Step 1: Build a superposition model of measured voltage.
Let \(V_{SP}\) be the static electrode SP (does not change with current reversal) and \(V_I\) be the ohmic voltage due to injected current (changes sign when current reverses). Then
\[
\Delta V_{\text{meas}} = V_{SP} \pm V_I.
\]
With given signs:
\[
\begin{aligned}
V_{SP}+V_I &= +158\ \text{mV}\quad\text{(forward)},
V_{SP}-V_I &= -214\ \text{mV}\quad\text{(reverse)}.
\end{aligned}
\]
Step 2: Solve the 2\(\times\)2 linear system.
Add equations to eliminate \(V_I\):
\[
2V_{SP} = (+158) + (-214) = -56 \Rightarrow V_{SP} = -28\ \text{mV}.
\]
(Then \(V_I=158-(-28)=186\ \text{mV}\) — optional check.)
Step 3: Consistency verification.
Insert into the second equation:
\[
V_{SP}-V_I = -28-186 = -214\ \text{mV}\quad\checkmark
\]
Thus the SP offset was \(-28\ \text{mV}\) (negative electrode at the second potential stake).
Final Answer:\ \(\boxed{-28\ \text{mV}}\)
While doing Bayesian inference, consider estimating the posterior distribution of the model parameter (m), given data (d). Assume that Prior and Likelihood are proportional to Gaussian functions given by \[ {Prior} \propto \exp(-0.5(m - 1)^2) \] \[ {Likelihood} \propto \exp(-0.5(m - 3)^2) \] 
The mean of the posterior distribution is (Answer in integer)
Consider a medium of uniform resistivity with a pair of source and sink electrodes separated by a distance \( L \), as shown in the figure. The fraction of the input current \( (I) \) that flows horizontally \( (I_x) \) across the median plane between depths \( z_1 = \frac{L}{2} \) and \( z_2 = \frac{L\sqrt{3}}{2} \), is given by \( \frac{I_x}{I} = \frac{L}{\pi} \int_{z_1}^{z_2} \frac{dz}{(L^2/4 + z^2)} \). The value of \( \frac{I_x}{I} \) is equal to 
Suppose a mountain at location A is in isostatic equilibrium with a column at location B, which is at sea-level, as shown in the figure. The height of the mountain is 4 km and the thickness of the crust at B is 1 km. Given that the densities of crust and mantle are 2700 kg/m\(^3\) and 3300 kg/m\(^3\), respectively, the thickness of the mountain root (r1) is km. (Answer in integer)