Specific Activity The concentration of radioactivity, or the relationship between the mass of radioactive material and the activity, is called the specific.

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Presentation transcript:

Specific Activity The concentration of radioactivity, or the relationship between the mass of radioactive material and the activity, is called the specific activity. Specific activity is the number of becquerels (or curies) per unit mass or volume. The specific activity of a carrier-free (pure) radioisotope—a radioisotope that is not mixed with any other isotope of the same element—may be calculated as follows:

If λ is the transformation constant in units of reciprocal seconds, then the number of transformations per second and, hence, the number of becquerels in an aggregation of N atoms, is simply given by λN. If the radionuclide under consideration weighs 1 g, then, the number of atoms is given by:

where A is the atomic weight of the nuclide where A is the atomic weight of the nuclide. The activity per unit weight or the specific activity, therefore, is: the desired relationship between the specific activity and weight of an isotope, can be calculated in terms of the isotope’s half-life by substituting λ in the above equation

Note that the above equations are valid only if λ and t1/2 are given in time units of seconds

Decay Schemes

Decay schemes are widely used to give a visual representation of radioactive decay. A scheme for a relatively straight-forward decay is shown below:

This scheme is for hydrogen-3 which decays to helium-3 with a half-life of 12.3 years through the emission of a beta-minus particle with an energy of 0.0057 MeV. A scheme for a more complicated decay is that of caesium-137:This isotope can decay through through two beta-minus processes. In one which occurs in 5% of disintegrations a beta-minus particle is emitted with an energy of 1.17 MeV to produce barium-137. In the second which occurs more frequently (in the remaining 95% of disintegrations) a beta-minus particle of energy 0.51 MeV is emitted to produce barium-137m - in other words a barium-137 nucleus in a metastable state. The barium-137m then decays via isomeric transition with the emission of a gamma-ray of energy 0.662 MeV.

The general method used for decay schemes is illustrated in the diagram below:

The energy is plotted on the vertical axis and atomic number on the horizontal axis - although these axes are rarely displayed in actual schemes. The isotope from which the scheme originates is displayed at the top - X in the case above. This isotope is referred to as the parent. The parent looses energy when it decays and hence the products of the decay referred to as daughters are plotted at a lower energy level.

The diagram illustrates the situation for common forms of radioactive decay. Alpha-decay is illustrated on the left where the mass number is reduced by 4 and the atomic number is reduced by 2 to produce daughter A. To its right the scheme for beta-plus decay is shown to produce daughter B. The situation for beta-minus decay followed by gamma-decay is shown on the right side of the diagram where daughters C and D respectively are produced.