Question 4 of 10: Assumptions of Conventional Log-Interpretation Techniques
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
National Examinations, 17-Pet-B1, Well Logging and Formation Evaluation — December 2019, 3 hours, closed book (Casio or Sharp approved calculators permitted), 10 questions, all marked.
Reference texts: Bassiouni, Theory, Measurement, and Interpretation of Well Logs (SPE Textbook Series Vol. 4); Asquith & Krygowski, Basic Well Log Analysis, 2nd ed. (AAPG); Ellis & Singer, Well Logging for Earth Scientists, 2nd ed.; Schlumberger, Log Interpretation Charts / Log Interpretation Principles and Applications.
Question 4: Assumptions of Conventional Log-Interpretation Techniques (6 marks)
"Conventional" (Archie-type) log interpretation — the resistivity-porosity-saturation workflow used throughout this paper — rests on six simplifying assumptions:
1. The formation is clean, granular, and intergranular-porous (no significant clay/shale, vugs, or fractures) so that Archie's law $R_t=aR_w/(\phi^mS_w^n)$ applies without a separate shale or dual-porosity correction.
2. The rock matrix and pore fluids are electrically non-conductive — all conduction is through the interconnected, continuous formation-water phase, so resistivity responds only to φ, Sw, and Rw.
3. Formation water resistivity Rw (and mud-filtrate resistivity Rmf) is uniform and known at the depth/temperature of interest, obtained either from a water sample, an SP calculation, or a nearby wet zone.
4. Invasion is radial and "piston-like" (a sharp, cylindrically symmetric front separating a uniformly filtrate-saturated flushed zone from the undisturbed formation), which is the geometric picture behind the Rxo/Ri/Rt profiles of Question 3.
5. The borehole is in gauge, mud-filled, and the tool is properly centralized (or decentralized, per its design) so that standard borehole/mudcake correction charts apply without an extra rugosity correction.
6. The bed is thick relative to the tool's vertical resolution (no unresolved thin-bed averaging) and the formation is macroscopically homogeneous and isotropic within the tool's depth of investigation.