Pu 94

Plutonium (Pu)

actinide
周期: 7 区: f

Solid

标准原子量

[244]

电子排布

[Rn] 7s2 5f6

熔点

639.85 °C

沸点

3227.85 °C

密度

1.984e+4 kg/m³

氧化态

+2, +3, +4, +5, +6, +7, +8

电负性(鲍林)

1.28

第一电离能

6.02576 eV

发现年份

1941

原子半径

175 pm

详细信息

名称来源 Named for the planet Pluto.
发现国家 United States
发现者 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.

图片

性质

物理性质

原子半径(经验值)
175 pm 比较所有元素的原子半径(经验值) →
共价半径
187 pm 比较所有元素的共价半径 →
范德华半径
243 pm 比较所有元素的范德华半径 →
密度
1.984 × 104 kg/m³ 比较所有元素的密度 →
标准温度和压力下的物相
固态 比较所有元素的标准温度和压力下的物相 →
熔点
639.85 °C 比较所有元素的熔点 →
沸点
3227.85 °C 比较所有元素的沸点 →
晶体结构
单斜 比较所有元素的晶体结构 →

化学性质

电负性(鲍林)
1.28 比较所有元素的电负性(鲍林) →
电子亲和能
-0.5 eV (负值——预计该原子不结合额外电子)
第一电离能
6.02576 eV 比较所有元素的第一电离能 →
第二电离能
11.50004 eV 比较所有元素的第二电离能 →
第三电离能
21.100073 eV 比较所有元素的第三电离能 →
第四电离能
35.00012 eV 比较所有元素的第四电离能 →
第五电离能
49.000169 eV 比较所有元素的第五电离能 →
氧化态
+2, +3, +4, +5, +6, +7, +8 比较所有元素的氧化态 →
价电子
3 比较所有元素的价电子 →
电子排布
[Rn] 7s2 5f6

热力学性质

熔化热
0.02922734 eV 比较所有元素的熔化热 →
汽化热
3.409856 eV 比较所有元素的汽化热 →
升华热
3.554957 eV
原子化热
3.554957 eV
原子化焓
3.575685 eV

核性质

质子
94 比较所有元素的质子 →
中子
150 比较所有元素的中子 →
已知同位素
27 比较所有元素的已知同位素 →
稳定同位素
0 比较所有元素的稳定同位素 →
质量数(最稳定同位素)
244
最稳定同位素
Pu-244
发现年份
1941

丰度

暂无

晶体结构

暂无

电子结构

各电子层电子数
2, 8, 18, 32, 24, 8, 2 比较所有元素的各电子层电子数 →

标识符

CAS登记号
7440-07-5 比较所有元素的CAS登记号 →
谱项符号
7F0
InChI
InChI=1S/Pu
InChI Key
OYEHPCDNVJXUIW-UHFFFAOYSA-N

电子排布 实测值

离子电荷
质子 94
电子 94
电荷 中性
电子排布 Pu: 5f⁶ 7s²
电子排布
实测值
[Rn] 5f⁶ 7s²
1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁶ 4f¹⁴ 5d¹⁰ 6s² 6p⁶ 5f⁶ 7s²
轨道图
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↑
电子总数: 94 未配对: 6 ?

原子模型

质子 94
中子 135
电子 94
质量数 229
稳定性 放射性

不同同位素的中子数、质量和稳定性不同,但中性原子的电子排布不变。

原子模型示意图,未按比例绘制。

原子指纹

发射 / 吸收光谱

0 / 0 (0 0条具有强度数据)
实测值
发射 可见光:380–750 nm

同位素分布

无稳定同位素。

质量数原子质量(u)天然丰度半衰期
242 放射性242.0587428 ± 0.000002暂无375 ky
230 放射性230.03965 ± 0.000016暂无105 秒
221 放射性221.038572 ± 0.000322暂无100 us
225 放射性225.03897 ± 0.000322暂无100 us
229 放射性229.040144 ± 0.000055暂无91 秒
实测值

物相 / 状态

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

原因: 低于熔点(639.85 °C)614.9 °C

熔点 639.85 °C
沸点 3227.85 °C
低于熔点的温差 614.9 °C
0 K 当前温度: 25 °C 6000 K
物相变化轴

示意图,未按比例绘制

固态
液态
气态
熔化
沸腾
25°C
固态
液态
气态
当前

相变点

熔点 文献值
639.85 °C
沸点 文献值
3227.85 °C
当前物相 计算值
固态

相变能

熔化热 文献值
0.02922734 eV

在熔点熔化1 mol物质所需的能量

汽化热 文献值
3.409856 eV

在沸点汽化1 mol物质所需的能量

升华热 文献值
3.554957 eV

在升华点升华1 mol物质所需的能量

密度

参考密度 文献值
1.984e+4 kg/m³

标准条件下

当前密度 计算值
1.984e+4 kg/m³

标准条件下

原子光谱

已显示10项,共94项。 按离子电荷升序排列。

收录谱线 ?

离子电荷谱线总数跃迁概率能级标记
Pu I 014100
Pu II +113500
NIST收录谱线 →

收录能级 ?

离子电荷能级
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收录能级 →
94 Pu 244

Plutonium — 原子轨道可视化工具

[Rn]7s25f6
能级 2 8 18 32 24 8 2
氧化态 +2, +3, +4, +5, +6, +7, +8
HOMO 5f n=5 · l=3 · m=-3
Plutonium — 原子轨道可视化预览
Three.js仅在需要时加载
94 Pu 244

Plutonium — 晶体结构可视化工具

暂无晶体结构数据

晶体结构: monoclinic

离子半径

电荷配位自旋半径
+36暂无100 pm
+39暂无116.8 pm
+46暂无86 pm
+48暂无96 pm
+56暂无74 pm
+66暂无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

同位素 (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:

质量数原子质量(u)天然丰度半衰期衰变方式
242 放射性242.0587428 ± 0.000002暂无375 ky
α =100%SF =5.510e-4±4.1%
230 放射性230.03965 ± 0.000016暂无105 秒
α ≈100%β+ ?
221 放射性221.038572 ± 0.000322暂无100 us
α ?SF ?
225 放射性225.03897 ± 0.000322暂无100 us
α ?SF ?
229 放射性229.040144 ± 0.000055暂无91 秒
α ≈50±2%β+ ≈50±2%SF<7%
242 放射性
原子质量(u) 242.0587428 ± 0.000002
天然丰度 暂无
半衰期 375 ky
衰变方式
α =100%SF =5.510e-4±4.1%
230 放射性
原子质量(u) 230.03965 ± 0.000016
天然丰度 暂无
半衰期 105 秒
衰变方式
α ≈100%β+ ?
221 放射性
原子质量(u) 221.038572 ± 0.000322
天然丰度 暂无
半衰期 100 us
衰变方式
α ?SF ?
225 放射性
原子质量(u) 225.03897 ± 0.000322
天然丰度 暂无
半衰期 100 us
衰变方式
α ?SF ?
229 放射性
原子质量(u) 229.040144 ± 0.000055
天然丰度 暂无
半衰期 91 秒
衰变方式
α ≈50±2%β+ ≈50±2% +1

扩展性质

共价半径(扩展)

共价半径(Pyykkö)
172 pm
共价半径(Pyykkö,双键)
135 pm

范德华半径

Alvarez
281 pm
UFF
342.4 pm
MM3
252 pm

原子半径与金属半径

原子半径(Rahm)
278 pm

编号标度

Mendeleev
24
Pettifor
43
Glawe
38

电负性标度

Ghosh
0
Miedema
4

极化率与色散

偶极极化率
132 a.u.
偶极极化率(不确定度)
20 a.u.

Miedema参数

Miedema摩尔体积
12.06 cm3/mol
Miedema电子密度
3

相变与同素异形体

熔点913.15 K
沸点3501.15 K

氧化态分类

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

高级参考数据

晶体半径详情 (6)
电荷CN自旋rcrystal (pm)来源
3VI114from r^3 vs V plots,
4VI100from r^3 vs V plots,
4VIII110
5VI88estimated,
6VI85from r^3 vs V plots,
3IX—130.8
同位素衰变方式 (57)
同位素模式强度
221A—
221SF—
222A—
222SF—
223A—
223SF—
224A—
224SF—
225A—
225SF—

补充数据

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.

许可证说明: 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/

许可证说明: 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.

最后更新:

数据已核实:

内容已依据最新科学数据进行审核。