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Isotopes of potassium

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(Redirected fromPotassium-41)

Isotopes ofpotassium (19K)
Main isotopesDecay
abun­dancehalf-life(t1/2)modepro­duct
39K93.3%stable
40K0.0120%1.248×109 yβ40Ca
ε40Ar
β+40Ar
41K6.73%stable
Standard atomic weightAr°(K)

Potassium (
19
K
) has 25 knownisotopes from34
K
to57
K
as well as31
K
, as well as an unconfirmed report of59
K
.[3] Three of those isotopes occur naturally: the two stable forms39
K
(93.3%) and41
K
(6.7%), and a very long-lived radioisotope40
K
(0.012%)

Naturally occurring radioactive40
K
decays with ahalf-life of 1.248×109 years. 89% of those decays are to stable40
Ca
bybeta decay, whilst 11% are to40
Ar
by eitherelectron capture orpositron emission. This latter decay branch has produced an isotopic abundance of argon on Earth which differs greatly from that seen ingas giants and stellar spectra.40
K
has the longest known half-life for any positron-emitternuclide. The long half-life of thisprimordial radioisotope is caused by a highlyspin-forbidden transition:40
K
has anuclear spin of 4, while both of its decay daughters areeven–even isotopes with spins of 0.

40
K
occurs in natural potassium in sufficient quantity that large bags ofpotassium chloride commercialsalt substitutes can be used as aradioactive source for classroom demonstrations.[citation needed]40
K
is the largest source of natural radioactivity in healthy animals and humans, greater even than14
C
. In a human body of 70 kg mass, about 4,400 nuclei of40
K
decay per second.[4]

The decay of40
K
to40
Ar
is used inpotassium-argon dating of rocks.Minerals are dated by measurement of the concentration of potassium and the amount of radiogenic40
Ar
that has accumulated. Typically, the method assumes that the rocks contained no argon at the time of formation and all subsequent radiogenic argon (i.e.,40
Ar
) was retained.[citation needed]40
K
has also been extensively used as aradioactive tracer in studies ofweathering.[citation needed]

All other potassium isotopes have half-lives under a day, most under a minute. The least stable is31
K
, a three-proton emitter discovered in 2019; its half-life was measured to be shorter than 10picoseconds.[5][6]

Stable potassium isotopes have been used for severalnutrient cycling studies since potassium is amacronutrient required forlife.[7]

List of isotopes

[edit]


Nuclide
[n 1]
ZNIsotopic mass(Da)[8]
[n 2][n 3]
Half-life[9]
[n 4]
Decay
mode
[9]
Daughter
isotope

[n 5]
Spin and
parity[9]
[n 6][n 4]
Natural abundance(mole fraction)
Excitation energy[n 4]Normal proportion[9]Range of variation
31
K
[5][6]
191231.03678(32)#<10 ps3p28S3/2+#
34K[10]191533.998404(18)p33Ar
35K191634.98800541(55)175.2(19) msβ+ (99.63%)35Ar3/2+
β+, p (0.37%)34Cl
36K191735.98130189(35)341(3) msβ+ (99.95%)36Ar2+
β+, p (0.048%)35Cl
β+,α (0.0034%)32S
37K191836.97337589(10)1.23651(94) sβ+37Ar3/2+
38K191937.96908111(21)7.651(19) minβ+38Ar3+
38m1K130.15(4) keV924.35(12) msβ+ (99.97%)38Ar0+
IT (0.0330%)38K
38m2K3458.10(17) keV21.95(11) μsIT38K(7)+
39K192038.9637064848(49)Stable3/2+0.932581(44)
40K[n 7][n 8]192139.963998165(60)1.248(3)×109 yβ (89.28%)40Ca4−1.17(1)×10−4
EC (10.72%)40Ar
β+ (0.001%)[11]
40mK1643.638(11) keV336(12) nsIT40K0+
41K192240.9618252561(40)Stable3/2+0.067302(44)
42K192341.96240231(11)12.355(7) hβ42Ca2−Trace[n 9]
43K192442.96073470(44)22.3(1) hβ43Ca3/2+
43mK738.30(6) keV200(5) nsIT43K7/2−
44K192543.96158698(45)22.13(19) minβ44Ca2−
45K192644.96069149(56)17.8(6) minβ45Ca3/2+
46K192745.96198158(78)96.30(8) sβ46Ca2−
47K192846.9616616(15)17.38(3) sβ47Ca1/2+
48K192947.96534118(83)6.83(14) sβ (98.86%)48Ca1−
β,n (1.14%)47Ca
49K193048.96821075(86)1.26(5) sβ, n (86%)48Ca1/2+
β (14%)49Ca
50K193149.9723800(83)472(4) msβ (71.4%)50Ca0−
β, n (28.6%)49Ca
β, 2n?48Ca
50mK172.0(4) keV125(40) nsIT50K(2−)
51K193250.975828(14)365(5) msβ, n (65%)50Ca3/2+
β (35%)51Ca
β, 2n?49Ca
52K193351.981602(36)110(4) msβ, n (72.2%)51Ca2−#
β (25.5%)52Ca
β, 2n (2.3%)50Ca
53K193452.98680(12)30(5) msβ, n (64%)52Ca3/2+
β (26%)53Ca
β, 2n (10%)51Ca
54K193553.99447(43)#10(5) msβ54Ca2−#
β, n?53Ca
β, 2n?52Ca
55K193655.00051(54)#10# ms
[>620 ns]
β?55Ca3/2+#
β, n?54Ca
β, 2n?53Ca
56K193756.00857(64)#5# ms
[>620 ns]
β?56Ca2−#
β, n?55Ca
β, 2n?54Ca
57K193857.01517(64)#2# ms
[>400 ns]
β?57Ca3/2+#
β, n?56Ca
β, 2n?55Ca
59K[3][n 10]194059.03086(86)#1# ms
[>400 ns]
β?59Ca3/2+#
β, n?58Ca
β, 2n?57Ca
This table header & footer:
  1. ^mK – 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. ^abc# – Values marked # are not purely derived from experimental data, but at least partly from trends of neighboring nuclides (TNN).
  5. ^Bold symbol as daughter – Daughter product is stable.
  6. ^( ) spin value – Indicates spin with weak assignment arguments.
  7. ^Used inpotassium-argon dating
  8. ^Primordialradionuclide
  9. ^Decay product of42Ar
  10. ^Discovery of this isotope is unconfirmed.

See also

[edit]

References

[edit]
  1. ^"Standard Atomic Weights: Potassium".CIAAW. 1979.
  2. ^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.
  3. ^abNeufcourt, Léo; Cao, Yuchen; Nazarewicz, Witold; et al. (14 February 2019). "Neutron Drip Line in the Ca Region from Bayesian Model Averaging".Physical Review Letters.122 (6): 062502.arXiv:1901.07632.Bibcode:2019PhRvL.122f2502N.doi:10.1103/PhysRevLett.122.062502.PMID 30822058.
  4. ^"Radioactive Human Body". Retrieved2011-05-18.
  5. ^ab"A peculiar atom shakes up assumptions of nuclear structure".Nature.573 (7773): 167. 6 September 2019.Bibcode:2019Natur.573T.167..doi:10.1038/d41586-019-02655-9.PMID 31506620.
  6. ^abKostyleva, D.; et al. (2019). "Towards the Limits of Existence of Nuclear Structure: Observation and First Spectroscopy of the Isotope31K by Measuring Its Three-Proton Decay".Physical Review Letters.123 (9): 092502.arXiv:1905.08154.Bibcode:2019PhRvL.123i2502K.doi:10.1103/PhysRevLett.123.092502.PMID 31524489.S2CID 159041565.
  7. ^"Soil potassium isotope composition during four million years of ecosystem development in Hawai'i".par.nsf.gov. June 2022.
  8. ^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.
  9. ^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.
  10. ^Dronchi, N.; Charity, R. J.; Sobotka, L. G.; Brown, B. A.; Weisshaar, D.; Gade, A.; Brown, K. W.; Reviol, W.; Bazin, D.; Farris, P. J.; Hill, A. M.; Li, J.; Longfellow, B.; Rhodes, D.; Paneru, S. N.; Gillespie, S. A.; Anthony, A. K.; Rubino, E.; Biswas, S. (2024-09-12). "Evolution of shell gaps in the neutron-poor calcium region from invariant-mass spectroscopy of37,38Sc,35Ca, and34K".Physical Review C.110 (3).doi:10.1103/PhysRevC.110.L031302.ISSN 2469-9985.
  11. ^Engelkemeir, D. W.; Flynn, K. F.; Glendenin, L. E. (1962). "Positron Emission in the Decay of K40".Physical Review.126 (5): 1818.Bibcode:1962PhRv..126.1818E.doi:10.1103/PhysRev.126.1818.
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
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