A rock contains 0.697 mg of 206pb for every 1.000 mg of 238 U 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 238 U and 206pb is negligible, calculate the age of the rock. (For 238 U, t₁/2 = 4.5x 109 years.) yr
A rock contains 0.697 mg of 206pb for every 1.000 mg of 238 U 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 238 U and 206pb is negligible, calculate the age of the rock. (For 238 U, t₁/2 = 4.5x 109 years.) yr
Chemistry
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ISBN:9781305957404
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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Problem 1RQ: Define and explain the differences between the following terms. a. law and theory b. theory and...
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
Transcribed Image Text:A rock contains 0.697 mg of 206pb for every 1.000 mg of 238 U present. Assuming that no lead was originally present, that all the 206pb formed over the years has remained in the rock, and that the
t1/2
number of nuclides in intermediate stages of decay between 238U and 206pb is negligible, calculate the age of the rock. (For 238U,
4.5x10⁹
years.)
yr
=
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