note: the data point for limestone is eliminated for regression
Derived regression:
k h 5.54 10 5 4.5 where permeability is in md and porosity as fraction
stone tone
Capillary Pressure Curves (data from Darling, 2005) Core data (SCAL):
System: Sample porosity phi permeability k
Air-Brine 1 0.131 67
Pressure Pc in psi 3 10 25 50 125 200
System: Sample porosity phi permeability k
Air-Brine 4 0.179 278
Pressure Pc in psi 3 10 25 50 125 200
Sw 0.861 0.617 0.388 0.290 0.239 0.216
0.730 0.430 0.282 0.214 0.176 0.144
a) Capillary Pressure Curve (laboratory data air-brine) in 200
. i s p n i c P
150 100 50 0 0.0
0.5 Sw
c) Water saturation from Capillary Press Curve versus elevation above FWL in . m
200.00
n i l e v e l r e t a w e e r f e v o b a
150.00 100.00 50.00 0.00 0.0
0.5 Sw
Conversion from air-brine (laboratory) to kerosene-brine (reservoir) Depth of FWL (m) = 646 Parameter: s cos Q System Air/Brine 72 Kerosene/Brine 26 Capillary pressure in kPa air-brine 20.68 68.94 172.35 344.70 861.75 1378.80
Archie parameter Part 1: Formation factor (F) vs. Porosity (phi) Scal analyses data For regression with two parameters ( a and m ) the first table (SCAL data) is used and pl For regression with one parameters ( m ) the second table (logarithms of data) is used a porosity 0.10 0.15 0.17 0.08 0.14 0.13