Chapter 21: Problem 16
Compare and contrast positron-emission and electron-capture processes.
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Chapter 21: Problem 16
Compare and contrast positron-emission and electron-capture processes.
These are the key concepts you need to understand to accurately answer the question.
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Potassium- 40 is a radioactive isotope of potassium, a very common element in terrestrial rocks, which decays to \(^{40}\) Ar with a half-life of \(1.28 \times 10^{9}\) years. By measuring the ratio of \(^{40} \mathrm{Ar}\) to \(^{40} \mathrm{K},\) geologists can to determine the age of ancient rocks. a. Balance the nuclear equations for the decay of \(^{40} \mathrm{K}\) by identifying the missing isotope or particle.$$\begin{array}{l}^{40} \mathrm{K} \rightarrow^{40} \mathrm{Ar}+? \\\^{40} \mathrm{K} \rightarrow +_{-1}^{0} \beta\end{array}$$.b. Why might \(^{40} \mathrm{K}\) decay by two different pathways? c. Only about \(11 \%\) of the \(^{40} \mathrm{K}\) decays to \(^{40} \mathrm{Ar}\). If the ratio of \(^{40} \mathrm{Ar}\) to \(^{40} \mathrm{K}\) in a rock is found to be \(0.435,\) how old is the rock? d. Why don't geologists measure the \(^{40} \mathrm{Ca}:^{40} \mathrm{K}\) ratio instead?
Calculate the neutron-to-proton ratios for each of the following and predict the decay pathways of the following radioactive isotopes: \((\mathrm{a})^{238} \mathrm{U} ;(\mathrm{b})^{186} \mathrm{Re} ;(\mathrm{c})^{86} \mathrm{Y}\).
Describe the dangers of exposure to radon-222.
What nuclide is produced in the core of a giant star by each of the following fusion reactions? Assume there is only one product in each reaction. a. \(28 \mathrm{Si}+^{4} \mathrm{He} \rightarrow\) b. \(^{40} \mathrm{Ca}+^{4} \mathrm{He} \rightarrow\) c. \(^{24} \mathrm{Mg}+^{4} \mathrm{Hc} \rightarrow\)
Dating Cave Paintings Cave paintings in Gua Saleh Cave in Borneo have been dated by measuring the amount of \(^{14} \mathrm{C}\) in calcium carbonate deposits that formed over the pigments used in the paint. The source of the carbonate ion was atmospheric \(\mathrm{CO}_{2}\).a. What is the ratio of the \(^{14} \mathrm{C}\) radioactivity in calcium carbonate that formed 9900 years ago to that in calcium carbonate formed today? b. The archaeologists also used a second method, uranium-thorium dating, to confirm the age of the paintings by measuring trace quantities of these elements present as contaminants in the calcium carbonate. Shown below are two candidates for the U-Th dating method. Which isotope of uranium do you suppose was chosen? Explain your answer. $$\begin{aligned} &t_{1 / 2}=^{233} \mathrm{U} \quad 7.04 \times 10^{8} \mathrm{yr} \quad^{231} \mathrm{Th} \quad \rightarrow \quad^{231} \mathrm{p}_{2} \quad 3 \quad \rightarrow \quad\\\ &t_{1 / 2}=^{234} \mathrm{U} \quad \begin{array}{rl}\rightarrow & ^{230} \mathrm{Th} \\ 2.44 \times 10^{5} \mathrm{yr} & 7.7 \times 10^{4} \mathrm{hr}\end{array} \quad \begin{array}{rl} 226 \mathrm{p}_{2} & \rightarrow \\\1600 & \mathrm{yr}\end{array}\end{aligned}$$
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