Use artificial intelligence to predict lithofacies in 500 wells and fill a 3D volume with lithofacies constrained porosity, permeability and gas saturations.
Council Grove facies identification is important to reservoir characterization because petrophysical properties vary between facies. At porosities > 6% permeability in grainstone/bafflestones can be 30X greater than mudstones and >100X greater than marine siltstones of similar porosity. Differences in permeabilities between nonmarine silt/sandstones and shaly siltstones range from 3.3X at 12% porosity to 7X at 18%. Capillary pressures and corresponding
water saturations also vary between facies. For example, at 7% porosity
(which represents >50% of all Mstn/Wkstn) at 200 ft above free water
Mudstones are 100% water saturated while grainstones exhibit water saturations
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Last updated May 2003
http://www.kgs.ku.edu/PRS/publication/2003/ofr2003-30/P1-08.html