Page 124 - Corrosion Engineering Principles and Practice
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98   C h a p t e r   5     C o r r o s i o n   K i n e t i c s   a n d   A p p l i c a t i o n s   o f   E l e c t r o c h e m i s t r y    99


                         An  alternating  current  from  the  soil  resistance  meter  causes
                      current to flow through the soil, between pins C1 and C2 and the
                      voltage or potential is measured between pins P1 and P2. Resistivity
                      of the soil is then computed from the instrument reading, according
                      to the following formula [1]:
                                             r = 2π aR                     (5.18)


                      where r is the soil resistivity (Ω cm)
                            a is the distance between probes (cm)
                            R is the soil resistance (Ω), instrument reading
                            p  is 3.1416
                         The resistivity values obtained represent the average resistivity of
                      the soil to a depth equal to the pin spacing. Resistance measurements
                      are typically performed to a depth equal to that of the buried system
                      (pipeline) being evaluated. Typical probe spacing is in increments of
                      0.5 to 1 m.
                         If  the  line  of  soil  pins  used  when  making  four-pin  resistivity
                      measurements is closely parallel to a bare underground pipeline or
                      other metallic structure, the presence of the bare metal may cause the
                      indicated soil resistivity values to be lower than it actually is. Because
                      a  portion  of  the  test  current  will  flow  along  the  metallic  structure
                      rather  than  through  the  soil,  measurements  along  a  line  closely
                      parallel to pipelines should therefore be avoided.
                         The recorded values from four-pin resistivity measurements can
                      be  misleading  unless  it  is  remembered  that  the  soil  resistivity
                      encountered with each additional depth increment is averaged, in the
                      test,  with  that  of  all  the  soil  in  the  layers  above.  With  experience,
                      much can be learned about the soil structure by inspecting series of
                      readings  to  increasing  depths.  The  indicated  resistivity  to  a  depth
                      equal to any given pipe spacing is a weighted average of the soils
                      from  the  surface  to  that  depth.  Trends  can  be  illustrated  best  by
                      inspecting the sets of soil resistivity readings in Table 5.5.

                                                    Soil Resistivity (W cm)
                  Pin Spacing    Pin Pacing
                      (m)          (F)      Set A  Set B   Set C   Set D
                  0.76          2.5         960    1100    3300       760
                  1.5           5           965    1000    2200       810
                  2.3           7.5         950    1250    1150      1900
                  3.0          10           955    1500      980     3800
                  3.8          12.5         960    1610      840     6900
                  4.6          15           955    1710      780    12,500

                 TABLE 5.5  Examples of Soil Resistivity Readings Using Four-Pin Method
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