IP Library Granted Patent US 10,947,839
Granted Patent B2
US 10,947,839 · App. 15/316,494 · Granted Mar 16, 2021

Downhole thermal anomaly detection for passive ranging to a target wellbore

Inventors: Andrew J. Cuthbert (Houston, TX); Joseph E. Hess (Richmond, TX); Carl J. Cramm (Houston, TX)
Assignee: Halliburton Energy Sendees, Inc.
E21B47/103E21B7/04E21B47/022E21B47/047E21B47/07G01V9/005
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Quick Facts
Patent No.
US 10,947,839
App. No.
15/316,494
Granted
Mar 16, 2021
Kind
B2
Abstract

A method can include measuring temperature along a relief wellbore, thereby detecting a temperature anomaly in an earth formation penetrated by the relief wellbore, and determining a location of an influx into a target wellbore, based on the temperature anomaly detecting. A thermal anomaly ranging system for use with a subterranean well can include a temperature sensor in a relief wellbore that penetrates an earth formation, the temperature sensor detecting a temperature anomaly in the formation, and the temperature anomaly being caused by an influx into a target wellbore. Another method can include measuring optical scattering in an optical waveguide positioned in a relief wellbore, thereby detecting a temperature anomaly in an earth formation penetrated by the relief wellbore, and determining a location of an influx into a target wellbore, based on the temperature anomaly detecting.

Claims (25)

1. A method, comprising:

measuring temperature along a relief wellbore, thereby detecting a temperature anomaly in an earth formation penetrated by the relief wellbore; and

determining a location of an influx into a target wellbore, based on the temperature anomaly detecting.

2. The method of claim 1 , wherein the temperature anomaly is produced in response to the influx into the target wellbore.

3. The method of claim 1 , further comprising determining a flow rate of the influx into the target wellbore, based on the temperature anomaly detecting.

4. The method of claim 1 , further comprising determining a composition of the influx into the target wellbore, based on the temperature anomaly detecting.

5. The method of claim 1 , wherein the temperature anomaly comprises a deviation from a geothermal gradient in the formation.

6. The method of claim 1 , wherein the measuring comprises detecting optical scattering in an optical waveguide positioned in the relief wellbore.

7. The method of claim 1 , further comprising establishing fluid communication between the relief and target wellbores after the determining.

8. The method of claim 1 , wherein the location of the influx is at an open hole portion of the target wellbore.

9. A thermal anomaly ranging system for use with a subterranean well, comprising:

a temperature sensor in a relief wellbore that penetrates an earth formation, wherein the temperature sensor detects a temperature anomaly in the formation, the temperature anomaly being caused by an influx into a target wellbore.

10. The system of claim 9 , wherein the temperature sensor comprises an optical waveguide.

11. The system of claim 10 , further comprising an optical interrogator that measures scattering in the optical waveguide.

12. The system of claim 9 , wherein the temperature anomaly comprises a deviation from a geothermal profile in the formation.

13. The system of claim 9 , wherein the influx is at an open hole portion of the target wellbore.

14. A method, comprising:

measuring optical scattering in an optical waveguide positioned in a relief wellbore, thereby detecting a temperature anomaly in an earth formation penetrated by the relief wellbore; and

determining a location of an influx into a target wellbore, based on the temperature anomaly detecting.

15. The method of claim 14 , wherein the temperature anomaly is produced in response to the influx into the target wellbore.

16. The method of claim 14 , further comprising determining a flow rate of the influx into the target wellbore, based on the temperature anomaly detecting.

17. The method of claim 14 , further comprising determining a composition of the influx into the target wellbore, based on the temperature anomaly detecting.

18. The method of claim 14 , wherein the temperature anomaly comprises a deviation from a geothermal gradient in the formation.

19. The method of claim 14 , further comprising establishing fluid communication between the relief and target wellbores after the determining.

20. The method of claim 14 , wherein the location of the influx is at an open hole portion of the target wellbore.

Assignments (1)
ASSIGNMENT OF ASSIGNOR'S INTEREST Recorded Dec 5, 2016
From: CUTHBERT, ANDREW J.; HESS, JOSEPH E.; CRAMM, CARL J.
To: HALLIBURTON ENERGY SERVICES, INC.
Reel/Frame 040531/0013 →
Continuity (1)
Related Publication 20170145815A1 · May 25, 2017
Cited By (5)
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