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3.2. Neptunium series

T

Fig. 8. Thorium series

a

he 4n + 1 chain of Np-237 are commonly called the "neptunium series." In this series, only two of the isotopes involved are found naturally, namely those of bismuth and thallium. A smoke detector containing an americium-241 ionization chamber accumulates a significant amount of neptunium-237 as its americium decays; the following elements are also present in it, at least transiently, as decay products of the neptunium: actinium, astatine, bismuth, francium, lead, polonium, protactinium, radium, thallium, thorium, and uranium. Since this series was only studied more recently, its nuclides do not have historic names. [2]

Fig. 9. Neptunium series

a

nuclide

decay mode

half-life (a=year)

energy released, MeV

product of decay

249Cf

α

351 a

5.813+.388

245Cm

245Cm

α

8500 a

5.362+.175

241Pu

241Pu

β

14.4 a

0.021

241Am

241Am

α

432.7 a

5.638

237Np

237Np

α

2.14·106 a

4.959

233Pa

233Pa

β

27.0 d

0.571

233U

233U

α

1.592·105 a

4.909

229Th

229Th

α

7340 a

5.168

225Ra

225Ra

β

14.9 d

0.36

225Ac

225Ac

α

10.0 d

5.935

221Fr

221Fr

α

4.8 min

6.3

217At

217At

α

32 ms

7.0

213Bi

213Bi

β 97.80% α 2.20%

46.5 min

1.423 5.87

213Po 209Tl

213Po

α

3.72 μs

8.536

209Pb

209Tl

β

2.2 min

3.99

209Pb

209Pb

β

3.25 h

0.644

209Bi

209Bi

α

1.9·1019 a

3.137

205Tl

205Tl

.

stable

.

.

3.3. Radium series (also known as uranium series)

T he 4n+2 chain of U-238 are commonly called the "radium series" (sometimes "uranium series"). Beginning with naturally occurring uranium-238, this series includes the following elements: astatine, bismuth, lead, polonium, protactinium, radium, radon, thallium, and thorium. All are present, at least transiently, in any natural uranium-containing sample, whether metal, compound, or mineral.

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