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.