Uranium-lead (U-Pb) dating of geological samples is one of the oldest and most refined radiometric dating methods, able to determine ages of about 1 million years to over 4.5 billion years with precision in the 0.1–1% range. The U-Pb dating method relies on two separate decay chains, one of which is the uranium series from 238U to 206Pb, with a half-life of 4.47 billion years.Geologists unearth a sample of zircon that appears to be a closed system. They find 0.730 microgram of 206Pb for 1.000 microgram of 238U present. Approximately how old is the sample?Collect and OrganizeAssuming that the only loss of 238U is via radioactive decay and that all of the nuclides produced by the decay processes remain in the sample, the U-Pb radiometric dating method can be used to calculate the age of the zircon sample. 238U decays to 206Pb through a series of 14 steps with an apparent half-life of 4.47×109 years. What is the relationship between the number of 206Pb atoms present and the amount of 238U that has decayed? How much 238U has not yet decayed? Did you find the ratio, Nt/N0, the amount of 238U remaining relative to the amount of 238U initially present?

Respuesta :

Answer:

Explanation:

Here we will be using the radiactive decay equations :

Nt/N₀ = e^-kt  where k is the decay constant per year

                  t= time in years

                Nt = amount of  ²³⁸ U present at time t in μg ( μ =microgram)

                N₀ = amount of  ²³⁸ U originally present  in μg

We notice we dont have k, but this value can be obtained from t₁/₂ through

                k = 0.693 / t₁/₂

which is derived from Nt/N₀ = e^-kt for the half-life where  Nt/N₀ = 0.5

The hints given in the problem helps us greatly  to determine N and N₀

All the ²⁰⁶ Pb comes from ²³⁸ U and we know its mass = 0.730  in μg, so lets find moles   ²³⁸ U

0.730 ug  x  1 mol ²⁰⁶ Pb/206 umol = 0.3544 x 10⁻³ umol

This means  0.3544 x 10⁻³  in μmol of  ²³⁸ U decayed

To find the mass decayed multiply by the atomic weight:

0.3544 x 10⁻³  in μmol  x  238 g/ m in μmol = 8.434 x 10⁻²  in μg  ²³⁸ U decayed

N₀ =  8.434 x 10⁻² in μg + 1.000  in μg =  1.843   in μg

Now lets calculate the value for k and we will finally can compute the age of the sample:

k = 0.693/ 4.47 x 10⁹ yrs⁻¹ =1.550 x 10⁻¹⁰  yrs⁻¹

Nt/N₀ = e^-kt  ⇒   (1.000  in μg/ 1.843 μg) = e ^- ( 1.550 x 10⁻¹⁰yrs⁻¹   / x t)

Taking natural log to both sides of the equation:

ln (1.000/1.843 ) = - 1.550 x 10⁻¹⁰ yrs⁻¹  x  t

t= 3.94 x 10⁹ yrs = 3.94 billion years

To check our answer note that the time calculated is less than a half-life and the mass decayed is less than half the mass originally present.

(Note I left the mass in units of micrograms but could have also worked in grams but it would have been messier.)