US4817062A
Expired / Lapsed
US
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Method for estimating subsurface porosity
Assignee: Western Atlas International Inc
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Filing: 1987-10-02
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Granted: 1989-03-28
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Expires: 2007-10-02
Abstract
Abstract The instant invention is a method for accurately estimating the subsurface porosity and porosity-thickness of an interval of interest. A seismic acoustic model is constructed from data collected in a seismic survey. The acoustic model provides information from which predicted porosity values may be calculated. The predicted porosity valves are then cross-plotted with actual porosity valves obtained from well information, providing an accurate estimate of porosity away from the well locations. Porosity thickness is determined using the thickness information provided by the well data.
Inventors
- 👤 Marc H. De Buyl
- 👤 Thomas M. Guidish
Bibliographic Details
Application Number
—
Jurisdiction
US
Data Source
google_patents
Last Synchronized
2026-11-05 12:45
CPC Classifications
G; G01; G01V; G01V1/00; G01V1/28; G01V1/282; G01V2210/00; G01V2210/60; G01V2210/61; G01V2210/614
Claims Analysis
Total Claims: 6
Claim 1
Independent Claim
233 words
A method for estimating the porosity of a subsurface interval of the earth, comprising the steps of: (a) gathering seismic data from the subsurface interval, the seismic data consisting of a plurality of seismic samples representing a plurality of locations along the surface of the earth; (b) deriving an acoustic model of the subsurface interval, from the seismic samples; (c) assigning an average acoustic impedance value for each of said plurality of seismic samples in said acoustic model, using data from available well control; (d) calculating a predicted porosity value for each average acoustic impedance value according to the expression: ##EQU6## where φ 1 is the calculated porosity; ρυ is the average acoustic impedance of the inverval; V 2 is a percentage of minor matrix constituents in the subsurface interval; ρ 1 is a density of major matrix constituents comprising the subsurface interval; Δt 1 is a transit time of a seismic signal in the major matrix constituents; ρ 2 is a density of the minor matrix constituents; Δt 2 is a transit time of the seismic signal in the minor matrix constituents; ρ f is a density of the fluid; and Δt f is a transit time of the seismic signal in the fluid of the interval; (e) calibrating the predicted porosity value with welllog and core-derived data; and (f) plotting or displaying the predicted porosity values for each modeled seismic location.
Claim 2
Independent Claim
233 words
A method for estimating the porosity of a subsurface interval of the earth, comprising the steps of: (a) gathering seismic data from the subsurface interval, the seismic data consisting of a plurality of seismic samples representing a plurality of locations along the surface of the earth; (b) deriving an acoustic model of the subsurface interval, from the seismic samples; (c) assigning an average acoustic impedance value for each of said plurality of seismic samples in said acoustic model, using data from available well control; (d) calculating a predicted porosity value for each average acoustic impedance value according to the expression: ##EQU6## where φ 1 is the calculated porosity; ρυ is the average acoustic impedance of the inverval; V 2 is a percentage of minor matrix constituents in the subsurface interval; ρ 1 is a density of major matrix constituents comprising the subsurface interval; Δt 1 is a transit time of a seismic signal in the major matrix constituents; ρ 2 is a density of the minor matrix constituents; Δt 2 is a transit time of the seismic signal in the minor matrix constituents; ρ f is a density of the fluid; and Δt f is a transit time of the seismic signal in the fluid of the interval; (e) calibrating the predicted porosity value with welllog and core-derived data; and (f) plotting or displaying the predicted porosity values for each modeled seismic location.
Claim 3
Dependent Claim
134 words
A method for calculating porosity as defined by claim 1, wherein the step of assigning an acoustic impedance value for each of said plurality of seismic data samples, comprises the steps of: (a) generating a lithologic model of the subsurface interval, said lithologic model derived from said plurality of seismic data samples; (b) assigning a first set of rock properties and model parameters to said lithologic model and generating a plurality of synthetic seismic traces; (c) measuring the goodness of fit between said plurality of synthetic seismic traces and the corresponding previously gathered seismic data samples; (d) systematically perturbing said first set of rock properties and model parameters in said lithologic model; (e) generating new synthetic seismic traces after said systematic perturbation until there is found a best fit between the synthetic data samples;
Claim 4
Dependent Claim
35 words
The method for calculating porosity as recited in claim 2, wherein the density variables P s , P sh , and P f are constants derived from well log data taken from the subsurface interval.
Claim 5
Dependent Claim
26 words
The method according to claim 3, wherein the transit time variables t s , t sh , and t f are determined from the well data.
Claim 6
Dependent Claim
23 words
The method according to claim 1, further comprising the step of calculating a corrected porosity by cross-plotting well-log porosity and predictable porosity values.
References Cited (Backward Citations)
US3883841A
Cited
US4679174A
Cited
USPTO Annuity & Maintenance Windows
| Annuity Stage | Window Opens | Payment Deadline | Surcharge Period Until | Estimated Fee | Status |
|---|---|---|---|---|---|
| 3.5 Years (Year 4) | 1992-03-27 | 1992-09-26 | 1993-03-28 | $2000.00 | Window Closed / Lapsed |
| 7.5 Years (Year 8) | 1996-03-27 | 1996-09-26 | 1997-03-28 | $3760.00 | Window Closed / Lapsed |
| 11.5 Years (Year 12) | 2000-03-27 | 2000-09-26 | 2001-03-28 | $7700.00 | Window Closed / Lapsed |