FIGURE 30.16 235U decay series. Alpha decay reduces A by 4 and Z by 2. + Beta decay increases Z by 1. 239 235U 235 231 Some nuclei can undergo either a or B decay. 227 223 219 215 211 207 - 207 Pb is stable. 203 80 82 84 86 88 90 92 Atomic number, Z Mass number, A

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Chapter1: Units, Trigonometry. And Vectors
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235U decays to 207Pb via the decay series as shown. The first decay in the chain, that of 235U, has a halflife of 7.0 × 108 years. The subsequent decays are much more rapid, so we can take this as the half-life for the complete decay of 235U to 207Pb. Certain minerals exclude lead but not uranium from their crystal structure, so when the minerals form they have no lead, only uranium. As time goes on, the uranium decays to lead, so measuring the ratio of lead atoms to uranium atoms allows investigators to determine the ages of the minerals. If a sample of a mineral contains 3 atoms of 207Pb for every 1 atom of 235U, how many years ago was it formed?

FIGURE 30.16 235U decay series.
Alpha decay reduces A by 4 and Z by 2.
+ Beta decay increases Z by 1.
239
235U
235
231
Some nuclei can
undergo either
a or B decay.
227
223
219
215
211
207 -
207 Pb is stable.
203
80 82 84 86 88 90 92
Atomic number, Z
Mass number, A
Transcribed Image Text:FIGURE 30.16 235U decay series. Alpha decay reduces A by 4 and Z by 2. + Beta decay increases Z by 1. 239 235U 235 231 Some nuclei can undergo either a or B decay. 227 223 219 215 211 207 - 207 Pb is stable. 203 80 82 84 86 88 90 92 Atomic number, Z Mass number, A
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