Geologists can estimate the age of rocks by their uranium-238 (U-238) content. The uranium is incorporated in the rocks as it hardens and then decays with first-order kinetics and a half-life of 4.5 billion years. 33.6% of U-238 in the rock was decayed. How old (billion years, 1 billion years+ 10^9 years) is the rock?
Geologists can estimate the age of rocks by their uranium-238 (U-238) content. The uranium is incorporated in the rocks as it hardens and then decays with first-order kinetics and a half-life of 4.5 billion years. 33.6% of U-238 in the rock was decayed. How old (billion years, 1 billion years+ 10^9 years) is the rock?
Chemistry for Engineering Students
4th Edition
ISBN:9781337398909
Author:Lawrence S. Brown, Tom Holme
Publisher:Lawrence S. Brown, Tom Holme
Chapter11: Chemical Kinetics
Section: Chapter Questions
Problem 11.40PAE: In Exercise 11.39, if the initial concentration of N2Oj is 0.100 .\1. how long will it take for the...
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Geologists can estimate the age of rocks by their uranium-238 (U-238) content. The uranium is incorporated in the rocks as it hardens and then decays with first-order kinetics and a half-life of 4.5 billion years. 33.6% of U-238 in the rock was decayed. How old (billion years, 1 billion years+ 10^9 years) is the rock?
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