Pu 94

Plutonium (Pu)

actinide
주기: 7 블록: f

Solid

표준 원자량

[244]

전자 배치

[Rn] 7s2 5f6

녹는점

639.85 °C

끓는점

3227.85 °C

밀도

1.984e+4 kg/m³

산화 상태

+2, +3, +4, +5, +6, +7, +8

전기 음성도(Pauling)

1.28

제1 이온화 에너지

6.02576 eV

발견 연도

1941

원자 반지름

175 pm

상세 정보

이름의 유래 Named for the planet Pluto.
발견 국가 United States
발견자 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.

이미지

특성

화학적 특성

전기 음성도(Pauling)
1.28 모든 원소의 전기 음성도(Pauling) 비교 →
전자 친화도
-0.5 eV (음수 값 — 추가 전자를 결합하지 않을 것으로 예측됨)
제1 이온화 에너지
6.02576 eV 모든 원소의 제1 이온화 에너지 비교 →
제2 이온화 에너지
11.50004 eV 모든 원소의 제2 이온화 에너지 비교 →
제3 이온화 에너지
21.100073 eV 모든 원소의 제3 이온화 에너지 비교 →
제4 이온화 에너지
35.00012 eV 모든 원소의 제4 이온화 에너지 비교 →
제5 이온화 에너지
49.000169 eV 모든 원소의 제5 이온화 에너지 비교 →
산화 상태
+2, +3, +4, +5, +6, +7, +8 모든 원소의 산화 상태 비교 →
원자가 전자
3 모든 원소의 원자가 전자 비교 →
전자 배치
[Rn] 7s2 5f6

열역학적 특성

융해열
0.02922734 eV 모든 원소의 융해열 비교 →
기화열
3.409856 eV 모든 원소의 기화열 비교 →
승화열
3.554957 eV
원자화열
3.554957 eV
원자화 엔탈피
3.575685 eV

핵 특성

양성자 수
94 모든 원소의 양성자 수 비교 →
중성자 수
150 모든 원소의 중성자 수 비교 →
알려진 동위원소 수
27 모든 원소의 알려진 동위원소 수 비교 →
안정 동위원소 수
0 모든 원소의 안정 동위원소 수 비교 →
질량수(가장 안정한 동위원소)
244
가장 안정한 동위원소
Pu-244
발견 연도
1941

존재비

해당 없음

결정 구조

해당 없음

전자 구조

전자껍질별 전자 수
2, 8, 18, 32, 24, 8, 2 모든 원소의 전자껍질별 전자 수 비교 →

식별자

CAS 등록 번호
7440-07-5 모든 원소의 CAS 등록 번호 비교 →
항 기호
7F0
InChI
InChI=1S/Pu
InChI 키
OYEHPCDNVJXUIW-UHFFFAOYSA-N

전자 배치 측정값

이온 전하
양성자 94
전자 94
전하 중성
배치 Pu: 5f⁶ 7s²
전자 배치
측정값
[Rn] 5f⁶ 7s²
1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁶ 4f¹⁴ 5d¹⁰ 6s² 6p⁶ 5f⁶ 7s²
오비탈 도표
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↑
총 전자 수: 94 홀전자: 6 ?

원자 모형

양성자 94
중성자 135
전자 94
질량수 229
안정성 방사성

동위원소에 따라 중성자 수, 질량, 안정성은 달라지지만, 중성 원자의 전자 배치는 달라지지 않습니다.

개략적인 원자 모형이며 실제 비율과 다릅니다.

원자 지문

방출 / 흡수 스펙트럼

0 / 0 (0 세기 정보가 있는 선 0개)
측정값
방출 가시광선: 380–750 nm

동위원소 분포

안정 동위원소가 없습니다.

질량수원자 질량(u)천연 존재비반감기
242 방사성242.0587428 ± 0.000002해당 없음375 ky
230 방사성230.03965 ± 0.000016해당 없음105 초
221 방사성221.038572 ± 0.000322해당 없음100 us
225 방사성225.03897 ± 0.000322해당 없음100 us
229 방사성229.040144 ± 0.000055해당 없음91 초
측정값

상 / 상태

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

이유: 녹는점(639.85 °C)보다 614.9 °C 낮음

녹는점 639.85 °C
끓는점 3227.85 °C
녹는점 미달 온도 614.9 °C
0 K 현재 온도: 25 °C 6000 K
상 변화 도표

개략도이며 실제 비율과 다름

고체
액체
기체
녹는점
끓는점
25°C
고체
액체
기체
현재

상전이점

녹는점 문헌값
639.85 °C
끓는점 문헌값
3227.85 °C
현재 상 계산값
고체

전이 에너지

융해열 문헌값
0.02922734 eV

녹는점에서 1 mol을 녹이는 데 필요한 에너지

기화열 문헌값
3.409856 eV

끓는점에서 1 mol을 기화시키는 데 필요한 에너지

승화열 문헌값
3.554957 eV

승화점에서 1 mol을 승화시키는 데 필요한 에너지

밀도

기준 밀도 문헌값
1.984e+4 kg/m³

표준 조건에서

현재 밀도 계산값
1.984e+4 kg/m³

표준 조건에서

원자 스펙트럼

전체 94개 중 10개를 표시합니다. 이온 전하순으로 정렬되었습니다(오름차순).

보유 스펙트럼선 데이터 ?

이온전하총 스펙트럼선 수전이 확률준위 표기
Pu I 014100
Pu II +113500
NIST 보유 스펙트럼선 데이터 →

보유 에너지 준위 데이터 ?

이온전하준위
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 보유 에너지 준위 데이터 →
94 Pu 244

Plutonium — 원자 오비탈 시각화 도구

[Rn]7s25f6
에너지 준위 2 8 18 32 24 8 2
산화 상태 +2, +3, +4, +5, +6, +7, +8
HOMO 5f n=5 · l=3 · m=-3
Plutonium — 원자 오비탈 시각화 도구 미리보기
Three.js는 요청할 때만 불러옵니다
94 Pu 244

Plutonium — 결정 구조 시각화 도구

결정 구조 데이터 없음

결정 구조: monoclinic

이온 반지름

전하배위스핀반지름
+36해당 없음100 pm
+39해당 없음116.8 pm
+46해당 없음86 pm
+48해당 없음96 pm
+56해당 없음74 pm
+66해당 없음71 pm

화합물

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

동위원소 (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:

질량수원자 질량(u)천연 존재비반감기붕괴 방식
242 방사성242.0587428 ± 0.000002해당 없음375 ky
α =100%SF =5.510e-4±4.1%
230 방사성230.03965 ± 0.000016해당 없음105 초
α ≈100%β+ ?
221 방사성221.038572 ± 0.000322해당 없음100 us
α ?SF ?
225 방사성225.03897 ± 0.000322해당 없음100 us
α ?SF ?
229 방사성229.040144 ± 0.000055해당 없음91 초
α ≈50±2%β+ ≈50±2%SF<7%
242 방사성
원자 질량(u) 242.0587428 ± 0.000002
천연 존재비 해당 없음
반감기 375 ky
붕괴 방식
α =100%SF =5.510e-4±4.1%
230 방사성
원자 질량(u) 230.03965 ± 0.000016
천연 존재비 해당 없음
반감기 105 초
붕괴 방식
α ≈100%β+ ?
221 방사성
원자 질량(u) 221.038572 ± 0.000322
천연 존재비 해당 없음
반감기 100 us
붕괴 방식
α ?SF ?
225 방사성
원자 질량(u) 225.03897 ± 0.000322
천연 존재비 해당 없음
반감기 100 us
붕괴 방식
α ?SF ?
229 방사성
원자 질량(u) 229.040144 ± 0.000055
천연 존재비 해당 없음
반감기 91 초
붕괴 방식
α ≈50±2%β+ ≈50±2% +1

확장 특성

공유 결합 반지름(확장)

공유 결합 반지름(Pyykkö)
172 pm
공유 결합 반지름(Pyykkö, 이중 결합)
135 pm

반데르발스 반지름

Alvarez
281 pm
UFF
342.4 pm
MM3
252 pm

원자 및 금속 반지름

원자 반지름(Rahm)
278 pm

번호 척도

Mendeleev
24
Pettifor
43
Glawe
38

전기 음성도 척도

Ghosh
0
Miedema
4

분극률 및 분산

쌍극자 분극률
132 a.u.
쌍극자 분극률(불확도)
20 a.u.

미데마 매개변수

미데마 몰 부피
12.06 cm3/mol
미데마 전자 밀도
3

상전이 및 동소체

녹는점913.15 K
끓는점3501.15 K

산화 상태 분류

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

심화 참고 데이터

결정 반지름 상세 정보 (6)
전하CN스핀rcrystal (pm)기원
3VI114from r^3 vs V plots,
4VI100from r^3 vs V plots,
4VIII110
5VI88estimated,
6VI85from r^3 vs V plots,
3IX—130.8
동위원소 붕괴 방식 (57)
동위원소모드세기
221A—
221SF—
222A—
222SF—
223A—
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224A—
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225A—
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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:

참고 문헌 (1)

참고 문헌

(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.

라이선스 안내: 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/

라이선스 안내: 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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