Deuterium Wars Review
Isotope of hydrogen with 1 neutronDeuterium, hydrogen-2, 2HGeneral2Hdeuterium, H-2, hydrogen-2110.0115% (Earth)2.11 +13135.720± 0.0012224.52± 0.20 keVDeuterium (or hydrogen-2, symbol 2HorD, also known as heavy hydrogen) is one of two of (the other being, or hydrogen-1). The of a deuterium atom, called a deuteron, contains one and one, whereas the far more common protium has no neutrons in the nucleus. Deuterium has a in Earth's of about one in 6420 of hydrogen. Thus deuterium accounts for approximately 0.02% (0.03% by mass) of all the naturally occurring hydrogen in the oceans, while protium accounts for more than 99.98%. The abundance of deuterium changes slightly from one kind of natural water to another (see ).The name deuterium is derived from the Greek deuteros, meaning 'second', to denote the two particles composing the nucleus. Deuterium was discovered and named in 1931.
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When the neutron was discovered in 1932, this made the nuclear structure of deuterium obvious, and Urey won the in 1934 “for his discovery of heavy hydrogen”. Soon after deuterium's discovery, Urey and others produced samples of ' in which the deuterium content had been highly concentrated.Deuterium is destroyed in the interiors of stars faster than it is produced. Other natural processes are thought to produce only an insignificant amount of deuterium. Nearly all deuterium found in nature was produced in the 13.8 billion years ago, as the basic or primordial ratio of hydrogen-1 to deuterium (about 26 atoms of deuterium per million hydrogen atoms) has its origin from that time.
This is the ratio found in the gas giant planets, such as Jupiter. The analysis of deuterium–protium ratios in comets found results very similar to the mean ratio in Earth's oceans (156 atoms of deuterium per million hydrogen atoms). This reinforces theories that much of Earth's ocean water is of cometary origin. The deuterium–protium ratio of the comet, as measured by the, is about three times that of earth water. This figure is the highest yet measured in a comet.Deuterium–protium ratios thus continue to be an active topic of research in both astronomy and climatology. Deuterium discharge tubeDeuterium is frequently represented by the D.

Since it is an isotope of with 2, it is also represented by 2H. Allows both D and 2H, although 2His preferred. A distinct chemical symbol is used for convenience because of the isotope's common use in various scientific processes. Also, its large mass difference with ( 1H) (deuterium has a mass of 2.014 102, compared to the hydrogen of 1.007 947 u, and protium's mass of 1.007 825 u) confers non-negligible chemical dissimilarities with protium-containing compounds, whereas the isotope weight ratios within other chemical elements are largely insignificant in this regard.Spectroscopy In the energy levels of electrons in atoms depend on the of the system of electron and nucleus.
For the, the role of reduced mass is most simply seen in the of the atom, where the reduced mass appears in a simple calculation of the and Rydberg equation, but the reduced mass also appears in the, and the for calculating atomic energy levels.The reduced mass of the system in these equations is close to the mass of a single electron, but differs from it by a small amount about equal to the ratio of mass of the electron to the atomic nucleus. For hydrogen, this amount is about 1837/1836, or 1.000545, and for deuterium it is even smaller: 3671/3670, or 1.0002725. The energies of spectroscopic lines for deuterium and light hydrogen therefore differ by the ratios of these two numbers, which is 1.000272.
The wavelengths of all deuterium spectroscopic lines are shorter than the corresponding lines of light hydrogen, by a factor of 1.000272. In astronomical observation, this corresponds to a blue Doppler shift of 0.000272 times the speed of light, or 81.6 km/s.The differences are much more pronounced in vibrational spectroscopy such as and, and in rotational spectra such as because the of the deuterium is markedly higher than that of protium. In, deuterium has a very different frequency (e.g.
61 MHz when protium is at 400 MHz) and is much less sensitive. Deuterated solvents are usually used in protium NMR to prevent the solvent from overlapping with the signal, although on its own right is also possible.Big Bang nucleosynthesis. Main article:Deuterium is thought to have played an important role in setting the number and ratios of the elements that were formed in the Big Bang. Combining thermodynamics and the changes brought about by cosmic expansion, one can calculate the fraction of protons and neutrons based on the temperature at the point that the universe cooled enough to allow formation of nuclei.
This calculation indicates seven protons for every neutron at the beginning of nucleogenesis, a ratio that would remain stable even after nucleogenesis was over. This fraction was in favor of protons initially, primarily because the lower mass of the proton favored their production. As the universe expanded, it cooled. And protons are less stable than helium nuclei, and the protons and neutrons had a strong energetic reason to form helium-4. However, forming helium-4 requires the intermediate step of forming deuterium.Through much of the few minutes after the big bang during which nucleosynthesis could have occurred, the temperature was high enough that the mean energy per particle was greater than the binding energy of weakly bound deuterium; therefore any deuterium that was formed was immediately destroyed. This situation is known as the deuterium bottleneck. The bottleneck delayed formation of any helium-4 until the universe became cool enough to form deuterium (at about a temperature equivalent to 100 keV).
At this point, there was a sudden burst of element formation (first deuterium, which immediately fused to helium). However, very shortly thereafter, at twenty minutes after the Big Bang, the universe became too cool for any further nuclear fusion and nucleosynthesis to occur. At this point, the elemental abundances were nearly fixed, with the only change as some of the products of big bang nucleosynthesis (such as ) decay.
The deuterium bottleneck in the formation of helium, together with the lack of stable ways for helium to combine with hydrogen or with itself (there are no stable nuclei with mass numbers of five or eight) meant that an insignificant amount of carbon, or any elements heavier than carbon, formed in the Big Bang. These elements thus required formation in stars. At the same time, the failure of much nucleogenesis during the Big Bang ensured that there would be plenty of hydrogen in the later universe available to form long-lived stars, such as our Sun.Abundance Deuterium occurs in trace amounts naturally as deuterium, written 2H2 or D 2, but most natural occurrence in the is bonded with a typical 1Hatom, a gas called (HD or 1H2H).The existence of deuterium on Earth, elsewhere in the (as confirmed by planetary probes), and in the spectra of, is also an important datum in. Gamma radiation from ordinary nuclear fusion dissociates deuterium into protons and neutrons, and there are no known natural processes other than the, which might have produced deuterium at anything close to its observed natural abundance (deuterium is produced by the rare, and occasional absorption of naturally occurring neutrons by light hydrogen, but these are trivial sources). There is thought to be little deuterium in the interior of the Sun and other stars, as at these temperatures the that consume deuterium happen much faster than the that creates deuterium. However, deuterium persists in the outer solar atmosphere at roughly the same concentration as in Jupiter, and this has probably been unchanged since the origin of the Solar System.
The natural abundance of deuterium seems to be a very similar fraction of hydrogen, wherever hydrogen is found, unless there are obvious processes at work that concentrate it.The existence of deuterium at a low but constant primordial fraction in all hydrogen is another one of the arguments in favor of the theory over the of the universe. The observed ratios of hydrogen to helium to deuterium in the universe are difficult to explain except with a Big Bang model. It is estimated that the abundances of deuterium have not evolved significantly since their production about 13.8 billion years ago. Measurements of Milky Way galactic deuterium from ultraviolet spectral analysis show a ratio of as much as 23 atoms of deuterium per million hydrogen atoms in undisturbed gas clouds, which is only 15% below the estimated primordial ratio of about 27 atoms per million from the Big Bang. This has been interpreted to mean that less deuterium has been destroyed in star formation in our galaxy than expected, or perhaps deuterium has been replenished by a large in-fall of primordial hydrogen from outside the galaxy.
In space a few hundred light years from the Sun, deuterium abundance is only 15 atoms per million, but this value is presumably influenced by differential adsorption of deuterium onto carbon dust grains in interstellar space.The abundance of deuterium in the atmosphere of has been directly measured by the as 26 atoms per million hydrogen atoms. ISO-SWS observations find 22 atoms per million hydrogen atoms in Jupiter. And this abundance is thought to represent close to the primordial solar system ratio. This is about 17% of the terrestrial deuterium-to-hydrogen ratio of 156 deuterium atoms per million hydrogen atoms.Cometary bodies such as and have been measured to contain relatively more deuterium (about 200 atoms D per million hydrogens), ratios which are enriched with respect to the presumed protosolar nebula ratio, probably due to heating, and which are similar to the ratios found in Earth seawater. The recent measurement of deuterium amounts of 161 atoms D per million hydrogen in Comet (a former object), a ratio almost exactly that in Earth's oceans, emphasizes the theory that Earth's surface water may be largely comet-derived. Most recently the deuterium–protium (D–H) ratio of as measured by Rosetta is about three times that of Earth water, a figure that is high.
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This has caused renewed interest in suggestions that Earth's water may be partly of asteroidal origin.Deuterium has also observed to be concentrated over the mean solar abundance in other terrestrial planets, in particular Mars and Venus.Production. This section does not any. Unsourced material may be challenged and.Find sources: – ( February 2019) Deuterium is produced for industrial, scientific and military purposes, by starting with ordinary water—a small fraction of which is naturally-occurring —and then separating out the heavy water by the, distillation, or other methods.In theory, deuterium for heavy water could be created in a nuclear reactor, but separation from ordinary water is the cheapest bulk production process.The world's leading supplier of deuterium was until 1997, when the last heavy water plant was shut down. Canada uses heavy water as a for the operation of the design.Another major producer of heavy water is India. All but one of India's atomic energy plants are pressurised heavy water plants, which use natural (i.e., not enriched) uranium. India has eight heavy water plants, of which seven are in operation. Six plants, of which five are in operation, are based on D–H exchange in ammonia gas.
The other two plants extract deuterium from natural water in a process that uses hydrogen sulphide gas at high pressure.While India is self-sufficient in heavy water for its own use, India now also exports reactor-grade heavy water.Properties Physical properties The physical properties of deuterium compounds can exhibit significant and other physical and chemical property differences from the protium analogs., for example, is more than. Chemically, there are differences in bond energy and length for compounds of heavy hydrogen isotopes compared to protium, which are larger than the isotopic differences in any other element. Bonds involving deuterium and are somewhat stronger than the corresponding bonds in protium, and these differences are enough to cause significant changes in biological reactions. Pharmaceutical firms are interested in the fact that deuterium is harder to remove from carbon than protium.Deuterium can replace protium in water molecules to form heavy water (D 2O), which is about 10.6% denser than normal water (so that ice made from it sinks in ordinary water).
Heavy water is slightly toxic in animals, with 25% substitution of the body water causing cell division problems and sterility, and 50% substitution causing death by cytotoxic syndrome (bone marrow failure and gastrointestinal lining failure). Organisms, however, can survive and grow in pure heavy water, though they develop slowly. Despite this toxicity, consumption of heavy water under normal circumstances does not pose a to humans.
It is estimated that a 70 kg (154 lb) person might drink 4.8 litres (1.3 US gal) of heavy water without serious consequences. Small doses of heavy water (a few grams in humans, containing an amount of deuterium comparable to that normally present in the body) are routinely used as harmless metabolic tracers in humans and animals.Quantum properties The deuteron has +1 (') and is thus a.
The frequency of deuterium is significantly different from common light hydrogen. Also easily differentiates many deuterated compounds, due to the large difference in IR absorption frequency seen in the vibration of a chemical bond containing deuterium, versus light hydrogen. The two stable isotopes of hydrogen can also be distinguished by using.The triplet deuteron nucleon is barely bound at E B = 2.23 MeV, and none of the higher energy states are bound. The singlet deuteron is a virtual state, with a negative binding energy of 60 keV. There is no such stable particle, but this virtual particle transiently exists during neutron-proton inelastic scattering, accounting for the unusually large neutron scattering cross-section of the proton.
Nuclear properties (the deuteron) Deuteron mass and radius The nucleus of deuterium is called a deuteron. It has a mass of 2.013 553 212 745(40) u (equal to 1875.612 928(12) MeV)The of the deuteron is 2.127 99(14).Like the, measurements using deuterium produce a smaller result: 2.125 62(78). Ionized deuterium in a reactor giving off its characteristic pinkish-red glowDeuterium is used in, usually as liquid D 2O, to slow neutrons without the high neutron absorption of ordinary hydrogen. This is a common commercial use for larger amounts of deuterium.In, liquid D 2 is used in to moderate neutrons to very low energies and wavelengths appropriate for.Experimentally, deuterium is the most common nuclide used in reactor designs, especially in combination with, because of the large reaction rate (or ) and high yield of the D–T reaction. There is an even higher-yield D– fusion reaction, though the of D– 3Heis higher than that of most other fusion reactions; together with the scarcity of 3He, this makes it implausible as a practical power source until at least D–T and D–D fusion reactions have been performed on a commercial scale. Commercial nuclear fusion is not yet an accomplished technology.NMR spectroscopy. Emission spectrum of an ultravioletDeuterium is most commonly used in hydrogen in the following way.
NMR ordinarily requires compounds of interest to be analyzed as dissolved in solution. Because of deuterium's nuclear spin properties which differ from the light hydrogen usually present in organic molecules, NMR spectra of hydrogen/protium are highly differentiable from that of deuterium, and in practice deuterium is not 'seen' by an NMR instrument tuned for light-hydrogen. Deuterated solvents (including heavy water, but also compounds like deuterated chloroform, CDCl 3) are therefore routinely used in NMR spectroscopy, in order to allow only the light-hydrogen spectra of the compound of interest to be measured, without solvent-signal interference.Nuclear magnetic resonance spectroscopy can also be used to obtain information about the deuteron's environment in isotopically labelled samples. For example, the flexibility in the tail, which is a long hydrocarbon chain, in deuterium-labelled lipid molecules can be quantified using solid state deuterium NMR.Deuterium NMR spectra are especially informative in the solid state because of its relatively small quadrupole moment in comparison with those of bigger quadrupolar nuclei such as chlorine-35, for example.Tracing In, and, deuterium is used as a non-radioactive, for example, in the. In and, deuterium behaves somewhat similarly to ordinary hydrogen (with a few chemical differences, as noted).
It can be distinguished from ordinary hydrogen most easily by its mass, using. Deuterium can be detected by spectroscopy, since the mass difference drastically affects the frequency of molecular vibrations; deuterium-carbon bond vibrations are found in spectral regions free of other signals.Measurements of small variations in the natural abundances of deuterium, along with those of the stable heavy oxygen isotopes 17O and 18O, are of importance in, to trace the geographic origin of Earth's waters.

The heavy isotopes of hydrogen and oxygen in rainwater (so-called ) are enriched as a function of the environmental temperature of the region in which the precipitation falls (and thus enrichment is related to mean latitude). The relative enrichment of the heavy isotopes in rainwater (as referenced to mean ocean water), when plotted against temperature falls predictably along a line called the (GMWL). This plot allows samples of precipitation-originated water to be identified along with general information about the climate in which it originated. Evaporative and other processes in bodies of water, and also ground water processes, also differentially alter the ratios of heavy hydrogen and oxygen isotopes in fresh and salt waters, in characteristic and often regionally distinctive ways. The ratio of concentration of 2H to 1H is usually indicated with a delta as δ 2H and the geographic patterns of these values are plotted in maps termed as isoscapes. Stable isotopes are incorporated into plants and animals and an analysis of the ratios in a migrant bird or insect can help suggest a rough guide to their origins. Contrast properties techniques particularly profit from availability of deuterated samples: The H and D cross sections are very distinct and different in sign, which allows contrast variation in such experiments.
Further, a nuisance problem of ordinary hydrogen is its large incoherent neutron cross section, which is nil for D. The substitution of deuterium atoms for hydrogen atoms thus reduces scattering noise.Hydrogen is an important and major component in all materials of organic chemistry and life science, but it barely interacts with X-rays. As hydrogen (and deuterium) interact strongly with neutrons, neutron scattering techniques, together with a modern deuteration facility, fills a niche in many studies of macromolecules in biology and many other areas.Nuclear weapons This is discussed below. It is notable that although most stars, including the Sun, generate energy over most of their lives by fusing hydrogen into heavier elements, such fusion of light hydrogen (protium) has never been successful in the conditions attainable on Earth.
Thus, all artificial fusion, including the hydrogen fusion that occurs in so-called hydrogen bombs, requires heavy hydrogen (either tritium or deuterium, or both) in order for the process to work.Drugs. Main article:A deuterated drug is a medicinal product in which one or more of the atoms contained in the drug molecule have been replaced by deuterium. Because of the, deuterium-containing drugs may have significantly lower rates of, and hence a longer.
In 2017, became the first deuterated drug to receive FDA approval. Reinforced essential nutrients Deuterium can be used to reinforce specific oxidation-vulnerable C-H bonds within essential or conditionally, such as certain, or (PUFA), making them more resistant to oxidative damage. Polyunsaturated, such as, slow down the chain reaction of that damage living cells. Deuterated ethyl ester of linoleic acid , developed by Retrotope, is in a in and has successfully completed a Phase I/II trial in.
History Suspicion of lighter element isotopes The existence of nonradioactive isotopes of lighter elements had been suspected in studies of neon as early as 1913, and proven by mass spectrometry of light elements in 1920. The prevailing theory at the time was that isotopes of an element differ by the existence of additional protons in the nucleus accompanied by an equal number of. In this theory, the deuterium nucleus with mass two and charge one would contain two protons and one nuclear electron. However, it was expected that the element hydrogen with a measured average atomic mass very close to 1 u, the known mass of the proton, always has a nucleus composed of a single proton (a known particle), and could not contain a second proton. Thus, hydrogen was thought to have no heavy isotopes.Deuterium detected.
Harold UreyIt was first detected spectroscopically in late 1931 by, a chemist at. Urey's collaborator, five of to 1 of liquid, using the low-temperature physics laboratory that had recently been established at the National Bureau of Standards in Washington, D.C. The technique had previously been used to isolate heavy isotopes of neon. The cryogenic boiloff technique concentrated the fraction of the mass-2 isotope of hydrogen to a degree that made its spectroscopic identification unambiguous.
Naming of the isotope and Nobel Prize Urey created the names protium, deuterium, and tritium in an article published in 1934. The name is based in part on advice from who had proposed the name 'deutium'. The name is derived from the, Greek deuteros (second), and the nucleus to be called 'deuteron' or 'deuton'. Isotopes and new elements were traditionally given the name that their discoverer decided.
Some British scientists, such as, wanted the isotope to be called 'diplogen', from the Greek diploos (double), and the nucleus to be called diplon.The amount inferred for normal abundance of this heavy isotope of hydrogen was so small (only about 1 atom in 6400 hydrogen atoms in ocean water (156 deuteriums per million hydrogens)) that it had not noticeably affected previous measurements of (average) hydrogen atomic mass. This explained why it hadn't been experimentally suspected before. Urey was able to concentrate water to show partial enrichment of deuterium. Lewis had prepared the first samples of pure heavy water in 1933. The discovery of deuterium, coming before the discovery of the in 1932, was an experimental shock to theory, but when the neutron was reported, making deuterium's existence more explainable, deuterium won Urey the in 1934. Lewis was embittered by being passed over for this recognition given to his former student. 'Heavy water' experiments in World War II.
Main article:Shortly before the war, and moved their research on neutron moderation from France to Britain, smuggling the entire global supply of heavy water (which had been made in Norway) across in twenty-six steel drums.During, was known to be conducting experiments using heavy water as moderator for a design. Such experiments were a source of concern because they might allow them to produce for an. Ultimately it led to the operation called the ', the purpose of which was to destroy the deuterium production/enrichment facility in Norway.
At the time this was considered important to the potential progress of the war.After World War II ended, the Allies discovered that Germany was not putting as much serious effort into the program as had been previously thought. They had been unable to sustain a chain reaction.
The Germans had completed only a small, partly built experimental reactor (which had been hidden away). By the end of the war, the Germans did not even have a fifth of the amount of heavy water needed to run the reactorpartially due to the Norwegian heavy water sabotage operation. However, even had the Germans succeeded in getting a reactor operational (as the U.S. Did with a graphite reactor in late 1942), they would still have been at least several years away from development of an with maximal effort. The engineering process, even with maximal effort and funding, required about two and a half years (from first critical reactor to bomb) in both the U.S. And, for example.In thermonuclear weapons. A view of the Sausage device casing of the, with its instrumentation and cryogenic equipment attached.
This bomb held a cryogenic Dewar flask containing room for as much as 160 kilograms of liquid deuterium. The bomb was 20 feet tall. Kris star ghost loop pictures. Note the seated man at the right of the photo for the scale.The 62-ton device built by the United States and exploded on 1 November 1952, was the first fully successful '. In this context, it was the first bomb in which most of the energy released came from stages that followed the primary stage of the.
The Ivy Mike bomb was a factory-like building, rather than a deliverable weapon. At its center, a very large cylindrical, insulated or, held liquid deuterium in a volume of about 1000 (160 kilograms in mass, if this volume had been completely filled). Then, a conventional (the 'primary') at one end of the bomb was used to create the conditions of extreme temperature and pressure that were needed to set off the.Within a few years, so-called 'dry' hydrogen bombs were developed that did not need cryogenic hydrogen.
Released information suggests that all built since then contain of deuterium and lithium in their secondary stages. The material that contains the deuterium is mostly, with the lithium consisting of the isotope. When the lithium-6 is bombarded with fast from the atomic bombis produced, and then the deuterium and the tritium quickly engage in, releasing abundant energy, and even more free neutrons.Modern research In August 2018, scientists announced the transformation of gaseous deuterium into a. This may help researchers better understand, such as Jupiter, Saturn and related, since such planets are thought to contain a lot of liquid metallic hydrogen, which may be responsible for their observed powerful.