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Although helium-3 was found to be about 10,000 times rarer than helium-4 in the helium from the gas wells, its significant presence in underground gas deposits implied that either it did not decay, or else it had a very long [[half-life]] - billions of years. [[Hydrogen-1]] and helium-3 are the only stable nuclides in existence that contain more protons than they have neutrons.
Although helium-3 was found to be about 10,000 times rarer than helium-4 in the helium from the gas wells, its significant presence in underground gas deposits implied that either it did not decay, or else it had a very long [[half-life]] - billions of years. [[Hydrogen-1]] and helium-3 are the only stable nuclides in existence that contain more protons than they have neutrons.


Helium-3 occurs as a primordial nuclide, escaping from the Earth's crust into the atmosphere and into [[outer space]] over millions of years. Helium-3 is also thought to be a natural [[nucleogenic]] and [[cosmogenic nuclide]], one produced when lithium is bombarded by natural neutrons. Those are released by [[spontaneous fission]] and by [[nuclear reaction]]s with [[cosmic ray]]s. Some of the helium-3 found in the terrestrial atmosphere is also a relic of atmospheric and underwater [[nuclear weapons testing]], conducted by the three big nuclear powers before 1963. Most of this comes from the decay of [[tritium]] (hydrogen-3), which decays into helium-3 with a [[half life]] of about 12.3 years. Furthermore, some [[nuclear reactor]]s (landbound or shipbound) periodically release some helium-3 and tritium into the atmosphere, especially whenever something goes wrong. The [[Chernobyl disaster|nuclear reactor disaster at Chernobyl]] released a huge amount of radioactive tritium into the atmosphere, and smaller problems cause smaller releases. Furthermore, significant amounts of tritium and helium-3 have been deliberately produced in national arsenal nuclear reactors by the irradiation of [[lithium-6]]. The tritium is used to “boost” [[nuclear weapons]], and some of this inevitably escapes during its production, transportation, and storage. Hence, helium-3 enters the atmosphere both through its direct release and through the [[radioactive decay]] of tritium. The vast majority of these two gases have been produced and leaked by the former [[Soviet Union]], [[Russia]], the [[United Kingdom]], and the [[Republic of France]].
Helium-3 occurs as a primordial nuclide, escaping from the Earth's crust into the atmosphere and into [[outer space]] over millions of years. Helium-3 is also thought to be a natural [[nucleogenic]] and [[cosmogenic nuclide]], one produced when lithium is bombarded by natural neutrons. Those are released by [[spontaneous fission]] and by [[nuclear reaction]]s with [[cosmic ray]]s. Some of the helium-3 found in the terrestrial atmosphere is also a relic of atmospheric and underwater [[nuclear weapons testing]], conducted by the three big nuclear powers before 1963. Most of this comes from the decay of [[tritium]] (hydrogen-3), which decays into helium-3 with a [[half life]] of about 12.3 years. Furthermore, some [[nuclear reactor]]s (landbound or shipbound) periodically release some helium-3 and tritium into the atmosphere, especially whenever something goes wrong. The [[Chernobyl disaster|nuclear reactor disaster at Chernobyl]] released a huge amount of radioactive tritium into the atmosphere, and smaller problems cause smaller releases. Furthermore, significant amounts of tritium and helium-3 have been deliberately produced in national arsenal nuclear reactors by the irradiation of [[lithium-6]]. The tritium is used to “boost” [[nuclear weapons]], and some of this inevitably escapes during its production, transportation, and storage. Hence, helium-3 enters the atmosphere both through its direct release and through the [[radioactive decay]] of tritium. The vast majority of these two gases have been produced and leaked by the former [[Soviet Union]], [[Russia]], the [[United Kingdom]], and the [[Republic of France]] {{Citation needed}}.


Helium-3 is proposed as a second-generation fuel for [[nuclear fusion]] in hypothetical [[fusion power|fusion power plant]]s, but such plants are still very early in their development -- especially since the first generation has not entered service anywhere, yet. Helium-3 can be used in instruments for the detection of free neutrons, such as neutrons leaking from [[nuclear reactor]]s.
Helium-3 is proposed as a second-generation fuel for [[nuclear fusion]] in hypothetical [[fusion power|fusion power plant]]s, but such plants are still very early in their development -- especially since the first generation has not entered service anywhere, yet. Helium-3 can be used in instruments for the detection of free neutrons, such as neutrons leaking from [[nuclear reactor]]s.

Revision as of 14:35, 3 December 2012

This article is about the elemental isotope. For the record label, see Helium 3 (record label).
Helium-3, 3He
General
Symbol3He
Nameshelium-3, 3He, He-3,
Helium-3, He-3
Protons (Z)2
Neutrons (N)1
Nuclide data
Natural abundance0.000137% (% He on Earth)
Half-life (t1/2)stable
Isotope mass3.0160293 Da
Spin1/2+
Parent isotopes3H (beta decay of tritium)
Isotopes of helium
Complete table of nuclides

Helium-3 (He-3, sometimes called tralphium[1]) is a light, non-radioactive isotope of helium with two protons and one neutron. It is rare on the Earth, and it is sought for use in nuclear fusion research. The abundance of helium-3 is thought to be greater on the Moon (embedded in the upper layer of regolith by the solar wind over billions of years)[citation needed], though still low in quantity (28 ppm of lunar regolith is helium-4 and from one ppb to 50 ppb is helium-3)[2][3], and the solar system's gas giants (left over from the original solar nebula).

The helion, the nucleus of a helium-3 atom, consists of two protons but only one neutron, in contrast with two neutrons in common helium. Its hypothetical existence was first proposed in 1934 by the Australian nuclear physicist Mark Oliphant while he was working at the University of Cambridge Cavendish Laboratory. Oliphant had performed experiments in which fast deuterons collided with deuteron targets (incidentally, the first demonstration of nuclear fusion).[4]

Helium-3 was hypothesized to be a radioactive isotope until helions were also found in samples of natural helium, which is mostly helium-4, taken both from the terrestrial atmosphere and from natural gas wells. This was done by Luis W. Alvarez and Robert Cornog in cyclotron experiments at the Lawrence Berkeley National Laboratory in California in 1939.[5]

Although helium-3 was found to be about 10,000 times rarer than helium-4 in the helium from the gas wells, its significant presence in underground gas deposits implied that either it did not decay, or else it had a very long half-life - billions of years. Hydrogen-1 and helium-3 are the only stable nuclides in existence that contain more protons than they have neutrons.

Helium-3 occurs as a primordial nuclide, escaping from the Earth's crust into the atmosphere and into outer space over millions of years. Helium-3 is also thought to be a natural nucleogenic and cosmogenic nuclide, one produced when lithium is bombarded by natural neutrons. Those are released by spontaneous fission and by nuclear reactions with cosmic rays. Some of the helium-3 found in the terrestrial atmosphere is also a relic of atmospheric and underwater nuclear weapons testing, conducted by the three big nuclear powers before 1963. Most of this comes from the decay of tritium (hydrogen-3), which decays into helium-3 with a half life of about 12.3 years. Furthermore, some nuclear reactors (landbound or shipbound) periodically release some helium-3 and tritium into the atmosphere, especially whenever something goes wrong. The nuclear reactor disaster at Chernobyl released a huge amount of radioactive tritium into the atmosphere, and smaller problems cause smaller releases. Furthermore, significant amounts of tritium and helium-3 have been deliberately produced in national arsenal nuclear reactors by the irradiation of lithium-6. The tritium is used to “boost” nuclear weapons, and some of this inevitably escapes during its production, transportation, and storage. Hence, helium-3 enters the atmosphere both through its direct release and through the radioactive decay of tritium. The vast majority of these two gases have been produced and leaked by the former Soviet Union, Russia, the United Kingdom, and the Republic of France [citation needed].

Helium-3 is proposed as a second-generation fuel for nuclear fusion in hypothetical fusion power plants, but such plants are still very early in their development -- especially since the first generation has not entered service anywhere, yet. Helium-3 can be used in instruments for the detection of free neutrons, such as neutrons leaking from nuclear reactors.

Physical properties

Because of its lower atomic mass of about 3.00 atomic mass units, helium-3 has some physical properties different from those of from helium-4, with a mass of about 4.00 atomic mass units. Because of the weak, induced dipole-dipole interaction between helium atoms, their macroscopic physical properties are mainly determined by their zero point energy ("ground state kinetic energy"). Also, the microscopic properties of helium-3 cause it to have a higher zero point energy than helium-4. This implies that helium-3 can overcome dipole-dipole interaction with less thermal energy than helium-4 can.

The quantum mechanical effects on helium-3 and helium-4 are significantly different because with two protons, two neutrons, and two electrons, helium-4 has an overall "spin" of zero, making it a boson, but with one fewer neutron, helium-3 has an overall spin of plus or minus one half, making it a fermion.

Helium-3 boils at 3.19 kelvin compared with helium-4 at 4.23 kelvin, and its critical point is also lower at 3.35 kelvin, compared with helium-4 at 5.2 kelvin. Helium-3 has less than one-half of the density when it is at its boiling point: 59 gram per liter compared to the 125 gram per liter of helium-4 -- at a pressure of one atmosphere. Its latent heat of vaporization is also considerably lower at 0.026 kilojoule per mole compared with the 0.0829 kilojoule per mole of helium-4.[6]

Fusion reactions

Comparison of neutronicity of reactions[7][8][9][10][11]
Reactants Products Q n/MeV
First-generation fusion fuels
21H + 21H (D-D) → 32He + 10n 3.268 MeV 0.306
21H + 21H (D-D) → 31H + 11p 4.032 MeV 0
21H + 31H (D-T) → 42He + 10n 17.571 MeV 0.057
Second-generation fusion fuel
21H + 32He (D-3He) → 42He + 11p 18.354 MeV 0
Third-generation fusion fuels
32He + 32He → 42He+ 211p 12.86 MeV 0
115B + 11p → 3 42He 8.68 MeV 0
Net result of D burning (sum of first 4 rows)
6D → 2(4He + n + p) 43.225 MeV 0.046
Current nuclear fuel
235U + n → 2 FP+ 2.5n ~200 MeV 0.001
The fusion reaction rate increases rapidly with temperature until it maximizes and then gradually drops off. The DT rate peaks at a lower temperature (about 70 keV, or 800 million kelvins) and at a higher value than other reactions commonly considered for fusion energy.

Some fusion processes produce highly energetic neutrons which render reactor components radioactive with activation products through the continuous bombardment of the reactor's components with emitted neutrons. Because of this bombardment and irradiation, power generation must occur indirectly through thermal means, as in a fission reactor. However, the appeal of helium-3 fusion stems from the aneutronic nature of its reaction products. Helium-3 itself is non-radioactive. The lone high-energy by-product, the proton, can be contained using electric and magnetic fields. The momentum energy of this proton (created in the fusion process) will interact with the containing electromagnetic field, resulting in direct net electricity generation.[12]

Because of the higher Coulomb barrier, the temperatures required for 21H + 32He fusion are much higher than those of conventional 21H + 31H (deuterium + tritium) fusion. Moreover, since both reactants need to be mixed together to fuse, reactions between nuclei of the same reactant will occur, and the D-D reaction (21H + 21H) does produce a neutron. Reaction rates vary with temperature, but the D-3He reaction rate is never greater than 3.56 times the D-D reaction rate (see graph). Therefore fusion using D-3He fuel may produce a somewhat lower neutron flux than D-T fusion, but is by no means clean, negating some of its main attraction.

A second possibility, fusing 32He with itself (32He + 32He), requires even higher temperatures (since now both reactants have a +2 charge), and thus is even more difficult than the D-3He reaction. However, it does offer a possible reaction that produces no neutrons; the protons it produces possess charges and can be contained using electric and magnetic fields, which in turn results in direct electricity generation. 32He + 32He fusion has been demonstrated in the laboratory and is thus theoretically feasible and would have immense advantages, but commercial viability is many years in the future.[13]

The amounts of helium-3 needed as a replacement for conventional fuels are substantial by comparison to amounts currently available. The total amount of energy produced in the 21H + 32He reaction is 18.4 MeV, which corresponds to some 493 megawatt-hours (4.93×108 W·h) per three grams (one mole) of ³He. Even if that total amount of energy could be converted to electrical power with 100% efficiency (a physical impossibility), it would correspond to about 30 minutes of output of a gigawatt electrical plant; a year's production by the same plant would require some 17.5 kilograms of helium-3.

The amount of fuel needed for large-scale applications can also be put in terms of total consumption: According to the US Energy Information Administration, "Electricity consumption by 107 million U.S. households in 2001 totaled 1,140 billion kW·h" (1.14×1015 W·h). Again assuming 100% conversion efficiency, 6.7 tonnes of helium-3 would be required for that segment of the energy demand of the United States, 15 to 20 tonnes given a more realistic end-to-end conversion efficiency.[citation needed]

Neutron detection

Helium-3 is a most important isotope in instrumentation for neutron detection. It has a high absorption cross section for thermal neutron beams and is used as a converter gas in neutron detectors. The neutron is converted through the nuclear reaction

n + 3He → 3H + 1H + 0.764 MeV

into charged particles tritium (T, 3H) and protium (p, 1H) which then are detected by creating a charge cloud in the stopping gas of a proportional counter or a Geiger-Müller tube.[14]

Furthermore, the absorption process is strongly spin-dependent, which allows a spin-polarized helium-3 volume to transmit neutrons with one spin component while absorbing the other. This effect is employed in neutron polarization analysis, a technique which probes for magnetic properties of matter.[15][16][17][18]

The United States Department of Homeland Security had hoped to deploy detectors to spot smuggled plutonium in shipping containers by their neutron emissions, but the worldwide shortage of helium-3 following the drawdown in nuclear weapons production since the Cold War has to some extent prevented this.[19]

Cryogenics

A helium-3 refrigerator uses helium-3 to achieve temperatures of 0.2 to 0.3 kelvin. A dilution refrigerator uses a mixture of helium-3 and helium-4 to reach cryogenic temperatures as low as a few thousandths of a kelvin.[20]

An important property of helium-3, which distinguishes it from the more common helium-4, is that its nucleus is a fermion since it contains an odd number of spin 1/2 particles. Helium-4 nuclei are bosons, containing an even number of spin 1/2 particles. This is a direct result of the addition rules for quantized angular momentum. At low temperatures (about 2.17 K), helium-4 undergoes a phase transition: A fraction of it enters a superfluid phase that can be roughly understood as a type of Bose-Einstein condensate. Such a mechanism is not available for helium-3 atoms, which are fermions. However, it was widely speculated that helium-3 could also become a superfluid at much lower temperatures, if the atoms formed into pairs analogous to Cooper pairs in the BCS theory of superconductivity. Each Cooper pair, having integer spin, can be thought of as a boson. During the 1970s, David Lee, Douglas Osheroff and Robert Coleman Richardson discovered two phase transitions along the melting curve, which were soon realized to be the two superfluid phases of helium-3.[21][22] The transition to a superfluid occurs at 2.491 millikelvins (i.e., 0.002491 K) on the melting curve. They were awarded the 1996 Nobel Prize in Physics for their discovery. Tony Leggett won the 2003 Nobel Prize in Physics for his work on refining understanding of the superfluid phase of helium-3.[23]

In zero magnetic field, there are two distinct superfluid phases of 3He, the A-phase and the B-phase. The B-phase is the low-temperature, low-pressure phase which has an isotropic energy gap. The A-phase is the higher temperature, higher pressure phase that is further stabilized by a magnetic field and has two point nodes in its gap. The presence of two phases is a clear indication that 3He is an unconventional superfluid (superconductor), since the presence of two phases requires an additional symmetry, other than gauge symmetry, to be broken. In fact, it is a p-wave superfluid, with spin one, S=1, and angular momentum one, L=1. The ground state corresponds to total angular momentum zero, J=S+L=0 (vector addition). Excited states are possible with non-zero total angular momentum, J>0, which are excited pair collective modes. Because of the extreme purity of superfluid 3He (since all materials except 4He have solidified and sunk to the bottom of the liquid 3He and any 4He has phase separated entirely, this is the most pure condensed matter state), these collective modes have been studied with much greater precision than in any other unconventional pairing system.

Medical lung imaging

Helium-3 nuclei have an intrinsic nuclear spin of ½, and a relatively high magnetogyric ratio. Helium-3 can be hyperpolarized using non-equilibrium means such as spin-exchange optical pumping.[24] During this process, circularly polarized infrared laser light, tuned to the appropriate wavelength, is used to excite electrons in an alkali metal, such as caesium or rubidium inside a sealed glass vessel. The angular momentum is transferred from the alkali metal electrons to the noble gas nuclei through collisions. In essence, this process effectively aligns the nuclear spins with the magnetic field in order to enhance the NMR signal. The hyperpolarized gas may then be stored at pressures of 10 atm, for up to 100 hours. Following inhalation, gas mixtures containing the hyperpolarized helium-3 gas can be imaged with an MRI scanner to produce anatomical and functional images of lung ventilation. This technique is also able to produce images of the airway tree, locate unventilated defects, measure the alveolar oxygen partial pressure, and measure the ventilation/perfusion ratio. This technique may be critical for the diagnosis and treatment management of chronic respiratory diseases such as chronic obstructive pulmonary disease (COPD), emphysema, cystic fibrosis, and asthma.[25]

Production

Current US industrial consumption of Helium-3 is approximately 60,000 liters per year;[26] cost at auction has typically been approximately $100/liter although increasing demand has raised prices to as much as $2,000/liter in recent years.[27] Helium-3 is naturally present in small quantities due to radioactive decay, but virtually all helium-3 used in industry is manufactured. Helium-3 is a product of tritium decay, and tritium can be produced through neutron bombardment of deuterium, lithium, boron, or nitrogen targets. Production of tritium in significant quantities requires the high neutron flux of a nuclear reactor; breeding tritium with lithium-6 consumes the neutron, while breeding with lithium-7 produces a low energy neutron as a replacement for the consumed fast neutron.

Current supplies of helium-3 come, in part, from the dismantling of nuclear weapons where it accumulates,[28][29] however the need for warhead disassembly is diminishing. Consequently tritium itself is in short supply, and the US Department of Energy recently began producing it by the lithium irradiation method at the Tennessee Valley Authority's Watts Bar reactor.[26] Substantial quantities of tritium could also be extracted from the heavy water moderator in CANDU nuclear reactors.

Production of helium-3 from tritium at a rate sufficient to meet world demand will require significant investment, as tritium must be produced at the same rate as helium-3, and approximately eighteen times as much tritium must be maintained in storage as the amount of helium-3 produced annually by decay (production rate dN⁄dt from number of moles or other unit mass of tritium N, is N γ = N (ln 2)⁄t½ where the value of t½⁄(ln 2) is about 18 years; see radioactive decay). If commercial fusion reactors were to use helium-3 as a fuel, they would require tens of tonnes of helium-3 each year to produce a fraction of the world's power, requiring substantial expansion of facilities for tritium production and storage.[30]

Abundance

Solar nebula (primordial) abundance

One early estimate of the primordial ratio of 3He to 4He in the solar nebula has been the measurement of their ratio in the atmosphere of Jupiter, measured by the mass spectrometer of the Galileo atmospheric entry probe. This ratio is about 1:10,000,[31] or 100 parts of 3He per million parts of 4He. This is roughly the same ratio of the isotopes in lunar regolith, when it contains 28 ppm helium-4 and 2.8 ppb helium-3 (which is at the lower end of actual sample measurements, which vary from about 1.4 to 15 ppb). However, terrestrial ratios of the isotopes are lower by a factor of 100, mainly due to enrichment of helium-4 stocks in the mantle by billions of years of alpha decay from uranium and thorium.

Terrestrial abundance

Main article: isotope geochemistry

3He is a primordial substance in the Earth's mantle, considered to have become entrapped within the Earth during planetary formation. The ratio of 3He to 4He within the Earth's crust and mantle is less than that for assumptions of solar disk composition as obtained from meteorite and lunar samples, with terrestrial materials generally containing lower 3He/4He ratios due to ingrowth of 4He from radioactive decay.

3He is present within the mantle, in the ratio of 200–300 parts of 3He to a million parts of 4He. Ratios of 3He/4He in excess of atmospheric are indicative of a contribution of 3He from the mantle. Crustal sources are dominated by the 4He which is produced by the decay of radioactive elements in the crust and mantle.

The ratio of Helium-3 to Helium-4 in natural Earth-bound sources varies greatly.[32][33] Samples of the ore Spodumene from Edison Mine, South Dakota were found to contain 12 parts of helium-3 to a million parts of helium-4. Samples from other mines showed 2 parts per million.[32]

Helium is also present as up to 7% of some natural gas sources,[34] and large sources have over 0.5% (above 0.2% makes it viable to extract).[35] Algeria's annual gas production is assumed to contain 100 million normal cubic metres[35] and this would contain between 5 and 50 m3 of Helium-3 (about 1 to 10 kilograms) using the normal abundance range of 0.5 to 5 ppm. Similarly the US 2002 stockpile of 1 billion normal m3[35] would have contained about 10 to 100 kilograms of helium-3.

3He is also present in the Earth's atmosphere. The natural abundance of 3He in naturally occurring helium gas is 1.38×10−6 (1.38 parts per million). The partial pressure of helium in the Earth's atmosphere is about 0.52 Pa, and thus helium accounts for 5.2 parts per million of the total pressure (101325 Pa) in the Earth's atmosphere, and 3He thus accounts for 7.2 parts per trillion of the atmosphere. Since the atmosphere of the Earth has a mass of about 5.14×1015 tonnes,[36] the mass of 3He in the Earth's atmosphere is the product of these numbers, or about 37,000 tonnes of 3He.

3He is produced on Earth from three sources: lithium spallation, cosmic rays, and beta decay of tritium (3H). The contribution from cosmic rays is negligible within all except the oldest regolith materials, and lithium spallation reactions are a lesser contributor than the production of 4He by alpha particle emissions.

The total amount of helium-3 in the mantle may be in the range of 0.1–1 million tonnes. However, most of the mantle is not directly accessible. Some helium-3 leaks up through deep-sourced hotspot volcanoes such as those of the Hawaiian islands, but only 300 grams per year is emitted to the atmosphere. Mid-ocean ridges emit another 3 kilogram per year. Around subduction zones, various sources produce helium-3 in natural gas deposits which possibly contain a thousand tonnes of helium-3 (although there may be 25 thousand tonnes if all ancient subduction zones have such deposits). Wittenberg estimated that United States crustal natural gas sources may have only half a tonne total.[37] Wittenberg cited Anderson's estimate of another 1200 metric tonnes in interplanetary dust particles on the ocean floors.[38] In the 1994 study, extracting helium-3 from these sources consumes more energy than fusion would release.[39] Wittenberg also writes that extraction from US crustal natural gas, consumes ten times the energy available from fusion reactions.[40][clarification needed]

Extraterrestrial abundance

Materials on the Moon's surface contain helium-3 at concentrations on the order of between 1.4 and 15 ppb in sunlit areas,[41][42] and may contain concentrations as much as 50 ppb in permanently shadowed regions.[3] A number of people, starting with Gerald Kulcinski in 1986,[43] have proposed to explore the moon, mine lunar regolith and use the helium-3 for fusion. Recently, companies as Planetary_Resources have also stated to be interested in mining helium-3 on the moon. Because of the low concentrations of helium-3, any mining equipment would need to process extremely large amounts of regolith (over 150 million tonnes of regolith to obtain one ton of helium 3),[44] and some proposals have suggested that helium-3 extraction be piggybacked onto a larger mining and development operation.[citation needed]

The primary objective of Indian Space Research Organization's first lunar probe called Chandrayaan-I, launched on October 22, 2008, was reported in some sources to be mapping the Moon's surface for helium-3-containing minerals.[45] However, this is debatable; no such objective is mentioned in the project's official list of goals, while at the same time, many of its scientific payloads have noted helium-3-related applications.[46][47]

Cosmochemist and geochemist Ouyang Ziyuan from the Chinese Academy of Sciences who is now in charge of the Chinese Lunar Exploration Program has already stated on many occasions that one of the main goals of the program would be the mining of helium-3, from which operation "each year three space shuttle missions could bring enough fuel for all human beings across the world."[48] which is an extreme overstatement however, as one payload to GTO of current spacecraft designs is less than 4 tonnes. To "bring enough fuel for all human beings across the world",[30] more than one Space Shuttle load (and the processing of 4 million tonnes of regolith) per week would be necessary.[citation needed]

In January 2006, the Russian space company RKK Energiya announced that it considers lunar helium-3 a potential economic resource to be mined by 2020,[49] if funding can be found.[50][51]

Mining gas giants for helium-3 has also been proposed.[52] The British Interplanetary Society's hypothetical Project Daedalus interstellar probe design was fueled by helium-3 mines in the atmosphere of Jupiter, for example. Jupiter's high gravity makes this a less energetically favorable operation than extracting helium-3 from the other gas giants of the solar system, however.

Power generation

A second-generation approach to controlled fusion power involves combining helium-3 (32He) and deuterium (21H). This reaction produces a helium-4 ion (42He) (like an alpha particle, but of different origin) and a high-energy proton (positively charged hydrogen ion) (11p). The most important potential advantage of this fusion reaction for power production as well as other applications lies in its compatibility with the use of electrostatic fields to control fuel ions and the fusion protons. Protons, as positively charged particles, can be converted directly into electricity, through use of solid-state conversion materials as well as other techniques. Potential conversion efficiencies of 70% may be possible, as there is no need to convert proton energy to heat in order to drive a turbine-powered electrical generator[citation needed].

There have been many claims about the capabilities of helium-3 power plants. According to proponents, fusion power plants operating on deuterium and helium-3 would offer lower capital and operating costs than their competitors due to less technical complexity, higher conversion efficiency, smaller size, the absence of radioactive fuel, no air or water pollution, and only low-level radioactive waste disposal requirements. Recent estimates suggest that about $6 billion in investment capital will be required to develop and construct the first helium-3 fusion power plant. Financial breakeven at today's wholesale electricity prices (5 US cents per kilowatt-hour) would occur after five 1-gigawatt plants were on line, replacing old conventional plants or meeting new demand.[53]

The reality is not so clear-cut. The most advanced fusion programs in the world are inertial confinement fusion (such as National Ignition Facility) and magnetic confinement fusion (such as ITER and other tokamaks). In the case of the former, there is no solid roadmap to power generation. In the case of the latter, commercial power generation is not expected until around 2050.[54] In both cases, the type of fusion discussed is the simplest: D-T fusion. The reason for this is the very low Coulomb barrier for this reaction; for D+3He, the barrier is much higher, and it is even higher for 3He–3He. The immense cost of reactors like ITER and National Ignition Facility are largely due to their immense size, yet to scale up to higher plasma temperatures would require reactors far larger still. The 14.7 MeV proton and 3.6 MeV alpha particle from D–3He fusion, plus the higher conversion efficiency, means that more electricity is obtained per kilogram than with D-T fusion (17.6 MeV), but not that much more. As a further downside, the rates of reaction for helium-3 fusion reactions are not particularly high, requiring a reactor that is larger still or more reactors to produce the same amount of electricity.

To attempt to work around this problem of massively large power plants that may not even be economical with D-T fusion, let alone the far more challenging D–3He fusion, a number of other reactors have been proposed – the Fusor, Polywell, Focus fusion, and many more, though many of these concepts have fundamental problems with achieving a net energy gain, and generally attempt to achieve fusion in thermal disequilibrium, something that could potentially prove impossible,[55] and consequently, these long-shot programs tend to have trouble garnering funding despite their low budgets. Unlike the "big", "hot" fusion systems, however, if such systems were to work, they could scale to the higher barrier "aneutronic" fuels, and therefore their proponents tend to promote p-B fusion, which requires no exotic fuels like helium-3.

  • Helium-3 was harvested in the 2009 science fiction movie Moon, by the story's protagonist Sam Bell, the occupant of a mining station on the far side of the Moon.[56][57][58]

Notes and references

  1. ^ from tri alpha named by George Gamow Owen Gingerich (1999). "Report on the Progress in Stellar Evolution to 1950". Astrophysics and Space Science. 267 (1–4): 3–31. Bibcode:1999Ap&SS.267....3G. doi:10.1023/A:1002711422064.
  2. ^ Slyuta, E. N. (March 12–16, 2007). The Estimation of Helium-3 Probable Reserves in Lunar Regolith (PDF). 38th Lunar and Planetary Science Conference. p. 2175. {{cite conference}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  3. ^ a b F. H. Cocks (2010). "3He in permanently shadowed lunar polar surfaces". Icarus. 206 (2): 778–779. Bibcode:2010Icar..206..778C. doi:10.1016/j.icarus.2009.12.032.
  4. ^ Oliphant, M. L. E. (1934). "Transmutation Effects Observed with Heavy Hydrogen". Proceedings of the Royal Society of London. A. 144 (853): 692–703. Bibcode:1934RSPSA.144..692O. doi:10.1098/rspa.1934.0077. JSTOR 2935553. {{cite journal}}: Unknown parameter |coauthors= ignored (|author= suggested) (help)
  5. ^ "Lawrence and His Laboratory: Episode: A Productive Error". Newsmagazine Publication. 1981. Retrieved 2009-09-01.
  6. ^ Teragon's Summary of Cryogen Properties Teragon Research, 2005
  7. ^ "Inertial Electrostatic Confinement Fusion". Retrieved 2007-05-06.
  8. ^ "Nuclear Fission and Fusion". Archived from the original on 2007-04-04. Retrieved 2007-05-06.
  9. ^ "The Fusion Reaction". Retrieved 2007-05-06.
  10. ^ John Santarius (2006). "A Strategy for D – 3He Development" (PDF). Retrieved 2007-05-06. {{cite web}}: Unknown parameter |month= ignored (help)
  11. ^ "Nuclear Reactions". Retrieved 2007-05-06.
  12. ^ John Santarius (September 28, 2004). "Lunar 3He and Fusion Power" (PDF). Retrieved 2007-05-06.
  13. ^ Mark Williams (August 23, 2007). "Mining the Moon: Lab experiments suggest that future fusion reactors could use helium-3 gathered from the moon". MIT Technology Review. Retrieved 2011-01-25.
  14. ^ A Modular Neutron Detector | Summer 2003| Los Alamos National Laboratory. Lanl.gov. Retrieved on 2011-11-08.
  15. ^ NCNR Neutron Spin Filters. Ncnr.nist.gov (2004-04-28). Retrieved on 2011-11-08.
  16. ^ ILL 3He spin filters. Ill.eu (2010-10-22). Retrieved on 2011-11-08.
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Bibliography


Lighter:
diproton 		Helium-3 is an
isotope of helium 		Heavier:
helium-4
Decay product of:
lithium-4 (p)
hydrogen-3 (β−) 		Decay chain
of helium-3 		Decays to:
Stable
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