Helium-4
Encyclopedia : H : HE : HEL : Helium-4
Helium-4 is a non-radioactive and light isotope of helium. It is by far the most abundant of the two naturally-occurring isotopes of helium, making up about 99.99986% of the helium on earth. Its nucleus is an alpha particle, having two protons and two neutrons. Since the alpha decay is a common decay mode for many radioactive isotopes, this probably explains its abundance. In fact, alpha decay of heavy elements is the source of most naturally occurring helium-4 on earth.
When helium-4 is cooled to below 2.17 kelvin (-271 °C), it becomes a superfluid, with properties that are very unlike those of an ordinary liquid. For example, if helium-4 is kept in an open vessel, a thin film will climb up the sides of the vessel and overflow. This strange behaviour is a result of the Clausius-Clapeyron relation and cannot be explained by the current model of classical mechanics nor by nuclear or electrical models.
|- style="text-align: center;"
| width="30%" | Helium-3
| width="40%" | Isotopes of Helium
| width="30%" | Helium-5
|- style="text-align: center;"
| Produced from:
Lithium-5 (p)
Helium-5 (n)
Beryllium-6 (2p)'''
| Decay chain
| Decays to:
Stable
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