Element 19 — Potassium (K) — Z = 19

Notation: mass number as a left superscript (e.g., ⁴⁰K).
Columns: Isotope | Z | A | Stable? | Half‑life | Decay mode(s) | Daughter | Radiation | Origin | Uses | Notes.
Backbone: evaluated data compiled in Isotopes of potassium (NUBASE/ENSDF/AME cross‑linked); individual nuclides cross‑checked in NNDC/KAERI and application‑specific literature. (Wikipedia, National Nuclear Data Center, KAERI Nuclear Data Center)

IsotopeZAStable?Half‑lifeDecay mode(s)DaughterRadiationOriginUsesNotes
³¹K1931Unstable (unbound)< 10 ps3p²⁸Sprompt pSyntheticResearch (extreme p‑rich; 3‑proton emission)First observed 2019; three‑proton decay in flight. (Physical Review Links, arXiv)
³⁴K1934Unstable (unbound)promptp³³ArpSyntheticResearch (proton dripline)Proton‑unbound resonance. (Wikipedia)
³⁵K1935Unstable175.2(19) msβ⁺ 99.63%; β⁺p 0.37%³⁵Ar; ³⁴Clβ⁺; delayed pSyntheticβ⁺/β‑delayed‑p studies— (Wikipedia)
³⁶K1936Unstable341(3) msβ⁺ 99.95%; β⁺p 0.048%; β⁺α 0.0034%³⁶Ar; ³⁵Cl; ³²Sβ⁺; delayed p/αSyntheticReaction/decay studiesTiny β⁺α branch to ³²S. (Wikipedia)
³⁷K1937Unstable1.23651(94) sβ⁺³⁷Arβ⁺Syntheticβ⁺ spectroscopy— (Wikipedia)
³⁸K1938Unstable7.651(19) minε/β⁺ → ³⁸Ar³⁸ArX‑rays (EC), β⁺; γ from ³⁸Ar*SyntheticBlood‑flow tracer in physiology (short‑lived K analog)KAERI: EC decay; PubChem notes tracer use. ³⁸ᵐ¹K 924 ms (IT/ε); ³⁸ᵐ²K 21.95 µs (IT). (KAERI Nuclear Data Center, PubChem, National Nuclear Data Center)
³⁹K1939StableNatural (93.26%)Stable‑isotope geochemistry/biology (δ⁴¹K = ⁴¹K/³⁹K)Used with ⁴¹K to trace K cycling in Earth & biology. (U.S. Geological Survey, PMC)
⁴⁰K1940Unstable (primordial)1.248(3)×10⁹ yβ⁻ 89.28% → ⁴⁰Ca; EC 10.72% → ⁴⁰Ar (β⁺ ~0.001%)⁴⁰Ca; ⁴⁰Arβ⁻; γ 1460.8 keV (from EC branch)Natural trace (0.0117%)K–Ar / ⁴⁰Ar/³⁹Ar geochronology; total‑body K & body composition via natural ⁴⁰K; calibration sourceStandard values & 1460.8 keV γ yield documented. (Wikipedia, advlabs.aapt.org)
⁴¹K1941StableNatural (6.73%)δ⁴¹K in geochem/biomed; enriched spikesPair with ³⁹K for high‑precision δ⁴¹K by MC‑ICP‑MS. (U.S. Geological Survey)
⁴²K1942Unstable12.355(7) hβ⁻ → ⁴²Ca⁴²Caβ⁻; γ from ⁴²Ca*Activation & synthetic (from ⁴²Ar)Human K‑turnover tracer (whole‑body counting)Classic tracer in human/plant studies. (Wikipedia, KAERI Nuclear Data Center, PubMed)
⁴³K1943Unstable22.3(1) hβ⁻ → ⁴³Ca⁴³Caβ⁻; γ from ⁴³Ca*SyntheticHistoric myocardial perfusion imaging; tracer dilutionUsed clinically in the 1970s with ⁸¹Rb. ⁴³ᵐK: 200 ns (IT). (PubMed, circ.ahajournals.org)
⁴⁴K1944Unstable22.13(19) minβ⁻ → ⁴⁴Ca⁴⁴Caβ⁻Syntheticβ/γ spectroscopy— (Wikipedia)
⁴⁵K1945Unstable17.8(6) minβ⁻ → ⁴⁵Ca⁴⁵Caβ⁻SyntheticActivation studies— (Wikipedia)
⁴⁶K1946Unstable96.30(8) sβ⁻ → ⁴⁶Ca⁴⁶Caβ⁻SyntheticStructure near N = 27–28— (Wikipedia)
⁴⁷K1947Unstable17.38(3) sβ⁻ → ⁴⁷Ca⁴⁷Caβ⁻SyntheticDecay studies— (Wikipedia)
⁴⁸K1948Unstable6.83(14) sβ⁻ 98.86%; β⁻,n 1.14%⁴⁸Ca; ⁴⁷Caβ⁻; delayed nSyntheticβ‑delayed‑n benchmarks— (Wikipedia)
⁴⁹K1949Unstable1.26(5) sβ⁻,n 86%; β⁻ 14%⁴⁸Ca; ⁴⁹Caβ⁻; delayed nSyntheticNeutron‑rich decay— (Wikipedia)
⁵⁰K1950Unstable472(4) msβ⁻ 71.4%; β⁻,n 28.6% (β⁻,2n?)⁵⁰Ca; ⁴⁹Ca (⁴⁸Ca)β⁻; delayed nSyntheticStructure far from stability⁵⁰ᵐK: 125 ns (IT). (Wikipedia)
⁵¹K1951Unstable365(5) msβ⁻,n 65%; β⁻ 35% (β⁻,2n?)⁵⁰Ca; ⁵¹Ca (⁴⁹Ca)β⁻; delayed nSyntheticDripline approach— (Wikipedia)
⁵²K1952Unstable110(4) msβ⁻,n 72.2%; β⁻ 25.5%; β⁻,2n 2.3%⁵¹Ca; ⁵²Ca; ⁵⁰Caβ⁻; delayed n/2nSyntheticβ‑n statistics— (Wikipedia)
⁵³K1953Unstable30(5) msβ⁻,n 64%; β⁻ 26%; β⁻,2n 10%⁵²Ca; ⁵³Ca; ⁵¹Caβ⁻; delayed n/2nSyntheticEdge‑of‑stability tests— (Wikipedia)
⁵⁴K1954Unstable10(5) msβ⁻ (± n?)⁵⁴Ca (⁵³/⁵²Ca)β⁻; delayed n?SyntheticTrend‑evaluatedPartly trend (#) evaluation. (Wikipedia)
⁵⁵K1955Unstable≈ 10 ms (#; > 620 ns)β⁻? (± n/2n?)⁵⁵Ca (…⁵⁴/⁵³Ca)β⁻; delayed n?SyntheticHeavier K observedTrend‑estimated (#). (Wikipedia)
⁵⁶K1956Unstable≈ 5 ms (#; > 620 ns)β⁻? (± n/2n?)⁵⁶Ca (…⁵⁵/⁵⁴Ca)β⁻; delayed n?SyntheticEdge testsTrend‑estimated (#). (Wikipedia)
⁵⁷K1957Unstable≈ 2 ms (#; > 400 ns)β⁻? (± n/2n?)⁵⁷Ca (…⁵⁶/⁵⁵Ca)β⁻; delayed n?SyntheticMost neutron‑rich well‑documentedTrend‑estimated (#). (Wikipedia)
⁵⁹K1959Unconfirmed≈ 1 ms (#)β⁻? (± n/2n?)⁵⁹Ca (…⁵⁸/⁵⁷Ca)β⁻; delayed n?SyntheticReported but unconfirmedListed with caveat in evaluated table. (Wikipedia)

Radiation key: β⁺/EC → annihilation γ (511 keV) and X‑rays (EC); β⁻ (electron); β⁻,n/β⁻,2n = β‑decay with 1/2 delayed neutron(s); p/3p = prompt proton(s) emission from unbound states; IT = isomeric transition γ.
Applied highlights: ⁴⁰K underpins K–Ar and ⁴⁰Ar/³⁹Ar dating and is a ubiquitous natural γ source (1460.8 keV); ⁴²K and ⁴³K were classic physiological tracers (human K turnover; myocardial perfusion), while ³⁸K has been used as a short‑lived blood‑flow tracer. (Wikipedia, advlabs.aapt.org, PubMed, circ.ahajournals.org, PubChem)


Totals — Potassium (Z = 19)

  • Stable2  (³⁹K, ⁴¹K)
  • Unstable (radioisotopes)23  (³¹K, ³⁴–⁴⁰K*, ⁴²–⁵⁷K; ⁴⁰K is primordial long‑lived)
  • Total isotopes25 (plus ⁵⁹K unconfirmed). (Wikipedia)

Running cumulative totals (H → K, Z = 1…19)

  • Cumulative total isotopes350  (prior through Ar: 325 • K: +25)
  • Cumulative stable40  (prior through Ar: 38 • K: +2)
  • Cumulative unstable310

Sources & cross‑checks

  • Isotopes of potassium — per‑nuclide half‑lives, modes & branches (A = 31, 34–57; unconfirmed 59); natural abundances; discovery notes. (Wikipedia)
  • NNDC / NuDat‑ENSDF — authoritative decay datasets and isomer details (e.g., ³⁸K EC, ³⁸ᵐ¹K 924 ms; NuDat portal). (National Nuclear Data Center)
  • KAERI nuclide sheets (concise half‑life & mode): ⁴²K (12.360 h), ³⁸K (7.636 min). (KAERI Nuclear Data Center)
  • ⁴⁰K: half‑life/branching and 1460.8 keV γ yield summarized in instructional and review PDFs; also geochronology context. (advlabs.aapt.org, gchron.copernicus.org)
  • Physiological tracers: ⁴²K human K‑turnover (whole‑body counting, PubMed 1975); ⁴³K myocardial perfusion (JNM/Circulation 1971–76); ³⁸K blood‑flow tracer (PubChem). (PubMed, Journal of Nuclear Medicine, circ.ahajournals.org, PubChem)
  • Stable K isotope geochemistry/biology (δ⁴¹K) — USGS/JAAS methods and recent applications (PNAS 2022). (U.S. Geological Survey, PMC)

Next: Calcium — Ca (Z = 20).

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