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AbstractAbstract
[en] When measuring a radioactive source composed of a radionuclide NX together with its metastable state NXm decaying to the ground state, special attention should be given to the decay correction. Indeed the activity A of the radionuclide NX is the summation of the usual decaying activity AD of the initial NX with the growing activity AG of the NX coming from the disintegration of the metastable state to the ground state. If t0 is the time of production of the source (which is often not known by the user), the usual decay correction AD(t) = AD,0 exp[-(t-t0)/τ] allows an easy calculation of the correction D for any time difference Δt = t2-t1. Depending on the respective half-lives τ and τm of both states, the equilibrium (constant activity ratio) between NXm and the daughter NX may or may not be reached. In this short report, it is demonstrated that, perhaps surprisingly, the decay correction for the total activity A = AD + AG is independent of t0. No conditions on the respective half-lives of NX and NXm are imposed. The decay correction for the total activity of NX is given by C(t1, t2, R(t1)) for any time difference, i.e. whether equilibrium is reached or not. This expression is independent of the time of source production and is valid for any values of τ and τm
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2004; 3 p; 1 ref.
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Miscellaneous
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