Understanding Radioactive Decay and Half-Life

Aug 14, 2024

Lecture on Radioactive Decay and Half-Life

Introduction to Radioactive Decay

  • Atoms and isotopes can experience radioactive decay, turning into other atoms or releasing particles.
  • Types of decay include:
    • Beta decay: Electrons are released, turning neutrons into protons.
    • Positron emission: Protons are turned into neutrons.

Understanding Moles and Atomic Mass

  • Moles: A mole of carbon-12 weighs 12 grams and contains $6.02 \times 10^{23}$ atoms.
  • This is a huge number, illustrating the large amount of atoms even in small masses.

Probability of Decay

  • At any moment, isotopes have a probability of decaying, but the exact timing is unknown.
  • Decay is probabilistic due to the unknown state of the nucleus.
  • On a macro level, terms like "half-life" help understand decay over large numbers of atoms.

Concept of Half-Life

  • Half-Life: Time it takes for half of a sample of a radioactive isotope to decay.
  • Example: Carbon-14 decays to nitrogen-14 with a half-life of 5,740 years.
  • After one half-life, half of the atoms have decayed, but it's probabilistic which atoms decay.

Example with Carbon-14

  • Initial state: Start with 10 grams of carbon-14.
  • After one half-life (5,740 years):
    • 5 grams of C-14 remain, 5 grams decay to N-14.
  • After two half-lives:
    • 2.5 grams of C-14 remain, 7.5 grams of N-14.

Understanding Decay on a Micro Level

  • For a single carbon atom, decay probability over time varies:
    • After 1 second: Likely still carbon.
    • After 1 billion years: Likely decayed to nitrogen-14, but not guaranteed.

Calculating Time Passed Based on Remaining Sample

  • Example:
    • Start with 80 grams of a substance with a 2-year half-life.
    • After 2 years: 40 grams left.
    • After 4 years: 20 grams left.
    • After 6 years: 10 grams left.
    • Three half-lives have passed to get from 80 grams to 10 grams.

Key Formula

  • Use $\frac{1}{2}^{n}$ to determine remaining fraction of sample after n half-lives.
  • Example: After three half-lives, 1/8 of the original sample remains.

Conclusion

  • Understanding half-life helps predict decay in large samples, but individual atom decay remains probabilistic.

Note: Future lectures might address how to calculate decay for non-discrete times, such as exactly 10 days or 2.5 years.