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Earth Systems

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A radioisotope is an unstable radioactive nucleus. Examples include: carbon-14. deuterium (hydrogen with 1 neutron) all elements with atomic numbers above 83 – PowerPoint PPT presentation

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Title: Earth Systems


1
Radioactive Isotopes
  • Earth Systems

2
Journal 8 9/11/2012
  • Describe what you think is meant by the term
    half-life. What does it represent? Why do you, as
    an Earth Science student, think you need to
    understand half-life?

3
Journal 9 9/12/2012
  • Use the above diagram to answer the questions.
  • What is the half-life of the represented isotope?
  • The original sample has 100 atoms. How many atoms
    are left after 2 half-lifes?
  • How long does it take the original sample to
    decrease to 25 atoms?

4
Radioactivity
  • Radioactivity is the spontaneous process that
    occurs when an unstable nucleus releases
    particles and/or energy to form a more stable
    nucleus.

5
Radioisotopes
  • A radioisotope is an unstable radioactive
    nucleus.
  • Examples include
  • carbon-14
  • deuterium (hydrogen with 1 neutron)
  • all elements with atomic numbers above 83

6
Radioactive Decay
  • Radioactive decay is the release of subatomic
    particles and/or energy by radioactive isotopes.
  • Alpha and beta decay result in transformed atom.
  • Gamma decay results in same atom with release of
    energy.

ALPHA DECAY
BETA DECAY
GAMMA DECAY
7
Half-life
  • Half-life is the time it takes for half of the
    radioactive particles in a radioactive nucleus to
    decay.
  • Example
  • If an original sample of carbon-14 has a mass of
    10 grams and its half-life is 5700 years, how
    many grams of carbon-14 would remain after one
    half-life?
  • ANSWER 5 grams

8
Radiometric Dating
  • Because the rate of radioactive decay is
    constant, scientists use it to determine the
    absolute age of any object in which radioactive
    decay occurs.
  • This method of using radioactive isotopes to date
    an object is called radiometric dating.

9
Radiocarbon Dating
  • The tissues of all living organisms contain small
    amounts of Carbon-14 (C-14).
  • C-14 decays but is replenished by the process of
    respiration.
  • When the organism dies, the respiration process
    ends so the amount of C-14 decreases.
  • Scientists can measure the amount of C-14 in
    organic material to determine how much time has
    passed since the organisms death.
  • This process is called radiocarbon dating.
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