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96   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    97


                      can be made of any material provided it is inert to the electrolytic
                      environment. It basically consists of a bent tube generally filled with
                      the test solution with a large enough opening to accommodate a ref-
                      erence electrode at one end and a usually much smaller opening at
                      the other end to provide diffusional movement of the electrolyte.

                      5.4.2  Soil Resistivity Measurements
                      Soil resistivity is a function of soil moisture and the concentrations of
                      ionic soluble salts and is considered to be the most comprehensive
                      indicator of a soil’s corrosivity. Typically, the lower the resistivity, the
                      higher will be the corrosivity as discussed in more details in Chap. 10.
                      Typically, soil resistivity decreases with increasing water content and
                      the concentration of ionic species. Sandy soils, for example, are high
                      up on the resistivity scale and therefore considered the least corrosive
                      while clay soils are excellent at retaining water and at the opposite
                      end of the corrosivity spectrum.
                      Four-Pin Method (Wenner Method)
                      Field soil resistivity measurements are most often conducted using
                      the Wenner four-pin method and a soil resistance meter following the
                      principles laid out by Wenner nearly one century ago [2]. The Wenner
                      method requires the use of four metal probes or electrodes, driven
                      into the ground along a straight line, equidistant from each other, as
                      shown in Fig. 5.9 and Fig. 5.10. Soil resistivity is a relatively simple
                      function derived from the voltage drop between the center pair of
                      pins (P1 and P2 in Fig 5.9), with current flowing between the two
                      outside  pins  (C1  and  C2  in  Fig  5.9)  assuming  that  the  measured
                      resistivity is a measure of the hemispherical volume of earth probed
                      by the central pins.

                                                     Soil Resistivity Meter

                                                C1  C2

                                               P1    P2


                              Listed in Table 2.2

                                                                Ground



                              Pin C1        Pin P1         Pin P2        Pin C2
                                                  a

                      FIGURE 5.9  Wenner four-pin soil resistivity test setup.
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