1 / 11

Section 10–2: Rates of Nuclear Decay

Section 10–2: Rates of Nuclear Decay. Physical Science. Objectives. Define half-life, and relate half-life to the age of a radioactive sample. Compare and contrast nuclear reaction rates with chemical reaction rates. Describe how radioisotopes are used to estimate the age of materials.

vivien-clemons
Download Presentation

Section 10–2: Rates of Nuclear Decay

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Section 10–2:Rates of Nuclear Decay Physical Science

  2. Objectives • Define half-life, and relate half-life to the age of a radioactive sample. • Compare and contrast nuclear reaction rates with chemical reaction rates. • Describe how radioisotopes are used to estimate the age of materials.

  3. Time Travelers • A common theory is that Native Americans crossed the Bering Strait (between Russia and Alaska) about 13,000 years ago. • A discovery of bones, tools, and charcoal in Cactus Hill, Virginia in the 1990s may be as old as 15,000 years and may lead archaeologists to believe some came by boat. • How do we know how old the bones are?

  4. Half-Life • A nuclear decay rate describes how fast nuclear changes take place in a radioactive substance. Every radioisotope decays at a specific rate that can be expressed as a half-life. • A half-life is the time required for one half of a sample of a radioisotope to decay.

  5. Half-Life • After one half-life, half of the atoms in a radioactive sample have decayed, while the other half remain unchanged. After two half-lives, half of the remaining half decays, leaving one quarter of the original sample unchanged. • Iodine-131 has a half-life of 8.07 days. After two half-lives, or 16.14 days, the fraction of iodine-131 remaining is one quarter.

  6. Half-Life • Half-lives can vary from fractions of a second to billions of years. Uranium-238 has a half-life of 4.5 billion years. That means in 4.5 billion years, there will only be half as much uranium-238 on Earth as there is today. Or, 4.5 billion years ago, there was twice as much uranium-238 on Earth as there is today. • Unlike chemical reaction rates, nuclear decay rates are constant. Regardless of temperature, pressure, or surface area, the half-lives are constant.

  7. Radioactive Dating • The Cactus Hill artifacts were dated using carbon-14 dating. Carbon-14 has a half-life of 5,730 years and beta decays to nitrogen-14. • In radiocarbon dating, the age of an object is determined by comparing the object’s carbon-14 levels with carbon-14 levels in the atmosphere.

  8. Radioactive Dating • For example, if the ratio of carbon-14 to carbon-12 in a fossil is half the ratio in the atmosphere, then the organism lived about 5730 years ago. • Because atmospheric carbon-14 levels can change over time, the calculated age of the fossil is not totally accurate. For more accuracy, scientist will compare carbon-14 levels in objects of known age, like trees.

  9. Radioactive Dating • Radioactive dating can be used to date any carbon-containing object less than 50,000 years old. Objects older than 50,000 years old contain too little carbon-14 to be measurable. • To measure objects thought to be older than this, scientists will use radioisotopes with longer half-lives, like potassium-40, uranium-235, and uranium-238.

  10. Vocabulary • Half-life

More Related