04-Geol-B10 · May 2017
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
EGBC National Exam — Geological Engineering, 04-Geol-B10-2 Electrical Methods, 2017-May. Closed book; no calculator permitted. All ten questions require an answer in essay format, with diagrams used wherever appropriate. The exam instructs "choose six (6) of the following ten (10) questions, the first six as they appear in the answer book will be marked, each of equal value, about half an hour each".
Reference texts: Telford, Geldart & Sheriff, Applied Geophysics, 2nd ed. (electrical properties of rocks ch.5; self-potential ch.6; induced polarization ch.9; resistivity ch.8; electromagnetic methods ch.7; magnetotellurics ch.10); Kearey, Brooks & Hill, An Introduction to Geophysical Exploration, 3rd ed. (resistivity arrays, EM systems, MT surveying, ch.8–9); Simpson & Bahr, Practical Magnetotellurics (MT instrumentation and robust/remote-reference processing, ch.2–6).
Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.
Given. Point-source half-space potential V(r) = Iρ/(2πr); Wenner array C1–P1–P2–C2 collinear with equal spacing a between every adjacent electrode.
Find. The apparent-resistivity formula ρa for the Wenner array in terms of the measured potential difference ΔV, injected current I, and spacing a.
Superpose the potential from the two current electrodes (+I at C1, −I at C2) at each potential electrode, take the difference VP1 − VP2, and solve for ρ.
| Quantity | Result |
|---|---|
| Potential difference ΔV | Iρ/(2πa) |
| Wenner apparent resistivity ρa | 2πa(ΔV/I) |
| Geometric factor k (Wenner) | 2πa |
To deepen a Wenner sounding, ALL FOUR electrodes must be dug up and replanted farther apart at every reading — slow, and it repeatedly re-exposes the measurement to fresh near-surface lateral inhomogeneity under the moving potential electrodes. In a Schlumberger sounding, the potential pair P1P2 stays fixed (only the outer current electrodes are moved outward), so far fewer electrodes are relocated per sounding, the survey runs faster, and successive readings share the same potential-electrode footprint, improving internal consistency of the sounding curve.
For a profile at FIXED spacing (not a sounding), the whole four-electrode Wenner set simply advances together along the line at constant a, which is operationally simple and, critically, gives the strongest possible signal (smallest geometric factor 2πa of any array at that separation) with the potential electrodes always close to and symmetric about the current electrodes — giving the best sensitivity to lateral resistivity changes directly beneath the array as it is walked along the line, which is exactly what a profile is trying to resolve.