Radioactive Dating — Question 10

Section 42-6 · Physics pages 7110–7111

Question 10 A late loss of parent can make a daughter clock appear too old A mineral initially has no daughter, and each parent decay makes one stable daughter. After exactly one parent half-life, an instantaneous event removes 20 percent of the remaining parent but no daughter. Measurement follows immediately. .5P0 retained: .4P0 lost: .1P0 Schematic; labels, not drawing lengths, specify the data. (a) Find measured parent and daughter numbers in units of the original P0. (b) Calculate the apparent closed-system age from D/P and its error in half-life units.
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Question 10 - Solution A late loss of parent can make a daughter clock appear too old .5P0 retained: .4P0 lost: .1P0 (a) Method and calculation Before loss: P = P0/2, D = P0/2. Pmeas = .8(P0/2) = .4P0, Dmeas = .5P0 . (b) Interpretation and further calculation D/P = 1.25, tapp/T = log2(1 + 1.25) = 1.16993 . (tapp −ttrue)/T = .16993 an overestimate. Physical check The daughter-to-parent ratio rose without additional radioactive decay. This is why a measured ratio must be interpreted with a geological closure model.

Question 10

A late loss of parent can make a daughter clock appear too old

A mineral initially has no daughter, and each parent decay makes one stable daughter. After exactly one parent half-life, an instantaneous event removes 20 percent of the remaining parent but no daughter. Measurement follows immediately.

Diagram shown in the original SVG worksheet.

  1. Find measured parent and daughter numbers in units of the original P0P_0.

  2. Calculate the apparent closed-system age from D/P and its error in half-life units.

Question 10 - Solution

A late loss of parent can make a daughter clock appear too old

Diagram shown in the original SVG worksheet.

(a) Method and calculation

Before loss: P=P0/2,D=P0/2.\text{Before loss: }P=P_0/2,\quad D=P_0/2.Pmeas=.8(P0/2)=.4P0,Dmeas=.5P0.\boxed{P_{\mathrm{meas}}=.8(P_0/2)=.4P_0,\quad D_{\mathrm{meas}}=.5P_0}.

(b) Interpretation and further calculation

D/P=1.25,tapp/T=log⁡2(1+1.25)=1.16993.\boxed{D/P=1.25,\quad t_{\mathrm{app}}/T=\log_2(1+1.25)=1.16993}.(tapp−ttrue)/T=.16993an overestimate.\boxed{(t_{\mathrm{app}}-t_{\mathrm{true}})/T=.16993}\quad\text{an overestimate}.

Physical check

The daughter-to-parent ratio rose without additional radioactive decay. This is why a measured ratio must be interpreted with a geological closure model.