Isotopes of actinium

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Isotopes of actinium  (89Ac)
Main isotopes [1] Decay
abun­dance half-life (t1/2) mode pro­duct
225Ac trace 9.919 d α 221Fr
14C 211Bi
226Ac synth 29.37 h β 226Th
ε 226Ra
α 222Fr
227Actrace21.772 yβ 227Th
α 223Fr

Actinium (89Ac) has no stable isotopes and no characteristic terrestrial isotopic composition, thus a standard atomic weight cannot be given. There are 34 known isotopes, from 203Ac to 236Ac, and 7 isomers. Three isotopes are found in nature, 225Ac, 227Ac and 228Ac, as intermediate decay products of, respectively, 237Np, 235U, and 232Th. 228Ac and 225Ac are extremely rare, so almost all natural actinium is 227Ac.

Contents

The most stable isotopes are 227Ac with a half-life of 21.772 years, 225Ac with a half-life of 10.0 days, and 226Ac with a half-life of 29.37 hours. All other isotopes have half-lives under 10 hours, and most under a minute. The shortest-lived known isotope is 217Ac with a half-life of 69 ns.

Purified 227Ac comes into equilibrium with its decay products (227Th and 223Fr) after 185 days. [2]

List of isotopes

Nuclide
[n 1]
Historic
name
Z N Isotopic mass (Da)
[n 2] [n 3]
Half-life
Decay
mode

[n 4]
Daughter
isotope

[n 5]
Spin and
parity
[n 6] [n 7]
Isotopic
abundance
Excitation energy [n 7]
203Ac [3] 8911456+269
−26
 μs
α 199Fr(1/2+)
204Ac [4] 891157.4+2.2
−1.4
 ms
α200Fr
205Ac [5] 891167.7+2.7
−1.6
 ms
[4]
α201Fr9/2−?
206Ac89117206.01450(8)25(7) msα202Fr(3+)
206m1Ac80(50) keV15(6) msα202Fr
206m2Ac290(110)# keV41(16) msα202mFr(10−)
207Ac89118207.01195(6)31(8) ms
[27(+11−6) ms]
α203Fr9/2−#
208Ac89119208.01155(6)97(16) ms
[95(+24−16) ms]
α (99%)204Fr(3+)
β+ (1%)208Ra
208mAc506(26) keV28(7) ms
[25(+9−5) ms]
α (89%)204Fr(10−)
IT (10%)208Ac
β+ (1%)208Ra
209Ac89120209.00949(5)92(11) msα (99%)205Fr(9/2−)
β+ (1%)209Ra
210Ac89121210.00944(6)350(40) msα (96%)206Fr7+#
β+ (4%)210Ra
211Ac89122211.00773(8)213(25) msα (99.8%)207Fr9/2−#
β+ (.2%)211Ra
212Ac89123212.00781(7)920(50) msα (97%)208Fr6+#
β+ (3%)212Ra
213Ac89124213.00661(6)731(17) msα209Fr(9/2−)#
β+ (rare)213Ra
214Ac89125214.006902(24)8.2(2) sα (89%)210Fr(5+)#
β+ (11%)214Ra
215Ac89126215.006454(23)0.17(1) sα (99.91%)211Fr9/2−
β+ (.09%)215Ra
216Ac89127216.008720(29)0.440(16) msα212Fr(1−)
β+ (7×10−5%)216Ra
216mAc44(7) keV443(7) µsα212Fr(9−)
217Ac89128217.009347(14)69(4) nsα213Fr9/2−
β+ (6.9×10−9%)217Ra
217mAc2012(20) keV740(40) ns(29/2)+
218Ac89129218.01164(5)1.08(9) µsα214Fr(1−)#
218mAc584(50)# keV103(11) ns(11+)
219Ac89130219.01242(5)11.8(15) µsα215Fr9/2−
β+ (10−6%)219Ra
220Ac89131220.014763(16)26.36(19) msα216Fr(3−)
β+ (5×10−4%)220Ra
221Ac89132221.01559(5)52(2) msα217Fr9/2−#
222Ac89133222.017844(6)5.0(5) sα (99%)218Fr1−
β+ (1%)222Ra
222mAc200(150)# keV1.05(7) minα (88.6%)218Frhigh
IT (10%)222Ac
β+ (1.4%)222Ra
223Ac89134223.019137(8)2.10(5) minα (99%)219Fr(5/2−)
EC (1%)223Ra
CD (3.2×10−9%)209Bi
14C
224Ac89135224.021723(4)2.78(17) hβ+ (90.9%)224Ra0−
α (9.1%)220Fr
β (1.6%)224Th
225Ac [n 8] 89136225.023230(5)10.0(1) dα221Fr(3/2−)Trace [n 9]
CD (6×10−10%)211Bi
14C
226Ac89137226.026098(4)29.37(12) hβ (83%)226Th(1)(−#)
EC (17%)226Ra
α (.006%)222Fr
227AcActinium [n 10] 89138227.0277521(26)21.772(3) yβ (98.62%)227Th3/2−Trace [n 11]
α (1.38%)223Fr
228AcMesothorium 289139228.0310211(27)6.13(2) hβ228Th3+Trace [n 12]
229Ac89140229.03302(4)62.7(5) minβ229Th(3/2+)
230Ac89141230.03629(32)122(3) sβ230Th(1+)
231Ac89142231.03856(11)7.5(1) minβ231Th(1/2+)
232Ac89143232.04203(11)119(5) sβ232Th(1+)
233Ac89144233.04455(32)#145(10) sβ233Th(1/2+)
234Ac89145234.04842(43)#44(7) sβ234Th
235Ac89146235.05123(38)#60(4) sβ235Th1/2+#
236Ac [6] 89147236.05530(54)#72+345
−33
 s
β236Th
This table header & footer:
  1. mAc  Excited nuclear isomer.
  2. ()  Uncertainty (1σ) is given in concise form in parentheses after the corresponding last digits.
  3. #  Atomic mass marked #: value and uncertainty derived not from purely experimental data, but at least partly from trends from the Mass Surface (TMS).
  4. Modes of decay:
    CD: Cluster decay
    EC: Electron capture
    IT: Isomeric transition
  5. Bold italics symbol as daughter  Daughter product is nearly stable.
  6. () spin value  Indicates spin with weak assignment arguments.
  7. 1 2 #  Values marked # are not purely derived from experimental data, but at least partly from trends of neighboring nuclides (TNN).
  8. Has medical uses
  9. Intermediate decay product of 237Np
  10. Source of element's name
  11. Intermediate decay product of 235U
  12. Intermediate decay product of 232Th

Actinides vs fission products

Actinides [7] by decay chain Half-life
range (a)
Fission products of 235U by yield [8]
4n 4n + 1 4n + 2 4n + 3 4.5–7%0.04–1.25%<0.001%
228 Ra 4–6 a 155 Euþ
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
248 Bk [9] 249 Cfƒ 242m Amƒ141–351 a

No fission products have a half-life
in the range of 100 a–210 ka ...

241 Amƒ 251 Cfƒ [10] 430–900 a
226 Ra 247 Bk1.3–1.6 ka
240 Pu 229 Th 246 Cmƒ 243 Amƒ4.7–7.4 ka
245 Cmƒ 250 Cm8.3–8.5 ka
239 Puƒ24.1 ka
230 Th 231 Pa32–76 ka
236 Npƒ 233 Uƒ 234 U 150–250 ka 99 Tc 126 Sn
248 Cm 242 Pu 327–375 ka 79 Se
1.53 Ma 93 Zr
237 Npƒ 2.1–6.5 Ma 135 Cs 107 Pd
236 U 247 Cmƒ 15–24 Ma 129 I
244 Pu80 Ma

... nor beyond 15.7 Ma [11]

232 Th 238 U 235 Uƒ№0.7–14.1 Ga

See also

Related Research Articles

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Thorium (90Th) has seven naturally occurring isotopes but none are stable. One isotope, 232Th, is relatively stable, with a half-life of 1.405×1010 years, considerably longer than the age of the Earth, and even slightly longer than the generally accepted age of the universe. This isotope makes up nearly all natural thorium, so thorium was considered to be mononuclidic. However, in 2013, IUPAC reclassified thorium as binuclidic, due to large amounts of 230Th in deep seawater. Thorium has a characteristic terrestrial isotopic composition and thus a standard atomic weight can be given.

Radium (88Ra) has no stable or nearly stable isotopes, and thus a standard atomic weight cannot be given. The longest lived, and most common, isotope of radium is 226Ra with a half-life of 1600 years. 226Ra occurs in the decay chain of 238U. Radium has 34 known isotopes from 201Ra to 234Ra.

There are 39 known isotopes of radon (86Rn), from 193Rn to 231Rn; all are radioactive. The most stable isotope is 222Rn with a half-life of 3.823 days, which decays into 218
Po
. Six isotopes of radon, 217, 218, 219, 220, 221, 222Rn, occur in trace quantities in nature as decay products of, respectively, 217At, 218At, 223Ra, 224Ra, 225Ra, and 226Ra. 217Rn and 221Rn are produced in rare branches in the decay chain of trace quantities of 237Np; 222Rn is an intermediate step in the decay chain of 238U; 219Rn is an intermediate step in the decay chain of 235U; and 220Rn occurs in the decay chain of 232Th.

Lead (82Pb) has four observationally stable isotopes: 204Pb, 206Pb, 207Pb, 208Pb. Lead-204 is entirely a primordial nuclide and is not a radiogenic nuclide. The three isotopes lead-206, lead-207, and lead-208 represent the ends of three decay chains: the uranium series, the actinium series, and the thorium series, respectively; a fourth decay chain, the neptunium series, terminates with the thallium isotope 205Tl. The three series terminating in lead represent the decay chain products of long-lived primordial 238U, 235U, and 232Th. Each isotope also occurs, to some extent, as primordial isotopes that were made in supernovae, rather than radiogenically as daughter products. The fixed ratio of lead-204 to the primordial amounts of the other lead isotopes may be used as the baseline to estimate the extra amounts of radiogenic lead present in rocks as a result of decay from uranium and thorium.

Bismuth (83Bi) has 41 known isotopes, ranging from 184Bi to 224Bi. Bismuth has no stable isotopes, but does have one very long-lived isotope; thus, the standard atomic weight can be given as 208.98040(1). Although bismuth-209 is now known to be radioactive, it has classically been considered to be a stable isotope because it has a half-life of approximately 2.01×1019 years, which is more than a billion times the age of the universe. Besides 209Bi, the most stable bismuth radioisotopes are 210mBi with a half-life of 3.04 million years, 208Bi with a half-life of 368,000 years and 207Bi, with a half-life of 32.9 years, none of which occurs in nature. All other isotopes have half-lives under 1 year, most under a day. Of naturally occurring radioisotopes, the most stable is radiogenic 210Bi with a half-life of 5.012 days. 210mBi is unusual for being a nuclear isomer with a half-life multiple orders of magnitude longer than that of the ground state.

Promethium (61Pm) is an artificial element, except in trace quantities as a product of spontaneous fission of 238U and 235U and alpha decay of 151Eu, and thus a standard atomic weight cannot be given. Like all artificial elements, it has no stable isotopes. It was first synthesized in 1945.

Indium (49In) consists of two primordial nuclides, with the most common (~ 95.7%) nuclide (115In) being measurably though weakly radioactive. Its spin-forbidden decay has a half-life of 4.41×1014 years, much longer than the currently accepted age of the Universe.

Technetium (43Tc) is one of the two elements with Z < 83 that have no stable isotopes; the other such element is promethium. It is primarily artificial, with only trace quantities existing in nature produced by spontaneous fission or neutron capture by molybdenum. The first isotopes to be synthesized were 97Tc and 99Tc in 1936, the first artificial element to be produced. The most stable radioisotopes are 97Tc, 98Tc, and 99Tc.

Naturally occurring chromium (24Cr) is composed of four stable isotopes; 50Cr, 52Cr, 53Cr, and 54Cr with 52Cr being the most abundant (83.789% natural abundance). 50Cr is suspected of decaying by β+β+ to 50Ti with a half-life of (more than) 1.8×1017 years. Twenty-two radioisotopes, all of which are entirely synthetic, have been characterized, the most stable being 51Cr with a half-life of 27.7 days. All of the remaining radioactive isotopes have half-lives that are less than 24 hours and the majority of these have half-lives that are less than 1 minute. This element also has two meta states, 45mCr, the more stable one, and 59mCr, the least stable isotope or isomer.

Naturally occurring vanadium (23V) is composed of one stable isotope 51V and one radioactive isotope 50V with a half-life of 2.71×1017 years. 24 artificial radioisotopes have been characterized (in the range of mass number between 40 and 65) with the most stable being 49V with a half-life of 330 days, and 48V with a half-life of 15.9735 days. All of the remaining radioactive isotopes have half-lives shorter than an hour, the majority of them below 10 seconds, the least stable being 42V with a half-life shorter than 55 nanoseconds, with all of the isotopes lighter than it, and none of the heavier, have unknown half-lives. In 4 isotopes, metastable excited states were found (including 2 metastable states for 60V), which adds up to 5 meta states.

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 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.

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. 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.

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.

Berkelium (97Bk) 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 243Bk in 1949. There are 20 known radioisotopes, from 230Bk and 233Bk to 253Bk, and 6 nuclear isomers. The longest-lived isotope is 247Bk with a half-life of 1,380 years.

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.

Meitnerium (109Mt) is a synthetic element, and thus a standard atomic weight cannot be given. Like all synthetic elements, it has no stable isotopes. The first isotope to be synthesized was 266Mt in 1982, and this is also the only isotope directly synthesized; all other isotopes are only known as decay products of heavier elements. There are eight known isotopes, from 266Mt to 278Mt. There may also be two isomers. The longest-lived of the known isotopes is 278Mt with a half-life of 8 seconds. The unconfirmed heavier 282Mt appears to have an even longer half-life of 67 seconds.

Roentgenium (111Rg) is a synthetic element, and thus a standard atomic weight cannot be given. Like all synthetic elements, it has no stable isotopes. The first isotope to be synthesized was 272Rg in 1994, which is also the only directly synthesized isotope; all others are decay products of heavier elements. There are seven known radioisotopes, having mass numbers of 272, 274, and 278–282. The longest-lived isotope is 282Rg with a half-life of about 2 minutes, although the unconfirmed 283Rg and 286Rg may have longer half-lives of about 5.1 minutes and 10.7 minutes respectively.

<span class="mw-page-title-main">Actinium-225</span> Isotope of actinium

Actinium-225 is an isotope of actinium. It undergoes alpha decay to francium-221 with a half-life of 10 days, and is an intermediate decay product in the neptunium series. Except for minuscule quantities arising from this decay chain in nature, 225Ac is entirely synthetic.

References

  1. Kondev, F. G.; Wang, M.; Huang, W. J.; Naimi, S.; Audi, G. (2021). "The NUBASE2020 evaluation of nuclear properties" (PDF). Chinese Physics C. 45 (3): 030001. doi:10.1088/1674-1137/abddae.
  2. G. D. Considine, ed. (2005). "Chemical Elements". Van Nostrand's Encyclopedia of Chemistry. Wiley-Interscience. p. 332. ISBN   978-0-471-61525-5.
  3. Wang, J. G.; Gan, Z. G.; Zhang, Z. Y.; et al. (1 March 2024). "α-decay properties of new neutron-deficient isotope 203Ac". Physics Letters B. 850: 138503. doi: 10.1016/j.physletb.2024.138503 . ISSN   0370-2693 . Retrieved 6 February 2024.
  4. 1 2 Huang, M. H.; Gan, Z. G.; Zhang, Z. Y.; et al. (10 November 2022). "α decay of the new isotope 204Ac". Physics Letters B. 834: 137484. Bibcode:2022PhLB..83437484H. doi: 10.1016/j.physletb.2022.137484 . ISSN   0370-2693. S2CID   252730841.
  5. Zhang, Z. Y.; Gan, Z. G.; Ma, L.; et al. (January 2014). "α decay of the new neutron-deficient isotope 205Ac". Physical Review C. 89 (1): 014308. Bibcode:2014PhRvC..89a4308Z. doi:10.1103/PhysRevC.89.014308.
  6. Chen, L.; et al. (2010). "Discovery and investigation of heavy neutron-rich isotopes with time-resolved Schottky spectrometry in the element range from thallium to actinium" (PDF). Physics Letters B. 691 (5): 234–237. Bibcode:2010PhLB..691..234C. doi:10.1016/j.physletb.2010.05.078.
  7. Plus radium (element 88). While actually a sub-actinide, it immediately precedes actinium (89) and follows a three-element gap of instability after polonium (84) where no nuclides have half-lives of at least four years (the longest-lived nuclide in the gap is radon-222 with a half life of less than four days). Radium's longest lived isotope, at 1,600 years, thus merits the element's inclusion here.
  8. Specifically from thermal neutron fission of uranium-235, e.g. in a typical nuclear reactor.
  9. Milsted, J.; Friedman, A. M.; Stevens, C. M. (1965). "The alpha half-life of berkelium-247; a new long-lived isomer of berkelium-248". Nuclear Physics. 71 (2): 299. Bibcode:1965NucPh..71..299M. doi:10.1016/0029-5582(65)90719-4.
    "The isotopic analyses disclosed a species of mass 248 in constant abundance in three samples analysed over a period of about 10 months. This was ascribed to an isomer of Bk248 with a half-life greater than 9 [years]. No growth of Cf248 was detected, and a lower limit for the β half-life can be set at about 104 [years]. No alpha activity attributable to the new isomer has been detected; the alpha half-life is probably greater than 300 [years]."
  10. This is the heaviest nuclide with a half-life of at least four years before the "sea of instability".
  11. Excluding those "classically stable" nuclides with half-lives significantly in excess of 232Th; e.g., while 113mCd has a half-life of only fourteen years, that of 113Cd is eight quadrillion years.