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m, laying on a surface of resistivity ρ. The expression in ohms of the ground resistance Rf of such electrode is given in Eq. 1.16.

      If we assume that the two feet act as ground electrode in parallel, and that the plates do not interfere with each other, the body resistance-to-ground RBG equals 1.5ρ.

      Figure 1.13 Equivalent circuit for the computation of body currents due to a touch voltage.

      Rth is generally negligible if compared to RB +RBG, and therefore can be conservatively ignored; the fault source can be thought of as an ideal voltage generator.

      In these conditions, the body current iB can be calculated with Eq. 1.17.

      The step voltage is defined as the voltage between two points on the earth’s surface that are 1 m distant from each other, which is considered the standard stride length of a person.

      In the worst-case scenario, prospective touch voltages may equal the ground potential rise VG. To better clarify the concept, let us assume that in the event of a fault, a hemisphere of radius r0 , and resistance-to-ground RG leaks to ground the current i. Let us also assume a person standing in a region at zero potential; the person is touching a metallic structure electrically connected to the hemisphere for grounding purposes (Figure 1.14).

      Figure 1.15 Distribution of the ground-potential with a person standing in a region at zero potential.

      Figure 1.16 Distribution of the ground-potential with person standing in a region at non-zero potential.

      Figure 1.17 Equivalent circuit for the computation of body currents in the presence of an EXCP.

      Solution

      From Eq. 1.9, the ground potential rise of the hemisphere is:

V left parenthesis r subscript 0 right parenthesis equals rho fraction numerator i over denominator 2 pi r subscript 0 end fraction equals 1 comma 592.4 space straight V

      The touch voltage is V(r0)–V(r), where V(r) can be calculated with Eq. 1.8 with r = 10 m.

straight V left parenthesis straight r right parenthesis 
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