The radioactive isotope uranium−238 decays in a decay series to the stable lead−206.
The half−life of is 4.5 × 109 years, which is much larger than all the other half−lives of the decays in the series.
A rock sample, when formed originally, contained 6.0 × 1022 atoms of and no atoms. At any given time, most of the atoms are either or with a negligible number of atoms in other forms in the decay series.
(a)
Sketch on the axes below the variation of number of atoms and the number of atoms in the rock sample as they vary over a period of 1.0 × 1010 years from its formation. Label your graphs U and Pb.