Silicon-27
Properties and data of the isotope 27Si.
Silicon-27 is a radioisotope of the chemical element silicon, which has 13 neutrons in its atomic nucleus in addition to the element-specific 14 protons; the sum of the number of these atomic nucleus building blocks results in a mass number of 27. The very short-lived, only artificially produced, unstable and thus radioactive nuclide has no practical significance; the study of 27Si is exclusively for academic purposes.
Silicon-27 was discovered - according to a report from 1939 - by irradiating aluminium-27 (natural Al) with protons (charge exchange reaction):
27Al(p,n)27Si.
See also: List of individual Silicon isotopes (and general data sources).
General data
Name of the isotope:Silicon-27; Si-27Symbol:27Si or 2714SiMass number A:27 (= number of nucleons)Atomic number Z:14 (= number of protons)Neutrons N:13Nucleon pairing (Z - N):even - oddNuclear ratio (N/Z ratio):0.92857142857143 (= neutron-proton ratio)Neutron excess (N-Z):-1Isotopic mass:26.98670469(12) u (atomic weight of Silicon-27)Nuclide mass:26.9790247 u (calculated nuclear mass without electrons)Mass excess:-12.3845 MeVMass defect:0.235489666 u (per nucleus)Nuclear binding energy:219.35721094 MeV (per nucleus)
8.12434115 MeV (average binding energy per nucleon)Separation energy:SN = 13.31482(15) MeV (first neutron)
SP = 7.46334(13) MeV (first proton)Half-life:4.117(14) sDecay constant λ:0.16836220076754 s-1Specific activity α:3.899618801965 × 10+21 Bq g-1
105395102755.83 Ci g-1Spin and parity:
(nuclear angular momentum)5/2+Magnetic dipole moment:μ(μN) = 0.8652(3)Quadrupole moment Q:+ 0.063(14) barn (100 fm2)Nuclear g-factor:gl = 0.34608Mirror nucleus:Aluminium-27Year of discovery:1939
Radioactive Decay
Half-life T½ = 4.117(14) s.
Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|
| EC/β+ | 27Al | 100 % | 4.81236(12) MeV | |
Parent Nuclides
Direct parent isotopes are: 27P, 28S.
Isotones and Isobars
The following table shows the atomic nuclei that are isotonic (same neutron number N = 13) and isobaric (same nucleon number A = 27) with Silicon-27. Naturally occurring isotopes are marked in green; light green = naturally occurring radionuclides.
| Z | Isotone N = 13 | Isobar A = 27 |
| 5 | 18B | |
| 6 | 19C | |
| 7 | 20N | |
| 8 | 21O | 27O |
| 9 | 22F | 27F |
| 10 | 23Ne | 27Ne |
| 11 | 24Na | 27Na |
| 12 | 25Mg | 27Mg |
| 13 | 26Al | 27Al |
| 14 | 27Si | 27Si |
| 15 | 28P | 27P |
| 16 | 29S | 27S |
| 17 | 30Cl | |
| 18 | 31Ar | |
| 19 | 32K | |
External data and identifiers
Literature and References
[1] - G. Kuerti, S. N. van Voorhis:
Induced Radioactivity Produced by Bombarding Aluminum with Protons.
In: Physical Review, 56, 614, (1939), DOI 10.1103/PhysRev.56.614.
Last update: 2025-12-24
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