Abstract This invention relates to a novel method for both locating and evaluating subsurface uranium-bearing formations containing an apparent grade of up to approximately 5% of contained U 3 O 8 which comprises the steps of taking readings of the natural gamma count from an unknown radioactive formation on both the shielded and unshielded detectors with the external gamma source shielded, uncovering the external gamma source and reading the count-rate on both the shielded and unshielded detectors, comparing the ratio of the natural gamma count recorded by the unshielded and shielded detectors with a similar ratio recorded by the same detectors in a uranium-bearing matrix of known concentration no greater than approximately 5% in a state of equilibrium to ascertain first if a state of disequilibrium exists and, secondly, if a state of disequilibrium is found to exist then to determine if this state of apparent disequilibrium is being influenced by the presence of either thorium or potassium or, alternatively, is primarily the result of a disequilibrium between uranium and its daughter products. The natural radiation seen by the shielded probe provides the data for a determinatin of the apparent grade of U 3 O 8 used in later calculations. Finally, if the disequilibrium is found to exist between uranium and its daughter products, then determining the direction and approximate order of magnitude of the disequilibrium by analyzing the ratio of the count rates detected by the shielded and unsheilded detectors ascertained from a suspected uranium-bearing formation, the former seeing only the natural radiation while the latter looks at essentially all the radiation including that induced by the external source, and comparing it with a comparable ratio taken by the same detectors from a known uranium-bearing formation containing not more than approximately 5% U 3 O 8 at equilibrium to see whether the back-scattered radiation was substantially attenuated or not within the formation or, alternatively, increased due to induced X-ray fluorescence.
The method of locating and evaluating subsurface uranium-bearing ore bodies which comprises the steps of: independently determining the natural gamma radiation above approximately 60 Kev and above approximately 400 Kev emanating from an unknown radioactive formation to establish a ratio thereof, comparing said ratio and the apparent grade of uranium represented thereby with a similarly derived ratio and actual grade determined from a known uranium-bearing ore body in radiometric equilibrium to ascertain if a condition of apparent disequilibrium exists in the unknown formation, irradiating the unknown formation with a gamma ray source of an energy level effective to induce X-ray fluorescence in uranium and determining the total of the natural radiation and the induced radiation resulting therefrom above a level of approximately 60 Kev, comparing said total with similar data derived from a known uranium-bearing ore body to ascertain if any substantial attentuation of the induced radiation has taken place or if measurable X-ray fluorescence is observed, and determining the approximate actual concentration of U 3 O 8 present in said unknown formation based upon the observed attenuation of the induced radiation or, alternatively, the resultant X-ray fluorescence caused thereby.
Claim 2
Independent Claim
190 words
The method of locating and evaluating subsurface uranium-bearing ore bodies which comprises the steps of: independently determining the natural gamma radiation above approximately 60 Kev and above approximately 400 Kev emanating from an unknown radioactive formation to establish a ratio thereof, comparing said ratio and the apparent grade of uranium represented thereby with a similarly derived ratio and actual grade determined from a known uranium-bearing ore body in radiometric equilibrium to ascertain if a condition of apparent disequilibrium exists in the unknown formation, irradiating the unknown formation with a gamma ray source of an energy level effective to induce X-ray fluorescence in uranium and determining the total of the natural radiation and the induced radiation resulting therefrom above a level of approximately 60 Kev, comparing said total with similar data derived from a known uranium-bearing ore body to ascertain if any substantial attentuation of the induced radiation has taken place or if measurable X-ray fluorescence is observed, and determining the approximate actual concentration of U 3 O 8 present in said unknown formation based upon the observed attenuation of the induced radiation or, alternatively, the resultant X-ray fluorescence caused thereby.
Claim 3
Dependent Claim
32 words
The method as set forth in claim 1 in which the unknown formation is irradiated with gamma rays having an energy level above approximately 0.1 Mev but less than approximately 3 Mev.
Claim 4
Dependent Claim
37 words
The method as set forth in claim 1 in which the unknown formation is irradiated with a gamma source for which the mass absorption coefficients are of the same order of magnitude for uranium, thorium and radium.
Claim 5
Dependent Claim
26 words
The method as set forth in claim 1 in which the known uranium-bearing ore body irradiated to derive the data used for comparison is at equilibrium.