Table 1
Saturation models for rock types.
| Rocktype | Lithofacies | Saturation model |
|---|---|---|
| 1 | Globigerina wackestone | S w = 10(−1.914×log10(H)+0.962)/Phi |
| 2 | Globigerina wackestone | S w = 10(−0.835×log10(H)+0.651)/Phi |
| 3 | Algal wackestone | S w = 10(−0.557×log10(H)+0.144)/Phi |
| 4 | Algal packstone | S w = 10(−0.835×log10(H)+0.651)/Phi |
| 5 | Algal packstone | S w = 10(−0.564×log10(H)+0.177)/Phi |
| 6 | Algal packstone | S w = 10(−0.514×log10(H)+0.309)/Phi |
| 7 | Algal/intraclastic packstone | S w = 10(−0.528×log10(H)+0.231)/Phi |
| 8 | Intraclastic packstone | S w = 10(−0.749×log10(H)+0.051)/Phi |
| 9 | Intraclastic packstone | S w = 10(−0.749×log10(H)+0.051)/Phi |
| 10 | Grainstone | S w = 10(−0.482×log10(H)+0.409)/Phi |
| 11 | Grainstone | S w = 10(−0.482×log10(H)+0.419)/Phi |
| 12 | Echinoderm wackestone | S w = 10(−0.581×log10(H)+0.137)/Phi |
Here, S w refers to water saturation, H refers to the height above FWL and Phi refers to porosity of the specific grid.