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Nuclear Spectroscopy

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A P P E N D I X C<br />

Mathematics of Radioactive Decay<br />

Consider a chain of nuclides, one related to another<br />

by radioactive decay. Three so-related nuclides will<br />

suffice for this discussion. The initial nuclide, #1, is<br />

called the parent, the decay product of the parent is<br />

the daughter, #2, and the decay product of the daughter<br />

is the granddaughter, #3. A typical radioactive<br />

decay chain is shown symbolically in Figure C.1.<br />

where N(t) is the number of parent nuclei at time t,<br />

and dN is the number of parent nuclei that decayed<br />

in the time between t and t+dt. Integration of equation<br />

C.1 for the parent atoms, assuming the number<br />

of parent ions at time t=0, N 1<br />

(0), is zero, gives the<br />

number of parent nuclei remaining after time, t, as<br />

C.2<br />

N () t = N ( ) e<br />

−λ1t<br />

1 1<br />

0<br />

where λ 1 is related to the parent’s half-life, T 1/2<br />

, by<br />

C.3<br />

T 1 2<br />

= 2 λ 1<br />

= 0 693 λ 1<br />

/<br />

ln / . /<br />

Grandaughter<br />

#3<br />

Parent<br />

#1<br />

β<br />

–<br />

α<br />

Daughter<br />

#2<br />

N 1<br />

(t) is a mathematically smooth function that decreases<br />

exponentially with time, but N 1<br />

(t) is not a<br />

completely correct mathematical model for radioactive<br />

decay of a parent nucleus. It mathematically<br />

represents the number of parent nuclei that most<br />

probably survive after time, t. There can and will be<br />

statistical fluctuations in N 1<br />

(t). In fact it can be shown<br />

(see experiment 9 on counting statistics) that if N is<br />

the ‘most probable’ number of disintegrations in a<br />

period of time ∆t, there is about a 68% chance that the<br />

observed number is between<br />

Figure C1. A schematic representation of nuclear decay. The<br />

horizontal axis is the atomic number and the vertical axis is<br />

the mass/energy axis.<br />

The fundamental experimental foundation of radioactive<br />

decay is that the probability, P(t)dt =λdt, for<br />

any one nucleus to decay in a small time interval, dt,<br />

is independent of any external influence (in very<br />

special situations this is not true), including the decay<br />

of other nuclei. All nuclei of a particular nuclide have<br />

the same decay probability (rate, λ) such that<br />

C.1<br />

Z-1 Z Z+1<br />

− dN = N() t P() t dt = λN()<br />

t dt<br />

C.4<br />

N − N and N + N<br />

The rate at which atoms, say the parent of Figure C.1,<br />

decay, is called the activity, A(t), and is a function of<br />

time. Units for activity are the Curie (1 Ci = 3.7 x 10 10<br />

decays/sec) and the SI unit, the Becquerel (Bq = 1<br />

decay/sec). For the decay symbolized in Figure C.1,<br />

let [λ 1<br />

, N 1<br />

(t)], [λ 2<br />

, N 2<br />

(t)], and [λ 3<br />

=0, N 3<br />

(t)] represent<br />

the decay constants and the number of atoms of the<br />

parent, daughter, and granddaughter atoms, respectively.<br />

Then the rate of population change, dN, for<br />

each generation of atom is<br />

C.5<br />

C.6<br />

C.7<br />

dN<br />

=−λ N () t dt<br />

1 1 1<br />

dN = λ N () t dt −λ<br />

N () t dt<br />

2 1 1 2 2<br />

dN3 = λ<br />

2N2()<br />

t dt<br />

65

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