Meitnerium

Meitnerium,  ₁₀₉Mt

General properties
Name, symbol	meitnerium, Mt
Pronunciation	/maɪtˈnɪəriəm/ or /ˈmaɪtnəriəm/ myt-NEER-ee-əm or MYT-nər-ee-əm
Meitnerium in the periodic table
Ir ↑ Mt ↓ (Uhu) hassium ← meitnerium → darmstadtium
Atomic number (Z)	109
Group, block	group 9, d-block
Period	period 7
Element category	unknown, but probably a transition metal
Standard atomic weight (Ar)	[278]
Electron configuration	[Rn] 5f14 6d7 7s2 (calculated)
per shell	2, 8, 18, 32, 32, 15, 2 (predicted)
Physical properties
Phase	solid (predicted)
Density near r.t.	37.4 g/cm3 (predicted)
Atomic properties
Oxidation states	9, 8, 6, 4, 3, 1 ​(predicted)
Ionization energies	1st: 800.8 kJ/mol 2nd: 1823.6 kJ/mol 3rd: 2904.2 kJ/mol (more) (all estimated)
Atomic radius	empirical: 128 pm (predicted)
Covalent radius	129 pm (estimated)
Miscellanea
Crystal structure	​face-centered cubic (fcc) (predicted)
Magnetic ordering	paramagnetic (predicted)
CAS Number	54038-01-6
History
Naming	after Lise Meitner
Discovery	Gesellschaft für Schwerionenforschung (1982)
Most stable isotopes of meitnerium
iso NA half-life DM DE (MeV) DP 278Mt syn 7.6 s α 9.6 274Bh 276Mt syn 0.72 s α 9.71 272Bh 274Mt syn 0.44 s α 9.76 270Bh 270mMt ? syn 1.1 s α 266Bh

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. It is named for Lise Meitner.

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.

History

Meitnerium was named after the physicist Lise Meitner, one of the discoverers of nuclear fission.

Discovery

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:

209
83Bi + 58
26Fe → 266
109Mt + n

Naming

Using Mendeleev's nomenclature for unnamed and undiscovered elements, meitnerium should be known as eka-iridium. In 1979, during the Transfermium Wars (but before the synthesis of meitnerium), IUPAC published recommendations according to which the element was to be called unnilennium (with the corresponding symbol of Une), a systematic element name as a placeholder, until the element was discovered (and the discovery then confirmed) and a permanent name was decided on. Although widely used in the chemical community on all levels, from chemistry classrooms to advanced textbooks, the recommendations were mostly ignored among scientists in the field, who either called it "element 109", with the symbol of (109) or even simply 109, or used the proposed name "meitnerium".

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 (curium being named for both Pierre and Marie Curie).

Isotopes

For a detailed list of information on the discovery of each individual meitnerium isotope, see Isotopes of meitnerium.

List of meitnerium isotopes

Isotope	Half-life	Decay mode	Discovery year	Reaction
265Mt	2? min	α ?	unknown	—
266Mt	1.7 ms	α	1982	209Bi(58Fe,n)
267Mt	10? ms	α ?	unknown	—
268Mt	21 ms	α	1994	272Rg(—,α)
269Mt	0.2? s	α ?	unknown	—
270Mt	5.0 ms	α	2004	278Uut(—,2α)
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)
275Mt	9.7 ms	α	2003	287Uup(—,3α)
276Mt	0.72 s	α, SF	2003	288Uup(—,3α)
277Mt	~5 ms	SF	2012	293Uus(—,4α)
278Mt	7.6 s	α	2009	294Uus(—,4α)
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; 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; 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 predicted to have half-lives of 20 seconds and 1 minute respectively, but they were later found to have half-lives of only 0.44 seconds and 5 milliseconds respectively.

Predicted properties

Chemical

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. The oxidation state +9, represented only by iridium in [IrO₄]⁺, might be possible for its congener 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.

Experimental chemistry

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.

External links

• Meitnerium at The Periodic Table of Videos (University of Nottingham)