Half-Life
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The half-life of a radioactive isotope is the amount of time it takes for the isotope to decay so that only half of the original amount of the isotope remains. Half-lives can be measured from smaller than a millionth of a second to more than trillions of years. The shorter the half-life, the more radioactive an isotope is.[1]
Tables
Fraction remaining per half-life elapsed
Half-lives elapsed |
Fraction remaining |
Percentage of nuclei without disintegrating | |
---|---|---|---|
0 | 1/1 | 100 % | |
1 | 1/2 | 50 % | |
2 | 1/4 | 25 % | |
3 | 1/8 | 12.5 % | |
4 | 1/16 | 6.25 % | |
5 | 1/32 | 3.125 % | |
6 | 1/64 | 1.562 % | |
7 | 1/128 | 0.781 % | |
... | ... | ... | |
n | 1/2n | 100/(2n) |
Half-life of some radionuclides
Uranium-235 | 7,038·108 years | Uranium-238 | 4,468·109 years | Potassium-40 | 1,28·109 years |
Rubidium-87 | 4,88·1010 years | Calcium-41 | 1,03·105 years | Carbon-14 | 5760 years |
Radium-226 | 1620 years | Cesium-137 | 30,07 years | Bismuth-207 | 31,55 years |
Strontium-90 | 28,90 years | Cobalt-60 | 5,271 years | Cadmium-109 | 462,6 days |
Iodine-131 | 8,02 days | Radon-222 | 3,82 days | Oxygen-15 | 122 seconds |
References
- ↑ Chemistry:Precision and Design; Verne Biddle and Gregory Parker; p. 395; A Beka Book