One can locate resistivity anomalies in the ground as in Fig. 4-5. The current $I$ flowing between electrodes $C_{1}$ and $C_{2}$ establishes an electric field in the ground, and one measures the voltage $V$ between a pair of electrodes $P_{1}$ and $P_{2}$ maintained at a fixed spacing $b$. With $b \ll a, V / b$ is equal to $E$ at the position $x$. Anomalies in ground conductivity show up in the curve of $E$ as a function of $x$. Show that if the substrate conductivity is uniform and equal to $\sigma$, then
$$
\frac{V}{b}=-\frac{2 a x I}{\pi \sigma\left(x^{2}-a^{2}\right)^{2}}
$$
The electrodes are of finite size. However, you can perform the calculation on the assumption that they are infinitely small, disregarding the fact that $E$ and $J$ would then be infinite at their surfaces.
You can use the principle of superposition as follows. The current in the ground is the sum of a radial distribution emanating from $C_{1}$ plus another radial distribution converging on $C_{2}$. Thus, at a point $r_{1}, r_{2}$,
$$
\boldsymbol{E}=\frac{\boldsymbol{r}_{1}}{2 \pi \sigma r_{1}^{2}}-\frac{I \hat{r}_{2}}{2 \pi \sigma r_{2}^{2}}
$$