Nuclear Chemistry Study Notes

Nuclear Chemistry

Definition of a Radioisotope

  • A radioisotope is defined as follows:
    • Has an unstable nucleus and emits radiation.
    • Can be one or more isotopes of an element.
    • Includes the mass number in its name.
  • Example:
    • Carbon-14
    • Mass Number: 14
    • Atomic Number: 6
    • Application: Used for archeological dating.

Types of Radiation Emitted by Radioisotopes

  • Radioisotopes emit various types of radiation:
    • Alpha (α) particles:
    • Identical to a helium nucleus.
    • Beta (β) particles:
    • High-energy electrons.
    • Positrons (β+):
    • Positively charged counterparts of electrons.
    • Gamma (γ) rays:
    • Pure energy emitted as high-energy radiation.

Characteristics of Different Types of Particles

Alpha (α) Particles
  • Characteristics include:
    • Mass Number: 4
    • Charge: 2+
    • Contains 2 protons and 2 neutrons.
    • Compared to other radiation, alpha particles have low energy.
Beta (β) Particles
  • Characteristics include:
    • Mass Number: 0
    • Charge: 1− (negatively charged electron)
    • Forms in an unstable nucleus when a neutron converts into a proton and an electron.
Positrons (β+)
  • Characteristics include:
    • Mass Number: 0
    • Charge: 1+ (positively charged electron)
    • Forms in an unstable nucleus when a proton converts into a neutron and a positron.
Gamma (γ) Rays
  • Characteristics include:
    • Mass Number: 0
    • Charge: 0 (pure energy)
    • A form of energy emitted to achieve a more stable, lower-energy nucleus.

Radiation Protection

Properties of Radiation and Shielding Required


  • Table 5.3: Properties of Radiation

Type of RadiationTravel Distance in AirTissue DepthShieldingTypical Source
Alpha (α) Particle2 to 4 cm0.05 mmPaper, clothingRadium-226
Beta (β) Particle200 to 300 cm4 to 5 mmHeavy clothing, lab coats, glovesCarbon-14
Gamma (γ) Ray500 m50 cm or moreLead, thick concreteTechnetium-99m

Radioactive Decay

  • Radioactive decay is described as follows:
    • An unstable nucleus spontaneously breaks down by emitting radiation.
    • It is represented by a nuclear equation:
    • General form:
      ext{Radioactive nucleus}
      ightarrow ext{new nucleus} + ext{radiation (α, β, β+, γ)}

Balancing Nuclear Equations

  • In a balanced nuclear equation:
    • The sum of mass numbers on each side must be equal.
    • The sum of atomic numbers on each side must also be equal.
  • Example of balanced nuclear equation:
    • For curium-251:
    • 251 ext{Cf}
      ightarrow 247 ext{Cm} + 4 ext{He}
    • Mass numbers: 251=247+4251 = 247 + 4
    • Atomic numbers: 98=96+298 = 96 + 2

Example Problem: Beta Decay of Cobalt-60

  • Step 1: Write the incomplete nuclear equation:
    • Given Co-60, beta decay requires balancing mass and atomic numbers.
  • Step 2: Determine missing mass number:
    • 60=?+060 = ? + 0
    • ?=60? = 60
  • Step 3: Determine missing atomic number:
    • 27=?127 = ? - 1
    • ?=28? = 28
  • Step 4: Identify symbol of new nucleus:
    • Atomic number 28 corresponds to Nickel (Ni).
    • Complete nuclear equation:
    • ^{60}{27} ext{Co} ightarrow ^{60}{28} ext{Ni} + eta^-

Radiation Detection and Measurement

Geiger Counter
  • The Geiger counter is an instrument designed to:
    • Detect beta and gamma radiation.
    • Use ions produced by radiation to create an electrical current.
Units for Measuring Radiation Activity
  • Common units include:
    • Curie (Ci):
    • Defined as the number of disintegrations that occurs in 1 s for 1 g of radium, equal to 3.7imes1010extdisintegrations/s3.7 imes 10^{10} ext{ disintegrations/s}.
    • Becquerel (Bq):
    • The SI unit of radiation activity represented as 1 disintegration/s.
    • Rad (radiation absorbed dose):
    • Measures the amount of radiation absorbed by a gram of material.
    • Rem (radiation equivalent in humans):
    • Quantifies the biological effects of various types of radiation.
Equivalent Dose Calculation
  • To determine the equivalent dose in rems:
    • The equation is:
      extBiologicaldamage(rem)=extAbsorbeddose(rad)imesextFactorext{Biological damage (rem)} = ext{Absorbed dose (rad)} imes ext{Factor}
    • Factors for biological damage are:
    • For beta and gamma radiation: 1.
    • For high-energy protons and neutrons: about 10.
    • For alpha particles: 20.

Dosimeters

  • Used to measure radiation exposure for individuals working in radiation laboratories.
    • Types of radiation detected include:
    • X-rays
    • Gamma rays
    • Beta particles

Radiation Exposure Statistics

  • Average annual radiation exposure for a person in the U.S. is 3.6 mSv.
  • Sources of natural radiation exposure include:
    • Natural radioisotopes in:
    • Buildings
    • Food and water
    • Air
    • Notable source: Potassium-40 in potassium-rich foods.
  • Medical sources of radiation include X-rays and mammograms.

Effects of Radiation Exposure

  • Effects of radiation exposure based on dosage:
    • Less than 0.25 Sv often cannot be detected.
    • Whole body exposure of 1 Sv leads to a temporary reduction in white blood cells.
    • Exposure exceeding 1 Sv may induce radiation sickness:
    • Symptoms include nausea, vomiting, fatigue, and reduced white-cell counts.
    • An exposure of 5 Sv results in a 50% chance of death (LD50).

Half-Life of a Radioisotope

  • The half-life is defined as:
    • The time taken for the radiation level (activity) to decay to one-half of its original value.

Decay Curve

  • A decay curve graphically illustrates the decay of a radioactive isotope over time.
  • Example: For Iodine-131 with a half-life of 8 days, the decay curve shows that half of the sample decays while half remains radioactive.

Half-Life Equations

Example with Strontium-90
  • Given:
    • Strontium-90 has a half-life of 38.1 years.
    • Initial amount: 36 mg.
    • Find the remaining mass after 114.3 years.
  • Steps include:
    • 1. Analyze the number of half-lives:
    • extNumberofhalflives=114.3extyears38.1extyears/halflife=3ext{Number of half-lives} = \frac{114.3 ext{ years}}{38.1 ext{ years/half-life}} = 3
    • 2. Calculate remaining mass:
    • Remaining mass after 3 half-lives:
    • extRemainingmass=36extmg23=4.5extmgext{Remaining mass} = \frac{36 ext{ mg}}{2^3} = 4.5 ext{ mg} (approximate value)

Radiological Dating Techniques

Carbon Dating
  • Carbon-14 is used for dating ancient objects:
    • Produced via cosmic rays bombarding Nitrogen-14.
    • Reacts with oxygen to form radioactive carbon dioxide absorbed by living plants.
    • When the plant dies, carbon-14 uptake ceases; scientists can calculate time since death using its half-life (5730 years).

Medical Applications of Radioisotopes

  • Radioisotopes with short half-lives are favored in nuclear medicine because:
    • Body cells do not differentiate between radioactive and non-radioactive atoms, allowing targeted imaging.
  • Applications in imaging techniques include:
    • Thyroid scans using Iodine-131.
    • Positron Emission Tomography (PET) which uses short-lived positron emitters to study brain function.
    • Computed Tomography (CT) and MRI scans providing detailed organ images without radiation exposure (in the case of MRI).

Nuclear Reactions

Fission
  • In nuclear fission:
    • A large nucleus is bombarded by small particles (e.g., neutrons), causing it to split and release significant energy.
    • Example: Bombarding U-235 causes it to split into smaller nuclei such as Kr-91 and Ba-142.
Fusion
  • In nuclear fusion:
    • Smaller nuclei combine at extremely high temperatures (around 100,000,000 °C) to form larger nuclei, releasing large amounts of energy.
    • This process is continuous in stellar bodies like the Sun.