LEAD 349
4. CHEMICAL AND PHYSICAL INFORMATION
mineral with sulfur or oxygen. The most important Pb mineral is galena (PbS). Other common
Pb-containing minerals include anglesite (PbSO
4
), cerussite (PbCO
3
), and minium (Pb
3
O
4
) (Carr et al.
2004; Davidson et al. 2014; Haynes 2014).
Pb can exist in the 0 oxidation state in metallic Pb and in compounds as the +2 or +4 oxidation states. In
the environment, Pb is primarily found in the +2 state in inorganic compounds. The chemistry of
inorganic Pb compounds is generally similar to that of the Group 2(II) or alkaline earth metals. There are
three common oxides of Pb: lead(II) oxide (PbO); lead(II,IV) oxide or lead tetroxide (Pb
3
O
4
); and
lead(IV) oxide or lead dioxide (PbO
2
). The +4 state is only formed under strongly oxidizing conditions.
Inorganic Pb(+4) compounds are relatively unstable and would not be expected to be found under
ordinary environmental conditions. Pb is amphoteric, meaning that it can react with acids and bases. In
acid, Pb forms Pb(+2) (plumbous) and Pb(+4) (plumbic) salts and in basic solution, it forms plumbites
(PbO
2
2-
) and plumbates (Pb(OH)
6
2-
) (Carr et al. 2004). In organolead compounds, Pb is typically in the
tetravalent (+4) oxidation state (Carr et al. 2004; Haynes 2014).
Data on the physical and chemical properties of Pb and several of its compounds are provided in
Table 4-2.