A rock contains 0.617 mg of 206Pb for every 1.000 mg of 238U present. Assuming that no lead was originally present, that all the 206Pb formed over the years has remained in the rock, and that the number of nuclides in intermediate stages of decay between 238U and 206 Pb is negligible, calculate the age of the rock. (For 238U, t1/2 = 4.5 X 109 years.)
A rock contains 0.617 mg of 206Pb for every 1.000 mg of 238U present. Assuming that no lead was originally present, that all the 206Pb formed over the years has remained in the rock, and that the number of nuclides in intermediate stages of decay between 238U and 206 Pb is negligible, calculate the age of the rock. (For 238U, t1/2 = 4.5 X 109 years.)
Chemistry
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Author:Steven S. Zumdahl, Susan A. Zumdahl, Donald J. DeCoste
Publisher:Steven S. Zumdahl, Susan A. Zumdahl, Donald J. DeCoste
Chapter1: Chemical Foundations
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
Transcribed Image Text:A rock contains 0.617 mg of 206Pb for every
1.000 mg of 238U present. Assuming that no
lead was originally present, that all the 206Pb
formed over the years has remained in the rock,
and that the number of nuclides in intermediate
stages of decay between 238U and 206 Pb is
negligible, calculate the age of the rock. (For
238U, t1/2 = 4.5 X 109 years.)
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