You calculate the half-life from the amount of material that disappears in a given time.
Half-life (#t_½#) is the time required for the nuclei to decay to half of the original amount.
Radioactive nuclei decay according to the equation:
Equation 1: #N_t /N_0 = e^(—λt)#, where
#N_0# is the initial number of nuclei at time #t = 0#.
#N_t# is the number of nuclei that remain after time #t#. We can also use any number that is proportional to the number of nuclei, such as mass or disintegration counts.
#λ# is a constant called the decay constant. Each nucleus has its own decay constant.
The equation for half-life is
Equation 2: #t_½ = ln2/λ#
We can combine these two equations to get
Equation 3: #N_t/N_0 = 0.5^(t/t_½)#
EXAMPLE:
A 50 g sample of radium–226 decays to 5.7 g after 5000 years. What is the half-life of radium–226?