Measurement
Mercury is used in instruments because a physical property such as expansion, electrical response or atomic transition can be measured accurately.
Mercury is element 80 (Hg), located in period 6, group 12 and the d block. At room temperature its reference phase is liquid. Its electron configuration is [Xe] 4f14 5d10 6s2.
The d subshell participates in the chemistry of mercury. Transition metals can use electrons of similar energies in bonding, which is why variable oxidation states, coordination compounds and catalytic behaviour are common across the d block.
Its electron configuration, [Xe] 4f14 5d10 6s2, should be read together with the oxidation state of the compound: removing electrons changes which d orbitals are occupied and can alter colour, magnetism, bonding and reactivity.
For mercury, important chemical forms include metals and alloys, oxides, halides and coordination compounds. Variable oxidation states are common because s and d electrons have similar energies, and ligands around the metal ion can strongly alter colour, magnetism and reactivity.
The reference phase at room temperature is liquid. The listed density is 13.53 g/cm³. The melting point is 234.3 K (-38.8 °C). The boiling point is 629.9 K (356.7 °C). Pressure, purity and crystal structure can shift measured physical properties.
In practice, mercury is encountered in measurement, lamps and chemical synthesis.
Mercury is used in instruments because a physical property such as expansion, electrical response or atomic transition can be measured accurately.
Mercury is used in lamp gases, electrodes, phosphors or specialised light-producing components.
Mercury is used as an element, reagent, catalyst component or precursor in the manufacture of other chemicals.
Mercury is in period 6 and group 12. In the neighbourhood shown here, it lies between gold and thallium in the same period; cadmium is above it and copernicium below it in the same group. These positions make it possible to compare atomic size, ionisation energy and bonding behaviour with nearby elements.
Values describe the element or neutral atom where applicable. Physical data can depend on allotrope, pressure and measurement conditions.
Mercury was known before 2000 BCE, with no single discoverer identified in this record. Its early use predates modern chemistry, so use of the material, chemical identification and the later atomic-number definition are separate stages.
The standard atomic weight is 200.592(3). This value refers to the isotopic composition of natural terrestrial material, not to the mass of one specific atom.
Mercury has at least one stable isotope. Different isotopes have the same number of protons and therefore the same element identity, but different neutron numbers and atomic masses.
Mercury exposure depends strongly on chemical form. Vapour and some organic mercury compounds are particularly hazardous.