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BIO Radioactive Tracers. Radioactive isotopes are often introduced into the body through the bloodstream. Their spread through the body can then be monitored by detecting the appearance of radiation in different organs. \(^{131} \mathrm{I},\) a \(\beta^{-}\) emitter with a half-life of 8.0 \(\mathrm{d}\) , is one such tracer. Suppose a scientist introduces a sample with an activity of 375 \(\mathrm{Bq}\) and watches it spread to the organs. (a) Assuming that the sample all went to the thyroid gland, what will be the decay rate in that gland 24 d (about 3\(\frac{1}{2}\) weeks) later? (b) If the decay rate in the thyroid 24 d later is actually measured to be 17.0 Bq, what percentage of the tracer went to that gland? (c) What isotope remains after the I-131 decays?

Short Answer

Expert verified
(a) 46.875 Bq; (b) 36.26%; (c) Xenon-131.

Step by step solution

01

Understanding the Concept of Half-Life

The half-life of a radioactive isotope is the time it takes for half of the radioactive atoms in a sample to decay. For Iodine-131 (I-131), the half-life is given as 8 days.
02

Calculate Remaining Activity After 24 Days

To find the remaining activity after 24 days, we use the formula: \[ A = A_0 \left(\frac{1}{2}\right)^{\frac{t}{T_{1/2}}} \]where \( A \) is the remaining activity, \( A_0 = 375 \) Bq is the initial activity, \( t = 24 \) days, and \( T_{1/2} = 8 \) days. Substitute these values. \[ A = 375 \times \left(\frac{1}{2}\right)^{\frac{24}{8}} = 375 \times \left(\frac{1}{2}\right)^3 = 375 \times \frac{1}{8} = 46.875 \text{ Bq} \]
03

Calculate Observed Percentage of the Tracer in Thyroid

We know the measured decay rate in the thyroid after 24 days is 17.0 Bq. To find the percentage of the original tracer that ended up in the thyroid gland, we use the formula: \[ \text{Percentage} = \left(\frac{\text{Observed activity}}{\text{Calculated remaining activity}}\right) \times 100 \]Substitute the values:\[ \text{Percentage} = \left(\frac{17.0}{46.875}\right) \times 100 \approx 36.26\% \]
04

Identify the Decay Product of Iodine-131

Iodine-131 ( \(^{131}\mathrm{I}\)) decays by beta decay into Xenon-131 ( \(^{131}\mathrm{Xe}\)). Therefore, after Iodine-131 decays, Xenon-131 remains as a stable by-product.

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Key Concepts

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

Isotope Half-life Calculation
The concept of half-life is essential for understanding how radioactive isotopes behave over time. In nuclear physics, a half-life is the time required for half of the radioactive atoms in a sample to decay. This means that after one half-life, only half of the original radioactive material remains, and this fraction gets halved with each subsequent half-life.

For example, in the case of the isotope Iodine-131 (\(^{131} \text{I}\)), which has a half-life of 8 days, if you start with 375 Becquerels (Bq) of radioactivity, you'll have half of that, approximately 187.5 Bq, after 8 days. After another 8 days (which totals 16 days), it will have decreased to about 93.75 Bq, and so on.

Understanding this decay pattern is crucial for predicting how long an isotope will remain active in a biological system or how long it can be effectively used in applications such as medical diagnostics or treatments.
Radioactive Decay
Radioactive decay is a natural process by which an unstable atomic nucleus loses energy by emitting radiation. It's a fundamental concept in nuclear physics that explains how elements transform over time. In radioactive decay, isotopes may emit particles such as alpha particles, beta particles, or gamma rays.

In the case of Iodine-131, it undergoes beta decay. This means the isotope emits a beta particle, resulting in the transformation of a neutron into a proton, which changes the element from iodine to xenon (\(^{131} \text{I} \rightarrow ^{131} \text{Xe}\)). This process decreases the atomic number by one, but the mass number remains the same, as it's a balance maintained by a neutron-proton swap.

Radioactive decay is used in various fields to determine ages of archaeological findings, track biological processes, and as seen in medicine, to diagnose and treat diseases with radioactive tracers.
Essential Diagnostics in Medicine
Radioactive tracers are pivotal in medical diagnostics. They offer a non-invasive way to diagnose and monitor various conditions. Doctors introduce a small amount of a radioactive isotope into the body, often through the bloodstream, which then spreads to specific areas like organs.

Tools like gamma cameras detect the radiation emitted by these isotopes, creating images that help physicians see how organs and tissues function in real-time. For instance, Iodine-131 is often used to study and treat thyroid disorders. Once introduced, it accumulates in the thyroid gland, enabling doctors to observe thyroid activity through imaging derived from emitted radiation.

These techniques allow for an effective diagnosis with minimal discomfort to the patient, ensuring radioactive substances are used carefully, following strict safety standards to ensure that the benefits outweigh any potential risks.
Nuclear Physics Concepts
Nuclear physics covers a broad range of concepts essential for understanding how radioactive isotopes work in real-life applications. At its core, nuclear physics investigates the components and structure of atomic nuclei and the forces that bind them.

Fundamental topics within nuclear physics include the behavior of isotopes, radioactive decay mechanisms, nuclear reactions, and the energy released during these processes. These concepts are critical in both theoretical and applied physics, influencing areas such as medicine, energy production, and environmental science.

Understanding these principles empowers scientists to harness nuclear reactions for various uses, such as generating electricity in nuclear power plants or creating medical isotopes for diagnostics and treatments. In everyday life, these principles underpin a host of technologies that benefit society.

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Most popular questions from this chapter

BIO A 67 -kg person accidentally ingests 0.35 Ci of tritium. (a) Assume that the tritium spreads uniformly throughout the body and that each decay leads on the average to the absorption of 5.0 \(\mathrm{keV}\) of energy from the electrons emitted in the decay. The half-life of tritium is \(12.3 \mathrm{y},\) and the RBE of the electrons is \(1.0 .\) Calculate the absorbed dose in rad and the equivalent dose in rem during one week. (b) The \(\beta^{-}\) decay of tritium releases more than 5.0 keV of energy. Why is the average energy absorbed less than the total energy released in the decay?

A \(^{186}_{76} \mathrm{Os}\) nucleus at rest decays by the emission of a 2.76 -MeV \(\alpha\) particle. Calculate the atomic mass of the daughter nuclide produced by this decay, assuming that it is produced in its ground state. The atomic mass of \(^{186}_{76} \mathrm{Os}\) is 185.953838 \(\mathrm{u}\)

Hydrogen atoms are placed in an external magnetic field. The protons can make transitions between states in which the nuclear spin component is parallel and antiparallel to the field by absorbing or emitting a photon. What magnetic- field magnitude is required for this transition to be induced by photons with frequency 22.7 \(\mathrm{MHz} ?\)

What nuclide is produced in the following radioactive decays? (a) \(\alpha\) decay of \(^{239} \mathrm{Pu} ;\) (b) \(\beta^{-}\) decay of \(_{11}^{24} \mathrm{Na} ;(\mathrm{c}) \beta^{+}\) decay of \(_{8}^{15} \mathrm{O}\)

Use conservation of mass-energy to show that the energy released in alpha decay is positive whenever the mass of the original neutral atom is greater than the sum of the masses of the final neutral atom and the neutral \(^{4}\) He atom. (Hint: Let the parent nucleus have atomic number \(Z\) and nucleon number \(A .\) First write the reaction in terms of the nuclei and particles involved, and then add \(Z\) electron masses to both sides of the reaction and allot them as needed to arrive at neutral atoms.)

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