Monitoring a Geological Formation

• US 20170315261A1
• Filed: 04/14/2017
• Published: 11/02/2017
• Est. Priority Date: 04/29/2016
• Status: Active Grant

• Current Assignee: Optasense Holdings Limited (Luna Innovations, Inc.)
• Original Assignee: Optasense Holdings Limited (Luna Innovations, Inc.)
• Inventors: Bartling, William, Godfrey, Alastair
• Granted Patent: US 10,444,064 B2
• Time in Patent Office: Days
• CPC Class Codes: G01H 9/004 using fibre optic sensors light guides per se G02B6/00, acousto-optical devices specially adapted for gating or modulating in optical wave guides G02F1/125
• CPC Class Codes: G01V 2210/1429 Subsurface, e.g. in borehole or below weathering layer or mud line

Abstract

This application relates to methods and apparatus for monitoring a geological formation that is or has been subjected to steam injection using a distributed fibre optic sensor apparatus to perform distributed fibre optic sensing on an optical fibre deployed in a borehole running through the geological formation to acquire a first set of measurement signals being indicative of disturbances acting on each of a plurality of longitudinal sensing portions of the first optical fibre where at least part of the optical fibre is disposed adjacent to at least a first electrode spaced apart from a second electrode and the first and second electrode are separated by a void that is filled with a gas and an electrical source applies a potential difference to the first and second electrodes such that an ionisation event within the gas results in an avalanche multiplication.

Claims

1. A method of monitoring a geological formation subjected to steam injection, the method comprising:

performing distributed fibre optic sensing on a first optical fibre deployed in a borehole running through the geological formation to acquire a first set of measurement signals being indicative of disturbances acting on each of a plurality of longitudinal sensing portions of the first optical fibre;

wherein at least part of the first optical fibre is disposed adjacent to at least a first electrode spaced apart from a second electrode, with a gas between the first and second electrodes and wherein the potential difference between the first and second electrodes is such that an ionisation event within the gas results in an avalanche multiplication;

the method further comprising analysing the first set of measurement signals to determine a spatial distribution of radioactive sources throughout the geological formation.

2. A method as claimed in claim 1 wherein analysing the first set of measurement signals comprises identifying signals characteristic of avalanche multiplication in the gas between the first and second electrodes.

3. A method as in claim 1 further comprising mapping the distribution of steam and/or condensed steam in the geological formation, based on the spatial distribution of radioactive sources.

4. A method as in claim 1 further comprising determining a change in the distribution of radioactive sources over time.

5. A method as in claim 1 comprising analysing the concentration and/or the inflow or outflow of the steam and/or condensed steam based on the spatial distribution of radioactive sources to determine areas of steam penetration or areas where there is a lack of steam penetration in the geological formation.

6. A method as in claim 1 further comprising acquiring background noise signal by performing distributed fibre optical sensing when the potential difference between the electrodes is not sufficient to cause avalanche multiplication in response to an ionisation event and/or by performing distributed fibre optical sensing on a second sensing optical fibre which is spaced apart from the first and second electrodes so as to be substantially insensitive to any avalanche multiplication.

7. A method as in claim 6 wherein the method comprises subtracting the background noise signal from the first set of measurements.

8. A method as claimed in claim 1 further comprising:

performing distributed fibre optic sensing on a second optical fibre deployed in a borehole running through the geological formation to acquire a second set of measurement signals being indicative of disturbances acting on each of a plurality of longitudinal sensing portions of the first optical fibre;

wherein at least part of the second optical fibre is disposed adjacent to at least a third electrode spaced apart from a fourth electrode, with a gas between the third and fourth electrodes and wherein the potential difference between the third and fourth electrodes is such that an ionisation event within the gas results in an avalanche multiplication; and

analysing both the first and second set of measurement signals to determine a spatial distribution of radioactive sources throughout the geological formation.

9. A method as claimed in claim 8 wherein the first and second optical fibres are located in different areas of the geological formation.

10. A method as claimed in claim 1 further comprising the step of determining the spatial distribution of radioactive sources whilst steam is being injected and controlling at least one parameter of steam injection based on the determined spatial distribution of radioactive sources.

11. A method as claimed in claim 1 further comprising the step of determining the spatial distribution of radioactive sources whilst product is produced from the wellbore.

12. An apparatus for monitoring a geological formation subjected to steam injection, the apparatus comprising:

a fibre optic cable structure comprising a first optical fibre disposed adjacent first and second electrodes, the first and second electrodes being separated by a gas;

a distributed fibre optic sensor interrogator unit configured to, in use, perform distributed fibre optic sensing on the first optical fibre when the fibre optic cable structure is deployed in a borehole running through the geological formation to acquire a first set of measurement signals being indicative of disturbances acting on each of a plurality of longitudinal sensing portions of the first optical fibre;

an electrical source for generating a potential difference between the first and second electrodes such that an ionisation event within the gas results in an avalanche multiplication; and

a processor configured to analyse the first set of measurement signals to determine a spatial distribution of radioactive sources throughout the geological formation.

13. An apparatus as claimed in claim 12 wherein the processor is configured to analyse the first set of measurement signals to identify signals characteristic of avalanche multiplication in the gas between the first and second electrodes.

14. An apparatus as claimed in claim 12 wherein the processor is further configured to map the distribution of steam and/or condensed steam in the geological formation, based on the spatial distribution of radioactive sources.

15. An apparatus as claimed in claim 14 wherein the processor is further configured to map the concentration of steam and/or condensed steam in the geological formation, using the spatial distribution of radioactive sources.

16. An apparatus as claimed in claim 12 wherein the processor is further configured to determine a change in the distribution of radioactive sources over time.

17. An apparatus as claimed in claim 12 wherein the processor is further configured to analyse the concentration and/or the inflow or outflow of the steam and/or condensed steam based on the spatial distribution of radioactive sources to determine areas of steam penetration or areas where there is a lack of steam penetration in the geological formation.

18. An apparatus as claimed in claim 12 wherein the apparatus is operable in a background noise measurement mode, wherein in the background noise measurement mode the distributed fibre optic sensor interrogator unit is configured to perform distributed fibre optic sensing on the first optical fibre during a period when the electrical source is configured to operate such that the potential difference between the first and second electrodes is not sufficient to cause avalanche multiplication in response to an ionisation event so as to generate a background noise signal.

19. An apparatus as claimed in claim 12 further comprising a second sensing optical fibre which is spaced apart from the first and second electrodes so as to be substantially insensitive to any avalanche multiplication and wherein the apparatus is configured to perform distributed fibre optic sensing on the second optical fibre to provide a background noise signal.

20. An apparatus as claimed in claim 19 wherein said distributed fibre optic sensor interrogator unit is configured to perform distributed fibre optic sensing on both the first and second optical fibres.

21. An apparatus as claimed in claim 18 wherein the processor is configured to subtract the background noise signal from the first set of measurements.

22. A method of determining information about a geological formation subjected to steam injection, the method comprising:

accessing a first set of measurement signals, the first set of measurement signals having been acquired by performing distributed fibre optic sensing on a first optical fibre deployed in a borehole running through the geological formation and being indicative of disturbances acting on each of a plurality of longitudinal sensing portions of the first optical fibre;

wherein at least part of the first optical fibre was disposed adjacent to at least a first electrode spaced apart from a second electrode, with a gas between the first and second electrodes and wherein the potential difference between the first and second electrodes is such that an ionisation event within the gas results in an avalanche multiplication;

the method further comprising analysing the first set of measurement signals to determine a spatial distribution of radioactive sources throughout the geological formation.