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Radioactive decay HTML5


The nucleus of an atom is described by its proton number (Z, characteristic of the chemical species of the element), and its nucleon number (A or mass number). An atom of the same chemical species may contain a different number of nucleons, ie a different number of neutrons (N = A - Z). Isotopes are atoms which have the same number of protons but not the same number of neutrons. Isotopes of an atom all have the same chemical properties (same Z number) and remain in constant proportion in nature.

A nucleus is stable when the nuclear force compensates the electrical repulsion force between the positively charged protons. Some nuclei are unstable. They naturally release energy (radiation) generating new nuclei that can be stable or unstable. This decay is random, and it depends on the nature of the element: this is radioactivity.

The half-life of a given isotope is the amount of time it takes for half of the atoms in a sample to decay. This simulation allows you to address, using three different isotopes, notions like radioactive decay, carbon dating, half life constant.

Click on one of the three isotopes to select a half-life constant.
Click on [Play] to start the decay.

Learning goals

  • To illustrate how the decay of an unstable nucleus is a random process. 
  • To define the half-life constant for three representative radioactive nucleus.
  • To relate the Becquerel to the process of radioactive decay.
  • To visualize the exponential decay law.

Learn more

At the microscopic level, the decay of a nucleus is not predictable. By constrast, at the macroscopic level, the statistical behavior of a sample of nuclei is known. The decay law of a sample from…

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