Radiometric Dating Continuation of Journal Entry #5.
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Transcript of Radiometric Dating Continuation of Journal Entry #5.
Radiometric Dating
Continuation of Journal Entry #5
Radiometric Dating
• A technique used to date materials such as rocks based upon a comparison between the observed abundance of a naturally occurring radioactive isotope and its decay products using known rates of decay.
• Some elements have isotopes that predictably decay over time to more stable forms
Types of radioactive decay
• Alpha decay – Isotope emits 2 n0 and 2 p+
• Beta decay – Isotope emits 1 e-
• Neutron decay – Isotope emits 1 n0
Common radioactive isotopes and their products
• C-14 N-14 (beta decay)
• K-40 Ar-40 (beta decay)
• U-235 Pb-207 (all three forms of decay)
Radioactive Half-life
• The rate at which an isotope decays can be precisely measured in the lab and have been found to occur at a constant, predicable rate.
• An isotopes half-life is the amount of time necessary for ½ of the original amount of the radioactive isotope to decay to the more stable form.
Commonly used half-lives
• C-14 = 5,730 years• U-235 = 704 million years• K-40 = 1.25 billion years
• Question: If I found a bone with 12.5% of the expected amount of C-14, approximately how old is the bone?
• Question: If I found a bone with 12.5% of the expected amount of C-14, approximately how old is the bone?
• Answer: 5,730 years x 3 half-lives = 17,190 yrs
U-235 decay
• The geologic processes that form uranium are very different than those that form lead. Therefore, any lead found in a rock containing uranium must have been formed by decay. A measurement of the ratio of the two will reveal how many half-lives have passed – and thus will determine the age of the fossil.
Say hello to your lab partner!
Analysis Question
• If I found a fossil sample with 12 m&m’s remaining from the original sample, how old would it be if m&mdium has a half-life of 4.7 million years?
• #2 – Explain how an evolutionary biologist would use radiometric dating, relative dating, and fossils to determine something about how species have changed over time.
• #3 – Personal thoughts and reflections