How does U 238 change to U 235 in natural in earth

In summary, U-238 does not change into U-235 in nature. Uranium ore contains a small amount of U-235, and to enrich it, the two isotopes need to be separated. The original creation of these isotopes in equal quantities by stellar nucleosynthesis means that U-235 is much less abundant today due to its faster decay rate. The natural conversion of U-238 to U-235 is a rare occurrence, but there are also other factors that can contribute to the enrichment of U-235, such as spontaneous fission and neutron generation from alpha decay. Additionally, U undergoes chemical reactions in nature which can affect its isotope composition. The size of these natural isotope effects for U is yet to
  • #1
taregg
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how does U 238 change to U 235 in nature earth

or how does uranium enrichment in nature
 
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  • #2
U-238 doesn't change into U-235. Uranium ore contains about 0.72% U-235. To enrich uranium, you need to separate out U-235 from U-238.
 
  • #3
The original stellar nucleosynthesis created U235 and U238 in about equal quantities.

Since they have different decay rates the U235 is much scarcer today.

For an interesting story read about the natural nuclear reactor at Oklo, Gabon:
http://en.wikipedia.org/wiki/Natural_nuclear_fission_reactor
 
  • #4
There is both a natural conversion of U-238 to U-235, and enrichment. Both are tiny effects.
U-238 may capture a neutron. Then it becomes U-239, which beta decays first to Np-239 then to Pu-239. Pu-239 then alpha decays to U-235.
Neutrons are rare on Earth outside reactors. They may come from cosmic rays, and in U deposits, they may come from spontaneous fission of U-238, or from nuclei that collide with alpha particles. How common are these effects? Spontaneous fission of U-238 happens roughly once per 2 million initial alpha decays of U-238... how frequent is neutron generation by alpha decay in nature, seeing that an U-238 emits 8 alphas in the chain to Pb-206?

And of course U is enriched or depleted in nature, just like H, C-12, N-14, O-16 or S-32 are enriched or depleted. U undergoes chemical reactions - it is sometimes oxidized and dissolved into UO2(2+) cation, sometimes reduced and precipitated as UO2. All these reactions have nonzero isotope effects.
What is the size of natural isotope effects of U isotope compositions?
 
  • #5
occur

Uranium-238 (U-238) is a naturally occurring isotope of uranium with a half-life of 4.5 billion years. It is the most abundant isotope of uranium found on Earth, making up about 99.3% of all naturally occurring uranium. U-238 can change to U-235 through a process called radioactive decay, where the nucleus of an atom spontaneously breaks down and releases particles and energy.

In this case, U-238 decays by emitting an alpha particle (two protons and two neutrons) and transforms into thorium-234. Thorium-234 then undergoes a series of decays, eventually producing U-235. This process is known as the uranium decay chain.

In nature, this process occurs very slowly, as U-238 has a long half-life. However, in certain conditions, such as in nuclear reactors or during nuclear explosions, the rate of decay can be accelerated. This is because these environments provide high levels of energy and particles that can trigger and speed up the decay process.

Uranium enrichment, on the other hand, is a man-made process that artificially increases the concentration of U-235 in uranium. This is typically done for the production of nuclear fuel for power plants or for the creation of nuclear weapons. The most common method of uranium enrichment is through a process called gaseous diffusion, where uranium gas is passed through a series of membranes to separate out the desired isotope.

In summary, U-238 changes to U-235 in nature through the process of radioactive decay, which occurs very slowly over time. However, in certain conditions, this process can be accelerated. Uranium enrichment is a man-made process that artificially increases the concentration of U-235 and is typically used for the production of nuclear fuel or weapons.
 

1. How does U 238 change to U 235?

U 238 changes to U 235 through a process called radioactive decay. This is a natural process where the nucleus of an unstable atom (in this case, U 238) spontaneously breaks down into a more stable atom (U 235) by emitting radiation.

2. What is the half-life of U 238?

The half-life of U 238 is approximately 4.5 billion years. This means that it takes 4.5 billion years for half of the U 238 atoms in a sample to decay into U 235. The remaining half will decay over the next 4.5 billion years, and so on.

3. Is U 238 changing to U 235 a natural process?

Yes, the change of U 238 to U 235 is a natural process that has been occurring on Earth since its formation. U 238 is a naturally occurring element, and its radioactive decay to U 235 is a natural part of its lifecycle.

4. Does the change of U 238 to U 235 have any practical applications?

Yes, the process of U 238 changing to U 235 has practical applications in nuclear power and weapons. U 235 is a fissile isotope, meaning it can sustain a chain reaction of nuclear fission, making it a valuable source of energy. However, it must be carefully controlled and handled due to its potential for destructive use.

5. How does the change of U 238 to U 235 impact the environment?

The change of U 238 to U 235 does not have a significant impact on the environment as it is a natural process that occurs at a relatively slow rate. However, the release of U 238 and U 235 into the environment through human activities, such as nuclear testing and accidents, can have harmful effects on the environment and living organisms.

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