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The half-life of an isotope is the time taken for half the nuclei in a sample to decay or the time taken for the activity or count rate of a sample to decay by half. It cannot be predicted when any one nucleus will decay, but the half-life is a constant that enables the activity of a very large number of nuclei to be predicted during the decay.
Example Calculation:
It is suitable because it will not need to be replenished, and its weak activity means it won't be harmful to anyone.
Formula:
Radioactivity is a completely random process – unpredictable radiation given out by radioactive substances from the nuclei of their atoms can be measured with a Geiger-Muller tube and counter. This records the count rate = the number of radiation counts reaching it per second.
You can't predict which nucleus in a sample will decay next, but you can find out the time it takes for the amount of radiation emitted by a source to halve. This is known as the half-life. Half-life can be used to find a source's activity (Bq) – the rate at which it decays.
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