How to Calculate Mass from Activity?

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    Activity Mass
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Discussion Overview

The discussion revolves around the methods for calculating the mass of an isotope based on its activity, specifically in the context of radioactive isotopes and their decay properties. Participants explore various equations and concepts related to activity, half-life, and isotopic composition.

Discussion Character

  • Exploratory
  • Technical explanation
  • Mathematical reasoning
  • Debate/contested

Main Points Raised

  • One participant inquires about the equations needed to calculate the mass of an isotope that exhibits an activity of 200 Ci.
  • Another participant cautions against a simplistic approach and emphasizes the importance of understanding what activity measures and its units.
  • Activity is defined by some participants as having units of decays per second and is related to the concept of half-life.
  • It is suggested that from the activity and half-life, one can derive the number of atoms in the sample, which can then be used to calculate mass using Avogadro's number and atomic weight.
  • One participant mentions calculating specific activity or activity per unit mass, proposing that mass can be found by dividing activity by specific activity.
  • A follow-up question is raised regarding the calculation of specific activity for natural rubidium chloride, considering the presence of two isotopes, Rb-85 and Rb-87, with a specific abundance.
  • Another participant explains that activity for a radionuclide is the product of the decay constant and the number of atoms, and discusses how to determine the fraction of radioactive isotopes in a mixture.
  • In the context of a compound like RbCl, it is suggested to calculate the mass of Rb by subtracting the mass of Cl and applying the isotopic ratio for the nuclide.
  • Concerns are raised about self-shielding in large samples of Rb-87 due to its long half-life and low beta energy, recommending specific types of counters for accurate measurement.

Areas of Agreement / Disagreement

Participants express various viewpoints on the methods for calculating mass from activity, with no consensus reached on a single approach. Multiple competing models and methods are discussed, indicating an unresolved nature of the topic.

Contextual Notes

Limitations include assumptions about isotopic composition, the dependence on specific definitions of activity and half-life, and the complexity introduced by mixtures of isotopes. Mathematical steps for some proposed methods remain unresolved.

FlipStyle1308
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I was wondering what equations would be used to calculate the mass (in mg) of an isotope that gives an activity of 200 Ci.
 
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You shouldn't start out intending to plug'n'chug. What does activity mean (eg. what units does it measure)?
 
Activity has the units of decays/s, and it measures the rate of half-life.
 
From activity and half life, you can get the number of atoms in the sample. From that, you should be able to get the mass using Avogadro's number and the gram atomic weight
 
Using daveb's approach, one can calculate the specific activity or activity per unit mass. Activity divided by specific activity equals mass.

See this discussion on specific activity.
 
Last edited:
Astronuc said:
Using daveb's approach, one can calculate the specific activity or activity per unit mass. Activity divided by specific activity equals mass.

See this discussion on specific activity.

What if the element consists of two isotopes: example Stable Rb-85 and the radioactive Rb-87 with an abundance of 27.83%. How would you calculate the specific activity of natural rubidium chloride. I have figured the g.mol-1 for Rb-85=85.47g.mol-1 and 86.91g.mol-1 for the Rb-87, and M(r) =120.92g.mol-1?
 
Activity due to a particular radionuclide is simply the product of the decay constant and the number of atoms of the radionuclide present. In the case of a isotopic mix, if one know the mass and isotopic composition, then one can determine the fraction of atoms which are radioactive isotope.

Activity is measured - usually with a counter which interacts with the radiation.

In the case of a compound, e.g. RbCl, one subtracts the mass of the Cl, which gives the mass of Rb, then apply the isotopic ratio for the nuclide. Alternatively, know that there is one Rb atom for each Cl atom, determin the number of molecules of RbCl, which give the number of atoms, of which some fraction will be Rb-87. Rb-87 has a very long half-life, 4.81E+10 y, and consequently the beta energy is quite low, ~ 283.3 keV, so self-shielding would an issue for a large sample. A 4-pi or at least a 2 pi counter would be recommended for an accurate count.
 

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