Potassium-36
Properties and data of the isotope 36K.
Potassium-36 is a radioisotope of the chemical element potassium, which has 17 neutrons in its atomic nucleus in addition to the element-specific 19 protons; the sum of the number of these atomic nucleus building blocks results in a mass number of 36.
The discovery of the radioactive isotope upon irradiation of enriched argon-36 gas with protons of an energy of 23 MeV and the charge exchange reaction initiated by this was reported in 1967 [1]:
36Ar(p,n)36K.
See also: List of individual Potassium isotopes (and general data sources).
General data
Name of the isotope:Potassium-36; K-36Symbol:36K or 3619KMass number A:36 (= number of nucleons)Atomic number Z:19 (= number of protons)Neutrons N:17Nucleon pairing (Z - N):odd - oddNuclear ratio (N/Z ratio):0.89473684210526 (= neutron-proton ratio)Neutron excess (N-Z):-2Isotopic mass:35.9813019(3) u (atomic weight of Potassium-36)Nuclide mass:35.9708791 u (calculated nuclear mass without electrons)Mass excess:-17.41717 MeVMass defect:0.31467728000001 u (per nucleus)Nuclear binding energy:293.11999826 MeV (per nucleus)
8.14222217 MeV (average binding energy per nucleon)Separation energy:SN = 14.3156(6) MeV (first neutron)
SP = 1.6589(8) MeV (first proton)Half-life:341(3) msDecay constant λ:2.0326896790614 s-1Specific activity α:3.497469591956 × 10+22 Bq g-1
945262051880.11 Ci g-1Spin and parity:
(nuclear angular momentum)2+Magnetic dipole moment:μ(μN) = (+) 0.548(1)Mirror nucleus:Chlorine-36Year of discovery:1967
Radioactive Decay
Half-life T½ = 341(3) ms respectively 3.41 × 10-1 seconds s.
Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|
| EC/β+ | 36Ar | 99.95 % | 12.8144(3) MeV | |
| EC, p | 35Cl | 0.048(14) % | 4.298 MeV | |
| EC, α | 32S | 0.0034(13) % | 6,165 MeV | |
Parent Nuclides
Direct parent isotope is: 36Ca.
Isotones and Isobars
The following table shows the atomic nuclei that are isotonic (same neutron number N = 17) and isobaric (same nucleon number A = 36) with Potassium-36. Naturally occurring isotopes are marked in green; light green = naturally occurring radionuclides.
| Z | Isotone N = 17 | Isobar A = 36 |
| 7 | 24N | |
| 8 | 25O | |
| 9 | 26F | |
| 10 | 27Ne | |
| 11 | 28Na | 36Na |
| 12 | 29Mg | 36Mg |
| 13 | 30Al | 36Al |
| 14 | 31Si | 36Si |
| 15 | 32P | 36P |
| 16 | 33S | 36S |
| 17 | 34Cl | 36Cl |
| 18 | 35Ar | 36Ar |
| 19 | 36K | 36K |
| 20 | 37Ca | 36Ca |
| 21 | 38Sc | 36Sc |
| 22 | 39Ti | |
| 23 | 40V | |
| 24 | 41Cr | |
| 25 | 42Mn | |
External data and identifiers
Literature and References
[1] - R. E. Berg, J. L. Snelgrove, E. Kashy:
36K Decay and T = 1 Analog in 36Ar.
In: Physical Review, 153, 1165, (1967), DOI 10.1103/PhysRev.153.1165.
Last update: 2026-01-07
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