Protactinium

Protactinium is a chemical element; it has symbol Pa and atomic number 91. It is a dense, radioactive, silvery-gray actinide metal which readily reacts with oxygen, water vapor, and inorganic acids. It forms various chemical compounds, in which protactinium is usually present in the oxidation state +5, but it can also assume +4 and even +3 or +2 states. Concentrations of protactinium in the Earth's crust are typically a few parts per trillion, but may reach up to a few parts per million in some uraninite ore deposits. Because of its scarcity, high radioactivity, and high toxicity, there are currently no uses for protactinium outside scientific research, and for this purpose, protactinium is mostly extracted from spent nuclear fuel.

The element was first identified in 1913 by Kazimierz Fajans and Oswald Helmuth Göhring and named "brevium" because of the short half-life of the specific isotope studied, ^234mPa. A more stable isotope of protactinium, ²³¹Pa, was discovered in 1917/18 by Lise Meitner in collaboration with Otto Hahn, and they named the element protactinium. In 1949, the IUPAC chose the name "protactinium" and confirmed Hahn and Meitner as its discoverers. The new name meant "(nuclear) precursor of actinium," suggesting that actinium is a product of radioactive decay of protactinium. John Arnold Cranston (working with Frederick Soddy and Ada Hitchins) is also credited with discovering the most stable isotope in 1915, but he delayed his announcement due to being called for service in the First World War.

The longest-lived and most abundant (nearly 100%) naturally occurring isotope of protactinium, ²³¹Pa, has a half-life of 32,760 years and occurs in the decay chain of uranium-235. Much smaller trace amounts of the short-lived ²³⁴Pa and its nuclear isomer ^234mPa occur in the decay chain of uranium-238. ²³³Pa occurs as a result of the decay of thorium-233 as part of the chain of events necessary to produce uranium-233 by neutron irradiation of ²³²Th. It is an undesired intermediate product in thorium-based nuclear reactors, and is therefore removed from the active zone of the reactor during the breeding process. Ocean science uses the element to understand the ancient ocean's geography: analysis of the relative concentrations of various uranium, thorium, and protactinium isotopes in water and minerals is used in radiometric dating of sediments up to 175,000 years old, and in modeling of various geological processes.

Protactinium is unusual among non-primordial elements in that its natural isotopic composition is extremely uniform across typical terrestrial samples, because essentially all naturally occurring protactinium is ²³¹Pa, produced solely along a single pathway (namely, from the decay of primordial ²³⁵U).

History

thumb|left|upright=1.5|[[Dmitri Mendeleev's 1871 periodic table with a gap for protactinium on the bottom row of the chart, between thorium and uranium]]

In 1871, Dmitri Mendeleev predicted the existence of an element between thorium and uranium. For a long time, chemists searched for eka-tantalum as an element with similar chemical properties to tantalum, making a discovery of protactinium nearly impossible. Tantalum's heavier analogue was later found to be the transuranic element dubnium – although dubnium is more chemically similar to protactinium, not tantalum.

In 1900, William Crookes isolated protactinium as an intensely radioactive material from uranium; however, he could not characterize it as a new chemical element and thus named it uranium X (UX).<!--https://www.jstor.org/pss/96048 --> Crookes dissolved uranium nitrate in ether, and the residual aqueous phase contained most of the and . His method was used into the 1950s to isolate and from uranium compounds. Protactinium was first identified in 1913, when Kasimir Fajans and Oswald Helmuth Göhring encountered the isotope ^234mPa during their studies of the decay chains of uranium-238: → → → . They named the new element "brevium" (from the Latin word brevis, meaning brief or short) because of the short half-life of 1.16 minutes for (uranium&nbsp;X2). In 1917–18, two groups of scientists, Lise Meitner in collaboration with Otto Hahn of Germany and Frederick Soddy and John Cranston of Great Britain, independently discovered another isotope, ²³¹Pa, having a much longer half-life of 32,760 years. Meitner changed the name "brevium" to protactinium as the new element was part of the decay chain of uranium-235 as the parent of actinium (from the prôtos, meaning "first, before"). The IUPAC confirmed this naming in 1949. The discovery of protactinium completed one of the last gaps in early versions of the periodic table, and brought fame to the involved scientists.

Aristid von Grosse produced 2&nbsp;milligrams of Pa₂O₅ in 1927, and in 1934 first isolated elemental protactinium from 0.1&nbsp;milligrams of Pa₂O₅. He used two different procedures: in the first, protactinium oxide was irradiated by 35&nbsp;keV electrons in vacuum. In the other, called the van Arkel–de Boer process, the oxide was chemically converted to a halide (chloride, bromide or iodide) and then reduced in a vacuum with an electrically heated metallic filament:

: 2 PaI₅ → 2 Pa + 5 I₂

In 1961, the United Kingdom Atomic Energy Authority (UKAEA) produced 127&nbsp;grams of 99.9% pure protactinium-231 by processing 60&nbsp;tonnes of waste material in a 12-stage process, at a cost of about US$500,000.

==Isotopes==<!-- This section is linked from uranium -->

Thirty radioisotopes of protactinium have been discovered, ranging from ²¹⁰Pa to ²³⁹Pa. The most stable are ²³¹Pa with a half-life of 32,650 years, ²³³Pa with a half-life of 26.975 days, and ²³⁰Pa with a half-life of 17.4 days. All other isotopes have half-lives shorter than 1.6 days, and the majority of these have half-lives less than 1.8 seconds. Protactinium also has six nuclear isomers, with the most stable being ^234mPa (half-life 1.159 minutes).

The primary decay mode for the most stable isotope ²³¹Pa and lighter isotopes (²¹⁰Pa ²³³Pa, the other isotope of protactinium produced in nuclear reactors, also has a fission threshold of 1&nbsp;MeV.

Occurrence

Protactinium is one of the rarest and most expensive naturally occurring elements. It is found in the form of two isotopes, ²³¹Pa and ²³⁴Pa, with the isotope ²³⁴Pa occurring in two different energy states. Nearly all natural protactinium is ²³¹Pa. It is an alpha emitter and is formed by the decay of uranium-235, whereas the beta-radiating ²³⁴Pa is produced as a result of uranium-238 decay. Nearly all uranium-238 (99.8%) decays first to the shorter-lived ^234mPa isomer.

Protactinium occurs in uraninite (pitchblende) at concentrations of about 0.3–3 parts ²³¹Pa per million parts (ppm) of ore.), some ores from the Democratic Republic of the Congo have about 3&nbsp;ppm.

In nuclear reactors

Two major protactinium isotopes, ²³¹Pa and ²³³Pa, are produced from thorium in nuclear reactors; both are undesirable and are usually removed, thereby adding complexity to the reactor design and operation. In particular, ²³²Th, via (n, 2n) reactions, produces ²³¹Th, which quickly decays to ²³¹Pa (half-life 25.5 hours). The last isotope, while not a transuranic waste, has a long half-life of 32,760 years, and is a major contributor to the long-term radiotoxicity of spent nuclear fuel. ²³³Pa has a relatively long half-life of 27 days and high cross section for neutron capture (the so-called "neutron poison"). Thus, instead of rapidly decaying to the useful ²³³U, a significant fraction of ²³³Pa converts to non-fissile isotopes and consumes neutrons, degrading reactor efficiency. To limit the loss of neutrons, ²³³Pa is extracted from the active zone of thorium molten salt reactors during their operation, so that it can only decay into ²³³U. Extraction of ²³³Pa is achieved using columns of molten bismuth with lithium dissolved in it. In short, lithium selectively reduces protactinium salts to protactinium metal, which is then extracted from the molten-salt cycle, while the molten bismuth is merely a carrier, selected due to its low melting point of 271&nbsp;°C, low vapor pressure, good solubility for lithium and actinides, and immiscibility with molten halides.

Preparation

thumb|right|upright|Protactinium occurs in [[uraninite ores.]]

Before the advent of nuclear reactors, protactinium was separated for scientific experiments from uranium ores. Since reactors have become more common, it is mostly produced as an intermediate product of neutron capture on thorium, used for the production of the fissile ²³³U:

:<chem>^{232}_{90}Th + ^{1}_{0}n -> ^{233}_{90}Th ->[\beta^-][22.3\ \ce{min}] ^{233}_{91}Pa ->[\beta^-][26.975\ \ce{d}] ^{233}_{92}U.</chem>

The isotope ²³¹Pa can be prepared by irradiating ²³⁰Th with slow neutrons, converting it to the beta-decaying ²³¹Th; or, by irradiating ²³²Th with fast neutrons, generating (as one product) ²³¹Th and 2 neutrons.

Protactinium metal has been prepared by reduction of its fluoride with calcium, lithium, or barium at a temperature of 1300–1400&nbsp;°C. Protactinium is a metal with silvery-gray luster that is preserved for some time in air. Protactinium easily reacts with oxygen, water vapor, and acids, but not with alkalis. The thermal expansion coefficient of the tetragonal phase between room temperature and 700&nbsp;°C is 9.9/°C. It becomes superconductive at temperatures below 1.4&nbsp;K. Protactinium tetrachloride is paramagnetic at room temperature, but becomes ferromagnetic when cooled to 182&nbsp;K.

Protactinium exists in two major oxidation states: +4 and +5, both in solids and solutions; and the +3 and +2 states, which have been observed in some solids. As the electron configuration of the neutral atom is [Rn]5f²6d¹7s², the +5 oxidation state corresponds to the low-energy (and thus favored) 5f⁰ configuration. Both +4 and +5 states easily form hydroxides in water, with the predominant ions being Pa(OH)³⁺, , , and Pa(OH)₄, all of which are colorless. Other known protactinium ions include , , , , , , , , , and .

Chemical compounds

{| Class = "wikitable" style = "text-align: center"

! Formula

! color

! symmetry

! space group

! No

! Pearson symbol

! a (pm)

! b (pm)

! c (pm)

! Z

! density (g/cm³)

|-

| Pa

| silvery-gray

| tetragonal

| Fmm

| 225

| cF8

| 496.1

|

|

| 4

| 13.44

|-

| PaO₂

| black

| fcc

| I4₁/amd

| 141

| tI20

| 837.7

| 837.7

| 748.1

| 4

| 4.72

|-

| PaBr₄

| brown

| tetragonal

| C2/c

| 15

| mS24

| 797

| 1135

| 836

| 4

| 3.74

|-

| PaBr₅

| red

| monoclinic

| P2₁/c

| 14

| mP24

| 838.5

| 1120.5

| 1214.6

| 4

| 4.98

|-

| PaOBr₃

|

| monoclinic

|

|

|

| 696.9

| 895.9

| 1500.9

|

|

|-

| Pa₂P₂O₇

|

| cubic

|

|

|

| 709

| 875

| 1062

|

|

|}

Here, a, b, and c are lattice constants in picometers, No is the space group number, and Z is the number of formula units per unit cell; fcc stands for the face-centered cubic symmetry. Density was not measured directly but calculated from the lattice parameters.

Oxides and oxygen-containing salts

Protactinium oxides are known for the metal oxidation states +2, +4, and +5. The most stable is the white pentoxide Pa₂O₅, which can be produced by igniting protactinium(V) hydroxide in air at a temperature of 500&nbsp;°C. Its crystal structure is cubic, and the chemical composition is often non-stoichiometric, described as PaO_2.25. Another phase of this oxide with orthorhombic symmetry has also been reported. The monoxide PaO has only been observed as a thin coating on protactinium metal, but not in an isolated bulk form. The pentoxide Pa₂O₅ combines with rare-earth metal oxides R₂O₃ to form various nonstoichiometric mixed-oxides, also of perovskite structure.

Protactinium oxides are basic; they easily convert to hydroxides and can form various salts, such as sulfates, phosphates, nitrates, etc. The nitrate is usually white but can be brown due to radiolytic decomposition. Heating the nitrate in air at 400&nbsp;°C converts it to the white protactinium pentoxide. Protactinium(V) chloride forms yellow crystals where protactinium ions are arranged in pentagonal bipyramids and coordinated by 7 other ions. The coordination changes to octahedral in the brown protactinium(V) bromide, but is unknown for protactinium(V) iodide. The protactinium coordination in all its tetrahalides is 8, but the arrangement is square antiprismatic in protactinium(IV) fluoride and dodecahedral in the chloride and bromide. Brown-colored protactinium(III) iodide has been reported, where protactinium ions are 8-coordinated in a bicapped trigonal prismatic arrangement.

thumb|right|Coordination of protactinium (solid circles) and chlorine atoms (open circles) in protactinium(V) chloride.

Protactinium(V) chloride has a polymeric structure of monoclinic symmetry. There, within one polymeric chain, all chlorine atoms lie in one graphite-like plane and form planar pentagons around the protactinium ions. The 7-coordination of protactinium originates from the five chlorine atoms and two bonds to protactinium atoms belonging to the nearby chains. It easily hydrolyzes in water.

More complex protactinium fluorides are also known, such as Pa₂F₉ and ternary fluorides of the types MPaF₆ (M = Li, Na, K, Rb, Cs or NH₄), M₂PaF₇ (M = K, Rb, Cs or NH₄), and M₃PaF₈ (M = Li, Na, Rb, Cs), all of which are white crystalline solids. The MPaF₆ formula can be represented as a combination of MF and PaF₅. These compounds can be obtained by evaporating a hydrofluoric acid solution containing both complexes. For the small alkali cations like Na, the crystal structure is tetragonal, whereas it becomes orthorhombic for larger cations K⁺, Rb⁺, Cs⁺ or NH₄⁺. A similar variation was observed for the M₂PaF₇ fluorides: namely, the crystal symmetry was dependent on the cation and differed for Cs₂PaF₇ and M₂PaF₇ (M = K, Rb or NH₄).

Other inorganic compounds

Oxyhalides and oxysulfides of protactinium are known. PaOBr₃ has a monoclinic structure composed of double-chain units where protactinium has coordination 7 and is arranged into pentagonal bipyramids. The chains are interconnected through oxygen and bromine atoms, and each oxygen atom is related to three protactinium atoms.

Organometallic compounds

thumb|upright|The proposed structure of the protactinocene (Pa(C₈H₈)₂) molecule

Protactinium(IV) forms a tetrahedral complex tetrakis(cyclopentadienyl)protactinium(IV) (or Pa(C₅H₅)₄) with four cyclopentadienyl rings, which can be synthesized by reacting protactinium(IV) chloride with Be(C₅H₅)₂. One ring can be substituted with a halide atom. Another organometallic complex is the golden-yellow bis(π-cyclooctatetraene) protactinium, or protactinocene (Pa(C₈H₈)₂), which is analogous in structure to uranocene. There, the metal atom is sandwiched between two cyclooctatetraene ligands. Similar to uranocene, it can be prepared by reacting protactinium tetrachloride with dipotassium cyclooctatetraenide (K₂C₈H₈) in tetrahydrofuran. However, the possibility of criticality of ²³¹Pa has since been ruled out.

With the advent of highly sensitive mass spectrometers, an application of ²³¹Pa as a tracer in geology and paleoceanography has become possible. In this application, the ratio of ²³¹Pa to ²³⁰Th is used for radiometric dating of sediments which are up to 175,000 years old, and in modeling of the formation of minerals.<!--10.1016/S0016-7037(98)00255-5--> Some of the protactinium-related dating variations rely on analysis of the relative concentrations of several long-living members of the uranium decay chain – uranium, protactinium, and thorium, for example. These elements have 6, 5, and 4 valence electrons, thus favoring +6, +5, and +4 oxidation states respectively, and display different physical and chemical properties. Thorium and protactinium, but not uranium compounds, are poorly soluble in aqueous solutions and precipitate into sediments; the precipitation rate is faster for thorium than for protactinium. The concentration analysis for both protactinium-231 (half-life 32,760 years) and ²³⁰Th (half-life 75,380 years) improves measurement accuracy compared to when only one isotope is measured; this double-isotope method is also weakly sensitive to inhomogeneities in the spatial distribution of the isotopes and to variations in their precipitation rate.

Precautions

Protactinium is both toxic and highly radioactive; thus, it is handled exclusively in a sealed glove box. Its major isotope ²³¹Pa has a specific activity of per gram and primarily emits alpha particles, which can be stopped by a thin layer of any material. However, it slowly decays into ²²⁷Ac, and then follows the more rapid actinium series, making its total activity (alpha, beta, and gamma) greater than one would calculate from that figure.

As protactinium is present in small amounts in most natural products and materials, it is ingested with food or water and inhaled with air. Only about 0.05% of ingested protactinium is absorbed into the blood and the remainder is excreted. From the blood, about 40% of the protactinium deposits in the bones, about 15% goes to the liver, 2% to the kidneys, and the rest leaves the body. The biological half-life of protactinium is about 50 years in the bones, whereas its biological half-life in other organs has a fast and slow component. For example, 70% of the protactinium in the liver has a biological half-life of 10 days, and the remaining 30% for 60 days. The corresponding values for kidneys are 20% (10 days) and 80% (60 days). In each affected organ, protactinium promotes cancer via its radioactivity. The maximum allowed concentrations of ²³¹Pa in the air in Germany is .

See also

• Ada Hitchins, who helped Soddy in discovering the element protactinium

Notes