Carbonate Reservoir Characterization by F. Jerry Lucia (auth.)

By F. Jerry Lucia (auth.)

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Methods of obtaining this information are discussed in Chapter 2. References Amyx: JW, Bass DM Jr, Whiting RL (1960) Petroleum reservoir engineering. McGraw-Hill, NewYork,610 pp Archie GE (1952) Classification of carbonate reservoir rocks and petrophysical considerations. AAPG Bu1l36, 2: 278-298 Arps JJ (1964) Engineering concepts useful in oil finding. AAPG Bu1l43, 2: 157-165 Bachu S, Underschultz JR (1995) Large-scale underpressuring in the Mississippian-Cretaceous succession, Southwestern Alberta Basin.

I.... ' ~,e ........ , ........................ ;.... ..................... ' '.... ............... ,i@j '............ '" ...... I ..... ,. . . . , . . . . ' . . ,JA . ' . ~ 'e", ...... "' . I. ~ •. "' ..... .. ~.. ~. ....... 7. Geological/petrophysical cIassification of vuggy pore space based on vug interconnection. ;:;. ~ ~ .... ;:;. > 32 2 Rock-Fabric, Petrophysical Parameters, and Classification touching-vug pore types. Fenestral pore space is commonly connected on a reservoir scale and is grouped with touching vugs because the pores are normally much larger than the grain size (Major et al.

The oil becomes mobile only after attaining a saturation defined by the relative permeability curve that equates to a reservoir height defined by the capillary pressure curve. water contact. üil and water are produced above this reservoir height until the relative permeability to water becomes extremely low and only oil will flow. The reservoir height at which this occurs is defined by the capillary press ure curve. This depth interval is commonly referred to as the transition zone between water production and oil production.

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