Patent US4263509A successfully refreshed from Google Patents.
← Back to Patent Explorer
US4263509A Expired / Lapsed US ⏱️ 0.0 years remaining

Method for in situ determination of the cation exchange capacities of subsurface formations

Assignee: Western Atlas International Inc
•
Filing: 1979-02-26
•
Granted: 1981-04-21
•
Expires: 1999-02-26
📄 Original PDF 🌐 Google Patents 🔄 Sync Now

Abstract

Abstract A method is disclosed for the in situ examination of each subsurface formation penetrated by a borehole to ascertain the cation exchange capacity of such formations within a geological region. Natural gamma ray logging is used to develop signals functionally related to the total gamma radiation and to the potassium -40, uranium and thorium energy-band radiations. A first borehole is traversed by a potential gamma ray spectrometer to provide selected measurements of natural gamma radiation. Core samples are taken from the logged formation and laboratory tests performed to determine the cation exchange capacity thereof. The cation exchange capacities thus are developed then correlated with selected parameters provided by the gamma ray spectrometer to establish functional relationships. Cation exchange capacities of formations in subsequent boreholes within the region are then determined in situ by use of the natural gamma ray spectrometer and these established relationships.

Inventors

  • 👤 Walter H. Fertl
  • 👤 David W. Welker

Bibliographic Details

Application Number —
Jurisdiction US
Data Source google_patents
Last Synchronized 2026-10-23 19:10
CPC Classifications
G; G01; G01V; G01V5/00; G01V5/04; G01V5/06; E; E21; E21B; E21B49/00; E21B49/005

Claims Analysis

Total Claims: 10
Claim 1
Independent Claim 121 words
A method for determining the cation exchange of earth formations traversed by a borehole, comprising the steps of: generating signals functionally related to radioactive nuclides occurring naturally in the earth formations surrounding a first borehole; establishing depth-related cation exchange capacities from core sample taken from said first borehole at preselected depth intervals; establishing a functional relationship between said generated signals and said cation exchange capacities; generating additional signals functionally related to radioactive nuclides adjacent subsequent boreholes situated in the same geological region as said first borehole; and comparing said additional generated signals with said functional relationship established between said generated signals and said cation exchange capacity of said first borehole to determine the depth-related cation exchange capacity of said subsequent boreholes.
Claim 2
Independent Claim 121 words
A method for determining the cation exchange of earth formations traversed by a borehole, comprising the steps of: generating signals functionally related to radioactive nuclides occurring naturally in the earth formations surrounding a first borehole; establishing depth-related cation exchange capacities from core sample taken from said first borehole at preselected depth intervals; establishing a functional relationship between said generated signals and said cation exchange capacities; generating additional signals functionally related to radioactive nuclides adjacent subsequent boreholes situated in the same geological region as said first borehole; and comparing said additional generated signals with said functional relationship established between said generated signals and said cation exchange capacity of said first borehole to determine the depth-related cation exchange capacity of said subsequent boreholes.
Claim 3
Independent Claim 258 words
A method for in situ evaluation of the cation exchange capacity of earth formations traversed by a borehole, comprising the steps of: traversing said first borehole with a logging instrument containing a gamma ray detector; detecting natural gamma radiation occurring in the formations in the vicinity of said first borehole; generating signals functionally related to the energy and frequency of said detected gamma radiation; separating said signals into a plurality of energy regions, said energy regions corresponding to natural gamma radiation produced by the radioactive isotopes of potassium, uranium and thorium; removing core samples of said formations from various depth-related points along said first borehole; testing said formation samples to determine the cation exchange capacity of said samples; establishing a functional relationship between said test derived cation exchange capacities and a selected parameter relating to said plurality of energy regions; traversing a subsequent borehole within the same geological region with said logging instrument; detecting natural gamma radiation occurring in the earth formations in the vicinity of said subsequent borehole; generating signals functionally related to the energy and frequency of said detected gamma radiation; separating said signals into a plurality of energy regions corresponding to the natural gamma radiation produced by the radioactive isotopes of potassium, uranium and thorium; and determining the cation exchange capacity of said formations penetrated by said subsequent borehole by correlating said functional relationship established from said test derived cation exchange capacities and said selected parameter from said first borehole, and the same selected parameter derived from said signals obtained while logging said subsequent borehole.
Claim 4
Independent Claim 258 words
A method for in situ evaluation of the cation exchange capacity of earth formations traversed by a borehole, comprising the steps of: traversing said first borehole with a logging instrument containing a gamma ray detector; detecting natural gamma radiation occurring in the formations in the vicinity of said first borehole; generating signals functionally related to the energy and frequency of said detected gamma radiation; separating said signals into a plurality of energy regions, said energy regions corresponding to natural gamma radiation produced by the radioactive isotopes of potassium, uranium and thorium; removing core samples of said formations from various depth-related points along said first borehole; testing said formation samples to determine the cation exchange capacity of said samples; establishing a functional relationship between said test derived cation exchange capacities and a selected parameter relating to said plurality of energy regions; traversing a subsequent borehole within the same geological region with said logging instrument; detecting natural gamma radiation occurring in the earth formations in the vicinity of said subsequent borehole; generating signals functionally related to the energy and frequency of said detected gamma radiation; separating said signals into a plurality of energy regions corresponding to the natural gamma radiation produced by the radioactive isotopes of potassium, uranium and thorium; and determining the cation exchange capacity of said formations penetrated by said subsequent borehole by correlating said functional relationship established from said test derived cation exchange capacities and said selected parameter from said first borehole, and the same selected parameter derived from said signals obtained while logging said subsequent borehole.
Claim 5
Dependent Claim 47 words
The method of claim 2, further including the step of normalizing said cation exchange capacity estimation of said subsequent borehole formations using the porosity measurement of said formations to provide an indication of the concentration of counter ions in the formation water in contact with formation clay.
Claim 6
Dependent Claim 34 words
The method of claim 2 wherein said selected parameter used for establishing a functional relationship with said test derived cation exchange capacities correspond to the natural gamma radiation produced by radioactive isotopes of potassium.
Claim 7
Dependent Claim 34 words
The method of claim 2 wherein said selected parameter used for establishing a functional relationship with said test derived cation exchange capacities corresponds to the natural gamma radiation produced by radioactive isotopes of uranium.
Claim 8
Dependent Claim 34 words
The method of claim 2 wherein said selected parameter used for establishing a functional relationship with said test derived cation exchange capacities corresponds to the natural gamma radiation produced by radioactive isotopes of thorium.
Claim 9
Dependent Claim 36 words
The method of claim 2 wherein said selected parameter used for establishing a functional relationship with said test derived cation exchange capacities corresponds to a ratio functionally related to a plurality of said energy region signals.
Claim 10
Dependent Claim 32 words
The method of claim 3, further including the step of utilizing said cation exchange capacity evaluation to provide a correction factor for clay effect on resistivity measurements derived from said earth formations.

References Cited (Backward Citations)

US3711765A Cited
US3770378A Cited
US3940610A Cited

USPTO Annuity & Maintenance Windows

Annuity Stage Window Opens Payment Deadline Surcharge Period Until Estimated Fee Status
3.5 Years (Year 4) 1984-04-20 1984-10-20 1985-04-21 $2000.00 Window Closed / Lapsed
7.5 Years (Year 8) 1988-04-20 1988-10-20 1989-04-21 $3760.00 Window Closed / Lapsed
11.5 Years (Year 12) 1992-04-20 1992-10-20 1993-04-21 $7700.00 Window Closed / Lapsed

Assigned Categories & Tags

No categories assigned to this patent yet.

Assign Category Tag