Oxygen-18
Properties and data of the isotope 18O.
Oxygen-18 is a stable isotope of the chemical element oxygen, which has 10 neutrons in its atomic nucleus in addition to the element-specific 8 protons; the sum of the number of these atomic nucleus building blocks results in a mass number of 18. According to a report from 1929, 18O was identified as a distinct oxygen isotope based on the absorption bands of atmospheric oxygen [1].
See also: List of individual Oxygen isotopes (and general data sources).
General data
Name of the isotope:Oxygen-18; O-18Symbol:18O or 188OMass number A:18 (= number of nucleons)Atomic number Z:8 (= number of protons)Neutrons N:10Nucleon pairing (Z - N):even - evenNuclear ratio (N/Z ratio):1.25 (= neutron-proton ratio)Neutron excess (N-Z):2Isotopic mass:17.999159613(5) u (atomic weight of Oxygen-18)Nuclide mass:17.994771 u (calculated nuclear mass without electrons)Mass excess:-0.78282 MeVMass defect:0.150089803 u (per nucleus)Nuclear binding energy:139.80775096 MeV (per nucleus)
7.76709728 MeV (average binding energy per nucleon)Separation energy:SN = 8.0453702(10) MeV (first neutron)
SP = 15.942(15) MeV (first proton)Half-life:stableSpin and parity:
(nuclear angular momentum)0+Isobaric spin: 1Charge radius:2.7726(56) femtometer fmMirror nucleus:Neon-18Year of discovery:1929
Parent Nuclides
Direct parent isotopes are: 18N, 18F.
Occurrence
Comparison of the natural Oxygen isotopes including isotopic abundance (mole fraction of the isotope mixture in percent):
| | Atomic Mass ma | Quantity | Half-life | Spin |
|---|
Oxygen Isotopic mixture | 15.999 u | 100 % | | |
| Isotope 16O | 15.994914619(1) u | 99.757 % [99.738 - 99.776 %] | stable | 0+ |
| Isotope 17O | 16.999131757(5) u | 0.03835(96) % [0.0367 - 0.0400 %] | stable | 5/2+ |
| Isotope 18O | 17.999159613(5) u | 0.2045 % [0.187 - 0.222 %] | stable | 0+ |
Isotones and Isobars
The following table shows the atomic nuclei that are isotonic (same neutron number N = 10) and isobaric (same nucleon number A = 18) with Oxygen-18. Naturally occurring isotopes are marked in green; light green = naturally occurring radionuclides.
| Z | Isotone N = 10 | Isobar A = 18 |
| 3 | 13Li | |
| 4 | 14Be | |
| 5 | 15B | 18B |
| 6 | 16C | 18C |
| 7 | 17N | 18N |
| 8 | 18O | 18O |
| 9 | 19F | 18F |
| 10 | 20Ne | 18Ne |
| 11 | 21Na | 18Na |
| 12 | 22Mg | 18Mg |
| 13 | 23Al | |
| 14 | 24Si | |
| 15 | 25P | |
| 16 | 26S | |
External data and identifiers
Literature and References
[1] - W. F. Giauque, H. L. Johnston:
An isotope of oxygen, mass 18. Interpretation of the atmospheric absorption bands.
In: Journal of the American Chemical Society, 51, 5, (1929), DOI 10.1021/ja01380a018.
Last update: 2024-10-09
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