Exploring for subsurface hydrocarbons by sea floor temperature gradients preferably using a multiplexed thermistor probe

• US 4,676,664 A
• Filed: 07/15/1983
• Issued: 06/30/1987
• Est. Priority Date: 07/15/1983
• Status: Expired due to Term

• Current Assignee: Trustees Of Columbia University In The City Of New York (Columbia University)
• Original Assignee: Trustees Of Columbia University In The City Of New York (Columbia University)
• Inventors: Hobart, Michael A., Van Steveninck, William, Anderson, Roger N.
• Primary Examiner(s): Frankfort, Charles
• Assistant Examiner(s): NOT, DEFINED
• Application Number:
  US06/514,303
• Time in Patent Office: 1,446 Days
• Field of Search: 374/136, 374/183, 374/169, 73/154, 73/170 A, 73/432 R, 436/29, 175/50
• US Class Current: 374/136
• CPC Class Codes: E21B 47/07 Temperature
• CPC Class Codes: G01K 1/026 arrangements for monitoring a plurality of temperatures, e.g. by multiplexing
• CPC Class Codes: G01K 13/10 for measuring temperature within piled or stacked materials by special arrangements for conducting heat from the object to the sensitive heat element G01K1/16
• CPC Class Codes: G01V 9/005 by thermal methods, e.g. after generation of heat by chemical reactions

Abstract

Disclosed are a method and a system for measuring the sea floor temperature gradient several meters into the formation at each of an array of measurement sites, and using these gradients to explore for and characterize hydrocarbon deposits. The measurements can be taken with a special lance driven into the otherwise undisturbed sea floor.

Claims

1. A method of exploring the sea floor for subsurface hydrocarbons comprising the steps of:

selecting measurement sites arrayed along the sea floor in a pattern selected as a function of available geological information;

measuring substantially continuous temperature gradients at a plurality of depths within several meters into the sea floor at each of said sites by taking temperature readings at each of said sites, correcting said temperature readings for transient disturbances by ascertaining the temperature at each site at the same depth for a period of time and extrapolating from the temperatures so ascertained corresponding equilibrium temperatures which would be measured if taken after an infinitely long time in an unchanging environment and from said extrapolated equilibrium temperatures determining said temperature gradients;

determining the contribution to said temperature gradients caused by heat propagation through said sea floor resulting from long term bottom water temperature variations; and

differentiating any fluid advection contribution in the measured actual values of temperature when adjusted for the contributions due to said long term buttom water temperature variations at the respctive measurement sites;

calculating the surface heat flow at each site from the corresponding temperature gradient at said site while, eliminating the long term bottom water and fluid advection contributions determined at said site; and

producing a map of said surface heat flow, said map being indicative of characteristics of subsurface hydrocarbon convection through nearby subsurface formations and thereby the location of said subsurface hydrocarbons.

2. A method as in claim 1 in which said transient disturbances include frictional heat due to positioning of temperature measuring devices into the sea floor and characteristics of heat propagation from surrounding formations to said temperature measuring devices.

3. A method as in claim 1 in which the measuring step comprises, for each site, driving a temperature measuring lance into the sea bottom, determining whether the lance has been driven in to a sufficient depth, whether the lance has produced invalid temperature data and whether the site selection is consistent with available knowledge of the subsurface geology and lithology, and revising the measuring step as needed in accordance with the last recited determination.

4. A method as in claim 3 in which the measuring step including, for each site, verifying and revising as needed the selection of the next site in accordance with the last recited determination.

5. A method as in claim 1 in which the step of determining the contribution to said gradients due to heat propagation resulting from long term water temperature variations includes finding said contribution, for each measurement site, as a function of coefficients of a Fourier series representation of the long term bottom water temperature variations, thermal diffusivity of subsurface formations at the site, and phase shift for component waves of the Fourier series.

6. A method as in claim 1 in which the step of calculating heat flow at the respective sites and eliminating said fluid advection contribution comprises finding, for each site, a geothermal gradient by removing from the measured gradient the contribution due to heat propagation resulting from long term bottom water temperature variations, determining if the geothermal gradient varies substantially linearly with depth into the sea floor and, if not, correcting it for effects of significant fluid advection through the sea floor at the site.

7. A method as in claim 6 in which said correction for fluid advection at the site is made as a function of top and bottom temperatures which have been measured at the site and have been corrected for long term bottom water temperature variations, Peclet number, density of saturated medium around the site and heat capacity of said medium.

8. A method as in claim 1 including the steps of producing a geological model of subsurface formations in the vicinity of the measurement sites and adjusting the model as needed to achieve a substantial agreement thereof with the surface heat flow map.

9. A model as in claim 8 in which the step of adjusting the geological model includes taking into account effect, on the surface heat flow at each site, of sedimentation at the site.

10. A method as in claim 9 in which said accounting for sedimentation is as a function of an estimated sedimentation rate and duration of the sedimentation and thermal diffusivity of the sediment.

11. A method as in claim 10 including projecting the surface heat flow map downwardly to find temperature characteristics of a subsurface hydrocarbon trap.

12. A method as in claim 1 in which the step of measuring the temperature gradients comprises taking temperature readings using thermistor temperature sensors which are in a circuit establishing a substantially linear relationship between the log of the ratio of the resistances of a thermistor at two different temperatures and the difference between said temperatures over an expected operating temperature range.

13. A method as in claim 1 in which said measuring step includes taking temperature readings using temperature measuring sensors arrayed at a density of at least 25 per meter along a lance which has a length of several meters long, driving said lance into the sea floor, to a depth of several meters, at each measurement site and leaving said lance therein for a time period long enough to measure said temperature gradient, before being moved to the next site.

14. A method as in claim 13 in which outputs of said temperature measuring sensors are multiplexed up the lance over a set of conductors shared by all sensors, and the multiplexed outputs are recorded by apparatus coupled with the lance from site to site.

15. A method as in claim 13 in which said temperature measuring sensors comprise thermistors connected in an electrical circuit which provides electrical outputs which vary substantially linearly with temperature changes of the thermistors over temperature windows that are several decades of °

C. wide and include the typical range of ambient temperatures to which the sensors are likely to be exposed in said step of measuring temperature gradients.

19. A method as in claim 1 in which the step of measuring the temperature gradients comprises taking temperature readings using thermistor temperature sensors which are in a circuit establishing a substantially linear relationship between the log of the ratio of the resistance of one thermistor which is at one of said temperatures and of another thermistor which is at another of said temperatures and the difference between said temperatures over an expected operating temperature range.

16. A method of making geothermal measurements comprising establishing thermal contact between a thermistor and a geological formation whose temperature is to be measured and relating, through a circuit arrangement, (i) the log of the ratio of the resistance of the thermistor at a first temperature to the resistance at a second temperature and (ii) a difference between said temperatures, in a manner allowing said relating to remain substantially linear throughout a temperature range of several decades of °

C. of expected temperatures and said circuit implementing a product of (i) said first temperature plus an offset, and (ii) said second temperature plus an offset, wherein said offset is selected, for a given thermistor or set of thermistors, to be at a level satisfying said linearity.

17. A method of making geothermal measurements which comprises establishing thermal contact between at least two thermistors and a geological formation whose temperature is to be measured and relating, through a circuit arrangement, (i) the log of the ratio of resistance of a first thermistor at a first temperature to its resistance at a second temperature and (ii) the log of the ratio of the resistance of a second thermistor at a third temperature to its resistance at the second temperature, in a manner allowing said relationship to remain substantially linear throughout a temperature range of several decades of °

C. of expected temperatures said circuit implementing a product of (i) said first temperature plus an offset, and (ii) said second temperature plus an offset, wherein said offset is selected, for a given thermistor or set of thermistors, to be at a level satisfying said linearity.

18. A method of determining at a geological surface level strata heat flow emanating through the strata from below surface geothermal sources comprising:

measuring a substantially continuous temperature gradient in the strata at a site from the surface at a plurality of depths within several meters below the surface by taking temperature readings at said site, correcting said temperature readings for transient disturbances by ascertaining the temperature at the same depth for a period of time and extrapolating from the temperatures so ascertained corresponding equilibrium temperatures which would be measured if taken after an infinitely long time in an unchanging environment and from said extrapolated equilibrium temperatures determining said temperature gradient;

determining the contribution to said temperature gradient at said site in the strata from the surface to the depth of said several meters caused by above-surface heat propagation through said strata; and

differentiating any fluid advection contribution in the measured actual values of temperature when adjusted for the contribution due to above-surface heat propagation; and

calculating heat flow from said temperature gradient, while eliminating said above-surface heat propagation and fluid advection contributions during said heat flow calculation.