Specific activity

Specific activity (symbol ''a'') is the activity per unit mass of a radionuclide and is a physical property of that radionuclide.
It is usually given in units of becquerel per kilogram (Bq/kg), but another commonly used unit of specific activity is the curie per gram (Ci/g).

In the context of radioactivity, activity or total activity (symbol ''A'') is a physical quantity defined as the number of radioactive transformations per second that occur in a particular radionuclide. The unit of activity is the ''becquerel'' (symbol Bq), which is defined equivalent to reciprocal seconds (symbol s⁻¹). The older, non-SI unit of activity is the ''curie'' (Ci), which is radioactive decays per second. Another unit of activity is the ''rutherford'', which is defined as radioactive decays per second.

The specific activity should not be confused with level of exposure to ionizing radiation and thus the exposure or absorbed dose, which is the quantity important in assessing the effects of ionizing radiation on humans.

Since the probability of radioactive decay for a given radionuclide within a set time interval is fixed (with some slight exceptions, see changing decay rates), the number of decays that occur in a given time of a given mass (and hence a specific number of atoms) of that radionuclide is also a fixed (ignoring statistical fluctuations).

Formulation

Relationship between ''λ'' and T_1/2

Radioactivity is expressed as the decay rate of a particular radionuclide with decay constant ''λ'' and the number of atoms ''N'':

: $-\frac = \lambda N.$

The integral solution is described by exponential decay:

: $N = N_0 e^,$

where ''N''₀ is the initial quantity of atoms at time ''t'' = 0.

Half-life T_1/2 is defined as the length of time for half of a given quantity of radioactive atoms to undergo radioactive decay:

: $\frac = N_0 e^.$

Taking the natural logarithm of both sides, the half-life is given by

: $T_ = \frac.$

Conversely, the decay constant ''λ'' can be derived from the half-life ''T''_1/2 as

: $\lambda = \frac.$

Calculation of specific activity

The mass of the radionuclide is given by

: $= \frac$text\times text

where ''M'' is molar mass of the radionuclide, and ''N''_A is the Avogadro constant. Practically, the mass number ''A'' of the radionuclide is within a fraction of 1% of the molar mass expressed in g/mol and can be used as an approximation.

Specific radioactivity ''a'' is defined as radioactivity per unit mass of the radionuclide:

: $a$text= \frac = \frac.

Thus, specific radioactivity can also be described by

: $a = \frac.$

This equation is simplified to

: $a$text\approx \frac.

When the unit of half-life is in years instead of seconds:

: $a$text= \frac \approx \frac.

Example: specific activity of Ra-226

For example, specific radioactivity of radium-226 with a half-life of 1600 years is obtained as

: $a_\text$text= \frac \approx 3.7 \times 10^ text

This value derived from radium-226 was defined as unit of radioactivity known as the curie (Ci).

Calculation of half-life from specific activity

Experimentally measured specific activity can be used to calculate the half-life of a radionuclide.

Where decay constant ''λ'' is related to specific radioactivity ''a'' by the following equation:

: $\lambda = \frac.$

Therefore, the half-life can also be described by

: $T_ = \frac.$

Example: half-life of Rb-87

One gram of rubidium-87 and a radioactivity count rate that, after taking solid angle effects into account, is consistent with a decay rate of 3200 decays per second corresponds to a specific activity of . Rubidium atomic mass is 87 g/mol, so one gram is 1/87 of a mole. Plugging in the numbers:

: $T_ = \frac \approx \frac \approx 1.5 \times 10^\text \approx 47\text.$

Other calculations

For a given mass $m$ (in grams) of an isotope with atomic mass $m_\text$ (in g/mol) and a half-life of $t_$ (in s), the radioactivity can be calculated using:

:$A_\text = \frac N_\text \frac$

With $N_\text$ = , the Avogadro constant.

Since $m/m_\text$ is the number of moles ($n$), the amount of radioactivity $A$ can be calculated by:

:$A_\text = nN_\text \frac$

For instance, on average each gram of potassium contains 117 micrograms of ⁴⁰K (all other naturally occurring isotopes are stable) that has a $t_$ of = , and has an atomic mass of 39.964 g/mol, so the amount of radioactivity associated with a gram of potassium is 30 Bq.

Examples

Applications

The specific activity of radionuclides is particularly relevant when it comes to select them for production for therapeutic pharmaceuticals, as well as for immunoassays or other diagnostic procedures, or assessing radioactivity in certain environments, among several other biomedical applications.

References

Further reading

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Radioactivity quantities