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helium-4

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helium-4
Background#c0c0ff
CaptionA schematic representation of the helium-4 nucleus, containing two protons and two neutrons.
Abundance~99.99986% of helium
HalflifeStable
Spin0+
Excess energy2424.91565(9) keV
Binding energy28295.673(12) keV
Parent3H
Parent decayβ<sup>−</sup>
Parent mass3.0160492
Parent24Li
Parent mass24.02719
Parent34Be
Parent mass34.03587

helium-4 is the most common and stable isotope of the element helium, constituting nearly all naturally occurring helium. Its nucleus, the alpha particle, is exceptionally stable and is a fundamental product of both nuclear fusion in stars and radioactive decay processes on Earth. This isotope's unique quantum mechanical properties, such as superfluidity at temperatures near absolute zero, make it a critical substance for studying condensed matter physics and cosmology.

Properties

The nucleus of helium-4, known as an alpha particle, consists of two protons and two neutrons, giving it a mass number of four and a doubly magic configuration that results in extraordinary binding energy and stability. This isotope remains a liquid down to absolute zero under standard pressure, a consequence of its large zero-point energy and weak intermolecular forces described by the Lennard-Jones potential. Upon cooling below 2.17 kelvins, it undergoes a phase transition to a superfluid state, known as Helium II, exhibiting properties like zero viscosity and extremely high thermal conductivity, phenomena first extensively studied by Pyotr Kapitsa and John F. Allen. Its spin of zero makes it a boson, obeying Bose–Einstein statistics, which is fundamental to its superfluid behavior and its role in Bose–Einstein condensate research pioneered by Satendra Nath Bose and Albert Einstein.

Natural abundance and production

Helium-4 is overwhelmingly the most abundant helium isotope in the universe, formed primarily through nucleosynthesis during the Big Bang and later within stellar cores via the proton–proton chain and the CNO cycle in main sequence stars like the Sun. On Earth, the majority is generated from the alpha decay of heavy radioactive elements such as uranium and thorium found in the Earth's crust, accumulating in natural gas deposits, notably in the Hugoton Field in the United States and the Qatari North Field. Industrial production involves the fractional distillation of cryogenically cooled natural gas, a process commercialized following discoveries by the United States Bureau of Mines. Significant reserves are managed by entities like the United States Department of the Interior and the QatarEnergy company.

Applications

Liquid helium-4 is indispensable as a cryogen for cooling the superconducting magnets used in magnetic resonance imaging scanners, particle accelerators like the Large Hadron Collider at CERN, and nuclear magnetic resonance spectrometers. Its superfluid phase is crucial for specialized scientific applications, including cryogenics research, creating ultra-low temperature environments in dilution refrigerators, and experiments in quantum hydrodynamics. The gas is also used for purging and pressurizing rocket fuel tanks in programs like those of NASA and the European Space Agency, and as a protective shielding gas in arc welding processes such as gas tungsten arc welding for sensitive materials.

Role in physics and cosmology

Helium-4 is a cornerstone for understanding fundamental physical processes; its formation in the first few minutes of the universe, as described by Big Bang nucleosynthesis, provides a critical test for the Big Bang theory and estimates of baryon density. The study of superfluid helium-4 has led to profound insights into macroscopic quantum phenomena, topological defects like quantized vortex lines, and the application of the two-fluid model developed by Lev Landau and László Tisza. In astrophysics, the helium flash in red giant stars and the role of alpha particles in stellar evolution are key areas of research conducted at observatories like the Hubble Space Telescope and institutions such as the Max Planck Institute for Astrophysics.

Isotopic differences and helium-3

The lighter isotope helium-3, with one neutron, exhibits markedly different quantum statistical behavior as a fermion obeying Fermi–Dirac statistics, leading to distinct superfluid properties at much lower temperatures near 0.0025 K. While helium-4 is common, helium-3 is exceedingly rare on Earth, primarily originating from the beta decay of tritium produced in nuclear reactors and atmospheric testing of thermonuclear weapons during the Cold War. The dramatic difference in their superfluidity mechanisms—arising from Cooper pairing in helium-3 versus Bose–Einstein condensation in helium-4—makes comparative studies vital for condensed matter physics, with pioneering work by David Lee, Douglas D. Osheroff, and Robert Coleman Richardson earning the Nobel Prize in Physics. The mixture of the two isotopes enables the operation of the dilution refrigerator, an essential tool for achieving millikelvin temperatures in laboratories like the National Institute of Standards and Technology.

Category:Helium Category:Isotopes Category:Nuclear physics