Quote:
Originally Posted by Pigness
Trolly you're right of course, masque has made an error I think...
In what? You asked for a natural definition of λ. The half life is not a natural definition because it is log2/T
1/2.
The constant itself is not the inverse of the time it takes to have decay 50% of your radioactive material (just 1/e). So this is not a natural definition of it unless you say its the inverse of the time it takes to have 1/e of your original sample decay. But the activity is naturally introducing it as the fractional loss of radioactive material per unit of time (ie the rate of fractional loss).
Experimentally how on earth are you going to easily know when the sample has lost 50% of its initial population???
But you can always have a rate of decay it seems ie the activity. All you need for it is to count how many decays you measure per second and some knowledge of your initial sample size (or nuclei % in it) .
You do not need to wait 4.5 bil years for Uranium or even a few years to find the new number of U238 nuclei left to decay (ie to get to the half life connection i mean). All you need is to count how many decays you have in a given sample per minute say and you obtain λ. Use a Geiger counter etc.
λ=(dN/dt)/N is very simple to observe if you are not losing detections or you can estimate how much you are losing vs what you record. Then on course you can find the half life too by the above equation.
Even if you do not have the original size, ie N that you started with, you can still measure activity at different times and see how it changes and model it from there if it is not a very slow decay thing. In that case however that it is very slow you can estimate its mass and number of nuclei in other ways
Last edited by masque de Z; 10-14-2016 at 08:02 PM.