* 0.433 = the gradient of pure water at ambient conditions
* 0.433 = the gradient of pure water at ambient conditions
−
This information can be used to compare expected fluid saturations of different rock types at given levels in the reservoir ([[:File:charles-l-vavra-john-g-kaldi-robert-m-sneider_capillary-pressure_5.jpg|Figure 5]]). (For information on the application of capillary pressure data to evaluating [[fluid contacts]], see [[Fluid contacts]].)
+
This information can be used to compare expected fluid saturations of different rock types at given levels in the reservoir ([[:File:charles-l-vavra-john-g-kaldi-robert-m-sneider_capillary-pressure_5.jpg|Figure 5]]). (For information on the application of capillary pressure data to evaluating [[fluid contacts]].