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词条 Isotopes of potassium
释义

  1. List of isotopes

      Notes  

  2. References

{{infobox potassium isotopes}}

Potassium (19K) has 25 known isotopes from 32K to 57K, with unconfirmed detection of 59K. Three isotopes occur naturally: stable 39K (93.3%) and 41K (6.7%), and the long-lived radioisotope 40K (0.012%).

Naturally occurring radioactive 40K decays to stable 40Ar (10.72% of decays) by electron capture or positron emission (giving it the longest known positron-emitter nuclide half-life). Alternately, and most of the time (89.28%), it decays to stable 40Ca by beta decay. 40K has a half-life of 1.248×109 years. The long half life of this primordial radioisotope is caused by a highly spin-forbidden transition: 40K has a nuclear spin of 4, while both of its decay daughters are even-even isotopes with spins of 0.{{original research inline|date=May 2018}}

40K occurs in natural potassium (and thus in some commercial salt substitutes) in sufficient quantity that large bags of those substitutes can be used as a radioactive source for classroom demonstrations.{{citation needed|date=May 2018}} In healthy animals and people, 40K represents the largest source of radioactivity, greater even than 14C. In a human body of 70 kg mass, about 4,400 nuclei of 40K decay per second.[1]

The decay of 40K to 40Ar enables a commonly used method for dating rocks. The conventional K-Ar dating method depends on the assumption that the rocks contained no argon at the time of formation and that all the subsequent radiogenic argon (i.e., 40Ar) was quantitatively retained. Minerals are dated by measurement of the concentration of potassium and the amount of radiogenic 40Ar that has accumulated.

All other potassium isotopes have half-lives under a day, most under a minute. The least stable are 33K and 34K, both with half-lives shorter than 25 nanoseconds. The half-life of 32K is unknown.

Outside its use in dating, 40K has been used extensively as tracers in studies of weathering. Various potassium isotopes have also been used for nutrient cycling studies because potassium is a macronutrient required for life.{{citation needed|date=May 2018}}

List of isotopes

{{update|date=July 2018}}
nuclide
symbol
Z(p) N(n)  
isotopic mass (u)
 
half-lifedecay
mode(s)[2]
daughter
isotope(s)[3]
nuclear
spin and
parity
representative
isotopic
composition
(mole fraction)
excitation energy
32K1913 32.02192(54)# unknown p 31Ar 1+#
32mK950(100)# keV unknown 4+#
33K1914 33.00726(21)# <25 ns p 32Ar (3/2+)#
34K1915 33.99841(32)# <25 ns p 33Ar 1+#
35K191634.988010(21)178(8) ms β+ (99.63%) 35Ar3/2+
β+, p (.37%) 34Cl
36K191735.981292(8)342(2) ms β+ (99.94%) 36Ar2+
β+, p (.048%) 35Cl
β+, α (.012%) 32S
37K1918 36.97337589(10) 1.226(7) s β+ 37Ar 3/2+
38K1919 37.9690812(5) 7.636(18) min β+ 38Ar 3+
38m1K130.50(28) keV 924.2(3) ms 0+
38m2K3458.0(2) keV 21.98(11) µs (7+),(5+)
39K1920 38.96370668(20)Stable 3/2+ 0.932581(44)
40K[4][5]192139.96399848(21)1.248(3)×109 y β (89.28%) 40Ca41.17(1)×10−4
EC (10.72%)40Ar
β+ (0.001%)[6]
40mK1643.639(11) keV 336(12) ns 0+
41K1922 40.96182576(21)Stable 3/2+ 0.067302(44)
42K1923 41.96240281(24) 12.360(12) h β 42Ca 2
43K1924 42.960716(10) 22.3(1) h β 43Ca 3/2+
44K1925 43.96156(4) 22.13(19) min β 44Ca 2−
45K1926 44.960699(11) 17.3(6) min β 45Ca 3/2+
46K1927 45.961977(17) 105(10) s β 46Ca 2(−)
47K1928 46.961678(9) 17.50(24) s β 47Ca 1/2+
48K192947.965514(26)6.8(2) s β (98.86%) 48Ca(2−)
β, n (1.14%) 47Ca
49K193048.96745(8)1.26(5) s β, n (86%) 48Ca(3/2+)
β (14%) 49Ca
50K193149.97278(30)472(4) ms β (71%) 50Ca(0−,1,2−)
β, n (29%) 49Ca
51K193250.97638(54)#365(5) ms β (53%) 51Ca3/2+#
β, n (47%) 50Ca
52K193351.98261(75)#105(5) ms β, n (64%) 51Ca(2−)#
β, 2n (21%) 50Ca
β (15%) 52Ca
53K193452.98712(75)#30(5) ms β, n (67%) 52Ca(3/2+)#
β, 2n (17%) 51Ca
β (16%) 53Ca
54K193553.99420(97)#10(5) ms β (>99.9%) 54Ca2−#
β, n (<.1%) 53Ca
55K193654.99971(107)#3# ms β 55Ca3/2+#
β, n 54Ca
1. ^{{Cite web | url=http://www.fas.harvard.edu/~scdiroff/lds/QuantumRelativity/RadioactiveHumanBody/RadioactiveHumanBody.html | title=Radioactive Human Body |accessdate=2011-05-18}}
2. ^{{cite web |url=http://www.nucleonica.net/unc.aspx |title=Universal Nuclide Chart |publisher=nucleonica |registration=yes}}
3. ^Bold for stable isotopes, bold italic for nearly-stable isotopes (half-life longer than the age of the universe)
4. ^Used in potassium-argon dating
5. ^Primordial radionuclide
6. ^{{Cite journal| volume = 126| issue = 5| pages = 1818| last = Engelkemeir| first = D. W.| last2 = Flynn| first2 = K. F.| last3 = Glendenin| first3 = L. E.| title = Positron Emission in the Decay of K40| journal = Physical Review| date = 1962| doi = 10.1103/PhysRev.126.1818|bibcode = 1962PhRv..126.1818E }}

Notes

  • Values marked # are not purely derived from experimental data, but at least partly from systematic trends. Spins with weak assignment arguments are enclosed in parentheses.
  • Uncertainties are given in concise form in parentheses after the corresponding last digits. Uncertainty values denote one standard deviation, except isotopic composition and standard atomic mass from IUPAC, which use expanded uncertainties.
  • Nuclide masses are given by IUPAP Commission on Symbols, Units, Nomenclature, Atomic Masses and Fundamental Constants (SUNAMCO).
  • Isotope abundances are given by IUPAC Commission on Isotopic Abundances and Atomic Weights (CIAAW).

References

  • Isotope masses from:
    • {{NUBASE 2003}}
  • Isotopic compositions and standard atomic masses from:
    • {{CAWIA 2003}}
    • {{CIAAW 2005}}
  • Half-life, spin, and isomer data selected from the following sources. See editing notes on this article's talk page.
    • {{NUBASE 2003}}
    • {{NNDC}}
    • {{CRC85|chapter=11}}
{{Navbox element isotopes}}

3 : Potassium|Isotopes of potassium|Lists of isotopes by element

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