Page 343 - Corrosion Engineering Principles and Practice
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314    C h a p t e r   8                                                                                                           C o r r o s i o n   b y   W a t e r    315


                      level increases  beyond  1.0,  the  driving  force  for  the  precipitation  of
                      calcium carbonate increases.
                         The  following  sections  describe  some  indices  that  are  used  to
                      indicate  the  tendency  of  given  waters  to  deposit  scales  on  metal
                      substrates and by extension to predict the corrosivity of specific waters.
                      Generally speaking, scales precipitated onto metal surfaces can provide
                      protection of the substrate from general corrosion. If on the other hand,
                      the scales are defective and contain voids and/or cracks, they could
                      lead to localized corrosion. However, the assumption that water below
                      saturation  with  respect  to  calcium  carbonate  is  corrosive,  while
                      occasionally correct, is not always reliable.

                      8.7.1  Langelier Saturation Index
                      The Langelier saturation index (LSI) is probably the most widely used
                      indicator of a water scale potential. This index indicates the driving force
                      for scale formation and growth in terms of pH as a master variable. In
                      order to calculate the LSI, it is necessary to know the alkalinity (mg L as
                                                                             −1
                                                              2+
                      CaCO  or calcite), the calcium hardness (mg L  Ca  as CaCO ), the total
                                                           −1
                           3
                                                                       3
                                        −1
                      dissolved solids (mg L , TDS), the actual pH, and the temperature of the
                      water (°C). If TDS is unknown, but conductivity is, one can estimate mg
                      L TDS using a conversion table (Table 8.15). LSI is defined as
                       −1
                                          LSI =  pH −  pH s                (8.26)
                      where pH is the measured water pH
                            pH   is the pH at saturation in calcite or calcium carbonate and
                              s
                               is defined as:
                               pH =  (9.3 +  A +  ) B −  (C +  D )         (8.27)
                                  s
                                     [Log  (TDS) −  1]
                                 A =     10  10                            (8.28)

                                                  o
                                 B = − 13.12 ×  Log ( C +  273) +  34.55    (8.29)
                                               10
                                             2+
                                 C =  Log 10  (Ca as CaCO ) −  0.4         (8.30)
                                                     3
                                D =  Log  (alkalinity as CaCO )            (8.31)
                                        10               3
                         As for the SL reasoning described earlier, the LSI indicates three
                      situations:
                          •  If LSI is negative: No potential to scale, the water will dissolve
                             CaCO .
                                  3
                          •  If LSI is positive: Scale can form and CaCO  precipitation may
                                                                3
                             occur.
                          •  If LSI is close to zero: Borderline scale potential. Water qual-
                             ity or changes in temperature, or evaporation could change
                             the index.
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