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By measuring the amounts of parent isotope and daughter product in the minerals contained in a rock, and by knowing the half-life of the parent isotope, a geologist can calculate the absolute age of the rock. A rock contains 125 g of a radioisotope with a half-life of 150,000 years and 875 g of its daughter product. How old is the rock according to the radiometric dating method? Make sure to share the math of how you came up with your answer…

Respuesta :

Answer:

450,000 years

Explanation:

The equation that describes the decay of a radioactive isotope is:

[tex]m(t) = m_0 (\frac{1}{2})^{\frac{t}{\tau}}[/tex]

where

[tex]m_0[/tex] is the mass of the isotope at time t = 0

[tex]m(t)[/tex] is the mass of the isotope at time t

[tex]\tau[/tex] is the half-life of the isotope, which is the time it takes for the isotope to halve its mass

In this problem:

[tex]\tau = 150,000 y[/tex] is the half-life of the radioisotope

m(t) = 125 g is the mass of radioisotope left after time t

[tex]m_0 = 125+875 = 1000 g[/tex] is the initial mass of the radioisotope (the sum of the mass of the final radioisotope + the mass of the daughter nuclei, since mass is conserved)

So, we can re-arrange the equation to find t:

[tex](\frac{1}{2})^{\frac{t}{\tau}}=\frac{m(t)}{m_0}\\t=-\tau log_2 (\frac{m(t)}{m_0})=-(150,000) log_2(\frac{125}{1000})=450,000 y[/tex]

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