Charcoal samples from Stonehenge in England wereburned in O2, and the resultant CO2 gas bubbled into asolution of Ca(OH)2 (limewater), resulting in the precipitationof CaCO3. The CaCO3 was removed by filtration anddried. A 788-mg sample of the CaCO3 had a radioactivityof 1.5x 10-2 Bq due to carbon-14. By comparison, livingorganisms undergo 15.3 disintegrations per minute pergram of carbon. Using the half-life of carbon-14, 5700 yr,calculate the age of the charcoal sample.
Charcoal samples from Stonehenge in England wereburned in O2, and the resultant CO2 gas bubbled into asolution of Ca(OH)2 (limewater), resulting in the precipitationof CaCO3. The CaCO3 was removed by filtration anddried. A 788-mg sample of the CaCO3 had a radioactivityof 1.5x 10-2 Bq due to carbon-14. By comparison, livingorganisms undergo 15.3 disintegrations per minute pergram of carbon. Using the half-life of carbon-14, 5700 yr,calculate the age of the charcoal sample.
Materials Science And Engineering Properties
1st Edition
ISBN:9781111988609
Author:Charles Gilmore
Publisher:Charles Gilmore
Chapter5: Phase Transformations And Phase Diagrams
Section: Chapter Questions
Problem 5.19P
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Question
Charcoal samples from Stonehenge in England were
burned in O2, and the resultant CO2 gas bubbled into a
solution of Ca(OH)2 (limewater), resulting in the precipitation
of CaCO3. The CaCO3 was removed by filtration and
dried. A 788-mg sample of the CaCO3 had a radioactivity
of 1.5x 10-2 Bq due to carbon-14. By comparison, living
organisms undergo 15.3 disintegrations per minute per
gram of carbon. Using the half-life of carbon-14, 5700 yr,
calculate the age of the charcoal sample.
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