Apparatus and method for determining subsurface formation properties

• US 4,158,165 A
• Filed: 06/16/1977
• Issued: 06/12/1979
• Est. Priority Date: 06/16/1977
• Status: Expired due to Term

• Current Assignee: Schlumberger Technology Corporation (SLB)
• Original Assignee: Schlumberger Technology Corporation (SLB)
• Inventors: Coates, George R.
• Primary Examiner(s): Strecker, Gerard R.
• Application Number:
  US05/806,983
• Time in Patent Office: 726 Days
• Field of Search: 324/6
• US Class Current: 324/338
• CPC Class Codes: E21B 49/00 Testing the nature of borehole walls; Formation testing; Methods or apparatus for obtaining samples of soil or well fluids, specially adapted to earth drilling or wells
• CPC Class Codes: G01V 3/30 operating with electromagnetic waves
• CPC Class Codes: Y02A 90/30 Assessment of water resources

Abstract

The disclosure is directed to an apparatus and method for determining the water-filled porosity of formations surrounding a borehole. Alternatively, where porosity is known from other logging information, the disclosed techniques can be utilized for determining the conductivity of the water in formations surrounding a borehole or for determining water saturation. The formations are assumed to comprise a matrix, which may be any subsurface solid material, and fluids contained in the matrix, such as in pore spaces or interstices therein. In accordance with one embodiment, means are provided for deriving a first quantity which is representative of the attenuation of microwave electromagnetic energy propagating between spaced locations in the borehole, the first quantity being, for example, the attenuation constant, α. Means are also provided for deriving a second quantity representative of the relative phase shift of microwave electromagnetic energy propagating between the spaced locations, the second quantity being, for example, the phase constant, β. Further means are provided for deriving a third quantity representative of the conductivity of the water in the formations surrounding the spaced locations. In the preferred form of the invention, the investigated formations are in the invaded zone surrounding the borehole and the conductivity of the water is determinable from the conductivity of the drilling mud being utilized and the nature of the mud filtrate resulting from invasion of the formations by the drilling mud. Means are also provided for generating a fourth quantity which is proportional to the product of the first and second quantities and inversely proportional to the third quantity. The generated fourth quantity is indicative of the water-filled porosity, φ_w, of the formations adjacent the region of the spaced locations in the borehole. In alternative forms of the invention, where porosity is known, the conductivity, σ_w, or the apparent conductivity, σ_w '"'"', of the water in formations surrounding the borehole is determined.

Claims

1. Apparatus for determining the water-filled porosity of formations surrounding a borehole, comprising:

means for deriving a first quantity representative of the attenuation of microwave electromagnetic energy propagating between spaced locations in the borehole;

means for deriving a second quantity representative of the relative phase shift of microwave electromagnetic energy propagating between said spaced locations in the borehole;

means for deriving a third quantity representative of the conductivity of the water in the formations surrounding said spaced locations; and

means for generating a fourth quantity which is proportional to the product of said first and second quantities and inversely proportional to said third quantity;

said fourth quantity being indicative of the water-filled porosity of said formations.

2. Apparatus as defined by claim 1 wherein said first quantity is the attenuation constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

3. Apparatus as defined by claim 1 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

4. Apparatus as defined by claim 2 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

5. Apparatus as defined by claim 1 wherein said borehole is filled with drilling mud and said third quantity is the conductivity of the mud filtrate in the formations invaded by said drilling mud.

6. Apparatus as defined by claim 4 wherein said borehole is filled with drilling mud and said third quantity is the conductivity of the mud filtrate in the formations invaded by said drilling mud.

7. Apparatus as defined by claim 1 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

8. Apparatus as defined by claim 4 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

9. Apparatus as defined by claim 6 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

10. Apparatus for determining the conductivity of the water in formations surrounding a borehole, comprising:

means for deriving a first quantity representative of the attenuation of microwave electromagnetic energy propagating between spaced locations in the borehole;

means for deriving a second quantity representative of the relative phase shift of microwave electromagnetic energy propagating between said spaced locations in the borehole;

means for deriving a third quantity representative of the porosity of the formations surrounding said spaced locations; and

means for generating a fourth quantity which is proportional to the product of said first and second quantities and inversely proportional to said third quantity;

said fourth quantity being indicative of the conductivity of the water in said formations.

11. Apparatus as defined by claim 10 wherein said third quantity is representative of the water-filled porosity of said formations.

12. Apparatus as defined by claim 10 wherein said third quantity is representative of the total porosity of said formations and said fourth quantity is indicative of the apparent conductivity of the water in said formations.

13. Apparatus as defined by claim 10 wherein said first quantity is the attenuation constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

14. Apparatus as defined by claim 10 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

15. Apparatus as defined by claim 13 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

16. Apparatus as defined by claim 10 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

17. Apparatus as defined by claim 15 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

18. Apparatus for determining the water-filled porosity of formations surrounding a borehole, comprising:

means for injecting microwave electromagnetic energy into the formations;

means for measuring a first quantity representative of the attenuation of microwave electromagnetic energy propagating between spaced locations in the borehole;

means for measuring a second quantity representative of the relative phase shift of microwave electromagnetic energy propagating between said spaced locations in the borehole;

means for deriving a third quantity representative of the conductivity of the water in the formations surrounding said spaced locations; and

means for generating a fourth quantity which is proportional to the product of said first and second quantities and inversely proportional to said third quantity;

said fourth quantity being indicative of the water-filled porosity of said formations.

19. Apparatus as defined by claim 18 wherein said first quantity is the attenuation constant of said microwave electromagnetic energy propagating between said space locations in the borehole.

20. Apparatus as defined by claim 18 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

21. Apparatus as defined by claim 20 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

22. Apparatus as defined by claim 18 wherein said borehole is filled with drilling mud and said third quantity is the conductivity of the mud filtrate in the formations invaded by said drilling mud.

23. Apparatus as defined by claim 21 wherein said borehole is filled with drilling mud and said third quantity is the conductivity of the mud filtrate in the formations invaded by said drilling mud.

24. Apparatus as defined by claim 18 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

25. Apparatus as defined by claim 21 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

26. Apparatus as defined by claim 23 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

27. Apparatus for determining the conductivity of the water in formations surrounding a borehole, comprising:

means for injecting microwave electromagnetic energy into the formations;

means for measuring a first quantity representative of the attenuation of microwave electromagnetic energy propagating between spaced locations in the borehole;

means for measuring a second quantity representative of the relative phase shift of microwave electromagnetic energy propagating between said spaced locations in the borehole;

means for deriving a third quantity representative of the porosity of the formations surrounding said spaced locations; and

means for generating a fourth quantity which is proportional to the product of said first and second quantities and inversely proportional to said third quantity;

said fourth quantity being indicative of the conductivity of the water in said formations.

28. Apparatus as defined by claim 27 wherein said third quantity is representative of the water-filled porosity of said formations.

29. Apparatus as defined by claim 27 wherein said third quantity is representative of the total porosity of said formations and said fourth quantity is indicative of the apparent conductivity of the water in said formations.

30. Apparatus as defined by claim 27 wherein said first quantity is the attenuation constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

31. Apparatus as defined by claim 27 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

32. Apparatus as defined by claim 30 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

33. Apparatus as defined by claim 27 wherein said microwave electromagnetic energy has a frequency of about

35. Apparatus as defined by claim 32 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

37. The method as defined by claim 35 wherein said first quantity is the attenuation constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

38. The method as defined by claim 35 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

40. The method as defined by claim 35 wherein said borehole is filled with drilling mud and said third quantity is the conductivity of the mud filtrate in the formations invaded by said drilling mud.

41. The method as defined by claim 38 wherein said borehole is filled with drilling mud and said third quantity is the conductivity of the mud filtrate in the formations invaded by said drilling mud.

42. The method as defined by claim 35 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

43. The method as defined by claim 38 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

44. The method as defined by claim 40 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

46. The method as defined by claim 44 wherein said third quantity is representative of the water-filled porosity of said formations.

47. The method as defined by claim 44 wherein said third quantity is representative of the total porosity of said formations and said fourth quantity is indicative of the apparent conductivity of the water in said formations.

48. The method as defined by claim 44 wherein said first quantity is the attenuation constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

49. The method as defined by claim 44 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

50. The method as defined by claim 47 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

51. The method as defined by claim 44 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

52. The method as defined by claim 47 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

54. The method as defined by claim 52 wherein said first quantity is the attenuation constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

55. The method as defined by claim 52 wherein said second quantity is the phase constant of said microwave electro-magnetic energy propagating between said spaced locations in the borehole.

56. The method as defined by claim 52 wherein said borehole is filled with drilling mud and said third quantity is the conductivity of the mud filtrate in the formations invaded by said drilling mud.

57. The method as defined by claim 52 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

59. The method as defined by claim 57 wherein said third quantity is representative of the water-filled porosity of said formations.

60. The method as defined by claim 57 wherein said third quantity is representative of the total porosity of said formations and said fourth quantity is indicative of the apparent conductivity of the water in said formations.

61. The method as defined by claim 57 wherein said first quantity is the attenuation constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

62. The method as defined by claim 57 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

63. The method as defined by claim 57 wherein said microwave electromagnetic energy has a frequency of about 1.1 GHz.

65. Apparatus as defined by claim 63 wherein said borehole is filled with drilling mud and wherein σ

_w is derived from the conductivity of the mud filtrate in the formations invaded by said drilling mud.

34. 1 GHz.

36. A method for determining the water-filled porosity of formations surrounding a borehole, comprising the steps of:

deriving a first quantity representative of the attenuation of microwave electromagnetic energy propagating between spaced locations in the borehole;

deriving a second quantity representative of the relative phase shift of microwave electromagnetic energy propagating between said spaced locations in the borehole;

deriving a third quantity representative of the conductivity of the water in the formations surrounding said spaced locations; and

generating a fourth quantity which is proportional to the product of said first and second quantities and inversely proportional to said third quantity;

said fourth quantity being indicative of the water-filled porosity of said formations.

39. The method as defined by claim 36 wherein said second quantity is the phase constant of said microwave electromagnetic energy propagating between said spaced locations in the borehole.

45. A method for determining the conductivity of the water in formations surrounding a borehole, comprising the steps of:

deriving a first quantity representative of the attenuation of microwave electromagnetic energy propagating between spaced locations in the borehole;

deriving a second quantity representative of the relative phase shift of microwave electromagnetic energy propagating between said spaced locations in the borehole;

deriving a third quantity representative of the porosity of the formations surrounding said spaced locations; and

generating a fourth quantity which is proportional to the product of said first and second quantities and inversely proportional to said third quantity;

said fourth quantity being indicative of the conductivity of the water in said formations.

53. A method for determining the water-filled porosity of formations surrounding a borehole, comprising the steps of:

injecting microwave electromagnetic energy into the formations;

measuring a first quantity representative of the attenuation of microwave electromagnetic energy propagating between spaced locations in the borehole;

measuring a second quantity representative of the relative phase shift of microwave electromagnetic energy propagating between said spaced locations in the borehole;

deriving a third quantity representative of the conductivity of the water in the formations surrounding said spaced locations; and

generating a fourth quantity which is proportional to the product of said first and second quantities and inversely proportional to said third quantity;

said fourth quantity being indicative of the water-filled porosity of said formations.

58. A method for determining the conductivity of the water in formations surrounding a borehole, comprising the steps of:

injecting microwave electromagnetic energy into the formations;

measuring a first quantity representative of the attenuation of microwave electromagnetic energy propagating between spaced locations in the borehole;

measuring a second quantity representative of the relative phase shift of microwave electromagnetic energy propagating between said spaced locations in the borehole;

deriving a third quantity representative of the porosity of the formations surrounding said spaced locations; and

generating a fourth quantity which is proportional to the product of said first and second quantities and inversely proportional to said third quantity;

said fourth quantity being indicative of the conductivity of the water in said formations.

64. Apparatus for determining the water-filled porosity of formations surrounding a particular location in a borehole, comprising:

means for deriving the conductivity, σ

_EMP, of said formations as measured by a microwave electromagnetic propagation logging device;

means for deriving the water conductivity, σ

_w, of said formations; and

means for generating a quantity which is substantially proportional to the ratio of σ

_EMP to σ

_w, said quantity being indicative of the water-filled porosity of said formations.

66. Apparatus for determining the conductivity of the water in formations surrounding a particular location in a borehole, comprising:

means for deriving the conductivity, σ

_EMP, of said formations as measured by a microwave electromagnetic propagation logging device;

means for deriving the water-filled porosity, φ

_w, of said formations; and

means for generating a quantity which is substantially proportional to the ratio of σ

_EMP to φ

_w, said quantity being indicative of the conductivity of the water in said formations.

67. Apparatus for determining the apparent conductivity of the water in formations surrounding a particular location in a borehole, comprising:

means for deriving the conductivity, σ

_EMP, of said formations as measured by microwave electromagnetic propagation logging device;

means for deriving the total porosity, φ

_t, of said formations; and

means for generating a quantity which is substantially proportional to the ratio of σ

_EMP to φ

_t ;

said quantity being indicative of the apparent conductivity of the water in said formations.

69. Apparatus as defined by claim 67 wherein said borehole is filled with drilling mud and wherein σ

_w is derived from the conductivity of the mud filtrate in the formations invaded by said drilling mud.

68. Apparatus for determining the water saturation of formations surrounding a particular location in a borehole, comprising:

means for deriving the conductivity, σ

_EMP, of said formations as measured by a microwave electromagnetic propagation logging device;

means for deriving the water conductivity, σ

_w, of said formations;

means for deriving the total porosity, σ

_t, of said formations; and

means for generating a quantity which is substantially proportional to σ

_EMP and substantially inversely proportional to the product of σ

_w and φ

_t ;

said quantity being indicative of the water saturation of said formations.