Nobelium (No)
actinideSolid
Standard Atomic Weight
[259]Electron configuration
[Rn] 7s2 5f14Melting point
826.85 °C (1100 K)Boiling point
N/ADensity
9900 kg/m³Oxidation states
+2, +3Electronegativity (Pauling)
1.3Ionization energy (1st)
Discovery year
1957Atomic radius
N/ADetails
Nobelium is a synthetic actinide with atomic number 102. It is produced only in particle-accelerator experiments and is studied in atom-at-a-time quantities. Its longest-lived confirmed isotopes have half-lives of only minutes, so no macroscopic sample or ordinary material application exists. Chemically, nobelium is notable because the +2 oxidation state is unusually stable for an actinide, in contrast to the more common +3 state of many neighboring elements.
Nobelium does not occur naturally in the Earth’s crust. It was first synthesized in 1966 by Russian scientists from the Joint Institute for Nuclear Research (JINR) in Dubna, Russia under Georgi Flerov. Earlier claims to have synthesized “nobelium” beginning in 1957 were shown to be erroneous. This element was originally named for Alfred Nobel (Fig. IUPAC.102.1), the inventor of dynamite and founder of the Nobel prizes. The name was later retained because of its widespread use throughout the scientific literature [636], [638]. There are no uses for isotopes of nobelium outside of scientific research.
Nobelium is named after Alfred Nobel.
In 1957, a group of scientists working at the Nobel Institute of Physics in Stockhlom, Sweden, announced the discovery of a new element. They produced this new element, which they named nobelium, by bombarding a target of curium-244 with ions of carbon-13 with a device called a cyclotron. The isotope they created had a half-life of 10 minutes. In 1958, another group of scientists, Albert Ghiorso, Glenn T. Seaborg, Torbørn Sikkeland and John R. Walton, working at the Lawrence Radiation Laboratory in Berkeley, California, attempted to confirm the Nobel Institute's discovery. They were unable to produce any isotope of nobelium with a half-life of 10 minutes, but were able to produce nobelium-254, with a half-life of three seconds, by bombarding curium-246 with carbon-12. A third group, working at the Joint Institute for Nuclear Research in Dubna, Russia, also could not duplicate the Nobel Institute's work but were able to confirm the Berkeley group's work. Credit for discovering nobelium was eventually given to the scientists working at Lawrence Radiation Laboratory, who decided to keep the name nobelium. Today, the Lawrence Radiation Laboratory is known as the Lawrence Berkeley Laboratory. Nobelium's most stable isotope, nobelium-259, has a half-life of about 58 minutes. It decays into fermium-255 through alpha decay, into mendelevium-259 through electron capture or through spontaneous fission.
Named after Alfred Nobel, inventor of dynamite. Nobelium was unambiguously discovered and identified in April 1958 at Berkeley by A. Ghiorso, T. Sikkeland, J.R. Walton, and G.T. Seaborg, who used a new double-recoil technique. A heavy-ion linear accelerator (HILAC) was used to bombard a thin target of curium (95%244Cm and 4.5% 246Cm) with 12C ions to produce 102No according to the 246Cm(12C, 4n) reaction.
In 1957 workers in the United States, Britain, and Sweden announced the discovery of an isotope of element 102 with a 10-minute half-life at 8.5 MeV, as a result of bombarding 244Cm with 13C nuclei. On the basis of this experiment, the name nobelium was assigned and accepted by the Commission on Atomic Weights of the International Union of Pure and Applied Chemistry.
The acceptance of the name was premature because both Russian and American efforts now completely rule out the possibility of any isotope of Element 102 having a half-life of 10 min in the vicinity of 8.5 MeV. Early work in 1957 on the search for this element, in Russia at the Kurchatov Institute, was marred by the assignment of 8.9 +/- 0.4 MeV alpha radiation with a half-life of 2 to 40 sec, which was too indefinite to support discovery claims.
Confirmatory experiments at Berkeley in 1966 have shown the existence of 254102 with a 55-s half-life, 252102 with a 2.3-s half-life, and 257102 with a 23-s half-life.
Following tradition giving the right to name an element to the discoverer(s), the Berkeley group in 1967, suggested that the hastily given name nobelium along with the symbol No , be retained.
Images
Properties
Physical
Chemical
Thermodynamic
Nuclear
Abundance
N/A
Reactivity
N/A
Crystal Structure
N/A
Electronic Structure
Identifiers
Electron Configuration Measured
No: 5f¹⁴ 7s²[Rn] 5f¹⁴ 7s²1s² 2s² 2p⁶ 3s² 3p⁶ 3d¹⁰ 4s² 4p⁶ 4d¹⁰ 5s² 5p⁶ 4f¹⁴ 5d¹⁰ 6s² 6p⁶ 5f¹⁴ 7s²Atomic model
Isotopes change neutron count, mass, and stability — not the electron configuration of a neutral atom.
Schematic atomic model, not to scale.
Atomic Fingerprint
Emission / Absorption Spectrum
Isotope Distribution
No stable isotopes.
| Mass number | Atomic mass (u) | Natural abundance | Half-life |
|---|---|---|---|
| 251 Radioactive | 251.08894 ± 0.00012 | N/A | 800 ms |
| 260 Radioactive | 260.10264 ± 0.00022 | N/A | 106 ms |
| 259 Radioactive | 259.10103 ± 0.00011 | N/A | 58 minutes |
| 249 Radioactive | 249.0878 ± 0.0003 | N/A | 57 us |
| 254 Radioactive | 254.090956 ± 0.000011 | N/A | 51.2 seconds |
Phase / State
Reason: 801.9 °C below sublimation point (826.85 °C)
Schematic, not to scale
Phase transition points
Transition energies
Energy required to sublime 1 mol at sublimation point
Density
At standard conditions
At standard conditions
Atomic Spectra
Showing 10 of 102 Atomic Spectra. Sorted by ion charge (ascending).
Levels Holdings ?
| Ion | Charge | Levels |
|---|---|---|
| No I | 0 | 2 |
| No II | +1 | 2 |
| No III | +2 | 2 |
| No IV | +3 | 2 |
| No V | +4 | 2 |
| No VI | +5 | 2 |
| No VII | +6 | 2 |
| No VIII | +7 | 2 |
| No IX | +8 | 2 |
| No X | +9 | 2 |
Crystal structure data not available
Ionic Radii
| Charge | Coordination | Spin | Radius |
|---|---|---|---|
| +2 | 6 | N/A | 110.00000000000001 pm |
| +3 | 9 | N/A | 108.5 pm |
Compounds
Isotopes (5)
Ten isotopes are now recognized, one of which 255102 has a half-life of 3 minutes.
| Mass number | Atomic mass (u) | Natural abundance | Half-life | Decay mode | |
|---|---|---|---|---|---|
| 251 Radioactive | 251.08894 ± 0.00012 | N/A | 800 ms | α =83±1.6%β+ ?SF<0.3% | |
| 260 Radioactive | 260.10264 ± 0.00022 | N/A | 106 ms | SF =100% | |
| 259 Radioactive | 259.10103 ± 0.00011 | N/A | 58 minutes | α =75±0.4%ε =25±0.4%SF<10% | |
| 249 Radioactive | 249.0878 ± 0.0003 | N/A | 57 us | β+ ?α ? | |
| 254 Radioactive | 254.090956 ± 0.000011 | N/A | 51.2 seconds | α =90±0.1%β+ =10±0.1%SF =0.17±0.2% |
Extended Properties
Covalent Radii (Extended)
Van der Waals Radii
Numbering Scales
Electronegativity Scales
Polarizability & Dispersion
Phase Transitions & Allotropes
| Melting point | 1100.15 K |
Oxidation State Categories
Advanced Reference Data
Crystal Radii Detail (2)
| Charge | CN | Spin | rcrystal (pm) | Origin |
|---|---|---|---|---|
| 2 | VI | 124 | estimated, | |
| 3 | IX | — | 122.5 |
Isotope Decay Modes (39)
| Isotope | Mode | Intensity |
|---|---|---|
| 248 | SF | — |
| 249 | B+ | — |
| 249 | A | — |
| 250 | SF | 100% |
| 250 | A | — |
| 250 | B+ | — |
| 251 | A | 83% |
| 251 | B+ | — |
| 251 | SF | 0.3% |
| 252 | A | 67.6% |
Additional Data
Estimated Crustal Abundance
The estimated element abundance in the earth's crust.
Not Applicable
References (1)
- [5] Nobelium https://education.jlab.org/itselemental/ele102.html
Estimated Oceanic Abundance
The estimated element abundance in the earth's oceans.
Not Applicable
References (1)
- [5] Nobelium https://education.jlab.org/itselemental/ele102.html
References
(9)
Data deposited in or computed by PubChem
The half-life and atomic mass data was provided by the Atomic Mass Data Center at the International Atomic Energy Agency.
Element data are cited from the Atomic weights of the elements (an IUPAC Technical Report). The IUPAC periodic table of elements can be found at https://iupac.org/what-we-do/periodic-table-of-elements/. Additional information can be found within IUPAC publication doi:10.1515/pac-2015-0703 Copyright © 2020 International Union of Pure and Applied Chemistry.
The information are cited from Pure Appl. Chem. 2018; 90(12): 1833-2092, https://doi.org/10.1515/pac-2015-0703.
Thomas Jefferson National Accelerator Facility (Jefferson Lab) is one of 17 national laboratories funded by the U.S. Department of Energy. The lab's primary mission is to conduct basic research of the atom's nucleus using the lab's unique particle accelerator, known as the Continuous Electron Beam Accelerator Facility (CEBAF). For more information visit https://www.jlab.org/
The periodic table at the LANL (Los Alamos National Laboratory) contains basic element information together with the history, source, properties, use, handling and more. The provenance data may be found from the link under the source name.
The periodic table contains NIST's critically-evaluated data on atomic properties of the elements. The provenance data that include data for atomic spectroscopy, X-ray and gamma ray, radiation dosimetry, nuclear physics, and condensed matter physics may be found from the link under the source name. Ref: https://www.nist.gov/pml/atomic-spectra-database
This section provides all form of data related to element Nobelium.
The element property data was retrieved from publications.
