How far do fission products travel?

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In summary, fission products can travel varying distances depending on several factors, including the type of fission event, the medium through which they move, and environmental conditions. Generally, heavier fission products tend to remain closer to the source, while lighter isotopes can be dispersed over larger areas. Atmospheric conditions, such as wind and precipitation, also play a significant role in determining the extent of their spread.
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Hey guys, about how far do fission products travel on average in UO2? This will obviously be a fairly short distance, but does anyone have any ideas or links to information on this?
 
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mesa said:
Indeed, yes.
Have you had any luck finding info about this online with your searches? If not, @Alex A or @Astronuc may have thoughts...
 
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10um is commonly quoted as a rule of thumb and that is all I had in my head so I did a quick google. This rather fun paper https://www.osti.gov/servlets/purl/6868318 on fission fragment rockets gives a value of 6.2um in Uranium Carbide and 16.2um in carbon. Uranium dioxide will probably be quite close to UC. There could be some variation according to the fragment type. Energy loss is probably roughly proportional to track length. Think alpha particle like ionisation paths.

Papers on fission counters may give more information.
 
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I've seen some numbers, but I can't remember the text/source.

The lighter fission products, e.g., isotopes of Br, Kr, Rb, Sr, Y, Zr . . . have higher energy and travel about 7-10 microns in UO2. The lighter the isotope, the higher the energy. The heavier fission products, e.g., isotopes of Sb, Te, I, Xe, Cs, La, . . . . travel about 4-6 microns in UO2. Two fission products may share between 160 and 170 MeV, and one might be 65 MeV (the heavier one) and the the other about 105 MeV, for example. The rest of the energy is carried away by neutrons and gammas, and internal to the fission products, which decay by beta decay. Neutrinos, or rather, antineutrinos carry away some energy as well, in conjunction with beta decay.

The text, Introduction to Nuclear Engineering, 3rd Edition, by John Lamarsh and Anthony J. Baratta, Prentice Hall, 2001, p. 108 shows ranges of fission products to be 6.6 microns in U and 14 microns in U3O8, so probably about 10 microns in UO2. Of course, this depends on porosity of the ceramic, which could increase the range, since the pores have little stopping power, even filled with gas.
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You can use the Bethe-Bloch formula, especially if you just want an estimate:

dE/dx for U2O is about 12 MeV per cen times Z2. So for E = 100 MeV and Z = 40, you get 50 microns. I am dropping some logarithmic terms here, so it's only good to a factor of a few, but you can use the full formula if you want better accuracy.
 
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Alex A said:
10um is commonly quoted as a rule of thumb and that is all I had in my head so I did a quick google. This rather fun paper https://www.osti.gov/servlets/purl/6868318 on fission fragment rockets gives a value of 6.2um in Uranium Carbide and 16.2um in carbon. Uranium dioxide will probably be quite close to UC. There could be some variation according to the fragment type. Energy loss is probably roughly proportional to track length. Think alpha particle like ionisation paths.

Papers on fission counters may give more information.
Great source, and a fun paper in general, you don't see proposals like these too often anymore.
 
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Astronuc said:
The text, Introduction to Nuclear Engineering, 3rd Edition, by John Lamarsh and Anthony J. Baratta, Prentice Hall, 2001, p. 108 shows ranges of fission products to be 6.6 microns in U and 14 microns in U3O8, so probably about 10 microns in UO2. Of course, this depends on porosity of the ceramic, which could increase the range, since the pores have little stopping power, even filled with gas.
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Good information as always Astronuc, I'll have to dust my copy off when I get into work tomorrow. This seems inline with the paper Alex A referenced.
 
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Vanadium 50 said:
You can use the Bethe-Bloch formula, especially if you just want an estimate:

dE/dx for U2O is about 12 MeV per cen times Z2. So for E = 100 MeV and Z = 40, you get 50 microns. I am dropping some logarithmic terms here, so it's only good to a factor of a few, but you can use the full formula if you want better accuracy.
Nice, looking into it more.
 
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One thing to keep in mind is that the terms I neglected tend to increase ionization at low energy (called the Bragg peak) so my estimate is too long. However, if you want to include this, you will need to integrate the equation, because the ionization changes as the fragment slows.
 
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FAQ: How far do fission products travel?

How far can fission products travel in the atmosphere?

Fission products can travel varying distances in the atmosphere depending on factors like wind speed, weather conditions, and the altitude at which they are released. Generally, they can travel hundreds to thousands of kilometers from the site of release.

What factors influence the distance fission products can travel?

The distance fission products can travel is influenced by atmospheric conditions, including wind patterns, temperature, and humidity. Additionally, the size and type of fission products, as well as their initial altitude of release, play significant roles.

How long do fission products remain airborne?

The time fission products remain airborne varies widely depending on their physical and chemical properties. Some can settle to the ground within hours, while others may stay in the atmosphere for days, weeks, or even longer, potentially traveling great distances.

Do fission products pose a risk to human health over long distances?

Yes, fission products can pose a risk to human health over long distances. Radioactive particles can be inhaled or ingested, leading to internal exposure. The level of risk depends on the concentration of fission products and the duration of exposure.

Can fission products be detected far from their source?

Yes, fission products can be detected far from their source using sensitive instruments like Geiger counters, scintillation detectors, and mass spectrometers. These tools can measure low levels of radioactivity in the environment, even at considerable distances from the release site.

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