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398     C h a p t e r   1 0                                                             C o r r o s i o n   i n   S o i l s   a n d   M i c r o b i o l o g i c a l l y   I n f l u e n c e d   C o r r o s i o n    399


                      Cathode Scale
                      A third auxiliary effect is the deposition of compounds from the soil
                      on the buried system. This effect is extremely pronounced in seawater,
                      where a cathode scale resembling hard glossy enamel can build up
                      over time and grow as thick as 2 cm. When deposited in seawater, this
                      material  is  a  complex  mixture  of  calcium  and  magnesium  oxides,
                      hydroxides,  and  carbonates.  The  composition  of  this  hard  deposit
                      depends upon CP current density, among other factors (see Chap. 8
                      for details on calcareous deposits).
                         In fresh or brackish water cathode scale composition is even more
                      variable than the scale formed in seawater since its formation is based
                      on  highly  variable  ion  concentrations.  This  is  also  true  in  soils.
                      Some  soils  will  not  form  a  visible  scale,  although  there  is  enough
                      calcium present in most soils to favor scale formation. Often, when a
                      system has been polarized by CP, no scale will be visible until the
                      system surface dries out. It then appears as a whitish coloration. On a
                      buried  system  which  has  not  been  under  CP,  cathode  scale  is
                      frequently  found  in  an  irregular  mottled  pattern;  this  makes  the
                      actually active cathodic areas visible to the eye.
                      Pitting
                      When a buried system that has been in corrosive soil without adequate
                      protection for some time is examined, it is usually found that by far
                      the greater part of the area is unaffected. Where corrosion has taken
                      place, it is in the form of pits, which are relatively small areas where
                      the attack has been deep (Fig. 10.3).
                         In general, there will always be one spot on any buried system
                      where  all  of  the  conditions  combine  to  give  the  highest  rate  of
                      penetration.  This  hot  spot  is  exactly  where  the  first  pit  through
                      perforation will occur. Since the underground system is invisible to
                      the observer, the resulting leak will be the first place where corrosion
                      will make its presence known.

                      10.2.5  Examples of Buried Systems

                      Pipelines
                      Pipelines carrying oil, gas, and water are surely the most considerable
                      assets buried in soils from the deepest subsea exploitation fields to
                      the most remote tropical regions of the world. The subject of both
                      external and internal gas pipeline corrosion is covered in many details
                      in Chap. 12 and many details of the corrosion management of water
                      lines are discussed in Chap. 8.
                         Some pipelines deteriorate slowly, and in certain cases pipeline
                      life has been reliably targeted at 70 years or more. Other pipelines
                      have been built which have exhausted their useful life after one year
                      of  operation. Apart  from  the  quality  of  the  construction,  coatings,
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