Chapter 3: Q5E (page 111)
Potassium-40 Decay The chemical element potassium is a soft metal that can be found extensively throughout the Earth's crust and oceans. Although potassium occurs naturally in the form of three isotopes, only the isotope potassium-40 (K-40)is radioactive. This isotope is also unusual in that it decays by two different nuclear reactions. Over time, by emitting beta particles a great percentage of an initial amount of K-40 decays into the stable isotope calcium-40 (Ca40), whereas by electron capture a smaller percentage of decays into the stable isotope argon-40 (Ar-40). Because the rates at which the amounts C(t)of Ca-40 and A(t)of Ar-40increase are proportional to the amount K(t)of potassium present, and the rate at which K(t)decays is also proportional to K(t), we obtain the system of linear first-order equations
where and are positive constants of proportionality. By proceeding as in Problem 1 we can solve the foregoing mathematical model.
(a) From the last equation in the given system of differential equations find K(t)if . Then useto findandfrom the first and second equations. Assume that C(0)=0and A(0)=0.
(b) It is known that and . Find the half-life of K-40.
(c) Use C(t)and A(t)found in part (a) to determine the percentage of an initial amountof K-40that decays into Ca-40and the percentage that decays into Ar-40over a very long period of time.
Short Answer
(a)So, the value of.
(b) So, the half- life of K – 40 is .
(c) Percentage of an initial amount is 89.