A radioactive parent isotope P decays into a stable daughter isotope D. At the time a mineral crystallised, no daughter isotope was present. At present the measured number ratio is N(D):N(P) = 15:1. If the half-life of P is 500 million years, find the age of the mineral in million years.
Physics · Nuclear physics · radioactivity and law of decay
A radioactive parent isotope P decays into a stable daughter isotope D. At the time a mineral crystallised, no daughter isotope was present. At present the measured number ratio is N(D): N(P) = 15:1. If the half-life of P is 500 million years, find the age of the mineral in million years.