Radioactivity is a natural phenomenon where unstable atomic nuclei spontaneously decay, emitting energy in the form of radiation. This process is measured by the rate at which these decays occur, typically expressed as the number of disintegrations or decays per unit time.
The basic concept of radioactivity is expressed as:
\[A = \frac{dN}{dt}\]Where:
Common radioactivity units include:
To convert between radioactivity units, follow these steps:
Let's convert 1000 becquerels to curies:
\[1000 \text{ Bq} \times \frac{1 \text{ Ci}}{3.7 \times 10^{10} \text{ Bq}} \approx 2.70 \times 10^{-8} \text{ Ci}\]This diagram illustrates the concept of radioactivity. The central circle represents a radioactive source, and the radiating lines show the emitted radiation. The conversion demonstrates that the rate of radioactive decay remains constant, whether measured in becquerels or curies.
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