IP Library Granted Patent US 8,630,146
Granted Patent B2
US 8,630,146 · App. 12/748,213 · Granted Jan 14, 2014

Method and apparatus for estimating formation permeability and electroacoustic constant of an electrolyte-saturated multi-layered rock taking into account osmosis

Inventors: Vitaly N. Dorovsky (Novosibirsk, RU); Vladimir Dubinsky (Houston, TX); Yuriy A. Nefedkin (Novosibirsk, RU); Alexander I. Fedorov (Novosibirsk, RU); Maxim Y. Podberezhnyy (Novosibirsk, RU); Yury V. Perepechko (Novosibirsk, RU)
Assignee: Baker Hughes Incorporated
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Quick Facts
Patent No.
US 8,630,146
App. No.
12/748,213
Granted
Jan 14, 2014
Kind
B2
Abstract

An acoustic source on a logging tool is used to generate acoustic waves in a borehole. Acoustic detectors on the logging tool measure the generated acoustic waves. Electrodes on the logging tool are used to measure the potential resulting from the generated acoustic wave. The output of the hydrophones and the electrodes corresponding to Stoneley wave components of the acoustic wave are processed to provide an estimate of formation permeability, acoustoelectric constant, and a velocity of a propagating second compressional wave in the formation.

Claims (35)

1. A method of estimating a value of a property of a porous earth formation, the method comprising:

using an acoustic source in a borehole that is propagating Stoneley wave for generating an acoustic wave in the borehole;

producing a first signal indicative of a pressure associated with the generated acoustic wave in the borehole;

producing a second signal indicative of an electric potential associated with the generated acoustic wave; and

using an attenuation length for the propagating Stoneley wave derived from the first signal and the second signal for estimating the value of a property of the formation selected from: (i) a permeability of the formation, (ii) an electroacoustic constant of the formation

by estimating a second compressional velocity associated with the acoustic wave using at least the attenuation length for the acoustic wave.

2. The method of claim 1 wherein the second compressional velocity corresponds to a Biot wave of the second kind.

3. The method of claim 1 wherein the generated acoustic wave further comprises a Stoneley wave.

4. The method of claim 3 wherein estimating the value of the property further comprises estimating a Stoneley wave velocity and estimating a Stoneley wave attenuation length as a function of frequency.

5. The method of claim 1 further comprising measuring a salinity of a fluid in the borehole fluid and using the measured salinity for estimating the value of the property of the formation.

6. The method of claim 5 wherein estimating the value of the property of the formation further comprises using a partial pressure continuity condition at a boundary of the borehole.

7. The method of claim 1 further comprising conveying the acoustic source into the borehole on a wireline.

8. The method of claim 1 , further comprising:

using phase velocity derived from the first signal and the second signal for estimating the value of the property of the formation.

9. The method of claim 1 , further comprising:

estimating the value of the property of the formation by solving an inverse problem to determine the second compressional velocity and a theoretical acoustic friction coefficient.

10. The method of claim 1 , further comprising:

estimating the value of the property of the formation using a first compressional velocity associated with the acoustic wave and a transverse velocity associated with the acoustic wave, the first compressional velocity and the transverse velocity determined from the first signal and the second signal.

11. An apparatus configured to estimate a value of a property of a porous earth formation, the apparatus comprising:

a tool configured to be conveyed in a borehole;

an acoustic source on the tool configured to generate an acoustic wave in the borehole that is a propagating Stoneley wave;

an acoustic detector on the tool configured to produce a first signal indicative of a pressure associated with the generated acoustic wave in the borehole;

a second detector configured to produce a second signal indicative of an electric potential associated with the generated acoustic wave; and

a processor configured to use an attenuation length for the propagating Stoneley wave derived from the first signal and the second signal for estimating the value of a property of the formation selected from: (i) a permeability of the formation, (ii) an electroacoustic constant of the formation,

by estimating a second compressional velocity associated with the acoustic wave using at least the attenuation length for the acoustic wave.

12. The apparatus of claim 11 wherein the processor is configured to estimate the second compressional velocity of a Biot wave of the second kind.

13. The apparatus of claim 11 wherein the generated acoustic wave further comprises a Stoneley wave.

14. The apparatus of claim 13 wherein the processor is configured to estimate the value of the property by further estimating a Stoneley wave velocity as a function of frequency and estimating a Stoneley wave attenuation length.

15. The apparatus of claim 11 further comprising a salinity measuring device configured to measure a salinity of a fluid in the borehole fluid and wherein the processor is further configured to use the measured salinity for estimating the value of the property of the formation.

16. The apparatus of claim 15 wherein the processor is further configured to estimate the value of the property of the formation by using a partial pressure continuity condition at a boundary of the borehole.

17. The apparatus of claim 11 further comprising a wireline configured to convey the acoustic source into the borehole.

18. A non-transitory computer-readable medium product having stored thereon instructions that when read by a processor causes the processor to execute a method, the method comprising:

using an attenuation length for a propagating Stoneley wave in a borehole produced by an acoustic source, the attenuation length derived from a first signal indicative of a pressure associated with the propagating Stoneley wave and a second signal indicative of an electric potential associated with the propagating Stoneley wave for estimating a property of an earth formation selected from (i) a permeability of the formation, (ii) an electroacoustic constant of the formation

by estimating a second compressional velocity associated with the acoustic wave using at least the attenuation length for the acoustic wave.

19. The non-transitory computer-readable medium product of claim 18 further comprising at least one of: (i) a ROM, (ii) an EPROM, (iii) an EEPROM, (iv) a flash memory, and (v) an optical disk.

Assignments (2)
ASSIGNMENT OF ASSIGNOR'S INTEREST Recorded Jun 11, 2010
From: DUBINSKY, HEIR TO VLADIMIR
To: BAKER HUGHES INCORPORATED
Reel/Frame 024524/0053 →
ASSIGNMENT OF ASSIGNOR'S INTEREST Recorded Jun 11, 2010
From: DOROVSKY, VITALY N.; NEFEDKIN, YURIY A.; FEDEROV, ALEXANDER I.; PODBEREZHNYY, MAXIM Y.; PEREPECHKO, YURY V.
To: BAKER HUGHES INCORPORATED
Reel/Frame 024551/0922 →
Continuity (2)
Provisional Application 61166152 · Apr 2, 2009
Related Publication 20100254218A1 · Oct 7, 2010