Method of evaluating formations traversed by a borehole

• US 4,338,664 A
• Filed: 05/19/1980
• Issued: 07/06/1982
• Est. Priority Date: 05/19/1980
• Status: Expired due to Term

• Current Assignee: Schlumberger Technology Corporation (Schlumberger NV)
• Original Assignee: Schlumberger Technology Corporation (Schlumberger NV)
• Inventors: Mayer, Claude
• Primary Examiner(s): Gruber, Felix D.
• Application Number:
  US06/151,504
• Time in Patent Office: 778 Days
• Field of Search: 364/422, 364/300, 324/324, 324/338, 324/351, 73/152, 346/33 WL
• US Class Current: 702/11
• CPC Class Codes: G01V 11/002 Details, e.g. power supply systems for logging instruments, transmitting or recording data, specially adapted for well logging, also if the prospecting method is irrelevant means for transmitting well survey signals E21B47/12; signal transmission systems in general G08C; transmission in general H04B
• CPC Class Codes: G01V 3/38 Processing data, e.g. for analysis, for interpretation, for correction

Abstract

A method which determines output parameters (such as porosity φ or water saturation S_w of formations) from a set of logging measurements taken at each level of a borehole is proposed.

Measurement and response equation uncertainties of each logging apparatus are determined at each measurement level. Assumed values of the output parameters are chosen and, applying the response equations, calculated values of the measurements are determined. The calculated values of the measurements and the actual measurements are then compared to determine deviations which are weighted by factors calculated from the previously determined uncertainties. An incoherence function is determined from the weighted deviations and a number of "a-priori" constraints. Minimization of the incoherence function gives the most probable output parameters whose uncertainty is in turn calculated. The computed values of the measurements are plotted alongside an indication of the range of uncertainty of the actual measurements for their comparison so as to provide an indication of the reliability of the derived output parameters, which are also plotted with or without their own range of uncertainties.

Claims

1. A method for obtaining an improved display of an output parameter trace over a depth interval indicative of geologic formation characteristics from borehole derived raw data, including the steps of:

(1) deriving actual values of measurement parameters over said depth interval;

(2) assuming values for said output parameters over said depth interval;

(3) calculating theoretical values of said measurement parameters over said depth interval;

(4) displaying, over said depth interval, a trace of said assumed output parameters,

(5) displaying, for said depth interval, in juxtaposition, representations indicative of a trace of said actual values, and a trace of said calculated theoretical values, whereby the degree of agreement between said trace of actual values and said trace of theoretical values is indicative of the reliability of said trace of output parameters.

2. The method as recited in claim 1 further including the steps of:

(1) repetitively using different assumed values for said output parameters until the differences between the actual values and the calculated theoretical values for corresponding measurement parameters, as determined by an incoherence function, have been minimized;

(2) displaying, in juxtaposition with said trace of output parameters a trace of the minimum values of said incoherence function as an indication of reliability of said said trace of output parameters.

3. A method for obtaining an improved display of an output parameter trace over a depth interval indicative of geologic formation characteristics from borehole derived raw data, including the steps of:

(1) deriving actual values of measurement parameters over said depth interval from said raw data;

(2) assuming values for said output parameters over said depth interval from which are calculated theoretical values of said measurement parameters;

(3) repetitively calculating different theoretical values of said measurement parameters from different assumed values for said output parameters until the value of an incoherence function has reached a minimum, said incoherence function being dependent on the differences between said actual values and said calculated theoretical values;

(4) displaying, in the form of traces over said depth interval, in juxtaposition, the minimum values of said incoherence function and the corresponding assumed values of said output parameters.

4. A method for obtaining an improved display of a trace representing the behavior of output parameters characteristic of the geologic formations over a depth interval traversed by a borehole, said method including the steps of:

(a) physically logging said borehole depth interval by passing investigative logging tools through said borehole and recording the resultant raw data on formation characteristics and environmental conditions;

(b) from said raw data, obtaining actual values over said depth interval for a plurality of measurement parameters;

(c) deriving at least an equal plurality of response equations, each of which expresses a single measurement parameter as a function of one or more of said output parameters;

(d) assuming values for each of said output parameters at a particular depth in said depth interval;

(e) from said assumed values and said response equations, determining theoretical values for each of said measurement parameters;

(f) repeating steps d and e to obtain optimum theoretical values for which the difference between the actual values and their respective theoretical values have been made optimally small;

(g) repeating steps d, e and f for a plurality of different depths in said depth interval;

(h) recording, for comparison, on a visually readable medium, a trace indicative of said actual values over said depth interval along with a trace over said depth interval of respective optimum theoretical values and also recording at least one trace over said depth interval comprising those assumed values of said output parameters which correspond to the recorded trace of optimal theoretical values, whereby the visually ascertainable degree of agreement between said trace of actual values and said trace of optimal theoretical values is indicated of the reliability of said at least one trace of assumed values.

5. The method as recited in claim 4, further including the step of determining, from said data on environmental conditions and from the logging tools themselves, measurement parameter uncertainties of said actual values, and wherein said step of recording a trace indicative of said actual values includes the steps of separately modifying said trace indicative of said actual values by each of the positive and negative values of said corresponding measurement parameter uncertainties and recording each of the modified traces.

6. The method as recited in claim 5 wherein said method is practiced over a multiplicity of different levels in the borehole and in that the step of recording produces a number of continuous traces which not only contain information relative to each level but which also contain information relative to the degree and type of change of formation characteristics from level to level.

7. The method as recited in claim 5 wherein said step of determining measurement parameter uncertainties includes the determination of a positive uncertainty of a first magnitude and a negative uncertainty of a second, different magnitude.

8. The method as recited in claim 5 wherein said step of deriving an equal plurality of response equations includes the step of determining an uncertainty for each response equation.

9. The method as recited in claim 8, wherein said step of repeating steps d and e until the differences between the actual values and their respective theoretical values have been made optimally small, includes the further steps of:

(1) comparing the actual and the theoretical values of each of said measurement parameters to obtain a plurality of differences;

(2) constructing an incoherence function composed of each of said plurality of differences weighted by a factor dependent on both said measurement parameter and response equation uncertainties; and

(3) repetitively selecting subsequent assumed values of said output parameters in order to minimize said incoherence function.

10. The method according to claim 6, wherein the step of determining measurement parameter uncertainties includes the step of determining independent specific uncertainties due to distinct error sources.

11. The method according to claim 10, wherein the step of determining specific uncertainties comprises determining at least one specific uncertainty as a function of an environmental condition.

12. The method according to claim 11, wherein the step of determining specific uncertainties comprises determining said specific uncertainties as a function of actual values taken from among the measurement parameter actual values obtained at the examined level and at nearby levels.

13. The method according to one of the claims 10 to 12, wherein the step for determining specific uncertainties includes determining, for at least one measurement parameter, an uncertainty due to statistical variations, said statistical uncertainty being determined as a function of the actual value of said at least one measurement parameter at the examined level.

14. The method according to one of the claims 10 to 12, wherein the step for determining specific uncertainties at the examined level comprises:

determining, for at least one measurement parameter, an uncertainty being determined as a function of variations in the borehole diameter at levels near the examined level.

15. The method according to one of the claims 10 to 12, wherein the step for determining specific uncertainties at the examined level comprises determining, for at least one measurement parameter, an uncertainty due to depth correltion errors, said depth uncertainty being determined as a function of the actual value of said at least one measurement parameter at levels near the examined level.

16. The method according to claim 10, wherein the step for determining measurement parameter uncertainties comprises calculating the square root of the sum of the squares of said specific uncertainties.

17. The method according to claim 8, wherein the step of determining an uncertainty associated with each of said response equations comprises the step of determining, for each response equation, specific uncertainties which are respectively functions of said assumed values of said output parameters.

18. The method according to claim 17, wherein the step of determining uncertainties associated with each of said response equations comprises calculating the square root of the sum of the squares of said specific uncertainties.

19. The method according to claim 9 further including the step of determining said weighting factors by calculating the inverse of the sum of the squares of the uncertainties associated with the measurement parameters and the squares of the uncertainties associated with the response equations.

20. The method according to one of the claims 9 or 19, wherein said step of constructing an incoherence function includes carrying out the sum of the squares of said differences multiplied by said weighting factors.

21. The method according to claim 20, wherein the step of constructing an incoherence function includes combining, with said weighted differences, terms coming from a-priori constraints.

22. The method according to claim 21, wherein said step of constructing said incoherence function comprises:

calculating deviations between output parameters and limits which they must not exceed; and

multiplying the squares of these deviations by predetermined weighting factors to calculate the terms coming from a-priori constraints.

23. The method according to claim 4, further including the step consisting of determining at the examined level the uncertainties of said output parameters.

24. The method according to claim 23, further including the step of representing each of said output parameters by recording the limits of its uncertainty range at each level.

25. The method according to claim 9, further including the step of recording the minimum value of said incoherence function as an indication of reliability.

26. A method of obtaining an improved display of a trace over a depth interval of values of output parameters characteristic of the geologic formations traversed by a borehole, said method including the steps of:

(a) generating signals indicative of actual values for a plurality of borehole and/or formation parameters;

(b) deriving a plurality of response equations which functionally relate at least some of said formation parameters to said output parameters;

(c) utilizing said response equations and assumed values of said output parameters to obtain signals indicative of calculated or theoretical values for each of said at least some of said formation parameters;

(d) generating signals indicative of uncertainties for said responsive equations and for each of said at least some of said formation parameters;

(e) generating signals indicative of the differences between said calculated or theoretical value signals and said actual value signals;

(f) generating signals indicative of weighting factors dependent on said response equation uncertainty signals and said formation parameter uncertainty signals, said weighting factor signals being functionally related to the inverse of the sum of the squares of said uncertainty signals;

(g) combining said difference signals and said weighting factor signals to generate an incoherence function signal functionally related to the sum of the squares of said difference signals and directly related to said weighting factor signals;

(h) varying said assumed values of said output parameters until said incoherence signal has obtained a minimum value and generating output parameter signals indicative of the assumed values corresponding to said minimum incoherence signal;

(i) recording on a medium a trace representation over said depth interval of an output parameter signal and a trace representation over said depth interval of said minimum incoherence function signal.