Lithium is mixed (alloyed) with aluminium and magnesium for
light-weight alloys, and is also used in batteries, some greases, some glasses,
and in medicine.
Lithium does not occur as the free metal in nature because
of its high reactivity. Deposits are known all around the world. It is a minor
component of nearly all igneous rocks and is a component of many natural
brines.
•Name: Lithium
•Symbol: Li
•Atomic number: 3
•Atomic weight: [6.941]
•Standard state: solid at 298 K
•CAS Registry ID: 7439-93-2
•Group in periodic table: 1
•Group name: Alkali metal
•Period in periodic table: 2
•Block in periodic table: s-block
•Color: silvery white/grey
•Classification: Metallic
•Symbol: Li
•Atomic number: 3
•Atomic weight: [6.941]
•Standard state: solid at 298 K
•CAS Registry ID: 7439-93-2
•Group in periodic table: 1
•Group name: Alkali metal
•Period in periodic table: 2
•Block in periodic table: s-block
•Color: silvery white/grey
•Classification: Metallic
Historical information
Lithium was discovered by Johan August Arfvedson at 1817 in
Stockholm, Sweden. Origin of name: from the Greek word "lithos"
meaning "stone", apparently because it was discovered from a mineral
source whereas the other two common Group 1 elements, sodium and potassium,
were discovered from plant sources. The mineral petalite (which contains
lithium) was discovered by the Brazilian scientist José Bonifácio de Andrada e
Silva towards the end of the 18th century while visiting Sweden. Lithium was
discovered by Johan August Arfvedson in 1817 during an analysis of petalite
ore, an ore now recognized to be LiAl(Si2O5)2, taken from the Swedish island of
Utö. Arfvedson subsequently discovered lithium in the minerals spodumene and
lepidolite. C.G. Gmelin observed in 1818 that lithium salts color flames bright
red. Neither Gmelin nor Arfvedson were able to isolate the element itself from
lithium salts, for example in attempted reductions by heating the oxide with
iron or carbon.
The first isolation of elemental lithium was achieved later
by W.T. Brande and Sir Humphrey Davy by the electrolysis of lithium oxide. In
1855, Bunsen and Mattiessen isolated larger quantities of the metal by
electrolysis of lithium chloride.
In 1923 the first commercial production of lithium metal was
achieved by Metallgesellschaft AG in Germany using the electrolysis of a molten
mixture of lithium chloride and potassium chloride, exploiting a suggestion
made by Guntz in 1893.
Physical properties
•Melting point: 453.69 [or 180.54 °C (356.97 °F)] K
•Boiling point: 1615 [or 1342 °C (2448 °F)] K
•Density of solid: 535 kg m-3
•Boiling point: 1615 [or 1342 °C (2448 °F)] K
•Density of solid: 535 kg m-3
Orbital properties
•Ground state electron configuration: [He].2s1
•Shell structure: 2.1
•Term symbol: 2S1/2
•Pauling electronegativity: 0.98 (Pauling units)
•Shell structure: 2.1
•Term symbol: 2S1/2
•Pauling electronegativity: 0.98 (Pauling units)
Isolation
Lithium would not normally be made in the laboratory as it
is so readily available commercially. All syntheses require an electrolytic
step as it is so difficult to add an electron to the poorly electronegative
lithium ion Li+.
The ore spodumene, LiAl(SiO3)2, is the most important
commercial ore containing lithium. The α form is first converted into the
softer β form by heating to around 1100°C. This is mixed carefully with hot
sulphuric acid and extracted into water to form lithium sulphate, Li2SO4, solution.
The sulphate is washed with sodium carbonate, Na2CO3, to form a precipitate of
the relatively insoluble lithium carbonate, Li2CO3.
Li2SO4 + Na2CO3 → Na2SO4 + Li2CO3 (solid)
Reaction of lithium carbonate with HCl then provides lithium
chloride, LiCl.
Li2CO3 + 2HCl → 2LiCl + CO2 +H2O
Lithium chloride has a high melting point (> 600°C)
meaning that it sould be expensive to melt it in order to carry out the
electrolysis. However a mixture of LiCl (55%) and KCl (45%) melts at about
430°C and so much less energy and so expense is required for the electrolysis.
Cathode: Li+(l) + e- → Li (l) Anode: Cl-(l) → 1/2Cl2 (g) +
e-
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