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Why might \({ }^{123} \mathrm{I}\) be preferred for imaging over \({ }^{131} \mathrm{I} ?\) A. The atomic mass of \({ }^{123} \mathrm{I}\) is smaller, so the iodine particles travel farther through tissue with \({ }^{123} \mathrm{I}\). B. 123 I emits only gamma rays, so the radiation dose to the body is lower with \({ }^{123} \mathrm{I}\). C. The beta particles emitted by \({ }^{131} \mathrm{I}\) can leave the body, whereas the gamma rays emitted by \(123 \mathrm{I}\) cannot. D. \({ }^{123} \mathrm{I}\) is radioactive, whereas \({ }^{131} \mathrm{I}\) is not.

Short Answer

Expert verified
Option B: \(^{123} \mathrm{I}\) emits only gamma rays, reducing radiation dose.

Step by step solution

01

Understanding the Context

In medical imaging, different isotopes are used based on their radiation characteristics. Iodine-123 (\(^{123} \mathrm{I}\)) and Iodine-131 (\(^{131} \mathrm{I}\)) are isotopes of iodine commonly used for thyroid imaging and treatment due to their radioactive properties.
02

Analyzing Radiation Emission

\(^{123} \mathrm{I}\) primarily emits gamma rays. These rays are known for their ability to penetrate tissues and are ideal for imaging because they provide less radiation dose to the body, as they do not deposit energy in tissues like beta particles.
03

Comparing Radiation Types

\(^{131} \mathrm{I}\), on the other hand, emits both beta and gamma radiation. Beta particles are more biologically damaging as they can cause more harm to tissues. Hence, the use of \(^{123} \mathrm{I}\) with its gamma-only emission is preferred for reducing unnecessary radiation exposure.
04

Evaluating the Options

Option B correctly indicates that \(^{123} \mathrm{I}\) emits only gamma rays, leading to a reduced radiation dose to the body. Option A incorrectly relates atomic mass with imaging properties, Option C incorrectly describes the emissions, and Option D is false since both isotopes are radioactive.

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Key Concepts

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

Isotopes
Isotopes are atoms of the same element that have the same number of protons but different numbers of neutrons. This means they have the same atomic number but different atomic masses. In medical imaging, isotopes play a critical role because they can become radioactive, emitting radiation that is useful for diagnostic purposes.
For example, the isotopes Iodine-123 and Iodine-131 are used in medical settings. They are both forms of iodine, but they have different numbers of neutrons. This affects their stability and the types of radiation they emit. The difference in neutrons makes each isotope suitable for different applications in medical imaging.
Isotopes can be naturally occurring or artificially produced. In medicine, they are often produced in special reactors or by using particle accelerators. Their ability to emit radiation makes them valuable as tracers or treatment agents in various procedures.
Radiation Emission
Radiation emission is a process that occurs when an unstable nucleus releases energy to become more stable. This energy can be emitted in the form of particles or electromagnetic radiation. In the realm of medical imaging, understanding radiation emission is crucial because different types of radiation have different properties and uses.
The primary types of radiation emitted by isotopes are alpha particles, beta particles, and gamma rays. Each type has its unique features:
  • Alpha particles are heavy and highly charged, limiting their ability to travel far.
  • Beta particles are lighter and can penetrate tissues but can be damaging.
  • Gamma rays are not particles but electromagnetic waves that can penetrate deeply into tissues, making them ideal for imaging purposes.
In medical imaging, select isotopes are used that emit the most appropriate type of radiation for the intended diagnostic procedure.
Gamma Rays
Gamma rays are a form of electromagnetic radiation with very high energy and short wavelengths. Unlike particles, gamma rays do not have mass or charge, allowing them to penetrate thick materials, including human tissues, with little attenuation.
The ability of gamma rays to carry through the body makes them extremely useful in medical imaging, particularly in nuclear medicine, where they are used to create images of structures inside the body without invasive procedures.
In diagnostic imaging, the gamma rays emitted by certain isotopes, such as Iodine-123, help capture clear images by passing through body tissues and being detected outside the body. This property reduces the radiation dose a patient receives, making gamma-ray-emitting isotopes preferable for imaging.
Iodine-123
Iodine-123 is a radioisotope of iodine that is commonly used in medical imaging, particularly for thyroid diagnostics. It is preferred due to its low radiation dose and gamma-ray emission, which is ideal for imaging purposes.
When administered to a patient, Iodine-123 emits gamma rays as it decays. These rays are detected by specialized cameras to provide images of the thyroid, helping in the diagnosis of conditions such as hyperthyroidism or thyroid cancer.
One of the advantages of using Iodine-123 is that it has a relatively short half-life of about 13 hours. This short half-life minimizes the duration of radiation exposure to the patient while still allowing enough time to perform the imaging procedure effectively.
Iodine-131
Iodine-131 is another isotope of iodine, often used for therapeutic rather than imaging purposes. It emits both beta and gamma radiation, with the beta radiation being highly effective at destroying diseased thyroid tissue.
This ability makes Iodine-131 highly beneficial for treating conditions such as overactive thyroid glands or thyroid cancer. The beta particles can effectively target and destroy unhealthy thyroid cells, providing a targeted therapeutic effect.
However, due to the beta radiation's potential to cause tissue damage, Iodine-131 is used with precaution and primarily preferred in treatment rather than diagnostic imaging. This distinguishes it from Iodine-123, which is favored in situations when capturing clear images with minimal radiation exposure is the priority. Iodine-131's half-life of about eight days allows it to remain effective long enough to achieve its therapeutic goals.

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Most popular questions from this chapter

Radioactive isotopes used in cancer therapy have a "shelf-life" simply because the active nuclei decay away. Just after it has been manufactured in a nuclear reactor, the activity of a sample of \({ }^{60} \mathrm{Co}\) is \(5000 \mathrm{Ci}\). When its activity falls below \(3500 \mathrm{Ci}\), it is considered too weak a source to use in treatment. You work in the radiology department of a large hospital. One of the \({ }^{60}\) Co sources in your inventory was manufactured on October 20,2012 . It is now October 20,2014 . Is the source still usable? Explain. (The half-life of \({ }^{60} \mathrm{Co}\) is 5.3 years.)

Nuclear weapons tests in the \(1950 \mathrm{~s}\) and \(1960 \mathrm{~s}\) released significant amounts of radioactive tritium \(\left({ }_{1}^{3} \mathrm{H},\right.\) half-life 12.3 years \()\) into the atmosphere. The tritium atoms were quickly bound into water molecules and rained out of the air, most of them ending up in the ocean. For any of this tritium-tagged water that sinks below the surface, the amount of time during which it has been isolated from the surface can be calculated by measuring the ratio of the decay product, \({ }_{2}^{3} \mathrm{He},\) to the remaining tritium in the water. For example, if the ratio of \({ }_{2}^{3} \mathrm{He}\) to \({ }_{1}^{3} \mathrm{H}\) in a sample of water is \(1: 1,\) the water has been below the surface for one half-life, or approximately 12 years. This method has provided oceanographers with a convenient way to trace the movements of subsurface currents in parts of the ocean. Suppose that in a particular sample of water, the ratio of \({ }_{2}^{3} \mathrm{He}\) to \({ }_{1}^{3} \mathrm{H}\) is \(4.3: 1.0 .\) How many years ago did this water sink below the surface?

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 \(24 \mathrm{~d}\) (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 percent of the tracer went to that gland? (c) What isotope remains after the I-131 decays?

Which of the following reactions obey the conservation of baryon number? (a) \(\mathrm{p}+\mathrm{p} \rightarrow \mathrm{p}+\mathrm{e}^{+},\) (b) \(\mathrm{p}+\mathrm{n} \rightarrow 2 \mathrm{e}^{+}+\mathrm{e}^{-}\) (c) \(\mathrm{p} \rightarrow \mathrm{n}+\mathrm{e}^{-}+\bar{\nu}_{\mathrm{e}},(\mathrm{d}) \mathrm{p}+\overline{\mathrm{p}} \rightarrow 2 \gamma\)

In 2010 , the United States used approximately \(1.4 \times 10^{19} \mathrm{~J}\) of elec- trical energy. If all this energy came from the fission of \({ }^{235} \mathrm{U},\) which releases \(200 \mathrm{MeV}\) per fission event, (a) how many kilograms of \({ }^{235} \mathrm{U}\) would have been used during the year? (b) How many kilograms of uranium would have to be mined to provide that much \({ }^{235} \mathrm{U} ?\) (Recall that only \(0.70 \%\) of naturally occurring uranium is \({ }^{235} \mathrm{U} .\) )

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