The term transition metal (sometimes also called a transition element) has two possible meanings:
Jensen[2] has reviewed the historical usage of the terms transition element (or metal) and d-block. The word "transition" was first used to describe the elements now known as the d-block by the English chemist Charles Bury in 1921, who referred to a transition series of elements during the change of an inner layer of electrons (for example n=3 in the 4th row of the periodic table) from a stable group of 8 to one of 18, or from 18 to 32.[3]
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In the d-block the atoms of the elements have between 1 and 10 d electrons. The following table shows IUPAC definition of what is called "transition metal".
Group | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 | 12 |
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Period 4 | Sc 21 | Ti 22 | V 23 | Cr 24 | Mn 25 | Fe 26 | Co 27 | Ni 28 | Cu 29 | Zn 30 |
Period 5 | Y 39 | Zr 40 | Nb 41 | Mo 42 | Tc 43 | Ru 44 | Rh 45 | Pd 46 | Ag 47 | Cd 48 |
Period 6 | Hf 72 | Ta 73 | W 74 | Re 75 | Os 76 | Ir 77 | Pt 78 | Au 79 | Hg 80 | |
Period 7 | Rf 104 | Db 105 | Sg 106 | Bh 107 | Hs 108 | Mt 109 | Ds 110 | Rg 111 | Cn 112 |
Atoms of scandium and yttrium have a single d electron in the outermost shell, and thus are mostly considered transition metals. However, as all their compounds contain the ions Sc3+ and Y3+ in which there are no d electrons, these elements are not universally considered transition metals. This is disputed by people saying that classification must be lead by neutral atoms properties, and fact zirconium and titanium compounds also don't contain d-electrons.
Vacant place for 3 group element (and then a transition metal) for period 6 is disputed between lanthanum and lutetium and actinium and lawrencium for period 7. To prevent this, IUPAC placed all of these 4 as lanthanoids/actinoids, which makes both series 15 elements long, despite fact there are only 14 f-electrons possible and then f-block can't be any longer. This means IUPAC lanthanoids/actinoids contains one d-element. Modern scientists usually claim Lu and Lr as d-block elements rather the La and Ac, however, both variants are widely used.
The electronic structure of transition metal atoms can be written, with a few minor exceptions, as [Ng]ns2(n-1)dm, as the inner d orbital has more energy than the valence-shell s orbital. In divalent and trivalent ions of the transition metals the situation is reversed so that the s electrons have higher energy. Consequently an ion such as Fe2+ has no s electrons, it has the electronic configuration [Ar]3d6 as compared with the configuration of the atom, [Ar]4s23d6.
According to IUPAC, Zinc, cadmium, mercury and copernicium are transition metals, although some say they are not.[2] as they have the electronic configuration [Ng]d10s2, with no incomplete d shell.[4] People who count Zn, Cd and Hg as post-transition mention that in the oxidation state +2 the ions have the electronic configuration [ Ng ] d10. and while compounds in the +1 oxidation state, such as Hg22+, are known there are no unpaired electrons because of the formation of a covalent bond between the two atoms of the dimer. However, it is opposed by opinion that d-block must be equal by its content to transition metals, because if mercury has no incompleteness in d-orbital, thus ytterbium has no incompleteness in f-orbital and is a transition metal. Also, judging on some separated properties (like Irving-Williams series of stability constants of complexes) is also mostly denied.
There are a number of properties shared by the transition elements that are not found in other elements, which results from the partially filled d shell. These include
Colour in transition-series metal compounds is generally due to electronic transitions of two principal types.
In centrosymmetric complexes, such as octahedral complexes, d-d transitions are forbidden by the Laporte rule and only occur because of vibronic coupling in which a molecular vibration occurs together with a d-d transition. Tetrahedral complexes have somewhat more intense colour because mixing d and p orbitals is possible when there is no centre of symmetry, so transitions are not pure d-d transitions. The molar absorptivity (ε) of bands caused by d-d transitions are relatively low, roughly in the range 5-500 M−1cm−1 (where M = mol dm−3).[7] Some d-d transitions are spin forbidden. An example occurs in octahedral, high-spin complexes of manganese(II), which has a d5 configuration in which all five electron has parallel spins; the colour of such complexes is much weaker than in complexes with spin-allowed transitions. In fact many compounds of manganese(II) appear almost colourless. The spectrum of [Mn(H2O)6]2+ shows a maximum molar absorptivity of about 0.04 M−1cm−1 in the visible spectrum.
A characteristic of transition metals is that they exhibit two or more oxidation states, usually differing by one. For example, compounds of vanadium are known in all oxidation states between −1, such as [V(CO)6]−, and +5, such as VO3−4.
Main group elements in groups 13 to 17 also exhibit multiple oxidation states. The "common" oxidation states of these elements typically differ by two. For example, compounds of gallium in oxidation states +1 and +3 exist in which there is a single gallium atom. No compound of Ga(II) is known: any such compound would have an unpaired electron and would behave as a free radical and be destroyed rapidly. The only compounds in which gallium has a formal oxidation state of +2 are dimeric compounds, such as [Ga2Cl6]2−, which contain a Ga-Ga bond formed from the unpaired electron on each Ga atom.[8] Thus the main difference in oxidation states, between transition elements and other elements is that oxidation states are known in which there is a single atom of the element and one or more unpaired electrons.
The maximum oxidation state in the first row transition metals is equal to the number of valence electron from titanium (+4) up to manganese (+7), but decreases in the later elements. In the second and third rows the maximum occurs with ruthenium and osmium (+8). In compounds such as [MnO4]− and OsO4 the elements achieve a stable octet by forming four covalent bonds.
The lowest oxidation states are exhibited in such compounds as Cr(CO)6 (oxidation state zero) and [Fe(CO)4]2− (oxidation state −2) in which the 18-electron rule is obeyed. These complexes are also covalent.
Ionic compounds are mostly formed with oxidation states +2 and +3. In aqueous solution the ions are hydrated by (usually) six water molecules arranged octahedrally.
Transition metal compounds are paramagnetic when they have one or more unpaired d electrons.[9] In octahedral complexes with between four and seven d electrons both high spin and low spin states are possible. Tetrahedral transition metal complexes such as [FeCl4]2− are high spin because the crystal field splitting is small so that the energy to be gained by virtue of the electrons being in lower energy orbitals is always less that the energy needed to pair up the spins. Some compounds are diamagnetic. These include octahedral, low-spin, d6 and square-planar d8 complexes. In these cases, crystal field splitting is such that all the electrons are paired up.
Ferromagnetism occurs when individual atoms are paramagnetic and the spin vectors are aligned parallel to each other in a crystalline material. Metallic iron and the alloy alnico are examples of ferromagnetic materials involving transition metals. Antiferromagnetism is another example of a magnetic property arising from a particular alignment of individual spins in the solid state.
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