The radioactive isotopes of an element are called radioisotopes.
The number of protons in the atomic nuclei of different isotopes of the same element is the same, but the number of neutrons varies.
The radioactive isotopes of an element are called radioisotopes.
They can alternatively be described as atoms with surplus energy in their nucleus or unstable neutron-proton combinations.
An isotope will become radioactive if the neutron to proton ratio exceeds a certain threshold or the atomic number is higher than 83.
According to the idea, an isotope will become radioactive if its atomic number is higher than 83 or if the neutron-to-proton ratio rises over one or becomes excessively large.
Gamma rays, beta particles, and alpha particles are the three types of radiation that are released.
Typical instances of radioactive isotopes are Arsenic−74, Iodine−131 and Cobalt−60.
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