A radioactive parent isotope P decays into a stable daughter D. At the time the mineral formed, the number of daughter atoms was equal to the initial number of parent atoms. At present the measured ratio is N(D):N(P) = 7:1. If the parent half-life is 1000 years, find the age of the sample in years.
Physics · Nuclear physics · radioactivity and law of decay
A radioactive parent isotope P decays into a stable daughter D. At the time the mineral formed, the number of daughter atoms was equal to the initial number of parent atoms. At present the measured ratio is N(D): N(P) = 7:1. If the parent half-life is 1000 years, find the age of the sample in years.