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Isotopes of aluminium

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Isotopes ofaluminium (13Al)
Main isotopes[1]Decay
Isotopeabun­dancehalf-life(t1/2)modepro­duct
26Altrace7.17×105 yβ+26Mg
27Al100%stable
Standard atomic weightAr°(Al)

Aluminium oraluminum (13Al) has one stable isotope,27Al, comprising all natural aluminium. Theradioactive26Al, with half-life 717,000 years, occurs in traces from cosmic-rayspallation ofargon in theatmosphere.

Other than26Al, there are 22 known synthetic radioisotopes from20Al to43Al, and 4 knownmetastable states; all have half-lives under 7 minutes, most under a second.

26Al is anextinct radionuclide and has received attention as such, being used in the study of meteorites. Its terrestrial occurrence has also found practical application in datingmarinesediments,manganese nodules, glacial ice,quartz inrock exposures, andmeteorites. The ratio of26Al to10Be has been used to study the role ofsediment transport,deposition, and storage, as well as burial times, and erosion, on 105 to 106 year time scales.[4]

List of isotopes

[edit]


Nuclide
[n 1]
ZNIsotopic mass(Da)[5]
[n 2][n 3]
Half-life[1]
Decay
mode
[1]
[n 4]
Daughter
isotope

[n 5]
Spin and
parity[1]
[n 6][n 7]
Isotopic
abundance
Excitation energy[n 7]
20Al[6]13720.04326(13)>1.1 zsp19Mg(1−)
21Al[7]13821.0278(13)>1.1 zsp20Mg(5/2+)
22Al13922.01942310(32)[8]91.1(5) msβ+, p (55%)21Na(4)+
β+ (44%)22Mg
β+, 2p (1.10%)20Ne
β+,α (0.038%)18Ne
23Al131023.00724435(37)446(6) msβ+ (98.78%)23Mg5/2+
β+, p (1.22%)22Na
24Al131123.99994760(24)2.053(4) sβ+ (99.96%)24Mg4+
β+, α (0.035%)20Ne
β+, p (0.0016%)23Na
24mAl425.8(1) keV130(3) msIT (82.5%)24Al1+
β+ (17.5%)24Mg
β+, α (0.028%)20Ne
25Al131224.990428308(69)7.1666(23) sβ+25Mg5/2+
26Al[n 8]131325.986891876(71)7.17(24)×105 yβ+ (85%)26Mg5+Trace[n 9]
EC (15%)[9]
26mAl228.306(13) keV6.3460(5) sβ+26Mg0+
27Al131426.981538408(50)Stable5/2+1.0000
28Al131527.981910009(52)2.245(5) minβ28Si3+
29Al131628.98045316(37)6.56(6) minβ29Si5/2+
30Al131729.9829692(21)3.62(6) sβ30Si3+
31Al131830.9839498(24)644(25) msβ (>98.4%)31Si5/2+
β,n (<1.6%)30Si
32Al131931.9880843(77)32.6(5) msβ (99.3%)32Si1+
β, n (0.7%)31Si
32mAl956.6(5) keV200(20) nsIT32Al(4+)
33Al132032.9908777(75)41.46(9) msβ (91.5%)33Si5/2+
β, n (8.5%)32Si
34Al132133.9967819(23)53.73(13) msβ (74%)34Si4−
β, n (26%)33Si
34mAl46.4(17) keV22.1(2) msβ (89%)34Si1+
β, n (11%)33Si
35Al132234.9997598(79)38.16(21) msβ (64.2%)35Si(5/2+,3/2+)
β, n (35.8%)34Si
36Al132336.00639(16)90(40) msβ (>69%)36Si
β, n (<31%)35Si
37Al132437.01053(19)11.4(3) msβ, n (52%)36Si5/2+#
β (<47%)37Si
β, 2n (>1%)35Si
38Al132538.01768(16)#9.0(7) msβ, n (84%)37Si0−#
β (16%)38Si
39Al132639.02307(32)#7.6(16) msβ, n (97%)38Si5/2+#
β (3%)39Si
40Al132740.03094(32)#5.7(3 (stat), 2 (sys)) ms[10]β, n (64%)39Si
β, 2n (20%)38Si
β (16%)40Si
41Al132841.03713(43)#3.5(8 (stat), 4 (sys)) ms[10]β, n (86%)40Si5/2+#
β, 2n (11%)39Si
β (3%)41Si
42Al132942.04508(54)#3# ms
[>170 ns]
43Al133043.05182(64)#4# ms
[>170 ns]
β?43Si5/2+#
This table header & footer:
  1. ^mAl – Excitednuclear 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:
    IT:Isomeric transition
  5. ^Bold symbol as daughter – Daughter product is stable.
  6. ^( ) spin value – Indicates spin with weak assignment arguments.
  7. ^ab# – Values marked # are not purely derived from experimental data, but at least partly from trends of neighboring nuclides (TNN).
  8. ^Used inradiodating events early in the Solar System's history andmeteorites
  9. ^cosmogenic

Aluminium-26

[edit]
Main article:Aluminium-26
The decay level scheme for26Al and26mAl to26Mg.[11][12]

Cosmogenicaluminium-26 was first described in studies of theMoon and meteorites. Meteorite fragments, after departure from their parent bodies, are exposed to intense cosmic-ray bombardment during their travel through space, causing substantial26Al production. After falling to Earth, atmospheric shielding protects the meteorite fragments from further26Al production, and its decay can then be used to determine the meteorite's terrestrial age. Meteorite research has also shown that26Al was relatively abundant at the time of formation of our planetary system. Most meteoriticists believe that the energy released by the decay of26Al was responsible for the melting anddifferentiation of someasteroids after their formation 4.55 billion years ago.[13]

See also

[edit]

Daughter products other than aluminum

References

[edit]
  1. ^abcdKondev, 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. ^"Standard Atomic Weights: Aluminium".CIAAW. 2017.
  3. ^Prohaska, Thomas; Irrgeher, Johanna; Benefield, Jacqueline; Böhlke, John K.; Chesson, Lesley A.; Coplen, Tyler B.; Ding, Tiping; Dunn, Philip J. H.; Gröning, Manfred; Holden, Norman E.; Meijer, Harro A. J. (2022-05-04)."Standard atomic weights of the elements 2021 (IUPAC Technical Report)".Pure and Applied Chemistry.doi:10.1515/pac-2019-0603.ISSN 1365-3075.
  4. ^Dickin, A.P. (2005)."In situ Cosmogenic Isotopes".Radiogenic Isotope Geology. Cambridge University Press.ISBN 978-0-521-53017-0. Archived fromthe original on 6 December 2008. Retrieved16 July 2008.
  5. ^Wang, Meng; Huang, W.J.; Kondev, F.G.; Audi, G.; Naimi, S. (2021). "The AME 2020 atomic mass evaluation (II). Tables, graphs and references*".Chinese Physics C.45 (3) 030003.doi:10.1088/1674-1137/abddaf.
  6. ^Kostyleva, D.; Xu, X.-D.; Mukha, I.; et al. (2025-07-10)."Isospin Symmetry Breaking Disclosed in the Decay of Three-Proton Emitter20Al".Physical Review Letters.135 (2).doi:10.1103/hkmy-yfdk.hdl:10261/397616.ISSN 0031-9007.
  7. ^Kostyleva, D.; Xu, X.-D.; Mukha, I.; et al. (2024-09-03). "Observation and spectroscopy of the proton-unbound nucleus21Al".Physical Review C.110 (3).arXiv:2406.04771.doi:10.1103/PhysRevC.110.L031301.ISSN 2469-9985.
  8. ^Campbell, S. E.; Bollen, G.; Brown, B. A.; Dockery, A.; Ireland, C. M.; Minamisono, K.; Puentes, D.; Rickey, B. J.; Ringle, R.; Yandow, I. T.; Fossez, K.; Ortiz-Cortes, A.; Schwarz, S.; Sumithrarachchi, C. S.; Villari, A. C. C. (9 April 2024). "Precision Mass Measurement of the Proton Dripline Halo Candidate Al 22".Physical Review Letters.132 (15).doi:10.1103/PhysRevLett.132.152501.
  9. ^Mougeot, X. (2019)."Towards high-precision calculation of electron capture decays".Applied Radiation and Isotopes.154 (108884).doi:10.1016/j.apradiso.2019.108884.
  10. ^abCrawford, H. L.; Tripathi, V.; Allmond, J. M.; et al. (2022)."CrossingN = 28 toward the neutron drip line: first measurement of half-lives at FRIB".Physical Review Letters.129 (212501) 212501.Bibcode:2022PhRvL.129u2501C.doi:10.1103/PhysRevLett.129.212501.PMID 36461950.S2CID 253600995.
  11. ^"Physics 6805 Topics in Nuclear Physics". Ohio State University. Archived fromthe original on 2 September 2021. Retrieved12 June 2019.
  12. ^Diehl, R (13 Dec 2005)."26Al in the inner Galaxy"(PDF).Astronomy & Astrophysics.449 (3):1025–1031.doi:10.1051/0004-6361:20054301. Retrieved12 June 2019.
  13. ^R. T. Dodd (1986).Thunderstones and Shooting Stars. Harvard University Press. pp. 89–90.ISBN 978-0-674-89137-1.
Group12 3456789101112131415161718
PeriodHydrogen and
alkali metals
Alkaline
earth metals
Pnicto­gensChal­co­gensHalo­gensNoble gases
12
345678910
1112131415161718
192021222324252627282930313233343536
373839404142434445464748495051525354
55561 asterisk71727374757677787980818283848586
87881 asterisk103104105106107108109110111112113114115116117118
119120
1 asterisk5758596061626364656667686970 
1 asterisk8990919293949596979899100101102
International
Other
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