Introduction
The term ‘transition metals’ is mainly used to define any element in the d-block of the periodic table, this involves groups 3 to 12. A transition metal is an element whose atom possesses a partially filled d subshell, or it can give rise to cations having an incomplete d subshell. Some of the more commonly known transitional metals include titanium, iron, manganese, nickel, copper, cobalt, silver, mercury and gold. Three of the most common elements are those of iron, cobalt and nickel as they are the only elements that are known to produce a magnetic field. There are various different properties identified in the transition elements that are not found in other elements, as a result of their partially filled d shell.
Examples of Transition Elements
Scandium, Titanium, Vanadium, Chromium, Manganese, Iron, Cobalt, Nickel, Copper, Zinc, Yttrium, Zirconium, Niobium, Molybdenum, Technetium, Ruthenium, Rhodium, Palladium, Silver, Cadmium, Lanthanum, sometimes (often considered a rare earth, lanthanide), Hafnium, Tantalum, Tungsten, Rhenium, Osmium, Iridium, Platinum, Gold, Mercury, Actinium, sometimes (often considered a rare earth, actinide)Rutherfordium, Dubnium, Seaborgium, Bohrium, Hassium, Meitnerium, Darmstadtium, Roentgenium, Copernicium presumably is a transition metal.
Transition Metal Properties
The transition metals are the elements that we normally think of when we imagine a metal. These elements possess some properties in common with each other:
They are good conductors of heat and electricity.
The transition metals are malleable (they can be easily hammered into different shapes or bent).
These metals tend to be very hard in nature.
Transition metals look shiny and metallic. Majority of the transition metals are grayish or white (such as iron or silver), but gold and copper possess colors that are not seen in any other element in the periodic table.
The transition metals, represents a group that have high melting points. One of the common exceptions is mercury, it is liquid at room temperature. These elements also have high boiling points.
The d orbitals of the transition elements get progressively filled as we move from left to right across the periodic table. As the subshell is not filled, atoms of the transition metals should have positive oxidation states and also show more than one oxidation state. As seen in iron it mainly carries a 3+ or 2+ oxidation state. Copper might possess a 1+ or 2+ oxidation state. The positive oxidation state refers to the transition metals basically form ionic or partially ionic compounds.
Atoms of these elements possess low ionization energies.
Transition metals form colored complexes, thus their compounds and solutions may be colorful. The complexes split the d orbital into two different energy sublevels so that they can absorb specific wavelengths of light. Due to the different oxidation states, it becomes possible for one element to produce complexes and solutions in a wide range of colors.
As the transition metals are reactive, they are not as reactive as elements belonging to the alkali metals group.
Many transition metals are able to form paramagnetic compounds.