1. Chapter 7.2 – Half life Science 10

2. Types of decay Alpha Alpha

3. Types of decay Beta Beta

4. Types of decay Gamma Gamma

5. Ch 7.2 - Half-Life: the time it takes for half of a radioactive sample to decay the time it takes for half of a radioactive sample to decay –is a constant rate (always the same half life for each element) Example: Strontium-90 has a half-life of 29 years. If you have 10 g of strontium-90 today, there will be 5 g (half) remaining in 29 years. Terminology: Parent isotope: the original radioactive material Daughter isotope: the stable product that remains after decay has happened

6. Decay Curves: Show the rate of decay for radioactive elements Show the rate of decay for radioactive elements show the relationship between half-life and percentage of original substance remaining. show the relationship between half-life and percentage of original substance remaining.

7. Radioactive Dating: a method to determine age of objects a method to determine age of objects compares amount of parent isotope to daughter isotope. compares amount of parent isotope to daughter isotope. Example: Carbon dating measure the ratio of carbon-12 and carbon-14. –Stable carbon-12 and radioactive carbon-14 exist naturally in a constant ratio.  In nature, carbon-12 appears 98.9% of the time, while carbon-14 is very rare.

8. When an organism dies, carbon-14 stops being taken in and continues to slowly decay. When an organism dies, carbon-14 stops being taken in and continues to slowly decay. –Comparing the amounts of carbon-12 to carbon-14 is called radiocarbon dating and gives us an age for the object. –Radiocarbon dating only works for organisms less than 50,000 years old because the half-life of carbon-14 is 5730 years. (after 50,000 years, there isn’t enough C-14 left!)

9. There are many radioisotopes that can be used for dating

10. some elements require one step to decay, while others decay over many steps before reaching a stable daughter isotope. some elements require one step to decay, while others decay over many steps before reaching a stable daughter isotope. –Carbon-14 decays into nitrogen-14 in one step –Uranium-235 decays into lead-207 in fifteen steps. –Thorium-235 decays into lead-208 in ten steps.

11. The Potassium-40 Clock Radioisotopes with very long half-lives can help determine the age of very old things. Radioisotopes with very long half-lives can help determine the age of very old things. The potassium-40/argon-40 clock has a half-life of 1.3 billion years. The potassium-40/argon-40 clock has a half-life of 1.3 billion years. Argon-40 produced by the decay of potassium-40 becomes trapped in rock. Argon-40 produced by the decay of potassium-40 becomes trapped in rock. Ratio of potassium-40 : argon- 40 shows age of rock. Ratio of potassium-40 : argon- 40 shows age of rock.

12. Half-life Problems: 1. What mass of a 200g sample of carbon-14 remains after 22,920 years? 2. A rock has 420g of radioactive isotope. What percentage would remain after 5 half-lives?