Have a look at this simulation:
What happens? One particle can decay at any moment, but when you have hundreds or thousands (in real life, billions and billions) or particles we can find a characteristic time when half of the particles have decayed. This time is called the half-life. Once the time of the half-life has elapse, half of the sample remains. After another half-life, the sample is once again halved. A graph of the amount remaining looks like this:
- U-238 has a half life of 4.5 billion years.
- U-239 has a half life of 24 minutes.
- C-14 has a half life of 5700 years. (Used for carbon dating)
Here's the formula for calculating amount of material remaining:
Here are some examples:
Next we talked about fission:
Fission
A large nucleus breaks apart into smaller nuclei. This can be spontaneous (happens on its own) or induced (something “kicks off” the reaction).
Spontaneous. |
Induced. |
Induced fission can cause a chain reaction.
Nuclear Reactors
- Use enriched uranium to carry out a chain reaction producing thermal energy.
- Natural uranium has 0.7 % U-235
the rest is U-238
- Enriched uranium has 3-4% U-235
- Weapons grade: 90% U-235
How a nuclear power plant works. |
A simplified version of the image above. |
Moderator
- A substance used to slow down neutrons to control the chain reaction. graphite or heavy water.
Control Rods
- Cadmium or Boron is used to absorb neutrons to control the reaction.
- Nuclear bomb uses uncontrolled reactions to release massive amounts of energy.
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