|Name, symbol||meitnerium, Mt|
|Pronunciation||// or //
myt-NEER-ee-əm or MYT-nər-ee-əm
|Meitnerium in the periodic table|
|Standard atomic weight|||
|Element category||unknown, but probably a transition metal|
|Group, block||group 9, d-block|
|Electron configuration||[Rn] 5f14 6d7 7s2 (calculated)|
|per shell||2, 8, 18, 32, 32, 15, 2 (predicted)|
|Density near r.t.||37.4 g·cm−3 (predicted)|
|Oxidation states||9, 8, 6, 4, 3, 1 (predicted)|
|Ionization energies||1st: 800.8 kJ·mol−1
2nd: 1823.6 kJ·mol−1
3rd: 2904.2 kJ·mol−1
(more) (all estimated)
|Atomic radius||empirical: 128 pm (predicted)|
|Covalent radius||129 pm (estimated)|
|Crystal structure||face-centered cubic (fcc)
|Magnetic ordering||paramagnetic (predicted)|
|CAS Registry Number||54038-01-6|
|Naming||after Lise Meitner|
|Discovery||Gesellschaft für Schwerionenforschung (1982)|
|Most stable isotopes|
Meitnerium is a chemical element with symbol Mt and atomic number 109. It is an extremely radioactive synthetic element (an element not found in nature that can be created in a laboratory). The most stable known isotope, meitnerium-278, has a half-life of 7.6 seconds. The GSI Helmholtz Centre for Heavy Ion Research near Darmstadt, Germany, first created this element in 1982.
In the periodic table, meitnerium is a d-block transactinide element. It is a member of the 7th period and is placed in the group 9 elements, although no chemical experiments have been carried out to confirm that it behaves as the heavier homologue to iridium in group 9. Meitnerium is calculated to have similar properties to its lighter homologues, cobalt, rhodium, and iridium.
Meitnerium was first synthesized on August 29, 1982 by a German research team led by Peter Armbruster and Gottfried Münzenberg at the Institute for Heavy Ion Research (Gesellschaft für Schwerionenforschung) in Darmstadt. The team bombarded a target of bismuth-209 with accelerated nuclei of iron-58 and detected a single atom of the isotope meitnerium-266:
83Bi + 58
26Fe → 266
109Mt + n
The naming of meitnerium was discussed in the element naming controversy regarding the names of elements 104 to 109, but meitnerium was the only proposal and thus was never disputed. The name meitnerium (Mt) was suggested in honor of the Austrian physicist Lise Meitner, a co-discoverer of protactinium (with Otto Hahn), and one of the discoverers of nuclear fission. In 1994 the name was recommended by IUPAC, and was officially adopted in 1997. It is thus the only element named specifically after a non-mythological woman.
|265Mt||2? min||α ?||unknown||—|
|267Mt||10? ms||α ?||unknown||—|
|269Mt||0.2? s||α ?||unknown||—|
|271Mt||5? s||α ?||unknown||—|
|272Mt||10? s||α, SF ?||unknown||—|
|273Mt||20? s||α, SF ?||unknown||—|
|274Mt||0.44 s||α, SF||2006||282Uut(—,2α)|
|276Mt||0.72 s||α, SF||2003||288Uup(—,3α)|
|279Mt||6? min||α, SF ?||unknown||—|
Meitnerium has no stable or naturally-occurring isotopes. Several radioactive isotopes have been synthesized in the laboratory, either by fusing two atoms or by observing the decay of heavier elements. Eight different isotopes of meitnerium have been reported with atomic masses 266, 268, 270, and 274–278, two of which, meitnerium-268 and meitnerium-270, have known but unconfirmed metastable states. Most of these decay predominantly through alpha decay, although some undergo spontaneous fission.
Stability and half-lives
All meitnerium isotopes are extremely unstable and radioactive; in general, heavier isotopes are more stable than the lighter. The most stable known meitnerium isotope, 278Mt, is also the heaviest known meitnerium isotope; it has a half-life of 7.6 seconds. A metastable nuclear isomer, 270mMt, has been reported to also have a half-life of over a second. The isotopes 276Mt and 274Mt have half-lives of 0.72 and 0.44 seconds respectively. The remaining four isotopes have half-lives between 1 and 20 milliseconds. The undiscovered isotope 281Mt has been predicted to be the most stable towards beta decay; however, no known meitnerium isotope has been observed to undergo beta decay. Some unknown isotopes, such as 265Mt, 272Mt, 273Mt, and 279Mt, are predicted to have half-lives longer than the known isotopes. Before its discovery, 274Mt and 277Mt were also predicted to have long half-lives of 20 seconds and 1 minute respectively; however, they were later found to have shorter half-lives of only 0.44 seconds and 5 milliseconds respectively.
Meitnerium is the seventh member of the 6d series of transition metals. Since element 112 (copernicium) has been shown to be a transition metal, it is expected that all the elements from 104 to 112 would form a fourth transition metal series, with meitnerium as part of the platinum group metals. Calculations on its ionization potentials and atomic and ionic radii are similar to that of its lighter homologue iridium, thus implying that meitnerium's basic properties will resemble those of the other group 9 elements, cobalt, rhodium, and iridium.
Prediction of the probable chemical properties of meitnerium has not received much attention recently. Meitnerium is expected to be a noble metal. Based on the most stable oxidation states of the lighter group 9 elements, the most stable oxidation states of meitnerium are predicted to be the +6, +3, and +1 states, with the +3 state being the most stable in aqueous solutions. In comparison, rhodium and iridium show a maximum oxidation state of +6, while the most stable states are +4 and +3 for iridium and +3 for rhodium. Group 9 is the first group in the transition metals to show lower oxidation states than the group number, the +9 state not being known for any element. The oxidation state +9 might be possible for meitnerium in the nonafluoride (MtF9) and the [MtO4]+ cation, although [IrO4]+ is expected to be more stable. The tetrahalides of meitnerium have also been predicted to have similar stabilities to those of iridium, thus also allowing a stable +4 state. It is further expected that the maximum oxidation states of elements from bohrium (element 107) to darmstadtium (element 110) may be stable in the gas phase but not in aqueous solution.
Physical and atomic
Meitnerium is expected to be a solid under normal conditions and assume a face-centered cubic crystal structure, similarly to its lighter congener iridium. It should be a very heavy metal with a density of around 37.4 g/cm3, which would be the second-highest of any of the 118 known elements, second only to that predicted for its neighbor hassium (41 g/cm3). In comparison, the densest known element that has had its density measured, osmium, has a density of only 22.61 g/cm3. This results from meitnerium's high atomic weight, the lanthanide and actinide contractions, and relativistic effects, although production of enough meitnerium to measure this quantity would be impractical, and the sample would quickly decay. Meitnerium is also predicted to be paramagnetic.
Theoreticians have predicted the covalent radius of meitnerium to be 6 to 10 pm larger than that of iridium. For example, the Mt–O bond distance is expected to be around 1.9 Å. The atomic radius of meitnerium is expected to be around 128 pm.
Unambiguous determination of the chemical characteristics of meitnerium has yet to have been established due to the short half-lives of meitnerium isotopes and a limited number of likely volatile compounds that could be studied on a very small scale. One of the few meitnerium compounds that are likely to be sufficiently volatile is meitnerium hexafluoride (MtF
6), as its lighter homologue iridium hexafluoride (IrF
6) is volatile above 60 °C and therefore the analogous compound of meitnerium might also be sufficiently volatile; a volatile octafluoride (MtF
8) might also be possible. For chemical studies to be carried out on a transactinide, at least four atoms must be produced, the half-life of the isotope used must be at least 1 second, and the rate of production must be at least one atom per week. Even though the half-life of 278Mt, the most stable known meitnerium isotope, is 7.6 seconds, long enough to perform chemical studies, another obstacle is the need to increase the rate of production of meitnerium isotopes and allow experiments to carry on for weeks or months so that statistically significant results can be obtained. Separation and detection must be carried out continuously to separate out the meitnerium isotopes and automated systems can then experiment on the gas-phase and solution chemistry of meitnerium as the yields for heavier elements are predicted to be smaller than those for lighter elements; some of the separation techniques used for bohrium and hassium could be reused. However, the experimental chemistry of meitnerium has not received as much attention as that of the heavier elements from copernicium to livermorium.
The Lawrence Berkeley National Laboratory attempted to synthesize the isotope 271Mt in 2002–2003 for a possible chemical investigation of meitnerium because it was expected that it might be more stable than the isotopes around it as it has 162 neutrons, a magic number for deformed nuclei; its half-life was predicted to be a few seconds, long enough for a chemical investigation. However, no atoms of 271Mt were detected, and this isotope of meitnerium is currently unknown.
An experiment determining the chemical properties of a transactinide would need to compare a compound of that transactinide with analogous compounds of some of its lighter homologues: for example, in the chemical characterization of hassium, hassium tetroxide (HsO4) was compared with the analogous osmium compound, osmium tetroxide (OsO4). In a preliminary step towards determining the chemical properties of meitnerium, the GSI attempted sublimation of the rhodium compounds rhodium(III) oxide (Rh2O3) and rhodium(III) chloride (RhCl3). However, macroscopic amounts of the oxide would not sublimate until 1000 °C and the chloride would not until 780 °C, and then only in the presence of carbon aerosol particles: these temperatures are far too high for such procedures to be used on meitnerium, as most of the current methods used for the investigation of the chemistry of superheavy elements do not work above 500 °C.
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|Periodic table (Large cells)|