Question: Paleoclimate. Climatologists can determine the past temperature of the earth by comparing the ratio of the isotope oxygen-18 to the isotope oxygen-16 in air trapped
Where m16 and m18 are the masses of the two oxygen isotopes,
(b) The measured masses of the two isotopes are 2.66 X 10-26 kg (16O) and 2.99 X 10-26 kg (18O). If the magnetic field is 0.050 T, what must be the accelerating potential V so that these two isotopes will be separated by 4.00 cm at the detector?
Vzev Vm0) (Vms- Vm6) Ar
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