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Decay energy

physical science Maturity 11-13 Next article →

Decay energy describes the energy change during radioactive decay. This process occurs when an unstable atomic nucleus loses energy. To stabilize itself, the nucleus emits ionizing particles or radiation. This transformation changes the original atom into a new type. Scientists call the starting atom the parent nuclide. The resulting atom is known as the daughter nuclide. This energy change is often represented by the symbol Q.

The mechanism of decay energy relies on a change in mass. The decay energy is equal to the mass difference between the parent and the daughter products. This mass difference is denoted as delta m. This difference in mass is converted directly into the energy of radiation, or E. Scientists measure this energy using specific units. These units are typically megaelectronvolts (MeV) or kiloelectronvolts (keV).

There are several distinct types of radioactive decay. In alpha decay, the nucleus releases an alpha particle. Beta decay is another common process. During beta decay, the energy is divided between an emitted electron and a neutrino. A neutrino is a tiny particle emitted at the same time as the electron. Some decays also release gamma rays. These are high-energy rays that carry away energy.

Scientists can calculate the radiation power, or P, of a substance. This calculation involves the radioactive activity, which is the number of transforming atoms per unit of time. It also uses the molar mass, or M, of the substance. The radiation power tells us how much energy is released over time. Different isotopes show very different levels of power. For example, Polonium-210 has a high radiation power of 140 W/g. In contrast, Radium-226 has a much lower power of only 0.02 W/g.

One specific example involves the isotope Cobalt-60. Cobalt-60 decays into Nickel-60. The mass difference in this process results in radiated energy of approximately 2.8 MeV. Cobalt-60 has a radiation power of 17.9 W/g. It also has a half-life, or the time for half the atoms to decay, of 5.27 years. This specific isotope is useful for food irradiation. However, it is not ideal for certain long-term power uses.

Engineers use decay energy to create radioisotope thermoelectric generators, or RTGs. These are devices that turn nuclear decay into electricity. For an RTG, scientists look for specific qualities. They want high decay energy combined with a long half-life. They also prefer sources that do not emit strong gamma radiation. This preference helps reduce the weight and cost of radiation shielding. Plutonium-238 is an excellent choice for RTGs. It has a long half-life of roughly eighty years and low gamma emissions.

Other isotopes have been used in RTGs with different results. Strontium-90 was used widely in the 20th century for remote locations. It is a high-yield product of nuclear fission. It is also easy to extract chemically from other fission products. However, Strontium-90 performs worse than Plutonium-238 on most measures. It has a shorter life and is a beta emitter. It also releases significant gamma radiation when its daughter nuclide decays. This makes it harder to shield than alpha emitters.

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