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Beta Decay

Beta decay is a type of radioactive decay in which a beta particle (either an electron or a positron) is emitted from an atomic nucleus. This process allows the atom to move closer to a stable configuration. Beta decay is classified into two types based on the particle emitted: beta-minus (β⁻) decay and beta-plus (β⁺) decay. Here are some key points about each type:

- In beta-minus decay, a neutron in the nucleus is transformed into a proton.

- This process emits a beta particle, which is an electron, and an antineutrino.

- The atomic number of the element increases by one (due to the additional proton), but the mass number remains the same.

- An example is the decay of carbon-14 (⁶C¹⁴) into nitrogen-14 (⁷N¹⁴).

- In beta-plus decay, a proton in the nucleus is converted into a neutron.

- This process emits a positron (the antimatter counterpart of an electron) and a neutrino.

- The atomic number decreases by one, but the mass number remains unchanged.

- An example is the decay of carbon-11 (⁶C¹¹) into boron-11 (⁵B¹¹).

- In medicine, beta-plus decay is the basis for positron emission tomography (PET) scans.

- In archaeology and geology, beta-minus decay of carbon-14 is used in radiocarbon dating.

Understanding beta decay is important in nuclear physics, nuclear chemistry, and various applied fields like medical imaging and radiometric dating. It provides insight into the stability of atomic nuclei and the transmutation of elements.

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