Water saturation Archie water saturation Archie (1942); Asquith & Krygowski, Basic Well Log Analysis (2004) | Rt 10 ohm·m, φ 0.20, Rw 0.05 ohm·m, a 1, m 2, n 2 | 0.3536 v/v | 0.3536 v/v | < 0.000001 |
Water saturation Archie water saturation, non-unit constants Archie (1942); Humble formation factor, Winsauer et al. (1952) | Rt 10 ohm·m, φ 0.20, Rw 0.05 ohm·m, a 0.62, m 2.15, n 1.8 | 0.2762 v/v | 0.2762 v/v | < 0.000001 |
Water saturation Indonesia (shaly-sand) water saturation Poupon & Leveaux (1971) | Rt 10 ohm·m, φ 0.20, Rw 0.05 ohm·m, Vsh 0.10, Rsh 2 ohm·m, a 1, m 2, n 2 | 0.3247 v/v | 0.3247 v/v | < 0.000001 |
Water saturation Indonesia water saturation, non-unit constants Poupon & Leveaux (1971) | Rt 10 ohm·m, φ 0.20, Rw 0.05 ohm·m, Vsh 0.10, Rsh 2 ohm·m, a 0.62, m 2.15, n 1.8 | 0.2539 v/v | 0.2539 v/v | < 0.000001 |
Organic matter ΔlogR total organic carbon Passey et al. (1990), AAPG Bulletin 74(12) | ΔlogR 1.0, level of organic metamorphism (LOM) 10 | 4.064 wt% | 4.064 wt% | 0.000033 |
Organic matter ΔlogR total organic carbon, second point Passey et al. (1990), AAPG Bulletin 74(12) | ΔlogR 1.7, LOM 10.5 | 5.689 wt% | 5.689 wt% | 0.000030 |
Geomechanics Eaton sonic pore pressure Eaton (1975), SPE 5544 | Sv 10,000 psi, hydrostatic 4,650 psi, Δt ratio 0.8, exponent 3 | 7,260.8 psi | 7,260.8 psi | < 0.000001 |
Geomechanics Eaton fracture gradient Eaton (1969), JPT 21(10) | Sv 10,000 psi, Pp 4,650 psi, Poisson's ratio 0.25 | 6,433.3 psi | 6,433.3 psi | 0.0033 |
Geomechanics Bowers effective stress (loading curve) Bowers (1995), SPE 27488 | Vp 7,500 ft/s, A 5, B 1 | 500.0 psi | 500.0 psi | < 0.000001 |
Geomechanics Bowers effective stress, Gulf of Mexico coefficients Bowers (1995), SPE 27488 | Vp 7,500 ft/s, A 4.4567, B 0.8168 | 2,320.0 psi | 2,320.0 psi | 0.0040 |
Fluid properties Standing oil formation volume factor Standing (1947), API Drilling & Production Practice | Rs 500 scf/STB, gas gravity 0.8, 35 °API, 180 °F | 1.2927 rb/STB | 1.2927 rb/STB | 0.0000074 |
Production forecasting Arps exponential decline, one-year cumulative Arps (1945), Trans. AIME 160 | qi 1,000 bbl/d, Di 0.001 /day, t 365 days | 305,803 bbl | 305,803 bbl | 0.35 |
Production forecasting Arps hyperbolic decline, one-year cumulative Arps (1945), Trans. AIME 160 | qi 1,000 bbl/d, Di 0.002 /day, b 0.5, t 365 days | 267,399 bbl | 267,399 bbl | 0.27 |
Economics Net present value Standard discounted cash flow, end-of-period convention | Cash flows −100, 50, 50, 50 at a 10% discount rate | 24.34 $ | 24.34 $ | < 0.000001 |
Economics Internal rate of return Standard discounted cash flow | Cash flows −100, 50, 50, 50 | 23.38 % | 23.38 % | 0.0000071 |
Formation water Rw from NaCl-equivalent salinity Bateman & Konen (1977), The Log Analyst 18(5) | 100,000 ppm NaCl equivalent, 75 °F | 0.0735 ohm·m | 0.0735 ohm·m | 0.0000044 |
Formation water Rw to formation temperature (Arps) Arps (1953), Trans. AIME 198 | Water analysis Na 39,300 + Cl 60,700 ppm (100,000 ppm NaCl eq.), formation 200 °F | 0.0291 ohm·m | 0.0291 ohm·m | < 0.000001 |
Porosity Secondary porosity index Schlumberger Log Interpretation Principles; Asquith & Krygowski (2004) | Crossplot φ 0.12, sonic φ 0.08 | 0.040 v/v | 0.040 v/v | < 0.000001 |