waters accelerate corrosion by supplying hydrogen
                      ions to the corrosion process. Although even absolutely pure water
                      contains some free hydrogen ions, dissolved carbon dioxide (CO ) in
                                                                            2
                      the  water  can  increase  the  hydrogen  ion  concentration.  Dissolved
                      CO  may react with water to form carbonic acid (H CO ), as shown in
                         2
                                                                    3
                                                                2
                      Eq. (2.5):
                                                    [H CO ]
                                                      2
                                                               ×
                          CO +  H O   H CO with K eq  =  [CO ] 3  = 1 .7 × 10 − 3  at 25 C    (2.5)
                                                                      o
                                       2
                                          3
                             2
                                2
                                                        2
                      where K  is the reaction equilibrium expressed in equation.
                             eq
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