Suppose you have a one-gram sample of iridium-182, which undergoes beta decay to form osmium-182. The half-life of iridium-182 is 15 minutes. After 45 minutes, how much iridium-182 will remain in the sample? To solve this problem, you first need to calculate how many half-lives will elapse during the total time of decay.

Half-lives elapsed=Total time of decayHalf-life=45min15min=3

After three half-lives, the amount of iridium-182 has been reduced by half three times.

12×12×12=18

So after 45 minutes, 18×1 gram, or 0.125 gram, of iridium-182 remains while 0.875 gram of the sample has decayed into osmium-182.

Radioactive Dating

Now suppose you have a sample that was originally iridium-182, but three quarters of it have since decayed into osmium-182. Based on the fraction of iridium-182 left (one quarter), you can calculate the age of the sample to be two half-lives, or 30 minutes old.

The artifacts from Cactus Hill were dated by measuring levels of carbon-14, which has a half-life of 5730 years. Carbon-14 is formed in the upper atmosphere when neutrons produced by cosmic rays collide with nitrogen-14 atoms. The radioactive carbon-14 undergoes beta decay to form nitrogen-14.

C614N714+e-10


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Table of Contents

Physical Science CHAPTER 1 Science Skills CHAPTER 2 Properties of Matter CHAPTER 3 States of Matter CHAPTER 4 Atomic Structure CHAPTER 5 The Periodic Table CHAPTER 6 Chemical Bonds CHAPTER 7 Chemical Reactions CHAPTER 8 Solutions, Acids, and Bases CHAPTER 9 Carbon Chemistry CHAPTER 10 Nuclear Chemistry CHAPTER 11 Motion CHAPTER 12 Forces and Motion CHAPTER 13 Forces in Fluids CHAPTER 14 Work, Power, and Machines CHAPTER 15 Energy CHAPTER 16 Thermal Energy and Heat CHAPTER 17 Mechanical Waves and Sound CHAPTER 18 The Electromagnetic Spectrum and Light CHAPTER 19 Optics CHAPTER 20 Electricity CHAPTER 21 Magnetism CHAPTER 22 Earth's Interior CHAPTER 23 Earth's Surface CHAPTER 24 Weather and Climate CHAPTER 25 The Solar System CHAPTER 26 Exploring the Universe Skills and Reference Handbook