Uranium deposit -- location techniques question

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SUMMARY

This discussion focuses on the techniques used to locate uranium deposits underground, specifically through the use of neutron activation analysis and gamma radiation detection. It highlights the role of alpha emitters combined with beryllium to produce neutrons, which can penetrate geological layers and interact with uranium isotopes, particularly U-235. The conversation also addresses the challenges of neutron scattering and the importance of fine-tuning neutron energies to optimize detection. Additionally, it notes that uranium deposits are often found alongside other valuable elements, such as vanadium.

PREREQUISITES
  • Understanding of neutron activation analysis techniques
  • Familiarity with uranium isotopes, particularly U-235
  • Knowledge of geological formations and hydrogeology
  • Experience with radiation detection methods, including Geiger counters
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  • Research neutron activation analysis and its applications in mineral exploration
  • Learn about the properties and detection methods for U-235 and its daughter products
  • Explore the relationship between hydrogeology and uranium deposit formation
  • Investigate the use of alpha emitters and beryllium in neutron production
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Geologists, mining engineers, nuclear scientists, and professionals involved in mineral exploration and radiation detection will benefit from this discussion.

girts
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I read that one can find Uranium for its gamma radiation hence gamma can travel through even dense and thick stuff, but natural Uranium that hasn't gone through fission doesn't emit gamma correct, so I was reading how they find Uranium reserves underground and it says that they use a alpha emitter combined with beryllium which then undergoes spallation and produces neutrons, then it is said that they use these neutrons to see whether there is Uranium in the ground because if there is they can detect some delayed neutrons coming back from the induced fission of the neutrons that came out from the beryllium checking device.
Here is what I don't quite get, I suppose it is rarely when Uranium deposits simply lie close to ground, under grass or right on top of soil, I assume they are mostly rather deep below ground, now how do these neutrons penetrate deep enough to strike the U deposits and even get back some delayed fission neutrons, how come these neutrons simply don't get lost or scattered or else while they are traveling through the layers of rock and soil and other stuff in the ground?
Or do they "finetune" the neutron energies so that they don't interact with other elements but only either U 235 or U 2
 
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girts said:
I read that one can find Uranium for its gamma radiation hence gamma can travel through even dense and thick stuff, but natural Uranium that hasn't gone through fission doesn't emit gamma correct, so I was reading how they find Uranium reserves underground and it says that they use a alpha emitter combined with beryllium which then undergoes spallation and produces neutrons, then it is said that they use these neutrons to see whether there is Uranium in the ground because if there is they can detect some delayed neutrons coming back from the induced fission of the neutrons that came out from the beryllium checking device.
Here is what I don't quite get, I suppose it is rarely when Uranium deposits simply lie close to ground, under grass or right on top of soil, I assume they are mostly rather deep below ground, now how do these neutrons penetrate deep enough to strike the U deposits and even get back some delayed fission neutrons, how come these neutrons simply don't get lost or scattered or else while they are traveling through the layers of rock and soil and other stuff in the ground?
Or do they "finetune" the neutron energies so that they don't interact with other elements but only either U 235 or U 2
Neutron activation analysis is an active technique. One can use an (α,n) source, or a fusion-based d+t source of neutrons. The neutrons can be thermalized with something like water or polyethylene. U-235 has a higher cross-section for thermal neutrons, so thermal neutrons would react with U-235. One would normally bore a tunnel, or take a coring sample and assay the rock above ground. The technique is used for exploring geological formations bearing minerals.

U deposits also incorporate beta- and gamma-emitting daughter products, which are detectable by Geiger/proportional counters. This would be a passive method.
http://hyperphysics.phy-astr.gsu.edu/hbase/Nuclear/radser.html

Some deposits are near the surface, but many are not. Where the uranium is deposited has a lot to do with hydrogeology.

Uranium is often found with other valuable elements, e.g., vanadium.
https://pubs.usgs.gov/bul/1009b/report.pdf
 

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