Beta-decay stable isobars

 Beta-decay stable isobars are the set of nuclides which cannot undergo beta decay, that is, the transformation of a neutron to a proton or a proton to a neutron within the nucleus. A subset of these nuclides are also stable with regards to double beta decay or theoretically higher simultaneous beta decay, as they have the lowest energy of all nuclides with the same mass number.

Table isotopes en.svg

This set of nuclides is also known as the line of beta stability, a term already in common use in 1965.[1][2] This line lies along the bottom of the nuclear valley of stability.

IntroductionEdit

The line of beta stability can be defined mathematically by finding the nuclide with the greatest binding energy for a given mass number, by a model such as the classical semi-empirical mass formula developed by C. F. Weizsäcker. These nuclides are local maxima in terms of binding energy for a given mass number.

β decay stable / even A
βDSOneTwoThree
2-3417
36-5857
60-7252
74-1162191
118-1542116
156-192514
194-21063
212-262719
Total49757

All odd mass numbers have only one beta decay stable nuclide.

Among even mass number, seven (96, 124, 130, 136, 148, 150, 154) have three beta-stable nuclides. None have more than three, all others have either one or two.

  • From 2 to 34, all have only one.
  • From 36 to 72, only nine (36, 40, 46, 48, 50, 54, 58, 64, 70) have two, and the remaining 11 have one.
  • From 74 to 122, only three (88, 90, 118) have one, and the remaining 22 have two.
  • From 124 to 154, only one (140) has one, six have three, and the remaining 9 have two.
  • From 156 to 262, only eighteen have one, and the remaining 36 have two, though there may also exist some undiscovered ones.

All primordial nuclides are beta decay stable, with the exception of 40K, 50V, 87Rb, 113Cd, 115In, 138La, 176Lu, and 187Re. In addition, 123Te and 180mTa have not been observed to decay, but are believed to undergo beta decay with an extremely long half-life (over 1015 years). All elements up to and including nobelium, except technetium and promethium, are known to have at least one beta-stable isotope.

List of known beta-decay stable isobarsEdit

350 beta-decay stable nuclides are currently known.[3][4] Theoretically predicted or experimentally observed double beta-decay is shown by arrows, i.e. arrows point towards the lightest-mass isobar. (This is sometimes dominated by alpha decay or spontaneous fission, especially for the heavy elements.)

No beta-decay stable nuclide has proton number 43 or 61 and no beta-decay stable nuclide has neutron number 19, 21, 35, 39, 45, 61, 71, 89, 115, 123, or 147.

Even NOdd N
Even ZEven AOdd A
Odd ZOdd AEven A
All known beta-decay stable isobars sorted by mass number
Odd AEven AOdd AEven AOdd AEven AOdd AEven A
1H2H3He4He5He (n)6Li7Li8Be (α)
9Be10B11B12C13C14N15N16O
17O18O19F20Ne21Ne22Ne23Na24Mg
25Mg26Mg27Al28Si29Si30Si31P32S
33S34S35Cl36S ← 36Ar37Cl38Ar39K40Ar ← 40Ca
41K42Ca43Ca44Ca45Sc46Ca → 46Ti47Ti48Ca[a] → 48Ti
49Ti50Ti ← 50Cr51V52Cr53Cr54Cr ← 54Fe55Mn56Fe
57Fe58Fe ← 58Ni59Co60Ni61Ni62Ni63Cu64Ni ← 64Zn
65Cu66Zn67Zn68Zn69Ga70Zn → 70Ge71Ga72Ge
73Ge74Ge ← 74Se75As76Ge → 76Se77Se78Se ← 78Kr79Br80Se → 80Kr
81Br82Se → 82Kr83Kr84Kr ← 84Sr85Rb86Kr → 86Sr87Sr88Sr
89Y90Zr91Zr92Zr ← 92Mo93Nb94Zr → 94Mo95Mo96Zr[b] → 96Mo ← 96Ru
97Mo98Mo → 98Ru99Ru100Mo → 100Ru101Ru102Ru ← 102Pd103Rh104Ru → 104Pd
105Pd106Pd ← 106Cd107Ag108Pd ← 108Cd109Ag110Pd → 110Cd111Cd112Cd ← 112Sn
113In114Cd → 114Sn115Sn116Cd → 116Sn117Sn118Sn119Sn120Sn ← 120Te
121Sb122Sn → 122Te123Sb124Sn → 124Te ← 124Xe125Te126Te ← 126Xe127I128Te → 128Xe
129Xe130Te → 130Xe ← 130Ba131Xe132Xe ← 132Ba133Cs134Xe → 134Ba135Ba136Xe → 136Ba ← 136Ce
137Ba138Ba ← 138Ce139La140Ce141Pr142Ce → 142Nd143Nd144Nd (α) ← 144Sm
145Nd146Nd → 146Sm (α)147Sm (α)148Nd → 148Sm (α) ← 148Gd (α)149Sm150Nd → 150Sm ← 150Gd (α)151Eu (α)152Sm ← 152Gd
153Eu154Sm → 154Gd ← 154Dy (α)155Gd156Gd ← 156Dy157Gd158Gd ← 158Dy159Tb160Gd → 160Dy
161Dy162Dy ← 162Er163Dy164Dy ← 164Er165Ho166Er167Er168Er ← 168Yb
169Tm170Er → 170Yb171Yb172Yb173Yb174Yb ← 174Hf (α)175Lu176Yb → 176Hf
177Hf178Hf179Hf180Hf ← 180W (α)181Ta182W183W184W ← 184Os
185Re186W → 186Os (α)187Os188Os189Os190Os ← 190Pt (α)191Ir192Os → 192Pt
193Ir194Pt195Pt196Pt ← 196Hg197Au198Pt → 198Hg199Hg200Hg
201Hg202Hg203Tl204Hg → 204Pb205Tl206Pb207Pb208Pb
209Bi (α)210Po (α)211Po (α)212Po (α) ← 212Rn (α)213Po (α)214Po (α) ← 214Rn (α)215At (α)216Po (α) → 216Rn (α)
217Rn (α)218Rn (α) ← 218Ra (α)219Fr (α)220Rn (α) → 220Ra (α)221Ra (α)222Ra[c] (α)223Ra (α)224Ra (α) ← 224Th (α)
225Ac (α)226Ra (α) → 226Th (α)227Th (α)228Th (α)229Th (α)230Th (α) ← 230U (α)231Pa (α)232Th (α) → 232U (α)
233U (α)234U (α)235U (α)236U (α) ← 236Pu (α)237Np (α)238U (α) → 238Pu (α)239Pu (α)240Pu (α)
241Am (α)242Pu (α) ← 242Cm (α)243Am (α)244Pu (α) → 244Cm (α)245Cm (α)246Cm (α)247Bk (α)248Cm (α) → 248Cf (α)
249Cf (α)250Cf (α)251Cf (α)252Cf (α) ← 252Fm (α)253Es (α)254Cf (SF) → 254Fm (α)255Fm (α)256Cf (SF) → 256Fm (SF)
257Fm (α)258Fm (SF) ← 258No (SF)259Md (SF)260Fm (SF) → 260No (SF)262No (SF)
One chart of known and predicted nuclides up to Z = 149, N = 256. Black denotes the predicted beta-stability line, which is in good agreement with experimental data. Islands of stability are predicted to center near 294Ds and 354126, beyond which the model appears to deviate from several rules of the semi-empirical mass formula.[8]

All beta-decay stable nuclides with A ≥ 209 were observed to decay by alpha decay except some where spontaneous fission dominates. With the exception of 262No, no nuclides with A ≥ 260 have been definitively identified as beta-stable, although 260Fm and 262No are unconfirmed.[4]

The general patterns of beta-stability are expected to continue into the region of superheavy elements, though the exact location of the center of the valley of stability is model dependent. It is widely believed that an island of stability exists along the beta stability line for isotopes of elements around copernicium that are stabilized by shell closures in the region; such isotopes would decay primarily through alpha decay or spontaneous fission.[9] Beyond the island of stability, various models that correctly predict the known beta-stable isotopes predict anomalies in the beta-stability line that are unobserved in any known nuclides, such as the existence of two beta-stable nuclides with the same odd mass number.[8][10] This is a consequence of the fact that a semi-empirical mass formula must consider shell correction and nuclear deformation, which become far more pronounced for heavy nuclides.[10][11]

Beta decay toward minimum massEdit

Beta decay generally causes isotopes to decay toward the isobar with the lowest mass (which is often, but not always, the one with highest binding energy) with the same mass number, those not in italics in the table above. Thus, those with lower atomic number and higher neutron number than the minimum-mass isobar undergo beta-minus decay, while those with higher atomic number and lower neutron number undergo beta-plus decay or electron capture. However, there are four nuclides that are exceptions, in that the majority of their decays are in the opposite direction:

Chlorine-3635.96830698Potassium-4039.96399848Silver-108107.905956Promethium-146145.914696
2% to Sulfur-3635.9670807611.2% to Argon-4039.96238312253% to Palladium-108107.90389237% to Samarium-146145.913041
98% to Argon-3635.96754510689% to Calcium-4039.9625909897% to Cadmium-108107.90418463% to Neodymium-146145.9131169

This article uses material from the Wikipedia article
 Metasyntactic variable, which is released under the 
Creative Commons
Attribution-ShareAlike 3.0 Unported License
.