Helium
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Helium | |||||||||||||||||||||
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Pronunciation | /ˈhiːliəm/ | ||||||||||||||||||||
Appearance | colorless gas, exhibiting a gray, cloudy glow (or reddish-orange if an especially high voltage is used) when placed in an electric field | ||||||||||||||||||||
Standard atomic weight Ar°(He) | |||||||||||||||||||||
Helium in the periodic table | |||||||||||||||||||||
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kJ/mol | |||||||||||||||||||||
Heat of vaporization | 0.0829 kJ/mol | ||||||||||||||||||||
Molar heat capacity | 20.78 J/(mol·K)[3] | ||||||||||||||||||||
Vapor pressure (defined by ITS-90)
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Atomic properties | |||||||||||||||||||||
Oxidation states | common: (none) 0 Discovery Norman Lockyer (1868) | | |||||||||||||||||||
First isolation | William Ramsay, Per Teodor Cleve, Abraham Langlet (1895) | ||||||||||||||||||||
Isotopes of helium | |||||||||||||||||||||
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Helium (from
Helium was first detected as an unknown, yellow
Liquid helium is used in
On Earth, it is relatively rare—5.2
History
Scientific discoveries
The first evidence of helium was observed on August 18, 1868, as a bright yellow line with a

In 1881, Italian physicist Luigi Palmieri detected helium on Earth for the first time through its D3 spectral line, when he analyzed a material that had been sublimated during a recent eruption of Mount Vesuvius.[34]


On March 26, 1895, Scottish chemist
In 1907,
In 1913,
In 1938, Russian physicist
In 1961, Vignos and Fairbank reported the existence of a different phase of solid helium-4, designated the gamma-phase. It exists for a narrow range of pressure between 1.45 and 1.78 K.[67]
Extraction and use
![]() | The examples and perspective in this section may not represent a worldwide view of the subject. (February 2022) |

After an oil drilling operation in 1903 in
Following a suggestion by Sir
Although the extraction process using low-temperature
The
After the Helium Acts Amendments of 1960 (Public Law 86–777), the U.S. Bureau of Mines arranged for five private plants to recover helium from natural gas. For this helium conservation program, the Bureau built a 425-mile (684 km) pipeline from Bushton, Kansas, to connect those plants with the government's partially depleted Cliffside gas field near Amarillo, Texas. This helium-nitrogen mixture was injected and stored in the Cliffside gas field until needed, at which time it was further purified.[75]
By 1995, a billion cubic meters of the gas had been collected and the reserve was US$1.4 billion in debt, prompting the
Helium produced between 1930 and 1945 was about 98.3% pure (2% nitrogen), which was adequate for airships. In 1945, a small amount of 99.9% helium was produced for welding use. By 1949, commercial quantities of Grade A 99.95% helium were available.[79]
For many years, the United States produced more than 90% of commercially usable helium in the world, while extraction plants in Canada, Poland, Russia, and other nations produced the remainder. In the mid-1990s, a new plant in Arzew, Algeria, producing 17 million cubic metres (600 million cubic feet) began operation, with enough production to cover all of Europe's demand. Meanwhile, by 2000, the consumption of helium within the U.S. had risen to more than 15 million kg per year.[80] In 2004–2006, additional plants in Ras Laffan, Qatar, and Skikda, Algeria were built. Algeria quickly became the second leading producer of helium.[81] Through this time, both helium consumption and the costs of producing helium increased.[82] From 2002 to 2007 helium prices doubled.[83]
As of 2012[update], the
In 2013, Qatar started up the world's largest helium unit,
Characteristics
Atom
In quantum mechanics
In the perspective of
Related stability of the helium-4 nucleus and electron shell
The nucleus of the helium-4 atom is identical with an
For example, the stability and low energy of the electron cloud state in helium accounts for the element's chemical inertness, and also the lack of interaction of helium atoms with each other, producing the lowest melting and boiling points of all the elements. In a similar way, the particular energetic stability of the helium-4 nucleus, produced by similar effects, accounts for the ease of helium-4 production in atomic reactions that involve either heavy-particle emission or fusion. Some stable helium-3 (two protons and one neutron) is produced in fusion reactions from hydrogen, though its estimated abundance in the universe is about 10−5 relative to helium-4.[92]

The unusual stability of the helium-4 nucleus is also important
All heavier elements (including those necessary for rocky planets like the Earth, and for carbon-based or other life) have thus been created since the Big Bang in stars which were hot enough to fuse helium itself. All elements other than hydrogen and helium today account for only 2% of the mass of atomic matter in the universe. Helium-4, by contrast, comprises about 24% of the mass of the universe's ordinary matter—nearly all the ordinary matter that is not hydrogen.[92][94]
Gas and plasma phases

Helium is the second least reactive noble gas after
Helium is the least water-
Most extraterrestrial helium is plasma in stars, with properties quite different from those of atomic helium. In a plasma, helium's electrons are not bound to its nucleus, resulting in very high electrical conductivity, even when the gas is only partially ionized. The charged particles are highly influenced by magnetic and electric fields. For example, in the solar wind together with ionized hydrogen, the particles interact with the Earth's magnetosphere, giving rise to Birkeland currents and the aurora.[99]
Liquid phase

Helium liquifies when cooled below 4.2 K at atmospheric pressure. Unlike any other element, however, helium remains liquid down to a temperature of
Helium I
Below its
Helium I has a gas-like
Helium II
Liquid helium below its lambda point (called helium II) exhibits very unusual characteristics. Due to its high

Helium II is a superfluid, a quantum mechanical state of matter with strange properties. For example, when it flows through capillaries as thin as 10 to 100 nm it has no measurable viscosity.[28] However, when measurements were done between two moving discs, a viscosity comparable to that of gaseous helium was observed. Existing theory explains this using the two-fluid model for helium II. In this model, liquid helium below the lambda point is viewed as containing a proportion of helium atoms in a ground state, which are superfluid and flow with exactly zero viscosity, and a proportion of helium atoms in an excited state, which behave more like an ordinary fluid.[101]
In the fountain effect, a chamber is constructed which is connected to a reservoir of helium II by a sintered disc through which superfluid helium leaks easily but through which non-superfluid helium cannot pass. If the interior of the container is heated, the superfluid helium changes to non-superfluid helium. In order to maintain the equilibrium fraction of superfluid helium, superfluid helium leaks through and increases the pressure, causing liquid to fountain out of the container.[102]
The thermal conductivity of helium II is greater than that of any other known substance, a million times that of helium I and several hundred times that of
Helium II also exhibits a creeping effect. When a surface extends past the level of helium II, the helium II moves along the surface, against the force of
Solid phases
Helium remains liquid down to
Helium-4 and helium-3 both form several crystalline solid phases, all requiring at least 25 bar. They both form an α phase, which has a hexagonal close-packed (hcp) crystal structure, a β phase, which is face-centered cubic (fcc), and a γ phase, which is body-centered cubic (bcc).[112]
Isotopes
There are nine known
He for every million that are 4
He.[28] Unlike most elements, helium's isotopic abundance varies greatly by origin, due to the different formation processes. The most common isotope, helium-4, is produced on Earth by alpha decay of heavier radioactive elements; the alpha particles that emerge are fully ionized helium-4 nuclei. Helium-4 is an unusually stable nucleus because its nucleons are arranged into complete shells. It was also formed in enormous quantities during Big Bang nucleosynthesis.[113]
Helium-3 is present on Earth only in trace amounts. Most of it has been present since Earth's formation, though some falls to Earth trapped in
Liquid helium-4 can be cooled to about 1 K (−272.15 °C; −457.87 °F) using
It is possible to produce
Properties
Table of thermal and physical properties of helium gas at atmospheric pressure:[121][122]
Temperature (K) | Density (kg/m^3) | Specific heat (kJ/kg °C)
|
Dynamic viscosity (kg/m s)
|
Kinematic viscosity (m^2/s)
|
Thermal conductivity (W/m °C)
|
Thermal diffusivity (m^2/s) | Prandtl number |
100 | 5.193 | 9.63E-06 | 1.98E-05 | 0.073 | 2.89E-05 | 0.686 | |
120 | 0.406 | 5.193 | 1.07E-05 | 2.64E-05 | 0.0819 | 3.88E-05 | 0.679 |
144 | 0.3379 | 5.193 | 1.26E-05 | 3.71E-05 | 0.0928 | 5.28E-05 | 0.7 |
200 | 0.2435 | 5.193 | 1.57E-05 | 6.44E-05 | 0.1177 | 9.29E-05 | 0.69 |
255 | 0.1906 | 5.193 | 1.82E-05 | 9.55E-05 | 0.1357 | 1.37E-04 | 0.7 |
366 | 0.1328 | 5.193 | 2.31E-05 | 1.74E-04 | 0.1691 | 2.45E-04 | 0.71 |
477 | 0.10204 | 5.193 | 2.75E-05 | 2.69E-04 | 0.197 | 3.72E-04 | 0.72 |
589 | 0.08282 | 5.193 | 3.11E-05 | 3.76E-04 | 0.225 | 5.22E-04 | 0.72 |
700 | 0.07032 | 5.193 | 3.48E-05 | 4.94E-04 | 0.251 | 6.66E-04 | 0.72 |
800 | 0.06023 | 5.193 | 3.82E-05 | 6.34E-04 | 0.275 | 8.77E-04 | 0.72 |
900 | 0.05451 | 5.193 | 4.14E-05 | 7.59E-04 | 0.33 | 1.14E-03 | 0.687 |
1000 | 5.193 | 4.46E-05 | 9.14E-04 | 0.354 | 1.40E-03 | 0.654 |
Compounds


Helium has a
2, He2+
2, HeH+
, and HeD+
have been created this way.[123] HeH+ is also stable in its ground state but is extremely reactive—it is the strongest Brønsted acid known, and therefore can exist only in isolation, as it will protonate any molecule or counteranion it contacts. This technique has also produced the neutral molecule He2, which has a large number of band systems, and HgHe, which is apparently held together only by polarization forces.[30]
Theoretically, other true compounds may be possible, such as helium fluorohydride (HHeF), which would be analogous to HArF, discovered in 2000.[125] Calculations show that two new compounds containing a helium-oxygen bond could be stable.[126] Two new molecular species, predicted using theory, CsFHeO and N(CH3)4FHeO, are derivatives of a metastable FHeO− anion first theorized in 2005 by a group from Taiwan.[127]
Helium atoms have been inserted into the hollow carbon cage molecules (the fullerenes) by heating under high pressure. The endohedral fullerene molecules formed are stable at high temperatures. When chemical derivatives of these fullerenes are formed, the helium stays inside.[128] If helium-3 is used, it can be readily observed by helium nuclear magnetic resonance spectroscopy.[129] Many fullerenes containing helium-3 have been reported. Although the helium atoms are not attached by covalent or ionic bonds, these substances have distinct properties and a definite composition, like all stoichiometric chemical compounds.
Under high pressures helium can form compounds with various other elements. Helium-nitrogen
Occurrence and production
Natural abundance
Although it is rare on Earth, helium is the second most abundant element in the known Universe, constituting 23% of its baryonic mass. Only hydrogen is more abundant.[28] The vast majority of helium was formed by Big Bang nucleosynthesis one to three minutes after the Big Bang. As such, measurements of its abundance contribute to cosmological models. In stars, it is formed by the nuclear fusion of hydrogen in proton–proton chain reactions and the CNO cycle, part of stellar nucleosynthesis.[113]
In the
Most helium on Earth is a result of
As of 2021[update], the world's helium reserves were estimated at 31 billion cubic meters, with a third of that being in Qatar.[145] In 2015 and 2016 additional probable reserves were announced to be under the Rocky Mountains in North America[146] and in the East African Rift.[26]
The Bureau of Land Management (BLM) has proposed an October 2024 plan for managing natural resources in western Colorado. The plan involves closing 543,000 acres to oil and gas leasing while keeping 692,300 acres open. Among the open areas, 165,700 acres have been identified as suitable for helium recovery. The United States possesses an estimated 306 billion cubic feet of recoverable helium, sufficient to meet current consumption rates of 2.15 billion cubic feet per year for approximately 150 years.[147]
Modern extraction and distribution
For large-scale use, helium is extracted by
In 2008, approximately 169 million
In the United States, most helium is extracted from the natural gas of the
Diffusion of crude natural gas through special
Helium is generally extracted from natural gas because it is present in air at only a fraction of that of neon, yet the demand for it is far higher. It is estimated that if all neon production were retooled to save helium, 0.1% of the world's helium demands would be satisfied. Similarly, only 1% of the world's helium demands could be satisfied by re-tooling all air distillation plants.
Helium is commercially available in either liquid or gaseous form. As a liquid, it can be supplied in small insulated containers called
Conservation advocates
According to helium conservationists like Nobel laureate physicist
Applications
- Cryogenics (32%)
- Pressurizing and purging (18%)
- Welding (13%)
- Controlled atmospheres (18%)
- Leak detection (4%)
- Breathing mixtures (2%)
- Other (13.0%)
While balloons are perhaps the best-known use of helium, they are a minor part of all helium use.
Controlled atmospheres
Helium is used as a protective gas in growing silicon and germanium crystals, in titanium and zirconium production, and in gas chromatography,[108] because it is inert. Because of its inertness, thermally and calorically perfect nature, high speed of sound, and high value of the heat capacity ratio, it is also useful in supersonic wind tunnels[164] and impulse facilities.[165]
Gas tungsten arc welding
Helium is used as a
.Minor uses
Industrial leak detection

One industrial application for helium is leak detection. Because helium diffuses through solids three times faster than air, it is used as a tracer gas to detect leaks in high-vacuum equipment (such as cryogenic tanks) and high-pressure containers.[166] The tested object is placed in a chamber, which is then evacuated and filled with helium. The helium that escapes through the leaks is detected by a sensitive device (helium mass spectrometer), even at the leak rates as small as 10−9 mbar·L/s (10−10 Pa·m3/s). The measurement procedure is normally automatic and is called helium integral test. A simpler procedure is to fill the tested object with helium and to manually search for leaks with a hand-held device.[167]
Helium leaks through cracks should not be confused with gas permeation through a bulk material. While helium has documented permeation constants (thus a calculable permeation rate) through glasses, ceramics, and synthetic materials, inert gases such as helium will not permeate most bulk metals.[168]
Flight
Because it is
Minor commercial and recreational uses
Helium as a breathing gas has no
For its inertness and high
Helium, mixed with a heavier gas such as xenon, is useful for
Helium is also used in some hard disk drives.[177]
Scientific uses
The use of helium reduces the distorting effects of temperature variations in the space between
Helium is a commonly used carrier gas for gas chromatography.
The age of rocks and minerals that contain uranium and thorium can be estimated by measuring the level of helium with a process known as helium dating.[28][30]
Helium at low temperatures is used in
Medical uses
Helium was approved for medical use in the United States in April 2020 for humans and animals.[181][182]
As a contaminant
While chemically inert, helium contamination impairs the operation of
Inhalation and safety
Effects
Neutral helium at standard conditions is non-toxic, plays no biological role and is found in trace amounts in human blood.
The
Hazards
Inhaling helium can be dangerous if done to excess, since helium is a simple asphyxiant and so displaces oxygen needed for normal respiration.[28][186] Fatalities have been recorded, including a youth who suffocated in Vancouver in 2003 and two adults who suffocated in South Florida in 2006.[187][188] In 1998, an Australian girl from Victoria fell unconscious and temporarily turned blue after inhaling the entire contents of a party balloon.[189][190][191] Inhaling helium directly from pressurized cylinders or even balloon filling valves is extremely dangerous, as high flow rate and pressure can result in barotrauma, fatally rupturing lung tissue.[186][192]
Death caused by helium is rare. The first media-recorded case was that of a 15-year-old girl from Texas who died in 1998 from helium inhalation at a friend's party; the exact type of helium death is unidentified.[189][190][191]
In the United States, only two fatalities were reported between 2000 and 2004, including a man who died in North Carolina of barotrauma in 2002.[187][192] A youth asphyxiated in Vancouver during 2003, and a 27-year-old man in Australia had an embolism after breathing from a cylinder in 2000.[187] Since then, two adults asphyxiated in South Florida in 2006,[187][188][193] and there were cases in 2009 and 2010, one of whom was a Californian youth who was found with a bag over his head, attached to a helium tank,[194] and another teenager in Northern Ireland died of asphyxiation.[195] At Eagle Point, Oregon a teenage girl died in 2012 from barotrauma at a party.[196][197][198] A girl from Michigan died from hypoxia later in the year.[199]
On February 4, 2015, it was revealed that, during the recording of their main TV show on January 28, a 12-year-old member (name withheld) of Japanese all-girl singing group
The safety issues for cryogenic helium are similar to those of liquid nitrogen; its extremely low temperatures can result in cold burns, and the liquid-to-gas expansion ratio can cause explosions if no pressure-relief devices are installed. Containers of helium gas at 5 to 10 K should be handled as if they contain liquid helium due to the rapid and significant thermal expansion that occurs when helium gas at less than 10 K is warmed to room temperature.[108]
At high pressures (more than about 20 atm or two
See also
- Abiogenic petroleum origin
- Helium-3 propulsion
- Leidenfrost effect
- Superfluid
- Tracer-gas leak testing method
- Hamilton Cady
Notes
- ^ A few authors dispute the placement of helium in the noble gas column, preferring to place it above beryllium with the alkaline earth metals. They do so on the grounds of helium's 1s2 electron configuration, which is analogous to the ns2 valence configurations of the alkaline earth metals, and furthermore point to some specific trends that are more regular if helium is placed in group 2.[8][9][10][11][12] These tend to relate to kainosymmetry and the first-row anomaly: the first orbital of any type is unusually small, since unlike its higher analogues, it does not experience interelectronic repulsion from a smaller orbital of the same type. Because of this trend in the sizes of orbitals, a large difference in atomic radii between the first and second members of each main group is seen in groups 1 and 13–17: it exists between neon and argon, and between helium and beryllium, but not between helium and neon. This similarly affects the noble gases' boiling points and solubilities in water, where helium is too close to neon, and the large difference characteristic between the first two elements of a group appears only between neon and argon. Moving helium to group 2 makes this trend consistent in groups 2 and 18 as well, by making helium the first group 2 element and neon the first group 18 element: both exhibit the characteristic properties of a kainosymmetric first element of a group.[13] However, the classification of helium with the other noble gases remains near-universal, as its extraordinary inertness is extremely close to that of the other light noble gases neon and argon.[14]
References
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- ^ Rayet, G. (1868) "Analyse spectral des protubérances observées, pendant l'éclipse totale de Soleil visible le 18 août 1868, à la presqu'île de Malacca" (Spectral analysis of the protuberances observed during the total solar eclipse, seen on 18 August 1868, from the Malacca peninsula), Comptes rendus ... , 67 : 757–759. From p. 758: " ... je vis immédiatement une série de neuf lignes brillantes qui ... me semblent devoir être assimilées aux lignes principales du spectre solaire, B, D, E, b, une ligne inconnue, F, et deux lignes du groupe G." ( ... I saw immediately a series of nine bright lines that ... seemed to me should be classed as the principal lines of the solar spectrum, B, D, E, b, an unknown line, F, and two lines of the group G.)
- ^ Captain C. T. Haig (1868) "Account of spectroscopic observations of the eclipse of the sun, August 18th, 1868" Proceedings of the Royal Society of London, 17 : 74–80. From p. 74: "I may state at once that I observed the spectra of two red flames close to each other, and in their spectra two broad bright bands quite sharply defined, one rose-madder and the other light golden."
- ^ Pogson filed his observations of the 1868 eclipse with the local Indian government, but his report wasn't published. (Biman B. Nath, The Story of Helium and the Birth of Astrophysics (New York, New York: Springer, 2013), p. 8.) Nevertheless, Lockyer quoted from his report. From p. 320 Archived 17 August 2018 at the Wayback Machine of Lockyer, J. Norman (1896) "The story of helium. Prologue," Nature, 53 : 319–322 : "Pogson, in referring to the eclipse of 1868, said that the yellow line was "at D, or near D." "
- ^ Lieutenant John Herschel (1868) "Account of the solar eclipse of 1868, as seen at Jamkandi in the Bombay Presidency," Proceedings of the Royal Society of London, 17 : 104–120. From p. 113: As the moment of the total solar eclipse approached, " ... I recorded an increasing brilliancy in the spectrum in the neighborhood of D, so great in fact as to prevent any measurement of that line till an opportune cloud moderated the light. I am not prepared to offer any explanation of this." From p. 117: "I also consider that there can be no question that the ORANGE LINE was identical with D, so far as the capacity of the instrument to establish any such identity is concerned."
- ^ In his initial report to the French Academy of Sciences about the 1868 eclipse, Janssen made no mention of a yellow line in the solar spectrum. See:
- Janssen (1868) "Indication de quelques-uns des résultats obtenus à Cocanada, pendant l'éclipse du mois d'août dernier, et à la suite de cette éclipse" (Information on some of the results obtained at Cocanada, during the eclipse of the month of last August, and following that eclipse), Comptes rendus ... , 67 : 838–839.
- Wheeler M. Sears, Helium: The Disappearing Element (Heidelberg, Germany: Springer, 2015), p. 44.
- Françoise Launay with Storm Dunlop, trans., The Astronomer Jules Janssen: A Globetrotter of Celestial Physics (Heidelberg, Germany: Springer, 2012), p. 45.
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- ^ a b Sample, Ian (28 June 2016). "Huge helium gas find in east Africa averts medical shortage". The Guardian. Archived from the original on 29 June 2016. Retrieved 29 June 2016.
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Frankland and Lockyer find the yellow prominences to give a very decided bright line not far from D, but hitherto not identified with any terrestrial flame. It seems to indicate a new substance, which they propose to call Helium
- .
- ^ Palmieri, Luigi (1881). "La riga dell'Helium apparsa in una recente sublimazione vesuviana" [The line of helium appeared in a recently sublimated material [from Mt.] Vesuvius.]. Rendiconto dell'Accademia delle Scienze Fisiche e Matematiche (Naples, Italy). 20: 223. Archived from the original on 1 September 2018. Retrieved 1 May 2017.
Raccolsi alcun tempo fa una sostanza amorfa di consistenza butirracea e di colore giallo sbiadato sublimata sull'orlo di una fumarola prossima alla bocca di eruzione. Saggiata questa sublimazione allo spettroscopio, ho ravvisato le righe del sodio e del potassio ed una lineare ben distinta che corrisponde esattamente alla D3 che è quella dell'Helium. Do per ora il semplice annunzio del fatto, proponendomi di ritornare sopra questo argomento, dopo di aver sottoposta la sublimazione ad una analisi chimica. (I collected some time ago an amorphous substance having a buttery consistency and a faded yellow color which had sublimated on the rim of a fumarole near the mouth of the eruption. Having analyzed this sublimated substance with a spectroscope, I recognized the lines of sodium and potassium and a very distinct linear line which corresponds exactly to D3, which is that of helium. For the present, I'm making a mere announcement of the fact, proposing to return to this subject after having subjected the sublimate to a chemical analysis.)
- ^ Kirk, Wendy L. "Cleveite [not Clevite] and helium". Museums & Collections Blog. University College London. Archived from the original on 18 October 2018. Retrieved 18 August 2017.
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- ^ See:
- Crookes, William (1895). "The spectrum of the gas from clèveite". The Chemical News and Journal of Physical Science. 71 (1844): 151.
- Crookes, William (1895). "The spectrum of helium". The Chemical News and Journal of Physical Science. 72 (1865): 87–89.
- ^ See:
- Clève, P.T. (1895). "Sur la présence de l'hélium dans le clévéite" [On the presence of helium in cleveite]. Comptes rendus hebdomadaires des séances de l'Académie des sciences (in French). 120: 834.
- English translation: Clève, P.T. (1895). "On the presence of helium in clèveite". The Chemical News and Journal of Physical Science. 71 (1849): 212.
- Thorpe, T. E. (1895). "Terrestrial helium?". Nature. 51 (1329): 586.
- Clève (1895). "Sur la densité de l'hélium" [On the density of helium]. Comptes rendus hebdomadaires des séances de l'Académie des sciences (in French). 120: 1212.
- .
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- ^ See:
- Preliminary notice: Keesom, W. H. (17 July 1926) Letters to the Editor: "Solidification of helium," Nature, 118 : 81.
- Preliminary notice: Keesom, W. H. (1926) "L'hélium solidifié," Archived 2016-10-22 at the Wayback Machine Comptes rendus ... , 183 : 26.
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External links
General
- U.S. Government's Bureau of Land Management: Sources, Refinement, and Shortage. With some history of helium.
- U.S. Geological Survey publications on helium beginning 1996: Helium
- Where is all the helium? Aga website
- It's Elemental – Helium
- Chemistry in its element podcast (MP3) from the Royal Society of Chemistry's Chemistry World: Helium
- International Chemical Safety Cards – Helium includes health and safety information regarding accidental exposures to helium
More detail
- Helium at The Periodic Table of Videos(University of Nottingham)
- Helium Archived 2005-04-12 at the Wayback Machine at the Helsinki University of Technology; includes pressure-temperature phase diagrams for helium-3 and helium-4
- Lancaster University, Ultra Low Temperature Physics – includes a summary of some low temperature techniques
- Video: Demonstration of superfluid helium (Alfred Leitner, 1963, 38 min.)
Miscellaneous
- Physics in Speech with audio samples that demonstrate the unchanged voice pitch
- Article about helium and other noble gases
Helium shortage
- America's Helium Supply: Options for Producing More Helium from Federal Land: Oversight Hearing before the Subcommittee on Energy and Mineral Resources of the Committee on Natural Resources, U.S. House Of Representatives, One Hundred Thirteenth Congress, First Session, Thursday, July 11, 2013
- Helium Program: Urgent Issues Facing BLM's Storage and Sale of Helium Reserves: Testimony before the Committee on Natural Resources, House of Representatives Government Accountability Office
- Kramer, David (May 22, 2012). "Senate bill would preserve US helium reserve: Measure would give scientists first dibs on helium should a shortage develop. Physics Today web site". Archived from the original on October 27, 2012.
- Richardson, Robert C.; Chan, Moses (2009). "Helium, when will it run out?" (PDF). Archived from the original (PDF) on 2015-06-14.