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Pu 94

Plutonium (Pu)

actinide
Periode: 7 Blok: f

Solid

Bobot Atom Standar

[244]

Konfigurasi elektron

[Rn] 7s2 5f6

Titik lebur

639,85 °C

Titik didih

3227,85 °C

Massa jenis

1,984e+4 kg/m³

Bilangan oksidasi

+2, +3, +4, +5, +6, +7, +8

Keelektronegatifan (Pauling)

1,28

Energi ionisasi (ke-1)

6,02576 eV

Tahun penemuan

1941

Jari-jari atom

175 pm

Detail

Asal nama Named for the planet Pluto.
Negara penemuan United States
Penemu 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.

Gambar

Sifat

Kimia

Keelektronegatifan (Pauling)
1,28 Bandingkan Keelektronegatifan (Pauling) semua unsur →
Afinitas elektron
-0,5 eV (nilai negatif — atom tidak diprediksi mengikat elektron tambahan)
Energi ionisasi (ke-1)
6,02576 eV Bandingkan Energi ionisasi (ke-1) semua unsur →
Energi ionisasi (ke-2)
11,50004 eV Bandingkan Energi ionisasi (ke-2) semua unsur →
Energi ionisasi (ke-3)
21,100073 eV Bandingkan Energi ionisasi (ke-3) semua unsur →
Energi ionisasi (ke-4)
35,00012 eV Bandingkan Energi ionisasi (ke-4) semua unsur →
Energi ionisasi (ke-5)
49,000169 eV Bandingkan Energi ionisasi (ke-5) semua unsur →
Bilangan oksidasi
+2, +3, +4, +5, +6, +7, +8 Bandingkan Bilangan oksidasi semua unsur →
Elektron valensi
3 Bandingkan Elektron valensi semua unsur →
Konfigurasi elektron
[Rn] 7s2 5f6

Termodinamika

Kalor peleburan
0,02922734 eV Bandingkan Kalor peleburan semua unsur →
Kalor penguapan
3,409856 eV Bandingkan Kalor penguapan semua unsur →
Kalor sublimasi
3,554957 eV
Kalor atomisasi
3,554957 eV
Entalpi atomisasi
3,575685 eV

Nuklir

Proton
94 Bandingkan Proton semua unsur →
Neutron
150 Bandingkan Neutron semua unsur →
Isotop yang diketahui
27 Bandingkan Isotop yang diketahui semua unsur →
Isotop stabil
0 Bandingkan Isotop stabil semua unsur →
Nomor massa (paling stabil)
244
Isotop paling stabil
Pu-244
Tahun penemuan
1941

Kelimpahan

Tidak tersedia

Struktur Kristal

Tidak tersedia

Struktur Elektronik

Elektron per kulit
2, 8, 18, 32, 24, 8, 2 Bandingkan Elektron per kulit semua unsur →

Pengenal

Nomor CAS
7440-07-5 Bandingkan Nomor CAS semua unsur →
Simbol term
7F0
InChI
InChI=1S/Pu
Kunci InChI
OYEHPCDNVJXUIW-UHFFFAOYSA-N

Konfigurasi Elektron Diukur

Muatan ion
Proton 94
Elektron 94
Muatan Netral
Konfigurasi Pu: 5f⁶ 7s²
Konfigurasi elektron
Diukur
[Rn] 5f⁶ 7s²
1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁶ 4f¹⁴ 5d¹⁰ 6s² 6p⁶ 5f⁶ 7s²
Diagram orbital
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 elektron: 94 Tidak berpasangan: 6 ?

Model atom

Proton 94
Neutron 135
Elektron 94
Nomor massa 229
Kestabilan Radioaktif

Isotop mengubah jumlah neutron, massa, dan kestabilan — bukan konfigurasi elektron atom netral.

Model atom skematis, tidak sesuai skala.

Sidik Jari Atom

Spektrum Emisi / Absorpsi

0 / 0 (0 0 dengan intensitas)
Diukur
Emisi Tampak: 380–750 nm

Distribusi Isotop

Tidak memiliki isotop stabil.

Nomor massaMassa atom (u)Kelimpahan alamiWaktu paruh
242 Radioaktif242,0587428 ± 0,000002Tidak tersedia375 ky
230 Radioaktif230,03965 ± 0,000016Tidak tersedia105 detik
221 Radioaktif221,038572 ± 0,000322Tidak tersedia100 us
225 Radioaktif225,03897 ± 0,000322Tidak tersedia100 us
229 Radioaktif229,040144 ± 0,000055Tidak tersedia91 detik
Diukur

Fase / Wujud

1 atm / 101.325 kPa
Padat 25 °C (298,15 K)

Alasan: 614,9 °C di bawah titik lebur (639,85 °C)

Titik lebur 639,85 °C
Titik didih 3227,85 °C
Di bawah titik lebur sebesar 614,9 °C
0 K Suhu saat ini: 25 °C 6000 K
Linimasa fase

Skematis, tidak sesuai skala

Padat
Cair
Gas
Peleburan
Pendidihan
25°C
Padat
Cair
Gas
Saat ini

Titik transisi fase

Titik lebur Literatur
639,85 °C
Titik didih Literatur
3227,85 °C
Fase saat ini Dihitung
Padat

Energi transisi

Kalor peleburan Literatur
0,02922734 eV

Energi yang diperlukan untuk meleburkan 1 mol pada titik lebur

Kalor penguapan Literatur
3,409856 eV

Energi yang diperlukan untuk menguapkan 1 mol pada titik didih

Kalor sublimasi Literatur
3,554957 eV

Energi yang diperlukan untuk menyublimkan 1 mol pada titik sublimasi

Massa jenis

Massa jenis referensi Literatur
1,984e+4 kg/m³

Pada kondisi standar

Massa jenis saat ini Dihitung
1,984e+4 kg/m³

Pada kondisi standar

Spektrum Atom

Menampilkan 10 dari 94. Diurutkan berdasarkan muatan ion (menaik).

Data Garis Spektrum ?

IonMuatanTotal garisProbabilitas transisiPenamaan tingkat energi
Pu I 014100
Pu II +113500
Data Garis Spektrum NIST →

Data Tingkat Energi ?

IonMuatanTingkat energi
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
Data Tingkat Energi NIST →
94 Pu 244

Plutonium — Visualisasi Orbital Atom

[Rn]7s25f6
Tingkat energi 2 8 18 32 24 8 2
Bilangan oksidasi +2, +3, +4, +5, +6, +7, +8
HOMO 5f n=5 · l=3 · m=-3
Plutonium — Pratinjau Visualisasi Orbital Atom
Three.js hanya dimuat saat diminta
94 Pu 244

Plutonium — Visualisasi Struktur Kristal

Data struktur kristal tidak tersedia

Struktur kristal: monoclinic

Jari-jari Ion

MuatanKoordinasiSpinJari-jari
+36Tidak tersedia100 pm
+39Tidak tersedia116.8 pm
+46Tidak tersedia86 pm
+48Tidak tersedia96 pm
+56Tidak tersedia74 pm
+66Tidak tersedia71 pm

Senyawa

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

Isotop (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:

Nomor massaMassa atom (u)Kelimpahan alamiWaktu paruhMode peluruhan
242 Radioaktif242,0587428 ± 0,000002Tidak tersedia375 ky
α =100%SF =5.510e-4±4.1%
230 Radioaktif230,03965 ± 0,000016Tidak tersedia105 detik
α ≈100%β+ ?
221 Radioaktif221,038572 ± 0,000322Tidak tersedia100 us
α ?SF ?
225 Radioaktif225,03897 ± 0,000322Tidak tersedia100 us
α ?SF ?
229 Radioaktif229,040144 ± 0,000055Tidak tersedia91 detik
α ≈50±2%β+ ≈50±2%SF<7%
242 Radioaktif
Massa atom (u) 242,0587428 ± 0,000002
Kelimpahan alami Tidak tersedia
Waktu paruh 375 ky
Mode peluruhan
α =100%SF =5.510e-4±4.1%
230 Radioaktif
Massa atom (u) 230,03965 ± 0,000016
Kelimpahan alami Tidak tersedia
Waktu paruh 105 detik
Mode peluruhan
α ≈100%β+ ?
221 Radioaktif
Massa atom (u) 221,038572 ± 0,000322
Kelimpahan alami Tidak tersedia
Waktu paruh 100 us
Mode peluruhan
α ?SF ?
225 Radioaktif
Massa atom (u) 225,03897 ± 0,000322
Kelimpahan alami Tidak tersedia
Waktu paruh 100 us
Mode peluruhan
α ?SF ?
229 Radioaktif
Massa atom (u) 229,040144 ± 0,000055
Kelimpahan alami Tidak tersedia
Waktu paruh 91 detik
Mode peluruhan
α ≈50±2%β+ ≈50±2% +1

Sifat Lanjutan

Jari-jari Kovalen (Lanjutan)

Jari-jari kovalen (Pyykkö)
172 pm
Jari-jari kovalen (Pyykkö, ikatan rangkap dua)
135 pm

Jari-jari van der Waals

Alvarez
281 pm
UFF
342,4 pm
MM3
252 pm

Jari-jari Atom & Logam

Jari-jari atom (Rahm)
278 pm

Skala Penomoran

Mendeleev
24
Pettifor
43
Glawe
38

Skala Keelektronegatifan

Ghosh
0
Miedema
4

Polarizabilitas & Dispersi

Polarizabilitas dipol
132 a.u.
Polarizabilitas dipol (ketidakpastian)
20 a.u.

Parameter Miedema

Volume molar Miedema
12,06 cm3/mol
Kerapatan elektron Miedema
3

Transisi Fase & Alotrop

Titik lebur913,15 K
Titik didih3501,15 K

Kategori Bilangan Oksidasi

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

Data Referensi Lanjutan

Detail Jari-jari Kristal (6)
MuatanCNSpinrcrystal (pm)Asal
3VI114from r^3 vs V plots,
4VI100from r^3 vs V plots,
4VIII110
5VI88estimated,
6VI85from r^3 vs V plots,
3IX—130,8
Mode Peluruhan Isotop (57)
IsotopModeIntensitas
221A—
221SF—
222A—
222SF—
223A—
223SF—
224A—
224SF—
225A—
225SF—

Data Tambahan

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:

Referensi (1)

Referensi

(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.

Catatan lisensi: 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/

Catatan lisensi: 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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