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Pu 94

Plutonium (Pu)

actinide
周期: 7 ブロック: f

Solid

標準原子量

[244]

電子配置

[Rn] 7s2 5f6

融点

639.85 °C

沸点

3227.85 °C

密度

1.984e+4 kg/m³

酸化数

+2, +3, +4, +5, +6, +7, +8

電気陰性度(Pauling)

1.28

第1イオン化エネルギー

6.02576 eV

発見年

1941

原子半径

175 pm

詳細

名称の由来 Named for the planet Pluto.
発見国 United States
発見者 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.

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性質

物理的性質

原子半径(経験値)
175 pm 全元素の原子半径(経験値)を比較 →
共有結合半径
187 pm 全元素の共有結合半径を比較 →
ファンデルワールス半径
243 pm 全元素のファンデルワールス半径を比較 →
密度
1.984 × 104 kg/m³ 全元素の密度を比較 →
標準温度・圧力(STP)での相
固体 全元素の標準温度・圧力(STP)での相を比較 →
融点
639.85 °C 全元素の融点を比較 →
沸点
3227.85 °C 全元素の沸点を比較 →
結晶構造
単斜晶系 全元素の結晶構造を比較 →

化学的性質

電気陰性度(Pauling)
1.28 全元素の電気陰性度(Pauling)を比較 →
電子親和力
-0.5 eV (負の値—この原子は電子を取り込まないと予測される)
第1イオン化エネルギー
6.02576 eV 全元素の第1イオン化エネルギーを比較 →
第2イオン化エネルギー
11.50004 eV 全元素の第2イオン化エネルギーを比較 →
第3イオン化エネルギー
21.100073 eV 全元素の第3イオン化エネルギーを比較 →
第4イオン化エネルギー
35.00012 eV 全元素の第4イオン化エネルギーを比較 →
第5イオン化エネルギー
49.000169 eV 全元素の第5イオン化エネルギーを比較 →
酸化数
+2, +3, +4, +5, +6, +7, +8 全元素の酸化数を比較 →
価電子
3 全元素の価電子を比較 →
電子配置
[Rn] 7s2 5f6

熱力学的性質

融解熱
0.02922734 eV 全元素の融解熱を比較 →
蒸発熱
3.409856 eV 全元素の蒸発熱を比較 →
昇華熱
3.554957 eV
原子化熱
3.554957 eV
原子化エンタルピー
3.575685 eV

原子核

陽子数
94 全元素の陽子数を比較 →
中性子数
150 全元素の中性子数を比較 →
既知の同位体
27 全元素の既知の同位体を比較 →
安定同位体
0 全元素の安定同位体を比較 →
質量数(最も安定な同位体)
244
最も安定な同位体
Pu-244
発見年
1941

存在度

データなし

結晶構造

データなし

電子構造

各電子殻の電子数
2, 8, 18, 32, 24, 8, 2 全元素の各電子殻の電子数を比較 →

識別子

CAS登録番号
7440-07-5 全元素のCAS登録番号を比較 →
項記号
7F0
InChI
InChI=1S/Pu
InChI Key
OYEHPCDNVJXUIW-UHFFFAOYSA-N

電子配置 測定値

イオンの電荷
陽子 94
電子 94
電荷 中性
電子配置 Pu: 5f⁶ 7s²
電子配置
測定値
[Rn] 5f⁶ 7s²
1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁶ 4f¹⁴ 5d¹⁰ 6s² 6p⁶ 5f⁶ 7s²
軌道図
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↑
総電子数: 94 不対電子: 6 ?

原子モデル

陽子 94
中性子 135
電子 94
質量数 229
安定性 放射性

同位体によって中性子数、質量、安定性は変わりますが、中性原子の電子配置は変わりません。

模式的な原子モデルです。実際の縮尺とは異なります。

原子の指紋

発光/吸収スペクトル

0 / 0 (0 強度データあり:0本)
測定値
発光 可視光:380–750 nm

同位体分布

安定同位体はありません。

質量数原子質量(u)天然存在比半減期
242 放射性242.0587428 ± 0.000002データなし375 ky
230 放射性230.03965 ± 0.000016データなし105 秒
221 放射性221.038572 ± 0.000322データなし100 us
225 放射性225.03897 ± 0.000322データなし100 us
229 放射性229.040144 ± 0.000055データなし91 秒
測定値

相/状態

1 atm / 101.325 kPa
固体 25 °C (298.15 K)

理由: 融点(639.85 °C)より614.9 °C低い

融点 639.85 °C
沸点 3227.85 °C
融点との差(下) 614.9 °C
0 K 現在の温度: 25 °C 6000 K
相変化図

模式図、実際の縮尺とは異なります

固体
液体
気体
融解
沸騰
25°C
固体
液体
気体
現在

相転移点

融点 文献値
639.85 °C
沸点 文献値
3227.85 °C
現在の相 計算値
固体

相転移エネルギー

融解熱 文献値
0.02922734 eV

融点で1 molを融解させるのに必要なエネルギー

蒸発熱 文献値
3.409856 eV

沸点で1 molを蒸発させるのに必要なエネルギー

昇華熱 文献値
3.554957 eV

昇華点で1 molを昇華させるのに必要なエネルギー

密度

基準密度 文献値
1.984e+4 kg/m³

標準条件下

現在の密度 計算値
1.984e+4 kg/m³

標準条件下

原子スペクトル

全94件中10件を表示しています。 イオンの電荷の昇順で並べています。

スペクトル線データの収録状況 ?

イオン電荷スペクトル線の総数遷移確率準位の表記
Pu I 014100
Pu II +113500
NISTスペクトル線データの収録状況 →

準位データの収録状況 ?

イオン電荷準位
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
NIST準位データの収録状況 →
94 Pu 244

Plutonium — 原子軌道可視化ツール

[Rn]7s25f6
エネルギー準位 2 8 18 32 24 8 2
酸化数 +2, +3, +4, +5, +6, +7, +8
HOMO 5f n=5 · l=3 · m=-3
Plutonium — 原子軌道可視化ツールのプレビュー
Three.jsは必要な場合にのみ読み込まれます
94 Pu 244

Plutonium — 結晶構造可視化ツール

結晶構造のデータはありません

結晶構造: monoclinic

イオン半径

電荷配位スピン半径
+36データなし100 pm
+39データなし116.8 pm
+46データなし86 pm
+48データなし96 pm
+56データなし74 pm
+66データなし71 pm

化合物

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

同位体 (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:

質量数原子質量(u)天然存在比半減期崩壊形式
242 放射性242.0587428 ± 0.000002データなし375 ky
α =100%SF =5.510e-4±4.1%
230 放射性230.03965 ± 0.000016データなし105 秒
α ≈100%β+ ?
221 放射性221.038572 ± 0.000322データなし100 us
α ?SF ?
225 放射性225.03897 ± 0.000322データなし100 us
α ?SF ?
229 放射性229.040144 ± 0.000055データなし91 秒
α ≈50±2%β+ ≈50±2%SF<7%
242 放射性
原子質量(u) 242.0587428 ± 0.000002
天然存在比 データなし
半減期 375 ky
崩壊形式
α =100%SF =5.510e-4±4.1%
230 放射性
原子質量(u) 230.03965 ± 0.000016
天然存在比 データなし
半減期 105 秒
崩壊形式
α ≈100%β+ ?
221 放射性
原子質量(u) 221.038572 ± 0.000322
天然存在比 データなし
半減期 100 us
崩壊形式
α ?SF ?
225 放射性
原子質量(u) 225.03897 ± 0.000322
天然存在比 データなし
半減期 100 us
崩壊形式
α ?SF ?
229 放射性
原子質量(u) 229.040144 ± 0.000055
天然存在比 データなし
半減期 91 秒
崩壊形式
α ≈50±2%β+ ≈50±2% +1

詳細な性質

共有結合半径(詳細)

共有結合半径(Pyykkö)
172 pm
共有結合半径(Pyykkö、二重結合)
135 pm

ファンデルワールス半径

Alvarez
281 pm
UFF
342.4 pm
MM3
252 pm

原子半径と金属半径

原子半径(Rahm)
278 pm

番号付けの尺度

Mendeleev
24
Pettifor
43
Glawe
38

電気陰性度の尺度

Ghosh
0
Miedema
4

分極率と分散

双極子分極率
132 a.u.
双極子分極率(不確かさ)
20 a.u.

ミーデマパラメータ

ミーデマモル体積
12.06 cm3/mol
ミーデマ電子密度
3

相転移と同素体

融点913.15 K
沸点3501.15 K

酸化数の分類

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

専門参考データ

結晶半径の詳細 (6)
電荷CNスピンrcrystal (pm)由来
3VI114from r^3 vs V plots,
4VI100from r^3 vs V plots,
4VIII110
5VI88estimated,
6VI85from r^3 vs V plots,
3IX—130.8
同位体の崩壊形式 (57)
同位体モード強度
221A—
221SF—
222A—
222SF—
223A—
223SF—
224A—
224SF—
225A—
225SF—

追加データ

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:

参考文献 (1)

参考文献

(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.

ライセンスに関する注記: 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/

ライセンスに関する注記: 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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