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Published byLee Jayson O’Connor’ Modified over 6 years ago
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I. Absolute Dating A. The process of establishing the age of an object (fossil or rock layer) by determining how long it existed.
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II. Radioactive Decay The process by which radioactive isotopes break down into stable isotopes Isotopes – atoms of the same element with the same number of protons but a different number of neutrons
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III. Isotopes of Carbon Isotopes of Carbon Protons + Neutrons
Atomic Number & Stability C12 6 P + 6 N 12 and stable C13 6 P + 7 N 13 and unstable C14 6 P + 8 N 14 and unstable
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IV. HALF LIFE A. The time it takes for ½ of a radioactive sample to decay into a stable sample
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V. Half-life of an artifact containing Carbon-14
Half-life number Fraction of C14 left Age of artifact 1 1/2 5,730 2 1/4 11,460 3 1/8 17,190 4 1/16 22,920
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Parent to daughter material
VI. Radiometric Dating – Determining the absolute age of an artifact by comparing the ratios of parent material and daughter material Parent to daughter material Unstable to stable Half Life Time Uranium-238 to Lead-206 4.5 billion years Potassium-40 to Argon-40 1.3 billion years Carbon-14 to Nitrogen-14 5,730 years
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MICHIGAN’S STATE FOSSIL
ICEMAN CABON 14 Dating is only good for objects that are less than 50,000 years old MICHIGAN’S STATE FOSSIL MASTODON
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Uranium to Lead Method 10 million years and greater
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Half Life Problems Parent Material AGE OF SPECIMEN
1/8 of Potassium left = 1/2 – 1/4 - 1/8 - 1/16 ¼ of Uranium left = 3 x 1.3 = 3.9 Billion 2 x 4.5 = 9 Billion
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Amount of parent material (half-life # x decay time)
Half-Life Problems Amount of parent material Age of artifact (half-life # x decay time) 1/8 of Carbon-14 left (How many half-life cycles have occurred?) 3 X 5,730 ys = 17,190 years grams of Carbon-14. How much would be left after 4 half-life cycles? 20/2 = 10/2=5/2=2.5/2=1.25 grams
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Radioactive Decay Simulations
Radioactive Decay Simulations
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