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INTRODUCTION TO ABSOLUTE (RADIOMETRIC) DATING
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Learning Targets 4a) I can distinguish between absolute and relative dating. (DOK 1) 4b) I can define what an isotope is and describe how radioactive isotopes decay (DOK 1) 4e) I can identify and analyze key strengths and limitations of using radioactive decay in absolute dating. (DOK 1-2)
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ESSENTIAL QUESTION How do scientists use absolute dating to build a model of the Earth’s history?
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ABSOLUTE DATING
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Isotopes All atoms are isotopes!!! Number of protons stay the same Number of neutrons changes
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Isotopes Example: 14C and 12C Both have 6 protons, but 14C has 8 neutrons where 12C only has 6
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Radioactivity Some atoms are not stable
These atoms emit particles to achieve stability
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Radioactivity There are three types of particles emitted
Alpha particles Beta Particles Gamma Rays
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Alpha Particles Charge = +2 (2 protons)
Mass = 4 (2 protons + 2 neutrons) Large, easily stopped by paper © The Geological Society of America, 2003
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Beta Particles Charge = -1 Mass = negligible
Small, more penetrating particle, but still easily stopped
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Beta Particles Neutron decays Electron leaves nucleus
Atomic number goes up 1
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Gamma Rays Pure energy No change in atom
Very penetrating, but cause little damage
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ABSOLUTE (RADIOMETRIC) DATING
Based on decay rates of different atoms Rate of decay stated as half- life
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Half-life © The Geological Society of America, 2003 Time it takes for ½ of the radioactive atoms to decay into its daughter atoms
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Half-life Atoms used in geologic dating have long half-lives
Parent Daughter Half-life Uranium-238 Lead ,470 million years Uranium-235 Lead million years Potassium-40 Argon ,250 million years Rubidium-87 Strontium ,800 m. y. Carbon-14 Nitrogen-14 5,730 years
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Half life Scientists use both decay and production curves
© The Geological Society of America, 2003 Scientists use both decay and production curves
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Assigning Ages Using the proportion of daughter atom in a sample, its age can be determined
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Major Principle of Absolute dating
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CHECK FOR UNDERSTANDING
Explain the main concepts of how scientists use absolute (radiometric) dating to determine the age of objects.
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