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A wooden artifact from a Chinese temple has a \({ }^{14} \mathrm{C}\) activity of \(38.0\) counts per minute as compared with an activity of \(58.2\) counts per minute for a standard of zero age. From the halflife for \({ }^{14} \mathrm{C}\) decay, \(5715 \mathrm{yr}\), determine the age of the artifact.

Short Answer

Expert verified
The age of the wooden artifact from the Chinese temple is approximately 2578.1 years.

Step by step solution

01

Understand the radioactive decay formula

The radioactive decay formula is given by: \(N(t) = N_0 e^{(-\lambda t)}\) where \(N(t)\) is the remaining radioactive material, \(N_0\) is the initial amount of radioactive material, \(\lambda\) is the decay rate, and \(t\) is the time passed. For this problem, we are interested in finding the time \(t\), so we need to rearrange the formula for \(t\).
02

Rearrange the formula to find time

Divide both sides of the radioactive decay formula by \(N_0\) and take the natural logarithm of both sides: \(\frac{N(t)}{N_0} = e^{(-\lambda t)}\) \(\ln{\frac{N(t)}{N_0}} = -\lambda t\) Then, we can solve for \(t\): \(t = -\frac{1}{\lambda} *\ln{\frac{N(t)}{N_0}}\)
03

Calculate the decay constant

We are given the half-life of \({ }^{14}\mathrm{C}\) as \(T_{1/2} = 5715\) years. The decay constant \(\lambda\) can be calculated using the relation: \(\lambda = \frac{\ln{2}}{T_{1/2}}\) Substitute the given half-life value to find the decay constant: \(\lambda = \frac{\ln{2}}{5715} \approx 1.2097 * 10^{-4}\ \mathrm{yr}^{-1}\)
04

Substitute values in the time formula

Now plug the values of \(N(t) = 38.0\), \(N_0 = 58.2\) and \(\lambda = 1.2097 * 10^{-4}\ \mathrm{yr}^{-1}\) into the formula from step 2: \(t = -\frac{1}{1.2097 * 10^{-4}} * \ln{\frac{38.0}{58.2}}\)
05

Calculate the age of the artifact

Following the formula from step 4, \(t \approx -\frac{1}{1.2097 * 10^{-4}} * \ln{\frac{38.0}{58.2}} \approx 2578.1 \ \mathrm{years}\) The age of the wooden artifact from the Chinese temple is approximately 2578.1 years.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Radioactive Decay Formula
The essence of radioactive carbon dating lies in understanding the radioactive decay formula. It's crucial for revealing the age of archaeological artifacts or geological samples. At its core, the formula exemplifies the exponential nature of radioactive decay. To put it simply, the remaining amount of radioactive material, often notated as \(N(t)\), declines over time according to the initial amount \(N_0\) multiplied by an exponent involving the decay constant \(\lambda\) and the time passed \(t\):

\(N(t) = N_0 e^{(-\lambda t)}\)

Here, \(e\) is the base of the natural logarithm, and this particular form of the function evidences how the quantity of radioactive atoms dwindles over time. When scientists measure the current activity or count rate of a sample and compare it to a standard reference, they grasp the sample's age by manipulating this formula.
Half-Life Calculation
The concept of half-life is integral to carbon dating and understanding radioactivity in general. A half-life is the time required for half of the radioactive nuclei in a sample to undergo decay. In practical terms, it's like a clock that tells us how old a fossil or artifact is.

To calculate half-life from the decay constant, the following relationship is used:

\(T_{1/2} = \frac{\ln{2}}{\lambda}\)

This equation is derived from setting \(N(t) = \frac{N_0}{2}\) in the radioactive decay formula and solving for \(t\) when exactly half of the original material remains. For carbon-14, this constant provides a reliable half-life that scientists use as a reference for dating organic materials.
Decay Constant
The decay constant symbolized by \(\lambda\) reflects the probability of a single atom decaying per unit time, framing it as the pacemaker of the radioactive process. Once you know an isotope's half-life, which is a fixed value, calculating the decay constant is straightforward with the formula:

\(\lambda = \frac{\ln{2}}{T_{1/2}}\)

For carbon-14, whose half-life is quite well-known, pinning down the decay constant becomes a simple matter of plugging numbers into the formula. This decay constant feeds into the primary equation for determining the age of artifacts or samples, cementing its place as a pillar of radioactive dating methods.
Natural Logarithm
The natural logarithm, often abbreviated as \(\ln\), is a mathematical operation that's inseparable from the analysis of radioactive decay. Especially when scientists rearrange the decay formula to solve for time, they rely on taking the natural logarithm of both sides to linearize the equation. Here's why: the natural logarithm is the inverse function to exponentiation with base \(e\). So when the equation has an exponent that we need to isolate and solve for, the \(\ln\) is used to 'undo' the exponent.

The application of \(\ln\) in our context revolves around determining the time elapsed based on the remaining and initial quantities of radioactive material. As such, it's an indispensable tool for physicists and archaeologists when they perform carbon dating.

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Most popular questions from this chapter

One of the nuclides in each of the following pairs is radioactive. Predict which is radioactive and which is stable: (a) \({ }_{19}^{39} \mathrm{~K}\) and \({ }_{19}^{40} \mathrm{~K}\), (b) \({ }^{209} \mathrm{Bi}\) and \({ }^{208} \mathrm{Bi}\), (c) nickel-58 and nickel-65.

Cobalt-60, which undergoes beta decay, has a half-life of \(5.26 \mathrm{yr}\). (a) How many beta particles arc emitted in \(600 \mathrm{~s}\) by a \(3.75-\mathrm{mg}\) sample of \({ }^{60} \mathrm{Co}\) ? (b) What is the activity of the sample in Bq?

Putting Concepts Together Potassium ion is present in foods and is an essential nutrient in the human body. One of the naturally occurring isotopes of potassium, potassium- 40 , is radioactive. Potassium-40 has a natural abundance of \(0.0117 \%\) and a half- life \(t_{1 / 2}=1.28 \times 10^{9} \mathrm{yr}\). It undergoes radioactive decay in three ways: \(98.2 \%\) is by electron capture, \(1.35 \%\) is by beta emission, and \(0.49 \%\) is by positron emission. (a) Why should we expect \({ }^{40} \mathrm{~K}\) to be radioactive? (b) Write the nuclear equations for the three modes by which \({ }^{40} \mathrm{~K}\) decays. (c) How many \({ }^{40} \mathrm{~K}^{+}\)ions are present in \(1.00 \mathrm{~g}\) of \(\mathrm{KCl}\) ? (d) How long does it take for \(1.00 \%\) of the \({ }^{40} \mathrm{~K}\) in a sample to undergo radioactive decay? SOLUTION (a) The \({ }^{40} \mathrm{~K}\) nucleus contains 19 protons and 21 neutrons. There are very few stable nuclei with odd numbers of both protons and neutrons (Section 21.2). (b) Electron capture is capture of an inner-shell electron by the nucleus: $$ { }_{19}^{40} \mathrm{~K}+{ }_{-1}^{0} \mathrm{e} \longrightarrow{ }_{18}^{40} \mathrm{Ar} $$ Beta emission is loss of a beta particle \((-1 \mathrm{e})\) ) by the nucleus: $$ { }_{19}^{40} \mathrm{~K} \longrightarrow{ }_{20}^{40} \mathrm{Ca}+{ }_{-1}^{0} \mathrm{e} $$ Positron emission is loss of a positron \(\left(+{ }_{+}^{0} \mathrm{e}\right)\) by the nucleus: $$ { }_{19}^{40} \mathrm{~K} \longrightarrow{ }_{18}^{40} \mathrm{Ar}+{ }_{+1}^{0} \mathrm{e} $$ (c) The total number of \(\mathrm{K}^{+}\)ions in the sample is $$ (1.00 \mathrm{~g} \mathrm{KCl})\left(\frac{1 \mathrm{~mol} \mathrm{KCl}}{74.55 \mathrm{~g} \mathrm{KCl}}\right)\left(\frac{1 \mathrm{~mol} \mathrm{~K}}{1 \mathrm{~mol} \mathrm{KCl}}\right)\left(\frac{6.022 \times 10^{23} \mathrm{~K}^{+}}{1 \mathrm{~mol} \mathrm{~K}^{+}}\right)=8.08 \times 10^{21} \mathrm{~K}^{+} \text {ions } $$ Of these, \(0.0117 \%\) are \({ }^{40} \mathrm{~K}^{+}\)ions: $$ \left(8.08 \times 10^{21} \mathrm{~K}^{+} \text {ions }\right)\left(\frac{0.0117^{40} \mathrm{~K}^{+} \text {ions }}{100^{+} \text {ions }}\right)=9.45 \times 10^{17} \text { potassium-40 ions } $$ (d) The decay constant (the rate constant) for the radioactive decay can be calculated from the half-life, using Equation 21.20: $$ k=\frac{0.693}{t_{1 / 2}}=\frac{0.693}{1.28 \times 10^{9} \mathrm{yr}}=\left(5.41 \times 10^{-10}\right) / \mathrm{yr} $$ The rate equation, Equation \(21.19\), then allows us to calculate the time required: $$ \begin{aligned} \ln \frac{N_{t}}{N_{0}} &=-k t \\ \ln \frac{99}{100} &=-\left[\left(5.41 \times 10^{-10}\right) / \mathrm{yr}\right] t \\ -0.01005 &=-\left[\left(5.41 \times 10^{-10}\right) / \mathrm{yr}\right] t \\ t &=\frac{-0.01005}{\left(-5.41 \times 10^{-10}\right) / \mathrm{yr}}=1.86 \times 10^{7} \mathrm{yr} \end{aligned} $$ That is, it would take \(18.6\) million years for just \(1.00 \%\) of the \({ }^{40} \mathrm{~K}\) in a sample to decay.

The nuclear masses of \({ }^{7} \mathrm{Be},{ }^{9} \mathrm{Be}\), and \({ }^{10} \mathrm{Be}\) are \(7.0147,9.0100\), and 10.0113 amu, respectively. Which of these nuclei has the largest binding energy per nucleon?

A sample of an alpha emitter having an activity of \(0.18 \mathrm{Ci}\) is stored in a \(25.0\) - \(\mathrm{mL}\) sealed container at \(22{ }^{\circ} \mathrm{C}\) for 245 days. (a) How many alpha particles are formed during this time? (b) Assuming that each alpha particle is converted to a helium atom, what is the partial pressure of helium gas in the container after this 245 -day period?

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