Isotopes
Naturally occurring lithium is composed of 2 stable isotopes Li-6 and Li-7 with Li-7 being the most abundant (92.5% natural abundance). Six radioisotopes have been characterized with the most stable being Li-8 with a half-life of 838 ms and Li-9 with a half-life of 178.3 ms. All of the remaining radioactive isotopes have half-lifes that are less than 8.5 ms or are not known.
The isotopes of lithium range in atomic weight from 4.027 amu (Li-4) to 11.0438 amu (Li-11). The primary decay mode before the most abundant stable isotope, Li-7, is proton emission (with one case of alpha decay) and the primary mode after is beta emission (with some neutron emission). The primary decay products before Li-7 are element 2 (helium) isotopes and the primary products after are element 4 (beryllium) isotopes.
Lithium-7 is one of the primordial elements (produced in big bang nucleosysthesis). Lithium isotopes fractionate substantially during a wide variety of natural processes, including mineral formation (chemical precipitation), metabolism, ion exchange (Li substitutes for magnesium and iron in octahedral sites in clay minerals, where Li-6 is preferential over Li-7), hyperfiltration, and rock alteration.
Precautions
Like the other alkali metals, lithium in its pure form is highly flammable and slightly explosive when exposed to air and especially water. This metal is also corrosive and requires special handling to avoid skin contact. When it is stored it should be placed in an inflammable liquid hydrocarbon such as naphtha. Lithium plays no natural biological role and is considered to be slightly toxic. This means that when it is used as a drug, blood concentrations have to be carefully monitored.
See Also
External links