Shorter half-life and therefore very radioactive -- why?

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    Half-life Radioactive
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Discussion Overview

The discussion revolves around the relationship between the half-life of radionuclides and their radioactivity, specifically in the context of the decay chain of U-238. Participants explore both qualitative and quantitative aspects of radioactivity, including definitions and equations related to decay constants and activity.

Discussion Character

  • Technical explanation
  • Mathematical reasoning
  • Conceptual clarification

Main Points Raised

  • One participant suggests that short-lived descendants of U-238 are more radioactive because they have less time to emit particles compared to the long-lived parent, leading to higher frequency emissions.
  • Another participant provides a mathematical explanation, stating that activity (A) is related to the decay constant (λ) and the number of particles (N) in the sample, with a smaller half-life resulting in a larger decay constant and thus higher activity.
  • A further contribution clarifies that while intermediate nuclides may have higher specific activity (activity per gram), if decay products are in equilibrium, the overall activity remains the same regardless of their half-lives.

Areas of Agreement / Disagreement

Participants present multiple perspectives on the relationship between half-life and radioactivity, with no consensus reached on the implications of specific activity versus overall activity in equilibrium conditions.

Contextual Notes

The discussion includes assumptions about the constancy of the number of particles during measurements and the conditions under which decay products are in equilibrium, which may affect the interpretations of radioactivity.

CPW
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TL;DR
In reading through The Physics of Energy, the textbook describes the decay chain of U-238:
"The longest half-life of any descendent in the chain is less 1 million years. Many half-lives are much shorter, making those nuclides very radioactive."

Why does having a short half-life make a radionuclide very radioactive?
In reading through The Physics of Energy, the textbook describes the decay chain of U-238:
"The longest half-life of any descendent in the chain is less 1 million years. Many half-lives are much shorter, making those nuclides very radioactive."
Why does having a short half-life make a radionuclide very radioactive?

My answer, qualitatively:
Relative to the time available for particle emissions from the long-lived parent radionuclide (U-238), the short-lived descendants have much less time to perform all the necessary particle emissions. And therefore, the short-lived radionuclides will have much higher radioactivity, as they will be emitting particles more frequently.
(Am I correct?)

However, quantitatively, I'm stuck.
I'd like a more formal answer than my answer above.

The amount of radioactivity (Bq) must be related to the number of disintegrations per gram per second.
But is there an equation relating these quantities?
 
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The activity (##A##), which is the number of disintegration per unit time, is given by
$$A = \lambda N$$
where ##\lambda## is the decay-constant and ##N## is the number of particles in the sample. If you assume that the number of particles ##N## in the sample does not change significantly during the period of time in which you measure the radioactivity, then you see that the higher the ##\lambda##, the higher the activity (number of disintegrations). It also turns out that the decay-constant ##\lambda## and the half-life ##\tau_{1/2}## are related by:
$$\tau_{1/2} = \frac {\ln 2} {\lambda}$$.
To summarize, small half-life -> big decay-constant ->big number of disintegrations per seconds = high activity.
 
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Thank you.
 
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I just want to add that the intermediate nuclides are higher radioactive in the sense that the specific activity, i.e. the activity per gram of the nuclide is higher. However, if the decay products are in equilibrium with each other, the activity of all isotopes is the same, irrespective of their half live.
 

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