Remote detection of hydrocarbon seeps

• US 4,517,458 A
• Filed: 11/23/1981
• Issued: 05/14/1985
• Est. Priority Date: 11/23/1981
• Status: Expired due to Fees

• Current Assignee: Anthony R. Barringer
• Original Assignee: Anthony R. Barringer
• Inventors: Barringer, Anthony R.
• Primary Examiner(s): FALCONE, JANICE ARRINGTON
• Application Number:
  US06/324,248
• Time in Patent Office: 1,268 Days
• Field of Search: 250/253, 250/301, 250/372, 250/373, 250/461.1
• US Class Current: 250/253
• CPC Class Codes: G01V 8/02 Prospecting
• CPC Class Codes: G01V 9/007 by detecting gases or particles representative of underground layers at or near the surface analysing earth materials G01N33/24; analysing gases per se G01N

Abstract

A method of detecting hydrocarbon seeps in a sea or in earth is disclosed. The method involves interrogating aerosols formed above the sea or earth surface with an intense beam of primary light radiation generated aboard an aircraft or other vehicle. The spectral composition of the beam is selected to induce secondary light radiation in certain hydrocarbon materials contained in aerosols generated by hydrocarbon seeps rising to the sea or earth surface. The secondary light radiation is detected aboard the aircraft and subjected to spectral analysis to determine whether the composition of the aerosols is characteristic of aerosols generated by hydrocarbon seeps. Apparatus for implementing the method is also disclosed.

Claims

1. A method of interrogating aerosols formed above a sea or earth surface to detect hydrocarbon gas seeps below the surface, comprising the steps of:

generating a beam of primary light radiation and directing the beam towards the surface, the beam being sufficiently intense and of such a spectral composition that the beam causes the aerosols to emit secondary light radiation;

detecting the secondary light radiation emanating from the aerosols; and

,

analysing the spectral content of the detected secondary radiation to determine whether the composition of aerosols indicates the existence of a hydrocarbon gas seep.

2. The method of claim 1 in which the beam of primary light radiation comprises a series of light pulses, and in which the secondary light radiation is detected during a time interval of predetermined duration commencing a predetermined time after the occurrence of each light pulse, whereby only secondary light radiation originating in some predetermined zone above the surface tends to be detected.

3. The method of claim 2 in which the beam of primary light radiation is generated with a nitrogen laser producing light pulses having a spectral component with a wavelength of about 338 nanometers.

4. The method of claim 2 in which the beam of primary light radiation is generated with a krypton fluoride laser producing light pulses having a spectral component with a wavelength of about 248 nanometers.

5. Apparatus for detecting hydrocarbon seeps in a sea or in earth by interrogation of aerosols formed above the sea or earth surface, comprising:

p1 means for generating a beam of primary light radiation and directing the beam towards the surface, the beam being sufficiently intense and of such a spectral composition that the beam causes the aerosols to emit secondary light radiation;

means for detecting the secondary light radiation, including range-gate means for regulating operation of the detecting means so that only secondary radiation from sources in some predetermined zone above the surface containing aerosols tends to be detected; and

,

spectral analysis means for use in analysing the spectral content of the detected secondary radiation whereby a determination can be made whether the composition of the aerosols indicates the existence of a hydrocarbon gas seep.

6. Apparatus as claimed in claim 5 in which the beam of primary light radiation comprises a series of light pulses, and the range gate means activate the detecting means to respond to the secondary light radiation during a time interval of preselected duration commencing a pre-selected time after the occurrence of each light pulse whereby only secondary light radiation occurring in the predetermined zone above the surface tends to be detected,

7. Apparatus as claimed in claim 6 in which the detecting means comprise:

telescope means for receiving the secondary light radiation;

means for producing a spectral dispersion of the received secondary light radiation;

amplification means responsive to the spectral dispersion for producing signals indicative of the spectral content of the spectral dispersion, the amplification means being gated by the range gate means to produce the signals indicative of spectral content only during the time interval of preselected duration.

8. Apparatus as claimed in claim 7 in which the means for generating the beam of primary light radiation comprise a nitrogen laser that produces light pulses having a spectral component with wavelength of 338 nanometers.

9. Apparatus as claimed in claim 7 in which the means for generating the beam of primary light radiation comprise a krypton fluoride laser that produces light pulses having a spectral component with wavelength of 248 nanometers.

10. A method of detecting hydrocarbon gas seeps in the sea, comprising the steps of:

generating a beam of primary light radiation and directing the beam towards the sea surface, the beam being sufficiently intense and of such a spectral composition that the beam causes aerosols formed above the sea surface by hydrocarbon gas seeps to emit secondary light radiation;

detecting secondary light radiation emanating from a region above the sea surface containing aerosols; and

,

analysing the spectral content of the detected secondary light radiation to determine whether the composition of the aerosols above the sea surface indicates the existence of a hydrocarbon gas seep.

11. The method of claim 10 in which the beam of primary light radiation comprises a series of light pulses, and in which the secondary light radiation is detected during a time interval of predetermined duration commencing a predetermined time after the occurrence of each light pulse, whereby only secondary light radiation originating in some predetermined zone above the surface tends to be detected.

12. The method of claim 11 in which the beam of primary light radiation is generated with a nitrogen laser producing light pulses having a spectral component with a wavelength of about 338 nanometers.

13. The method of claim 11 in which the beam of primary light radiation is generated with a krypton fluoride laser producing light pulses having a spectral component with a wavelength of about 248 nanometers.

14. Apparatus for use in detecting hydrocarbon seeps in the sea, comprising:

means for generating a beam of primary light radiation and directing the beam towards the surface, the beam being sufficiently intense and of such a spectral composition that the beam causes aerosols formed above the sea surface by hydrocarbon gas seeps to emit secondary light radiation;

means for detecting the secondary light radiation, including range-gate means for regulating operation of the detecting means so that only secondary radiation from sources in a predetermined zone above the surface containing aerosols tends to be detected; and

,

spectral analysis means for use in analysing the spectral content of the detected secondary radiation whereby a determination can be made whether the composition of the aerosols indicates the existence of a hydrocarbon seep.

15. Apparatus as claimed in claim 14 in which the beam of primary light radiation comprises a series of light pulses, and the range-gate means activate the detecting means to respond to the secondary light radiation during a time interval of preselected duration commencing a preselected time after the occurrence of each light pulse whereby only secondary light radiation occurring in the predetermined zone above the surface tends to be detected.

16. Apparatus as claimed in claim 15 in which the detecting means comprise:

telescope means for receiving the secondary light radiation;

means for producing a spectral dispersion of the received secondary light radiation;

amplification means responsive to the spectral dispersion for producing signals indicative of the spectral content of the spectral dispersion, the amplification means being gated by the range-gate means to produce the signals indicative of spectral content only during the time interval of preselected duration.

17. Apparatus as claimed in claim 16 in which the means for generating the beam of primary light radiation comprise a nitrogen laser that produces light pulses having a spectral component with wavelength of 338 nanometers.

18. Apparatus as claimed in claim 16 in which the means for generating the beam of primary light radiation comprise a krypton fluoride laser that produces light pulses having a spectral component with wavelength of 248 nanometers.