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Americium (95Am) is an artificial element, and thus a standard atomic weight cannot be given. Like all artificial elements, it has no known stable isotopes. The first isotope to be synthesized was 241Am in 1944. The artificial element decays by ejecting alpha particles. Americium has an atomic number of 95 (the number of protons in the nucleus of the americium atom). Despite 243
Am being an order of magnitude longer lived than 241
Am, the former is harder to obtain than the latter as more of it is present in spent nuclear fuel.
Eighteen radioisotopes of americium, ranging from 229Am to 247Am with the exception of 231Am, have been characterized; another isotope, 223Am, has also been reported but is unconfirmed. The most stable isotopes are 243Am with a half-life of 7,370 years and 241Am with a half-life of 432.2 years. All of the remaining radioactive isotopes have half-lives that are less than 51 hours, and the majority of these have half-lives that are less than 100 minutes. This element also has 8 meta states, with the most stable being 242m1Am (t1/2 = 141 years). This isomer is unusual in that its half-life is far longer than that of the ground state of the same isotope.
Nuclide [n 1] | Z | N | Isotopic mass (Da) [n 2] [n 3] | Half-life [1] | Decay mode [1] [n 4] | Daughter isotope | Spin and parity [1] [n 5] [n 6] | ||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Excitation energy [n 6] | |||||||||||||||||||
223Am [n 7] | 95 | 128 | 223.04584(32)# | 10(9) ms | α | 219Np | 9/2–# | ||||||||||||
229Am | 95 | 134 | 229.04528(11) | 1.8(15) s | α | 225Np | 5/2–# | ||||||||||||
230Am | 95 | 135 | 230.04603(15)# | 40(9) s | β+ (<70%) | 230Pu | 1–# | ||||||||||||
β+ SF (>30%) | (various) | ||||||||||||||||||
232Am | 95 | 137 | 232.04661(32)# | 1.31(4) min | β+ (97%) | 232Pu | 1–# | ||||||||||||
α (3%) | 228Np | ||||||||||||||||||
β+SF (0.069%) | (various) | ||||||||||||||||||
233Am | 95 | 138 | 233.04647(12)# | 3.2(8) min | β+ (95.5%) | 233Pu | 5/2–# | ||||||||||||
α (4.5%) | 229Np | ||||||||||||||||||
234Am | 95 | 139 | 234.04773(17)# | 2.32(8) min | β+ (99.95%) | 234Pu | 0–# | ||||||||||||
α (0.039%) | 230Np | ||||||||||||||||||
β+, SF (0.0066%) | (various) | ||||||||||||||||||
235Am | 95 | 140 | 235.047906(57) | 10.3(6) min | β+ (99.60%) | 235Pu | 5/2−# | ||||||||||||
α (0.40%) | 231Np | ||||||||||||||||||
236Am | 95 | 141 | 236.04943(13)# | 3.6(1) min | β+ | 236Pu | 5− | ||||||||||||
α (4×10−3%) | 232Np | ||||||||||||||||||
236mAm | 50(50)# keV | 2.9(2) min | β+ | 236Pu | (1−) | ||||||||||||||
α ? | 232Np | ||||||||||||||||||
237Am | 95 | 142 | 237.049995(64)# | 73.6(8) min | β+ (99.975%) | 237Pu | 5/2− | ||||||||||||
α (.025%) | 233Np | ||||||||||||||||||
238Am | 95 | 143 | 238.051983(63) | 98(3) min | β+ | 238Pu | 1+ | ||||||||||||
α (1.0×10−4%) | 234Np | ||||||||||||||||||
238mAm | 2500(200)# keV | 35(18) μs | SF | (various) | |||||||||||||||
IT ? | 238Am | ||||||||||||||||||
239Am | 95 | 144 | 239.0530227(21) | 11.9(1) h | EC (99.99%) | 239Pu | 5/2− | ||||||||||||
α (0.01%) | 235Np | ||||||||||||||||||
239mAm | 2500(200) keV | 163(12) ns | SF | (various) | (7/2+) | ||||||||||||||
IT ? | 239Am | ||||||||||||||||||
240Am | 95 | 145 | 240.055298(15) | 50.8(3) h | β+ | 240Pu | (3−) | ||||||||||||
α (1.9×10−4%) | 236Np | ||||||||||||||||||
240mAm | 3000(200) keV | 940(40) μs | SF | (various) | |||||||||||||||
IT ? | 240Am | ||||||||||||||||||
241Am | 95 | 146 | 241.0568273(12) | 432.6(6) y | α | 237Np | 5/2− | ||||||||||||
SF (3.6×10−10%) | (various) | ||||||||||||||||||
241mAm | 2200(200) keV | 1.2(3) μs | SF | (various) | |||||||||||||||
242Am | 95 | 147 | 242.0595474(12) | 16.02(2) h | β− (82.7%) | 242Cm | 1− | ||||||||||||
EC (17.3%) | 242Pu | ||||||||||||||||||
242m1Am | 48.60(5) keV | 141(2) y | IT (99.54%) | 242Am | 5− | ||||||||||||||
α (.46%) | 238Np | ||||||||||||||||||
SF ? | (various) | ||||||||||||||||||
242m2Am | 2200(80) keV | 14.0(10) ms | SF | (various) | (2+, 3−) | ||||||||||||||
IT ? | 242Am | ||||||||||||||||||
243Am | 95 | 148 | 243.0613799(15) | 7,350(9) y | α | 239Np | 5/2− | ||||||||||||
SF (3.7×10−9%) | (various) | ||||||||||||||||||
243mAm | 2300(200) keV | 5.5(5) μs | SF | (various) | |||||||||||||||
IT ? | 243Am | ||||||||||||||||||
244Am | 95 | 149 | 244.0642829(16) | 10.01(3) h | β− | 244Cm | (6−) | ||||||||||||
244m1Am | 89.3(16) keV | 26.13(43) min | β− (99.96%) | 244Cm | 1+ | ||||||||||||||
EC (0.0364%) | 244Pu | ||||||||||||||||||
244m2Am | 2000(200)# | 900(150) μs | SF | (various) | |||||||||||||||
IT ? | 244Am | ||||||||||||||||||
244m3Am | 2200(200)# | ~6.5 μs | SF | (various) | |||||||||||||||
IT ? | 244Am | ||||||||||||||||||
245Am | 95 | 150 | 245.0664528(20) | 2.05(1) h | β− | 245Cm | 5/2+ | ||||||||||||
245mAm | 2400(400)# | 640(60) ns | SF | (various) | |||||||||||||||
IT ? | 245Am | ||||||||||||||||||
246Am | 95 | 151 | 246.069774(19)# | 39(3) min | β− | 246Cm | (7−) | ||||||||||||
246m1Am | 30(10)# keV | 25.0(2) min | β− | 246Cm | 2(−) | ||||||||||||||
IT ? | 246Am | ||||||||||||||||||
246m2Am | 2000(800)# keV | 73(10) μs | SF | (various) | |||||||||||||||
IT ? | 246Am | ||||||||||||||||||
247Am | 95 | 152 | 247.07209(11)# | 23.0(13) min | β− | 247Cm | 5/2# | ||||||||||||
This table header & footer: |
CD: | Cluster decay |
EC: | Electron capture |
IT: | Isomeric transition |
SF: | Spontaneous fission |
Actinides [3] by decay chain | Half-life range (a) | Fission products of 235U by yield [4] | ||||||
---|---|---|---|---|---|---|---|---|
4n | 4n + 1 | 4n + 2 | 4n + 3 | 4.5–7% | 0.04–1.25% | <0.001% | ||
228 Ra№ | 4–6 a | 155 Euþ | ||||||
248 Bk [5] | > 9 a | |||||||
244 Cmƒ | 241 Puƒ | 250 Cf | 227 Ac№ | 10–29 a | 90 Sr | 85 Kr | 113m Cdþ | |
232 Uƒ | 238 Puƒ | 243 Cmƒ | 29–97 a | 137 Cs | 151 Smþ | 121m Sn | ||
249 Cfƒ | 242m Amƒ | 141–351 a | No fission products have a half-life | |||||
241 Amƒ | 251 Cfƒ [6] | 430–900 a | ||||||
226 Ra№ | 247 Bk | 1.3–1.6 ka | ||||||
240 Pu | 229 Th | 246 Cmƒ | 243 Amƒ | 4.7–7.4 ka | ||||
245 Cmƒ | 250 Cm | 8.3–8.5 ka | ||||||
239 Puƒ | 24.1 ka | |||||||
230 Th№ | 231 Pa№ | 32–76 ka | ||||||
236 Npƒ | 233 Uƒ | 234 U№ | 150–250 ka | 99 Tc₡ | 126 Sn | |||
248 Cm | 242 Pu | 327–375 ka | 79 Se₡ | |||||
1.33 Ma | 135 Cs₡ | |||||||
237 Npƒ | 1.61–6.5 Ma | 93 Zr | 107 Pd | |||||
236 U | 247 Cmƒ | 15–24 Ma | 129 I₡ | |||||
244 Pu | 80 Ma | ... nor beyond 15.7 Ma [7] | ||||||
232 Th№ | 238 U№ | 235 Uƒ№ | 0.7–14.1 Ga | |||||
|
Americium-241 is the most common isotope of americium in nuclear waste. [8] It is the isotope used in an americium smoke detector based on an ionization chamber. It is a potential fuel for long-lifetime radioisotope thermoelectric generators.
Parameter | Value |
---|---|
Atomic mass | 241.056829 u |
Mass excess | 52930 keV |
Beta decay energy | −767 keV |
Spin | 5/2− |
Half-life | 432.6 years |
Spontaneous fissions | 1200 per kg s |
Decay heat | 114 watts/kg |
Possible parent nuclides: beta from 241Pu, electron capture from 241Cm, alpha from 245Bk.
241Am alpha decays, with a by-product of gamma rays. Its presence in plutonium is determined by the original concentration of 241Pu and the sample age. Due to the low penetration of alpha radiation, 241Am only poses a health risk when ingested or inhaled. Older samples of plutonium containing plutonium-241 contain a buildup of 241Am. A chemical removal of americium from reworked plutonium (e.g. during reworking of plutonium pits) may be required.
Probability | Decay mode | Decay energy | Decay product |
---|---|---|---|
99.54% | isomeric transition | 0.05 MeV | 242Am |
0.46% | alpha decay | 5.64 MeV | 238Np |
(1.5±0.6) × 10−10 [10] | spontaneous fission | ~200 MeV | fission products |
Americium-242m has a mass of 242.0595492 g/mol. It is one of the rare cases, like 108mAg, 166mHo, 180mTa, 186mRe, 192mIr, 210mBi, 212mPo and others, where a higher-energy nuclear isomer is more stable than the ground state, americium-242. [11]
242mAm is fissile with a low critical mass, comparable to that of 239Pu. [12] It has a very high fission cross section, and is quickly destroyed if it is produced in a nuclear reactor. It has been investigated whether this isotope could be used for a novel type of nuclear rocket. [13] [14]
Probability | Decay mode | Decay energy | Decay product |
---|---|---|---|
82.70% | beta decay | 0.665 MeV | 242 Cm |
17.30% | electron capture | 0.751 MeV | 242Pu |
Americium-243 has a mass of 243.06138 g/mol and a half-life of 7,370 years, the longest lasting of all americium isotopes. It is formed in the nuclear fuel cycle by neutron capture on plutonium-242 followed by beta decay. [15] Production increases exponentially with increasing burnup as a total of 5 neutron captures on 238U are required. If MOX-fuel is used, particularly MOX-fuel high in 241
Pu and 242
Pu, more americium overall and more 243
Am will be produced.
It decays by either emitting an alpha particle (with a decay energy of 5.27 MeV) [15] to become 239Np, which then quickly decays to 239Pu, or rarely, by spontaneous fission. [16]
As for the other americium isotopes, and more generally for all alpha emitters, 243Am is carcinogenic in case of internal contamination after being inhaled or ingested. 243Am also presents a risk of external irradiation associated with the gamma ray emitted by its short-lived decay product 239Np. The external irradiation risk for the other two americium isotopes (241Am and 242mAm) is less than 10% of that for americium-243. [8]
Americium is a synthetic chemical element; it has symbol Am and atomic number 95. It is radioactive and a transuranic member of the actinide series in the periodic table, located under the lanthanide element europium and was thus named after the Americas by analogy.
The actinide or actinoid series encompasses at least the 14 metallic chemical elements in the 5f series, with atomic numbers from 89 to 102, actinium through nobelium. The actinide series derives its name from the first element in the series, actinium. The informal chemical symbol An is used in general discussions of actinide chemistry to refer to any actinide.
Curium is a synthetic chemical element; it has symbol Cm and atomic number 96. This transuranic actinide element was named after eminent scientists Marie and Pierre Curie, both known for their research on radioactivity. Curium was first intentionally made by the team of Glenn T. Seaborg, Ralph A. James, and Albert Ghiorso in 1944, using the cyclotron at Berkeley. They bombarded the newly discovered element plutonium with alpha particles. This was then sent to the Metallurgical Laboratory at University of Chicago where a tiny sample of curium was eventually separated and identified. The discovery was kept secret until after the end of World War II. The news was released to the public in November 1947. Most curium is produced by bombarding uranium or plutonium with neutrons in nuclear reactors – one tonne of spent nuclear fuel contains ~20 grams of curium.
In nuclear engineering, fissile material is material that can undergo nuclear fission when struck by a neutron of low energy. A self-sustaining thermal chain reaction can only be achieved with fissile material. The predominant neutron energy in a system may be typified by either slow neutrons or fast neutrons. Fissile material can be used to fuel thermal-neutron reactors, fast-neutron reactors and nuclear explosives.
Mixed oxide fuel, commonly referred to as MOX fuel, is nuclear fuel that contains more than one oxide of fissile material, usually consisting of plutonium blended with natural uranium, reprocessed uranium, or depleted uranium. MOX fuel is an alternative to the low-enriched uranium fuel used in the light-water reactors that predominate nuclear power generation.
Fertile material is a material that, although not fissile itself, can be converted into a fissile material by neutron absorption.
Uranium (92U) is a naturally occurring radioactive element (radioelement) with no stable isotopes. It has two primordial isotopes, uranium-238 and uranium-235, that have long half-lives and are found in appreciable quantity in Earth's crust. The decay product uranium-234 is also found. Other isotopes such as uranium-233 have been produced in breeder reactors. In addition to isotopes found in nature or nuclear reactors, many isotopes with far shorter half-lives have been produced, ranging from 214U to 242U. The standard atomic weight of natural uranium is 238.02891(3).
Neptunium (93Np) is usually considered an artificial element, although trace quantities are found in nature, so a standard atomic weight cannot be given. Like all trace or artificial elements, it has no stable isotopes. The first isotope to be synthesized and identified was 239Np in 1940, produced by bombarding 238
U
with neutrons to produce 239
U
, which then underwent beta decay to 239
Np
.
Plutonium (94Pu) is an artificial element, except for trace quantities resulting from neutron capture by uranium, and thus a standard atomic weight cannot be given. Like all artificial elements, it has no stable isotopes. It was synthesized long before being found in nature, the first isotope synthesized being plutonium-238 in 1940. Twenty-one plutonium radioisotopes have been characterized. The most stable 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; and plutonium-240 with a half-life of 6,560 years. This element also has eight meta states; all have half-lives of less than one second.
Curium (96Cm) is an artificial element with an atomic number of 96. Because it is an artificial element, a standard atomic weight cannot be given, and it has no stable isotopes. The first isotope synthesized was 242Cm in 1944, which has 146 neutrons.
Californium (98Cf) is an artificial element, and thus a standard atomic weight cannot be given. Like all artificial elements, it has no stable isotopes. The first isotope to be synthesized was 245Cf in 1950. There are 20 known radioisotopes ranging from 237Cf to 256Cf and one nuclear isomer, 249mCf. The longest-lived isotope is 251Cf with a half-life of 898 years.
A minor actinide is an actinide, other than uranium or plutonium, found in spent nuclear fuel. The minor actinides include neptunium, americium, curium, berkelium, californium, einsteinium, and fermium. The most important isotopes of these elements in spent nuclear fuel are neptunium-237, americium-241, americium-243, curium-242 through -248, and californium-249 through -252.
Weapons-grade nuclear material is any fissionable nuclear material that is pure enough to make a nuclear weapon and has properties that make it particularly suitable for nuclear weapons use. Plutonium and uranium in grades normally used in nuclear weapons are the most common examples.
Plutonium-241 is an isotope of plutonium formed when plutonium-240 captures a neutron. Like some other plutonium isotopes, 241Pu is fissile, with a neutron absorption cross section about one-third greater than that of 239Pu, and a similar probability of fissioning on neutron absorption, around 73%. In the non-fission case, neutron capture produces plutonium-242. In general, isotopes with an odd number of neutrons are both more likely to absorb a neutron and more likely to undergo fission on neutron absorption than isotopes with an even number of neutrons.
Uranium-236 is an isotope of uranium that is neither fissile with thermal neutrons, nor very good fertile material, but is generally considered a nuisance and long-lived radioactive waste. It is found in spent nuclear fuel and in the reprocessed uranium made from spent nuclear fuel.
Plutonium-242 is one of the isotope of plutonium, the second longest-lived, with a half-life of 375,000 years. The half-life of 242Pu is about 15 times that of 239Pu; so it is one-fifteenth as radioactive, and not one of the larger contributors to nuclear waste radioactivity. 242Pu's gamma ray emissions are also weaker than those of the other isotopes.
Nuclear fission splits a heavy nucleus such as uranium or plutonium into two lighter nuclei, which are called fission products. Yield refers to the fraction of a fission product produced per fission.
Long-lived fission products (LLFPs) are radioactive materials with a long half-life produced by nuclear fission of uranium and plutonium. Because of their persistent radiotoxicity, it is necessary to isolate them from humans and the biosphere and to confine them in nuclear waste repositories for geological periods of time. The focus of this article is radioisotopes (radionuclides) generated by fission reactors.
Nuclear transmutation is the conversion of one chemical element or an isotope into another chemical element. Nuclear transmutation occurs in any process where the number of protons or neutrons in the nucleus of an atom is changed.
Americium-241 (241Am, Am-241) is an isotope of americium. Like all isotopes of americium, it is radioactive, with a half-life of 432.2 years. 241Am is the most common isotope of americium as well as the most prevalent isotope of americium in nuclear waste. It is commonly found in ionization type smoke detectors and is a potential fuel for long-lifetime radioisotope thermoelectric generators (RTGs). Its common parent nuclides are β− from 241Pu, EC from 241Cm, and α from 245Bk. 241Am is not fissile, but is fissionable, and the critical mass of a bare sphere is 57.6–75.6 kilograms (127.0–166.7 lb) and a sphere diameter of 19–21 centimetres (7.5–8.3 in). Americium-241 has a specific activity of 3.43 Ci/g (126.91 GBq/g). It is commonly found in the form of americium-241 dioxide (241AmO2). This isotope also has one meta state, 241mAm, with an excitation energy of 2.2 MeV (0.35 pJ) and a half-life of 1.23 μs. The presence of 241Am in plutonium is determined by the original concentration of plutonium-241 and the sample age. Because of the low penetration of alpha radiation, americium-241 only poses a health risk when ingested or inhaled. Older samples of plutonium containing 241Pu contain a buildup of 241Am. Chemical removal of americium-241 from reworked plutonium (e.g., during reworking of plutonium pits) may be required in some cases.