Saturation Height from Core Reducing Uncertainty

So whatever function we use must be a good fit to the match of data across the entire rock property range. J function as One of the many functions that are used is whatever it is, it has to be a good fit to the measurement data and it has to be able to be easily integrated into something like IRAP; Petrel–Gocad so We can calculate volumetric, the number of mathematics’ available Thomeer; Haselden; J function; Johnson Permeability; Power Function; FOIL function Skelt Harrison; or Lambda function and put the call of EQR method. These are all the available functions, and no one is better than the other, these should fit perfectly with particular lithology to the particular rock type,