Nucleus |
| Introduction
Radioactive decay process follows first order Kinetics i.e rate of reaction depends upon no. of nucleus raised to power one.
where disintegration / decay constant.or ![]() Integrating both sides ![]() ![]() for half life N = N0/2 ![]() Activity of a radioactive substance is the rate of decay or the number disintegration per second . it is denoted by A. ![]() Also A = A0 where A0
initial activity.Dumb Question: Why has the rate been taken as negative of rate of change of no. of nuclei Ans:- It is known that in a radioactive decay, the no. of nucleii always decreases, itself will be negative, so to get overall
rate as a positive quantity R = - ![]() • no. of nucleii remaining after n half lives is given by N = ![]() Illustration:- Uranium areas on the earth at present time typically have a composition consisting of 99.3% of the isotope 92U235 and 0.7% of the isotope 92U235. The half lives of those isotopes are 4.47 x 109y and 7.04 x 108y respectively. if then isotopes were equally abundant when the earth was formed, estimate the age of earth Solution:- let no be number of atoms of each isotope at the time of formation of the earth (T = 0) and N1 and N2 the number of atoms at present(t - t) then N1 = N0 .................................................................(i)N2 = N0 .................................................................(ii)![]() Further it is given that ![]() Equating (iii) and (iv) and taking log on both sides, we have ![]() Substituting the values, we have ![]() (1) Graphical Representation:- Since the radioactive decay process follows experential rate law hence it has graph as shown in adjacent figure. ![]() |




where
disintegration / decay constant.




where A0
initial activity.
itself will be negative, so to get overall
rate as a positive quantity R = - 








