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Specific activity

Activity per unit mass of a radionuclide


Activity per unit mass of a radionuclide

FieldValue
nameActivity
imageRadium 226 radiation source 1.jpg
captionRa 226 radiation source. Activity 3300 Bq (3.3 kBq)
unitbecquerel
otherunitsrutherford, curie
symbols*A*
baseunitss−1
Note

specific activity radioactivity

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). 1 Ci/g = 37 TBq/kg.

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 (37 GBq). Another unit of activity is the rutherford (Rd), which is defined as radioactive decays per second (1 MBq).

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''½

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

-\frac{dN}{dt} = \lambda N.

The integral solution is described by exponential decay:

N = N_0 e^{-\lambda t},

where N0 is the initial quantity of atoms at time t = 0.

Half-life t½ is defined as the length of time for half of a given quantity of radioactive atoms to undergo radioactive decay:

\frac{N_0}{2} = N_0 e^{-\lambda t_{1/2}}.

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

t_{1/2} = \frac{\ln 2}{\lambda}.

Conversely, the decay constant λ can be derived from the half-life t½ as

\lambda = \frac{\ln 2}{t_{1/2}}.

Calculation of specific activity

The mass of the radionuclide is given by

{m} = \frac{N}{N_\text{A}} [\text{mol}] \times {M} [\text{g/mol}],

where M is molar mass of the radionuclide, and NA 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{Bq/g}] = \frac{\lambda N}{M N/N_\text{A}} = \frac{\lambda N_\text{A}}{M}.

Thus, specific radioactivity can also be described by

a = \frac{N_\text{A} \ln 2}{t_{1/2} \times M}.

This equation is simplified to

a [\text{Bq/g}] \approx \frac{4.17 \times 10^{23} [\text{mol}^{-1}]}{t_{1/2} [\text{s}] \times M [\text{g/mol}]}.

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

\begin{align} a [\text{Bq/g}] &= \frac{4.17 \times 10^{23} [\text{mol}^{-1}]}{t_{1/2}[\text{year}] \times 365 \times 24 \times 60 \times 60 [\text{s/year}] \times M} \[1ex] &\approx \frac{1.32 \times 10^{16} [\text{mol}^{-1}{\cdot}\text{s}^{-1}{\cdot}\text{year}]}{t_{1/2} [\text{year}] \times M [\text{g/mol}]}. \end{align}

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{Ra-226}[\text{Bq/g}] = \frac{1.32 \times 10^{16}}{1600 \times 226} \approx 3.7 \times 10^{10} [\text{Bq/g}].

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{a \times M}{N_\text{A}}.

Therefore, the half-life can also be described by

t_{1/2} = \frac{N_\text{A} \ln 2}{a \times M}.

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-1, so one gram is 1/87 of a mole. Plugging in the numbers:

\begin{align} t_{1/2} = \frac{N_\text{A} \times \ln 2}{a \times M} &\approx \frac{6.022 \times 10^{23}\text{ mol}^{-1} \times 0.693} {3200\text{ s}^{-1}{\cdot}\text{g}^{-1} \times 87\text{ g/mol}} \[1ex] &\approx 1.5 \times 10^{18}\text{ s} \approx 47\text{ billion years}. \end{align}

Other calculations

For a given mass m (in grams) of an isotope with atomic mass ma (in g mol-1) and a half-life of t½ (in s), the radioactivity can be calculated using:

A_\text{Bq} = \frac{m} {m_\text{a}} N_\text{A} \frac{\ln 2} {t_{1/2}}

With N_\text{A} = , the Avogadro constant.

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

A_\text{Bq} = nN_\text{A} \frac{\ln 2} {t_{1/2}}

For instance, on average each gram of potassium contains 117 micrograms of 40K (all other naturally occurring isotopes are stable) that has a t½ 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

IsotopeHalf-lifeMass of 1 curieSpecific Activity (a) (activity per 1 kg)
232Thyears9.1 tonnes4.07 MBq (110 μCi or 4.07 Rd)
238Uyears2.977 tonnes12.58 MBq (340 μCi, or 12.58 Rd)
235Uyears463 kg79.92 MBq (2.160 mCi, or 79.92 Rd)
40Kyears140 kg262.7 MBq (7.1 mCi, or 262.7 Rd)
129Iyears5.66 kg6.66 GBq (180 mCi, or 6.66 kRd)
99Tcyears58 g629 GBq (17 Ci, or 629 kRd)
239Puyears16 g2.331 TBq (63 Ci, or 2.331 MRd)
240Pu6563 years4.4 g8.51 TBq (230 Ci, or 8.51MRd)
14C5730 years0.22 g166.5 TBq (4.5 kCi, or 166.5 MRd)
226Ra1601 years1.01 g36.63 TBq (990 Ci, or 36.63 MRd)
241Am432.6 years0.29 g126.91 TBq (3.43 kCi, or 126.91 MRd)
238Pu88 years59 mg629 TBq (17 kCi, or 629 MRd)
137Cs30.17 years12 mg3.071 PBq (83 kCi, or 3.071 GRd)
90Sr28.8 years7.2 mg5.143 PBq (139 kCi, or 5.143 GRd)
241Pu14 years9.4 mg3.922 PBq (106 kCi, or 3.922 GRd)
3H12.32 years104 μg355.977 PBq (9.621 MCi, or 355.977 GRd)
228Ra5.75 years3.67 mg10.101 PBq (273 kCi, or 10.101 GRd)
60Co1925 days883 μg41.884 PBq (1.132 MCi, or 41.884 GRd)
210Po138 days223 μg165.908 PBq (4.484 MCi, or 165.908 GRd)
131I8.02 days8 μg4.625 EBq (125 MCi, or 4.625 TRd)
123I13 hours518 ng71.41 EBq (1.93 GCi, or 71.41 TRd)
212Pb10.64 hours719 ng51.43 EBq (1.39 GCi, or 51.43 TRd)

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.{{Cite journal

References

References

  1. (2003). "Optimising conditions for radiolabelling of DOTA-peptides with 90Y, 111In and 177Lu at high specific activities". European Journal of Nuclear Medicine and Molecular Imaging.
  2. (2005). "How do we define the concepts specific activity, radioactive concentration, carrier, carrier-free and no-carrier-added?". Journal of Radioanalytical and Nuclear Chemistry.
  3. (1975). "SI units for ionizing radiation: becquerel". Resolutions of the 15th CGPM.
  4. (1990-06-01). "Table of Isotopes decay data". [[Lund University]].
  5. "Atomic Weights and Isotopic Compositions for All Elements". [[NIST]].
  6. Duursma, E. K. "Specific activity of radionuclides sorbed by marine sediments in relation to the stable element composition". Radioactive contamination of the marine environment (1973): 57–71.
  7. (1984). "Radionuclide selection and model absorbed dose calculations for radiolabeled tumor associated antibodies". Medical Physics.
  8. (2002). "Radionuclide production for therapeutic radiopharmaceuticals". Applied Radiation and Isotopes.
  9. (1993). "Selection of radionuclides for radioimmunotherapy". Medical Physics.
  10. (1987). "Analysis for naturally occuring radionuclides at environmental concentrations by gamma spectrometry". Journal of Radioanalytical and Nuclear Chemistry.
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