In nuclear physics, ββ decay is a type of radioactive decay in which a ββ particle (an electron or a positron) is emitted. In the case of electron emission, it is referred to as beta minus (ββ-), while in the case of a positron emission as beta plus (ββ+).
An electron and positron have identical physical characteristics except for opposite charge.
In certain types of radioactive nuclei that have too many neutrons, a neutron may be converted into a proton, an electron and another particle called a neutrino. The high energy electrons that are released in this way are the ββ - particles. This process can occur for an isolated neutron.
In ββ+ decay, energy is used to convert a proton into a neutron(n), a
positron (e+) and a neutrino (ννe):
energy
+
p
→
n
+
e
+
+
ν
e
energy
+
p
→
n
+
e
+
+
ν
e
(1)So, unlike ββ-, ββ+ decay cannot occur in isolation, because it requires energy, the mass of the neutron being greater than the mass of the
proton. ββ+ decay can only happen inside nuclei when the value of the binding energy of the mother nucleus is less than that of the daughter
nucleus. The difference between these energies goes into the reaction of
converting a proton into a neutron, a positron and a neutrino and into
the kinetic energy of these particles.
The diagram below shows what happens during β-β- decay:
During beta decay, the number of neutrons in the atom decreases by one, and the number of protons increases by one. Since the number of protons before and after the decay is different, the atom has changed into a different element. In Figure 4, Hydrogen has become Helium. The beta decay of the Hydrogen-3 atom can be represented as follows:
1
3
H
→
2
3
He
+
β
particle
+
ν
¯
1
3
H
→
2
3
He
+
β
particle
+
ν
¯
When scientists added up all the energy from the neutrons, protons and electrons involved in
ββ-decays, they noticed that there was always some energy missing. We know that energy is always conserved, which led Wolfgang Pauli in 1930 to come up with the idea that another particle, which was not detected yet, also had to be involved in the decay. He called this particle the neutrino (Italian for "little neutral one"), because he knew it had to be neutral, have little or no mass, and interact only very weakly, making it very hard to find experimentally! The neutrino was finally identified experimentally about 25 years after Pauli first thought of it.
Due to the radioactive processes inside the sun, each 1 cm2cm2 patch of the earth receives 70 billion (70×109×109) neutrinos each second! Luckily neutrinos only interact very weakly so they do not harm our bodies when billions of them pass through us every second.
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