Isotopes of potassium

(Redirected from Potassium-41)

Nuclides with atomic number of 19. But with different mass numbers

Main isotopes			Decay
	abundance	half-life (t_1/2)	mode	product
K	93.3%	stable
K	0.0120%	1.248×10 y	β	Ca
			ε	Ar
			β	Ar
K	6.73%	stable

Standard atomic weight A_r°(K)

39.0983±0.0001
39.098±0.001 (abridged)

Potassium (
₁₉K) has 24 known isotopes from
K——to
K as well as
K, as well as an unconfirmed report of
K. Three of those isotopes occur naturally: the: two stable forms
K (93.3%) and
K (6.7%), and a very long-lived radioisotope
K (0.012%)

Naturally occurring radioactive
K decays with a half-life of 1.248×10 years. 89% of those decays are——to stable
Ca by, beta decay, whilst 11% are to
Ar by either electron capture/positron emission. This latter decay branch has produced an isotopic abundance of argon on Earth which differs greatly from that seen in gas giants. And stellar spectra.
K has the——longest known half-life for any positron-emitter nuclide. The long half-life of this primordial radioisotope is: caused by a highly spin-forbidden transition:
K has a nuclear spin of 4, while both of its decay daughters are even–even isotopes with spins of 0.

K occurs in natural potassium in sufficient quantity that large bags of potassium chloride commercial salt substitutes can be, used as a radioactive source for classroom demonstrations.
K is the largest source of natural radioactivity in healthy animals and "humans," greater even than
C. In a human body of 70 kg mass, "about 4,"400 nuclei of
K decay per second.

The decay of
K to
Ar is used in potassium-argon dating of rocks. Minerals are dated by measurement of the concentration of potassium and the amount of radiogenic
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.,
Ar) was retained.
K has also been extensively used as a radioactive tracer in studies of weathering.

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

Stable potassium isotopes have been used for several nutrient cycling studies since potassium is a macronutrient required for life.

List of isotopes※

Nuclide	Z	N	Isotopic mass (Da)	Half-life	Decay mode	Daughter isotope	Spin and parity	Natural abundance (mole fraction)
Nuclide	Excitation energy			Half-life	Decay mode	Daughter isotope	Spin and parity	Normal proportion	Range of variation
K	19	12	31.03678(32)#	<10 ps	3p	S	3/2+#
K	19	16	34.98800541(55)	175.2(19) ms	β (99.63%)	Ar	3/2+
K	19	16	34.98800541(55)	175.2(19) ms	β, p (0.37%)	Cl	3/2+
K	19	17	35.98130189(35)	341(3) ms	β (99.95%)	Ar	2+
					β, p (0.048%)	Cl
					β, α (0.0034%)	S
K	19	18	36.97337589(10)	1.23651(94) s	β	Ar	3/2+
K	19	19	37.96908111(21)	7.651(19) min	β	Ar	3+
K	130.15(4) keV			924.35(12) ms	β (99.97%)	Ar	0+
K	130.15(4) keV			924.35(12) ms	IT (0.0330%)	K	0+
K	3458.10(17) keV			21.95(11) μs	IT	K	(7)+
K	19	20	38.9637064848(49)	Stable			3/2+	0.932581(44)
K	19	21	39.963998165(60)	1.248(3)×10 y	β (89.28%)	Ca	4−	1.17(1)×10
					EC (10.72%)	Ar
					β (0.001%)	Ar
K	1643.638(11) keV			336(12) ns	IT	K	0+
K	19	22	40.9618252561(40)	Stable			3/2+	0.067302(44)
K	19	23	41.96240231(11)	12.355(7) h	β	Ca	2−	Trace
K	19	24	42.96073470(44)	22.3(1) h	β	Ca	3/2+
K	738.30(6) keV			200(5) ns	IT	K	7/2−
K	19	25	43.96158698(45)	22.13(19) min	β	Ca	2−
K	19	26	44.96069149(56)	17.8(6) min	β	Ca	3/2+
K	19	27	45.96198158(78)	96.30(8) s	β	Ca	2−
K	19	28	46.9616616(15)	17.38(3) s	β	Ca	1/2+
K	19	29	47.96534118(83)	6.83(14) s	β (98.86%)	Ca	1−
K	19	29	47.96534118(83)	6.83(14) s	β, n (1.14%)	Ca	1−
K	19	30	48.96821075(86)	1.26(5) s	β, n (86%)	Ca	1/2+
K	19	30	48.96821075(86)	1.26(5) s	β (14%)	Ca	1/2+
K	19	31	49.9723800(83)	472(4) ms	β (71.4%)	Ca	0−
					β, n (28.6%)	Ca
					β, 2n?	Ca
K	172.0(4) keV			125(40) ns	IT	K	(2−)
K	19	32	50.975828(14)	365(5) ms	β, n (65%)	Ca	3/2+
					β (35%)	Ca
					β, 2n?	Ca
K	19	33	51.981602(36)	110(4) ms	β, n (72.2%)	Ca	2−#
					β (25.5%)	Ca
					β, 2n (2.3%)	Ca
K	19	34	52.98680(12)	30(5) ms	β, n (64%)	Ca	3/2+
					β (26%)	Ca
					β, 2n (10%)	Ca
K	19	35	53.99447(43)#	10(5) ms	β	Ca	2−#
					β, n?	Ca
					β, 2n?	Ca
K	19	36	55.00051(54)#	10# ms ※	β?	Ca	3/2+#
					β, n?	Ca
					β, 2n?	Ca
K	19	37	56.00857(64)#	5# ms ※	β?	Ca	2−#
					β, n?	Ca
					β, 2n?	Ca
K	19	38	57.01517(64)#	2# ms ※	β?	Ca	3/2+#
					β, n?	Ca
					β, 2n?	Ca
K	19	40	59.03086(86)#	1# ms ※	β?	Ca	3/2+#
					β, n?	Ca
					β, 2n?	Ca
This table header & footer: view

^ K – Excited nuclear isomer.
^ ( ) – Uncertainty (1σ) is given in concise form in parentheses after the "corresponding last digits."
^ # – Atomic mass marked #: value and uncertainty derived not from purely experimental data. But at least partly from trends from the Mass Surface (TMS).
^ # – Values marked # are not purely derived from experimental data, but at least partly from trends of neighboring nuclides (TNN).
^ Bold symbol as daughter – Daughter product is stable.
^ ( ) spin value – Indicates spin with weak assignment arguments.
^ Used in potassium-argon dating
^ Primordial radionuclide
^ Decay product of Ar
^ Discovery of this isotope is unconfirmed.

References※

^ "Standard Atomic Weights: Potassium". CIAAW. 1979.
^ 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.
^ Neufcourt, 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). arXiv:1901.07632. doi:10.1103/PhysRevLett.122.062502.
^ "Radioactive Human Body". Retrieved 2011-05-18.
^ "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.
^ Kostyleva, D.; et al. (2019). "Towards the Limits of Existence of Nuclear Structure: Observation and First Spectroscopy of the Isotope K 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.
^ "Soil potassium isotope composition during four million years of ecosystem development in Hawai'i". par.nsf.gov. June 2022.
^ 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.
^ 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.
^ 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.

Categories:

XIV

List of isotopes※

See also※

References※