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Pu 94

Plutonium (Pu)

actinide
Período: 7 Bloco: f

Solid

Peso atômico padrão

[244]

Configuração eletrônica

[Rn] 7s2 5f6

Ponto de fusão

639,85 °C

Ponto de ebulição

3227,85 °C

Densidade

1,984e+4 kg/m³

Estados de oxidação

+2, +3, +4, +5, +6, +7, +8

Eletronegatividade (Pauling)

1,28

Energia de ionização (1ª)

6,02576 eV

Ano da descoberta

1941

Raio atômico

175 pm

Detalhes

Origem do nome Named for the planet Pluto.
País da descoberta United States
Descobridores G.T.Seaborg, J.W.Kennedy, E.M.McMillan, A.C.Wohl

Plutonium is a radioactive actinide metal and the element after neptunium. It is produced mainly by neutron capture in uranium in nuclear reactors, although minute natural traces occur in uranium ores. Its chemistry is dominated by multiple accessible oxidation states and by strong hydrolysis and complex formation in water. The fissile isotope ²³⁹Pu is technologically important in nuclear weapons and in some reactor fuels, while ²³⁸Pu is valued as a compact heat source.

Plutonium is unique among the elements in its physicochemical complexities by virtue of its position at a transitional location in the periodic table where the 5f electrons are at the border between delocalized (not associated with a single atom) and localized (associated with a single atom) behavior and it is considered one of the most complex of the elements. Plutonium also sits near the juncture where the actinide series transitions from main d-block element chemistry to rare earth like behavior as a result of the actinide contraction. Because of its defense and commercial importance, plutonium is one of the most intensely investigated of elements.

Plutonium metal has a bright silvery appearance at first and takes on a dull gray, yellow or olive green tarnish when oxidized in air. A relatively large piece of plutonium is warm to the touch because of the energy given off by alpha decay. Larger pieces will produce enough heat to boil water. The metal readily dissolves in concentrated mineral acids. Plutonium metal normally has six allotropes or crystal structures; alpha (α), beta (β), gamma (γ), delta (δ), delta prime (δ') and epsilon (ε). It forms a seventh phase (zeta, ζ) under high temperature and a limited pressure range. These allotropes have very similar energy levels but significantly varying densities (from 16.00 to 19.86 grams/cm3) and crystal structures. This makes plutonium very sensitive to changes in temperature, pressure, or chemistry, and allows for dramatic volume changes following phase transitions. At room temperature plutonium is in its alpha (α) form, the most common structural form of the element. It is as hard and brittle as cast iron unless alloyed with other metals to form the room-temperature stabilized delta (δ) phase which makes it soft and ductile. Unlike most metals, it is not a good conductor of heat or electricity. It has a low melting point (640 °C) and an unusually high boiling point (3,228 °C).

Plutonium can form alloys and intermediate compounds with most other metals. Gallium, aluminum, americium, scandium and cerium can stabilize the δ phase of plutonium metal. Nuclear fuel pellets can be formed by alloying plutonium with various metals such as: aluminum; zirconium; cerium; cerium-cobalt; uranium-titanium, uranium-zirconium and uranium-molybdenum. Thorium-plutonium-uranium alloys were investigated as a nuclear fuel for fast breeder reactors. A plutonium-gallium-cobalt alloy (PuCoGa5) was found to be an unconventional superconductor, showing superconductivity below 18.5 Kelvin, an order of magnitude higher than the highest between heavy fermion systems known.

Plutonium forms compounds with a variety of other elements. Plutonium reacts with pure hydrogen, forming plutonium hydrides. It also reacts readily with oxygen, forming PuO and PuO2 as well as intermediate and sub-stoichiometric oxides. The metal reacts with the halogens, giving rise to trivalent Pu compounds with the general formula PuX3 where X can be F, Cl, Br or I and tetravalent plutonium compounds such as PuF4. The following oxyhalides are observed: PuOCl, PuOBr and PuOI. Plutonium reacts with carbon to form PuC, nitrogen to form PuN and silicon to form PuSi2. Pu3+ and Pu4+ oxalates are important intermediates that are calcined to form oxides as a step in plutonium processing. Other important compounds in reprocessing are fluoride, peroxide, acetylacetone, carbonate and hydroxide.

The color displayed by plutonium solutions depends on both the oxidation state and the extent of complexation by various ligands. In aqueous solution plutonium exhibits five ionic valence states: Pu+3 (blue lavender), Pu+4 (salmon-colored, when uncomplexed), PuO+ (lavender), PuO+2 (orange-brown) and PuOxOHy (dark green in basic solution). The pentavalent ion, PuO+ is unstable in aqueous solutions and it disproportionates into Pu+4 and PuO+2. However, PuO2+ can be stabilized in aqueous solution in a narrow pH range around 4.5. By virtue of the close proximity of the electrode potentials of the various plutonium redox couples (~ 1 Volt/NHE), four oxidation states can co-exist in solution simultaneously: Pu3+, Pu4+, PuO2+ and PuO22+.

Pu4+ is a "hard" (ionic) cation with the largest electronic charge of plutonium ions and it forms complexes with a variety of inorganic and organic ligands. In dilute perchloric acid, Pu4+ is un-complexed and is salmon-colored. However in concentrated acids, Pu4+ forms anionic complexes such as: Pu(NO3)62- (dark green) and Pu(Cl)62- (brick red). Pu4+, having a high ionic charge readily hydrolyzes (combines with hydroxide ion) at near-neutral pH values forming a green colloidal suspension that behaves like a solution but is actually a solid precipitate that can be separated by ultra-centrifugation.

Plutonium-organic complexes are very important for separation, reprocessing, and purification and include: Tributyl phosphate (TBP); Di-(2-ethylhexyl)phosphoric acid (DEHPA or HDEHP); octyl(phenyl)-N,N-diisobutyl-carbamoylmethylphosphine oxide (CMPO); crown-ethers; and many others.

Plutonium was first produced by Glenn T. Seaborg, Joseph W. Kennedy, Edward M. McMillan and Arthur C. Wohl by bombarding an isotope of uranium, uranium-238, with deuterons that had been accelerated in a device called a cyclotron. This created neptunium-238 and two free neutrons. Neptunium-238 has a half-life of 2.1 days and decays into plutonium-238 through beta decay. Although they conducted their work at the University of California in 1941, their discovery was not revealed to the rest of the scientific community until 1946 because of wartime security concerns. Plutonium's most stable isotope, plutonium-244, has a half-life of about 82,000,000 years. It decays into uranium-240 through alpha decay. Plutonium-244 will also decay through spontaneous fission.

Plutonium is the second transuranium element of the actinide series. Element 93 was discovered in 1940/41 by Glenn T. Seaborg, Edwin M. McMillan, J. W. Kennedy, and A. C. Wahl by deuteron bombardment of uranium-238 in the 60-inch cyclotron at the University of California, Berkeley Lab. They first synthesized neptunium-238 (half-life 2.1 days) which subsequently beta-decayed to form a new heavier element with atomic number 94 and atomic weight 238 (half-life 87.7 years). It was fitting that element 94 be named after the next planetoid, Pluto following the precedence that uranium was named after the planet Uranus and neptunium after the planet Neptune. Seaborg submitted a paper to the journal Physical Review in March 1941 documenting the discovery, but the paper was quickly withdrawn when it was found that an isotope of plutonium, Pu-239 could undergo nuclear fission making it useful in developing an atomic bomb. Pu-239 had a fission cross-section 50% greater than that of 235U, the best fissioning element known at that time.

Seaborg was called away from Berkeley to lead the Plutonium Production Lab or "Met Lab" at the University of Chicago. The Met Lab was to produce useful quantities of plutonium as part of the secret Manhattan Project during World War II to develop an atomic bomb. On August 18, 1942, a trace quantity of plutonium was isolated and measured at the Met Lab for the first time. About 50 micrograms of Pu-239 combined with uranium and fission products was produced and only about 1 microgram was isolated. This was enough material for chemists to determine the new element's atomic weight. In November 1943 a few milligrams of PuF3 was reduced to create the first sample of plutonium metal. Enough plutonium was produced to make it the first man-made element to be visible to the unaided eye.

The nuclear properties of plutonium-239 were also being studied and researchers found that when hit with a neutron it fissions by releasing energy and more neutrons. These neutrons can hit neighboring atoms of Pu-239 and so on, in an exponentially fast chain-reaction, releasing a tremendous amount of energy. This energy could result in an explosion large enough to destroy a city or fuel a nuclear reactor.

During WW II the three primary research and production sites of the Manhattan Project were the Plutonium Production Facility at what is now the Hanford Site, Washington, the Uranium Enrichment facilities at Oak Ridge, Tennessee, and the weapons research and design laboratory, now known as Los Alamos National Laboratory. In 1943, the first production reactor that made Pu-239 was the X-10 Graphite Reactor built at a facility in Oak Ridge, Tennessee that later became the Oak Ridge National Laboratory.

The Manhattan Project produced the plutonium for the "Trinity Test" conducted in New Mexico by Los Alamos Laboratory Director Robert Oppenheimer and Army General Leslie Groves. The world’s first atomic bomb ("The Gadget") was exploded near Socorro, New Mexico on July 16, 1945, resulting in an explosion with an energy equivalent of approximately 20,000 tons of TNT. The first atomic bomb used in war had a uranium core and was dropped on Hiroshima, Japan on August 6, 1945. The second atomic bomb used had a plutonium core and was nicknamed "Fat Man" because of its round shape. It was used to destroy Nagasaki, Japan in August 9, 1945, which put an end to WW II.

Publication of the discovery and the naming of the new element plutonium was delayed until a year after the end of World War II. Seaborg originally considered the name "plutium", but later thought that it did not sound as good as "plutonium."

Later, during the Cold-War era, large stockpiles of weapons-grade plutonium were built up by both the Soviet Union and the United States. Each year about 20 tons of plutonium is still produced as a by-product of the nuclear power industry. As of 2007 it was estimated that the plutonium stockpile was about 500 tons, world-wide. Since the end of the Cold War these stockpiles have become a focus of nuclear proliferation concerns. In 2000, the United States and the Russian Federation mutually agreed to each dispose of 34 tons of weapon grade plutonium before the end of 2019 by converting it to a mixed uranium-plutonium oxide (MOX) fuel to be used in commercial nuclear power reactors.

Today plutonium-239 remains an important component of nuclear weapons, and the United States maintains plutonium-related capabilities in support of national defense and global nuclear deterrence. Pu-239 for civilian nuclear power plants provides energy for many nations. Plutonium-238 continues to be vital to space exploration pushing the limits beyond which manned space exploration is possible and satisfying our quest for knowledge.

Imagens

Propriedades

Química

Eletronegatividade (Pauling)
1,28 Comparar Eletronegatividade (Pauling) de todos os elementos →
Afinidade eletrônica
-0,5 eV (valor negativo — prevê-se que o átomo não capte um eletrão adicional)
Energia de ionização (1ª)
6,02576 eV Comparar Energia de ionização (1ª) de todos os elementos →
Energia de ionização (2ª)
11,50004 eV Comparar Energia de ionização (2ª) de todos os elementos →
Energia de ionização (3ª)
21,100073 eV Comparar Energia de ionização (3ª) de todos os elementos →
Energia de ionização (4ª)
35,00012 eV Comparar Energia de ionização (4ª) de todos os elementos →
Energia de ionização (5ª)
49,000169 eV Comparar Energia de ionização (5ª) de todos os elementos →
Estados de oxidação
+2, +3, +4, +5, +6, +7, +8 Comparar Estados de oxidação de todos os elementos →
Elétrons de valência
3 Comparar Elétrons de valência de todos os elementos →
Configuração eletrônica
[Rn] 7s2 5f6

Termodinâmica

Calor de fusão
0,02922734 eV Comparar Calor de fusão de todos os elementos →
Calor de vaporização
3,409856 eV Comparar Calor de vaporização de todos os elementos →
Calor de sublimação
3,554957 eV
Calor de atomização
3,554957 eV
Entalpia de atomização
3,575685 eV

Nuclear

Prótons
94 Comparar Prótons de todos os elementos →
Nêutrons
150 Comparar Nêutrons de todos os elementos →
Isótopos conhecidos
27 Comparar Isótopos conhecidos de todos os elementos →
Isótopos estáveis
0 Comparar Isótopos estáveis de todos os elementos →
Número de massa (mais estável)
244
Isótopo mais estável
Pu-244
Ano da descoberta
1941

Abundância

N/D

Estrutura cristalina

N/D

Estrutura eletrônica

Elétrons por camada
2, 8, 18, 32, 24, 8, 2 Comparar Elétrons por camada de todos os elementos →

Identificadores

Número CAS
7440-07-5 Comparar Número CAS de todos os elementos →
Símbolo de termo
7F0
InChI
InChI=1S/Pu
Chave InChI
OYEHPCDNVJXUIW-UHFFFAOYSA-N

Configuração eletrônica Medido

Carga do íon
Prótons 94
Elétrons 94
Carga Neutro
Configuração Pu: 5f⁶ 7s²
Configuração eletrônica
Medido
[Rn] 5f⁶ 7s²
1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁶ 4f¹⁴ 5d¹⁰ 6s² 6p⁶ 5f⁶ 7s²
Diagrama de orbitais
1s
2/2
2s
2/2
2p
6/6
3s
2/2
3p
6/6
4s
2/2
3d
10/10
4p
6/6
5s
2/2
4d
10/10
5p
6/6
6s
2/2
4f
14/14
5d
10/10
6p
6/6
7s
2/2
5f
6/14 6↑
Total de elétrons: 94 Desemparelhados: 6 ?

Modelo atômico

Prótons 94
Nêutrons 135
Elétrons 94
Número de massa 229
Estabilidade Radioativo

Os isótopos alteram o número de nêutrons, a massa e a estabilidade — não a configuração eletrônica de um átomo neutro.

Modelo atômico esquemático, sem escala.

Assinatura atômica

Espectro de emissão / absorção

0 / 0 (0 0 com intensidade)
Medido
Emissão Visível: 380–750 nm

Distribuição isotópica

Sem isótopos estáveis.

Número de massaMassa atômica (u)Abundância naturalMeia-vida
242 Radioativo242,0587428 ± 0,000002N/D375 ky
230 Radioativo230,03965 ± 0,000016N/D105 segundos
221 Radioativo221,038572 ± 0,000322N/D100 us
225 Radioativo225,03897 ± 0,000322N/D100 us
229 Radioativo229,040144 ± 0,000055N/D91 segundos
Medido

Fase / Estado

1 atm / 101,325 kPa
Sólido 25 °C (298,15 K)

Motivo: 614,9 °C abaixo do ponto de fusão (639,85 °C)

Ponto de fusão 639,85 °C
Ponto de ebulição 3227,85 °C
Abaixo do ponto de fusão em 614,9 °C
0 K Temperatura atual: 25 °C 6000 K
Linha do tempo das fases

Esquemático, sem escala

Sólido
Líquido
Gás
Fusão
Ebulição
25°C
Sólido
Líquido
Gás
Atual

Pontos de transição de fase

Ponto de fusão Literatura
639,85 °C
Ponto de ebulição Literatura
3227,85 °C
Fase atual Calculado
Sólido

Energias de transição

Calor de fusão Literatura
0,02922734 eV

Energia necessária para fundir 1 mol no ponto de fusão

Calor de vaporização Literatura
3,409856 eV

Energia necessária para vaporizar 1 mol no ponto de ebulição

Calor de sublimação Literatura
3,554957 eV

Energia necessária para sublimar 1 mol no ponto de sublimação

Densidade

Densidade de referência Literatura
1,984e+4 kg/m³

Em condições padrão

Densidade atual Calculado
1,984e+4 kg/m³

Em condições padrão

Espectros atômicos

Mostrando 10 de 94. Ordenado por carga do íon (ordem crescente).

Dados de linhas disponíveis ?

ÍonCargaTotal de linhasProbabilidades de transiçãoDesignações dos níveis
Pu I 014100
Pu II +113500
Dados de linhas disponíveis no NIST →

Dados de níveis disponíveis ?

ÍonCargaNíveis
Pu I 02
Pu II +12
Pu III +22
Pu IV +32
Pu V +42
Pu VI +52
Pu VII +62
Pu VIII +72
Pu IX +82
Pu X +92
Dados de níveis disponíveis no NIST →
94 Pu 244

Plutonium — Visualizador de orbitais atômicos

[Rn]7s25f6
Níveis de energia 2 8 18 32 24 8 2
Estados de oxidação +2, +3, +4, +5, +6, +7, +8
HOMO 5f n=5 · l=3 · m=-3
Plutonium — Prévia do visualizador de orbitais atômicos
O Three.js é carregado apenas quando solicitado
94 Pu 244

Plutonium — Visualizador de estruturas cristalinas

Dados de estrutura cristalina indisponíveis

Estrutura cristalina: monoclinic

Raios iônicos

CargaCoordenaçãoSpinRaio
+36N/D100 pm
+39N/D116.8 pm
+46N/D86 pm
+48N/D96 pm
+56N/D74 pm
+66N/D71 pm

Compostos

Pu
244,064 u
Pu
238,050 u
Pu
239,052 u
Pu
240,054 u
Pu
241,057 u
Pu
237,048 u
Pu
242,059 u
Pu
236,046 u
Pu
244,064 u
Pu
230,040 u
Pu
235,045 u
Pu
243,062 u
Pu
234,043 u
Pu
246,070 u
Pu
245,068 u

Isótopos (5)

Twenty-three radioactive isotopes of plutonium have been characterized from mass numbers 228 to 247. Nine of these exhibit metastable states, though these all have half-lives less than one second. The longest-lived isotopes are plutonium-244, with a half-life of 80.8 million years, plutonium-242, with a half-life of 373,300 years, and plutonium-239, with a half-life of 24,110 years. All of the remaining radioactive isotopes have half-lives less than 7,000 years. The primary decay modes of isotopes with mass numbers lower than plutonium-244, are spontaneous fission and α emission, mostly forming uranium and neptunium isotopes as decay products along with a variety of daughter fission products. The primary decay mode for isotopes with mass numbers higher than plutonium-244 is by β emission, mostly forming americium isotopes as daughter decay products. Plutonium-241 is the parent isotope of the neptunium decay series, decaying to americium-241 via β decay. By far of greatest importance is the isotope 239Pu produced in extensive quantities in nuclear reactors from natural uranium:

Número de massaMassa atômica (u)Abundância naturalMeia-vidaModo de decaimento
242 Radioativo242,0587428 ± 0,000002N/D375 ky
α =100%SF =5.510e-4±4.1%
230 Radioativo230,03965 ± 0,000016N/D105 segundos
α ≈100%β+ ?
221 Radioativo221,038572 ± 0,000322N/D100 us
α ?SF ?
225 Radioativo225,03897 ± 0,000322N/D100 us
α ?SF ?
229 Radioativo229,040144 ± 0,000055N/D91 segundos
α ≈50±2%β+ ≈50±2%SF<7%
242 Radioativo
Massa atômica (u) 242,0587428 ± 0,000002
Abundância natural N/D
Meia-vida 375 ky
Modo de decaimento
α =100%SF =5.510e-4±4.1%
230 Radioativo
Massa atômica (u) 230,03965 ± 0,000016
Abundância natural N/D
Meia-vida 105 segundos
Modo de decaimento
α ≈100%β+ ?
221 Radioativo
Massa atômica (u) 221,038572 ± 0,000322
Abundância natural N/D
Meia-vida 100 us
Modo de decaimento
α ?SF ?
225 Radioativo
Massa atômica (u) 225,03897 ± 0,000322
Abundância natural N/D
Meia-vida 100 us
Modo de decaimento
α ?SF ?
229 Radioativo
Massa atômica (u) 229,040144 ± 0,000055
Abundância natural N/D
Meia-vida 91 segundos
Modo de decaimento
α ≈50±2%β+ ≈50±2% +1

Propriedades ampliadas

Raios covalentes (dados ampliados)

Raio covalente (Pyykkö)
172 pm
Raio covalente (Pyykkö, ligação dupla)
135 pm

Raios de van der Waals

Alvarez
281 pm
UFF
342,4 pm
MM3
252 pm

Raios atômicos e metálicos

Raio atômico (Rahm)
278 pm

Escalas de numeração

Mendeleev
24
Pettifor
43
Glawe
38

Escalas de eletronegatividade

Ghosh
0
Miedema
4

Polarizabilidade e dispersão

Polarizabilidade dipolar
132 a.u.
Polarizabilidade dipolar (incerteza)
20 a.u.

Parâmetros de Miedema

Volume molar de Miedema
12,06 cm3/mol
Densidade eletrônica de Miedema
3

Transições de fase e alótropos

Ponto de fusão913,15 K
Ponto de ebulição3501,15 K

Categorias de estados de oxidação

+5 extended
+7 extended
+8 extended
+6 extended
+4 main
+3 extended
+2 extended

Dados de referência avançados

Detalhes dos raios cristalinos (6)
CargaCNSpinrcrystal (pm)Origem
3VI114from r^3 vs V plots,
4VI100from r^3 vs V plots,
4VIII110
5VI88estimated,
6VI85from r^3 vs V plots,
3IX—130,8
Modos de decaimento dos isótopos (57)
IsótopoModoIntensidade
221A—
221SF—
222A—
222SF—
223A—
223SF—
224A—
224SF—
225A—
225SF—

Dados adicionais

Production

Production of this element (from raw materials or other compounds containing the element).

Plutonium is the heaviest primordial element in existence by virtue of its most stable isotope, plutonium-244, whose half-life of about 80 million years is just long enough for the element to be found in trace quantities in nature. In 1971 mass spectrometric measurements of plutonium isolated from Precambrian bastnasite (a lanthanide chloride-fluoride mineral) by Hoffman and coworkers confirmed the presence of Pu-244 in nature. Although the existence of Pu-244 as an extinct radioactive element had been postulated to explain the xenon isotope ratios observed in meteorites, this is the first indication of its present existence in nature. Plutonium also exists in trace quantities in naturally occurring uranium ores. It is formed in much the same manner as neptunium: by irradiation of natural uranium with the neutrons followed by beta decay. Exceedingly small amounts of Pu-238, attributed to the extremely rare double-beta decay of U-238, have been found in natural uranium samples. Plutonium was most likely formed by neutron activation of natural U-238 at the Oklo natural reactor but if formed it has long since decayed away. Plutonium is for the most part a by-product of nuclear reactions in reactors where some of the neutrons released by the fission process convert U-238 nuclei into plutonium. Plutonium-238 and -239 are the most widely synthesized isotopes. Plutonium-239 is synthesized via the following reaction using uranium (U) and neutrons (n) via beta decay (β-) with neptunium as an intermediate:

Plutonium-238 is synthesized by bombarding uranium-238 with deuterons in the following first discovery reaction:

Referências (1)

Referências

(9)
2 Atomic Mass Data Center (AMDC), International Atomic Energy Agency (IAEA)
Pu

The half-life and atomic mass data was provided by the Atomic Mass Data Center at the International Atomic Energy Agency.

3 IUPAC Commission on Isotopic Abundances and Atomic Weights (CIAAW)
Plutonium

Element data are cited from the Atomic weights of the elements (an IUPAC Technical Report). The IUPAC periodic table of elements can be found at https://iupac.org/what-we-do/periodic-table-of-elements/. Additional information can be found within IUPAC publication doi:10.1515/pac-2015-0703 Copyright © 2020 International Union of Pure and Applied Chemistry.

4 IUPAC Periodic Table of the Elements and Isotopes (IPTEI)

The information are cited from Pure Appl. Chem. 2018; 90(12): 1833-2092, https://doi.org/10.1515/pac-2015-0703.

Nota sobre a licença: Copyright (c) 2020 International Union of Pure and Applied Chemistry. The International Union of Pure and Applied Chemistry (IUPAC) contribution within Pubchem is provided under a CC-BY-NC-ND 4.0 license, unless otherwise stated.
5 Jefferson Lab, U.S. Department of Energy
Plutonium

Thomas Jefferson National Accelerator Facility (Jefferson Lab) is one of 17 national laboratories funded by the U.S. Department of Energy. The lab's primary mission is to conduct basic research of the atom's nucleus using the lab's unique particle accelerator, known as the Continuous Electron Beam Accelerator Facility (CEBAF). For more information visit https://www.jlab.org/

Nota sobre a licença: Please see citation and linking information: https://education.jlab.org/faq/index.html
6 Los Alamos National Laboratory, U.S. Department of Energy
Plutonium

The periodic table at the LANL (Los Alamos National Laboratory) contains basic element information together with the history, source, properties, use, handling and more. The provenance data may be found from the link under the source name.

7 NIST Physical Measurement Laboratory
Plutonium

The periodic table contains NIST's critically-evaluated data on atomic properties of the elements. The provenance data that include data for atomic spectroscopy, X-ray and gamma ray, radiation dosimetry, nuclear physics, and condensed matter physics may be found from the link under the source name. Ref: https://www.nist.gov/pml/atomic-spectra-database

8 PubChem Elements
Plutonium

This section provides all form of data related to element Plutonium.

9 PubChem Elements
Plutonium

The element property data was retrieved from publications.

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Dados verificados:

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