half-life = 4.47 billion years
decay constant = 0.693 / half life
= 0.693 / 4.47 x 10^9
= 1.55 x 10^-10 year-1
moles of lead = 0.706 / 206
= 3.427 x 10^-3 umol
moles of U = 1.00 / 238
= 4.20 x 10^-3 umol
total moles of U initially = 0.0042 + 0.0034 = 0.00763 umol
k = 1/t ln (Ao / At)
1.55 x 10^-10 = 1 / t ln (0.00763 / 0.0042)
t = 3.85 x 10^9 years
age = 3.85 x 10^9 years
9 Question (1 point) See page 978 Uranium-lead (U-Pb) dating of geological samples is one of...
Uranium-lead (U-Pb) dating of geological samples is one of the oldest and most refined radiometric dating methods, able to determine ages of about 1 million years to over 4.5 billion years with precision in the 0.1–1% range. The U-Pb dating method relies on two separate decay chains, one of which is the uranium series from 238U to 206Pb, with a half-life of 4.47 billion years. Geologists unearth a sample of zircon that appears to be a closed system. They find...
Uranium-lead (U-Pb) dating of geological samples is one of the oldest and most refined radiometric dating methods, able to determine ages of about 1 million years to over 4.5 billion years with precision in the 0.1–1% range. The U-Pb dating method relies on two separate decay chains, one of which is the uranium series from 238U to 206Pb, with a half-life of 4.47 billion years. Geologists unearth a sample of zircon that appears to be a closed system. They find...