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Carbonate Reservoir Characterization: Case Study - Berg - Hughes ...

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<strong>Carbonate</strong> <strong>Reservoir</strong><br />

<strong>Characterization</strong>: <strong>Case</strong> <strong>Study</strong> of<br />

Womack Hill Field<br />

S Southwest th t Alabama Al b<br />

Ernest Mancini<br />

2007


Location Map


Discovered in 1970<br />

Water Flood in 1975<br />

37 W Wells ll D Drilled ill d<br />

Field Field History<br />

History<br />

31.7 Million Barrels of Oil Produced (2006)


Womack Hill Production


Field Field Characteristics<br />

Characteristics<br />

Trap: Faulted, Faulted Salt Anticline<br />

<strong>Reservoir</strong>: Smackover Multiple Stacked<br />

Shoals<br />

Source: Smackover Basinal Lime<br />

M Mudstone d t<br />

Seal: Haynesville: Anhydrite


Sequence Stratigraphy


Smackover Cycles<br />

Cycle ‘A’ = Cycle 3, Cycle ‘B’ = Cycle 2, Cycle ‘C’ = Cycle 1


Well Log Patterns<br />

1667


Womack Hill<br />

Fi Field ld M Map


1678-WI<br />

Cross Section<br />

Possible<br />

SW-NEtrending<br />

normal<br />

fault


Cycle Facies


Dolotimized Zones,<br />

14 – 5#2Well 5 #2 Well


Dolotimized Zones,<br />

15 – 1 1#1Well 1 # 1 Well


18 – 12 Well Core


9 – 14 Well Core


9 – 14 Well Core<br />

(continued)


13 – 25 Well Core


13 – 5 Well Core


13 – 5 Well Core<br />

(continued)


13 – 6 Well Core


13 – 6 Well Core<br />

(continued)


14 – 5 # 2 Well Core


Buckner Anhydrite Member


Upper Smackover<br />

- G Grainstone<br />

i t


Cross Cross-bedded bedded Upper Smackover Grainstone


Ooid Grainstone


Upper Smackover – Packstone / Wackestone


Upper Smackover – Mudstone / Wackestone


Middle Smackover - Mudstone


Lower Smackover – Brown Dense


Isotope Geochemistry


Interparticle Porosity<br />

X40


Grain Moldic Porosity<br />

X40


Intercrystalline Dolomite Porosity<br />

X100


Mixed Moldic & Intercrystalline Porosity<br />

X100


Vuggy Porosity<br />

X100


Type I Dolomite, 13 – 25 Well


Type I Dolomite, 18 – 12 Well


Exposure Surface<br />

Exposure Surface in Core


Exposure Surface in Thin Section


Type 2 and 3 Dolomite, 14 -5 5 Well


Type 2 and 3 Dolomite, 14 -5 5 Well


Type 3 Dolomite, 9 – 14 Well


Grain Deformation, 13 – 6 Well


<strong>Reservoir</strong> <strong>Reservoir</strong> <strong>Characterization</strong><br />

<strong>Characterization</strong><br />

Stacked Stacked Porosity Cycles (A (A, B B, C)<br />

Cycles Consist of Lime Mudstone to<br />

Grainstone<br />

Depositional Model; Shoal Complex<br />

Porosity Enhancement; Dissolution &<br />

Dolomitization<br />

Pore Systems; Grain Moldic &<br />

Intercrystalline<br />

y


Subsurface Mapping


Womack Hill<br />

Fi Field ld M Map


Seismic Line


Structure Map, Top of Smackover


Structure Map, Top of Buckner


Smackover Isopach Map


Upper Smackover Isopach Map


Cycle A Isopach Map


Cycle B Isopach Map


Cycle C Isopach Map


<strong>Reservoir</strong> Engineering Engineering, Production<br />

and Petrophysics


Production by Well


Production History


Cumulative Production<br />

Production


Vertical vs. Horizontal Permeability, 1591 Well


Vertical vs. Horizontal Permeability, 4575 – B Well


Porosity Comparison,<br />

1591 1591 Well


Porosity Comparison,<br />

4575 – B BWell B Well


Permeability Comparison,<br />

1591 1591 Well


Permeability Comparison,<br />

4575 - B BWell B Well


Permeability Measurements


Porosity Measurements


Comparison of Porosity


Comparison of Porosity and Permeability


Porosity and Permeability Plot for <strong>Reservoir</strong> Cycles<br />

Cycle ‘A’, Well 1678


Porosity and Permeability Plot for <strong>Reservoir</strong> Cycles<br />

Cycle ‘B’, Well 1720


Porosity and Permeability Plot for <strong>Reservoir</strong> Cycles<br />

Cycle ‘C’, Well 1591


Porosity and Permeability Plot for <strong>Reservoir</strong> Cycles<br />

Below Cycle ‘C’, Well 4575B


Porosity vs. Median Pore Throat Aperture


Porosity vs. Median Pore Throat Aperture


Pore Types


Pore Type Associations


Decline Decline-type type curve analysis for an<br />

unfractured unfractured well model for well 1639<br />

After Doublet and Blasingame (1995)


Estimated ultimate recovery (EUR) analysis<br />

(oil flow rate/pressure drop vs vs.cumulative cumulative oil<br />

production) for well 1639


Dimensionless multiwell performance index (DMPI)<br />

computed computed for wells in the Womack Hill field<br />

Total oil and water rates<br />

Total oil rates


Dimensionless production rate rate-time time–type type curve,<br />

Womack Hill field<br />

(A) Exponential rate decline model compared to production data from the unitized western area.<br />

(B) H Harmonic i rate t d decline li model d l compared d t to production d ti data d t from f the th unitized iti d western t area.<br />

(C) Exponential rate decline model compared to production data from the eastern area.<br />

(D) Harmonic rate decline model compared to production from the eastern area.


Summary plots (no rate history) from the field field-testing testing<br />

sequence q of wells, , Womack Hill field<br />

Well 1655 Well 1678<br />

Well 1804 Well 4575B


Correlation of estimated ultimate recovery<br />

(EUR) ( ) vs. effective p permeability y ( (k) ) for wells in<br />

Womack Hill field


3D Modeling


3 – D Geologic Model


Cross – Section of Porosity Variability<br />

f for Upper U Smackover S k <strong>Reservoir</strong>s R i<br />

Possible<br />

SW-NEtrending<br />

normal<br />

fault


<strong>Reservoir</strong> Simulation<br />

Actual Field Watercut vs Simulated Watercut


<strong>Reservoir</strong> Simulation<br />

Oil S Saturation t ti on T Top of f Cycle C l ‘A’ I Interval<br />

t l


Simulated Production Profiles<br />

<strong>Reservoir</strong> Simulation<br />

Well 001<br />

Well 002


Prospective Drilling Targets

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