Isotopes of argon

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The main isotopes of argon (Ar) found on Earth are 40Ar, 36Ar, and 38Ar. Naturally occurring 40K with a half-life of 1.250×109 years, decays to stable 40Ar (11.2%) by electron capture and by positron emission, and also transforms to stable 40Ca (88.8%) via beta decay. These properties and ratios are used to determine the age of rocks through potassium-argon dating.[1]

In the Earth's atmosphere, 39Ar is made by cosmic ray activity, primarily with 40Ar. In the subsurface environment, it is also produced through neutron capture by 39K or alpha emission by calcium. The content of 39Ar in natural argon is measured to be of (8.0±0.6)×10−16 g/g, or (1.01±0.08) Bq/kg of natAr [2]. 37Ar is created from the decay of 40Ca as a result of subsurface nuclear explosions. It has a half-life of 35 days.[1] The content of 42Ar in the Earth's atmosphere is lower than 6×10−21 parts per part of natAr [3].


Standard atomic mass: 39.948(1) u.

Contents

[edit] Table

nuclide
symbol
Z(p) N(n)  
isotopic mass (u)
 
half-life nuclear
spin
representative
isotopic
composition
(mole fraction)
range of natural
variation
(mole fraction)
excitation energy
30Ar 18 12 30.02156(32)# <20 ns 0+
31Ar 18 13 31.01212(22)# 14.4(6) ms 5/2(+#)
32Ar 18 14 31.9976380(19) 98(2) ms 0+
32mAr 5600(100)# keV  ? 5-#
33Ar 18 15 32.9899257(5) 173.0(20) ms 1/2+
34Ar 18 16 33.9802712(4) 844.5(34) ms 0+
35Ar 18 17 34.9752576(8) 1.775(4) s 3/2+
36Ar 18 18 35.967545106(29) STABLE 0+ 0.003365(30)
37Ar 18 19 36.96677632(22) 35.04(4) d 3/2+
38Ar 18 20 37.9627324(4) STABLE 0+ 0.000632(5)
39Ar 18 21 38.964313(5) 269(3) a 7/2-
40Ar 18 22 39.9623831225(29) STABLE 0+ 0.996003(30)
41Ar 18 23 40.9645006(4) 109.61(4) min 7/2-
42Ar 18 24 41.963046(6) 32.9(11) a 0+
43Ar 18 25 42.965636(6) 5.37(6) min (5/2-)
44Ar 18 26 43.9649240(17) 11.87(5) min 0+
45Ar 18 27 44.9680400(6) 21.48(15) s (1/2,3/2,5/2)-
46Ar 18 28 45.96809(4) 8.4(6) s 0+
47Ar 18 29 46.97219(11) 1.23(3) s 3/2-#
48Ar 18 30 47.97454(32)# 0.48(40) s 0+
49Ar 18 31 48.98052(54)# 170(50) ms 3/2-#
50Ar 18 32 49.98443(75)# 85(30) ms 0+
51Ar 18 33 50.99163(75)# 60# ms [>200 ns] 3/2-#
52Ar 18 34 51.99678(97)# 10# ms 0+
53Ar 18 35 53.00494(107)# 3# ms (5/2-)#

[edit] Notes

  • The isotopic composition refers to that in air.
  • Geologically exceptional samples are known in which the isotopic composition lies outside the reported range. The uncertainty in the atomic mass may exceed the stated value for such specimens.
  • 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.

[edit] References

  1. ^ a b 40Ar/39Ar dating and errors. Retrieved on 2007-03-07.
  2. ^ P. Benetti et al., Measurement of the specific activity of 39Ar in natural argon. Nucl. Instr. Meth. A 574 (2007) 83 [1].
  3. ^ V. D. Ashitkov et al., New experimental limit on the 42Ar content in the Earth’s atmosphere. Nucl. Instr. Meth. A 416 (1998) 179 [2].

[edit] External links


Isotopes of chlorine Isotopes of argon Isotopes of potassium
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