: lead colors flame pale blue|alt=A flame with a small metal rod penetrating it; the flame near the rod is pale blue. When exposed to moist air, bulk lead develops a protective surface layer of variable composition.
Lead(II) carbonate is a common constituent, and in urban or maritime environments, lead(II)
sulfate or lead(II)
chloride may also be present. This layer renders bulk lead effectively inert under atmospheric conditions. In contrast, finely powdered lead, like many metals, is
pyrophoric and burns with a bluish-white flame. Lead reacts with
fluorine at room temperature to form
lead(II) fluoride. Its reaction with
chlorine is similar but requires heating, as the resulting chloride layer reduces further reactivity. Molten lead combines with the
chalcogens to produce lead(II) chalcogenides. The metal resists attack by
sulfuric and
phosphoric acids but not by
hydrochloric or
nitric acids; the difference arises from the insolubility and subsequent passivation of certain lead salts. Organic acids, such as
acetic acid, dissolve lead in the presence of oxygen. Concentrated
alkalis can also dissolve lead, producing
plumbites.
Inorganic compounds Lead exhibits two principal oxidation states: +4 and +2. While the
tetravalent state is characteristic of the carbon group, the divalent state is rare for
carbon and
silicon, less common for germanium, significant but not dominant for tin, and the most prevalent for lead. This predominance is linked to
relativistic effects—specifically the
inert pair effect—which occurs when there is a large
electronegativity difference between lead and anions such as
oxide,
halide, or
nitride. In such cases, lead develops a pronounced partial positive charge, causing a stronger contraction of the 6s orbital compared to the 6p orbital and rendering it relatively unreactive in ionic compounds. The inert pair effect is less pronounced in compounds where lead forms covalent bonds with elements of similar electronegativity, such as carbon in organolead compounds. In these, the 6s and 6p orbitals remain comparable in size, and sp3 hybridization remains energetically favorable, making lead predominantly tetravalent in such cases. The electronegativity values further reflect this behavior: lead(II) has a value of 1.87, and lead(IV) has 2.33. This represents a reversal in the general trend of increasing stability of the +4 oxidation state down the carbon group; by comparison, tin has electronegativities of 1.80 (+2 state) and 1.96 (+4 state).
Lead(II) |alt=Cream powderLead(II) compounds are characteristic of the inorganic chemistry of lead. Even strong
oxidizing agents like fluorine and chlorine react with lead to give only
PbF2 and
PbCl2. Lead(II) ions are usually colorless in solution, and partially hydrolyze to form Pb(OH)+ and finally [Pb4(OH)4]4+ (in which the
hydroxyl ions act as
bridging ligands), but are not
reducing agents as tin(II) ions are.
Techniques for identifying the presence of the Pb2+ ion in water generally rely on the precipitation of lead(II) chloride using dilute hydrochloric acid. As the chloride salt is sparingly soluble in water, in very dilute solutions the precipitation of
lead(II) sulfide is instead achieved by bubbling
hydrogen sulfide through the solution.
Lead monoxide exists in two
polymorphs,
litharge α-PbO (red) and
massicot β-PbO (yellow), the latter being stable only above around 488 °C. Litharge is the most commonly used inorganic compound of lead. There is no lead(II) hydroxide; increasing the pH of solutions of lead(II) salts leads to hydrolysis and condensation. Lead commonly reacts with heavier chalcogens.
Lead sulfide is a
semiconductor, a
photoconductor, and an extremely sensitive
infrared radiation detector. The other two chalcogenides,
lead selenide and
lead telluride, are likewise photoconducting. They are unusual in that their color becomes lighter going down the group. in a tetragonal
unit cell of
lead(II,IV) oxide|alt=Alternating dark gray and red balls connected by dark gray-red cylinders Lead dihalides are well-characterized; this includes the diastatide and mixed halides, such as PbFCl. The relative insolubility of the latter forms a useful basis for the
gravimetric determination of fluorine. The difluoride was the first solid
ionically conducting compound to be discovered (in 1834, by
Michael Faraday). The other dihalides decompose on exposure to ultraviolet or visible light, especially
the diiodide. Many lead(II)
pseudohalides are known, such as the cyanide, cyanate, and
thiocyanate. Lead(II) forms an extensive variety of halide
coordination complexes, such as [PbCl4]2−, [PbCl6]4−, and the [Pb2Cl9]
n5
n− chain anion.
Lead(II) sulfate is insoluble in water, like the sulfates of other heavy divalent
cations.
Lead(II) nitrate and
lead(II) acetate are very soluble, and this is exploited in the synthesis of other lead compounds.
Lead(IV) Few inorganic lead(IV) compounds are known. They are only formed in highly oxidizing solutions and do not normally exist under standard conditions. Lead(II) oxide gives a mixed oxide on further oxidation, Pb3O4. It is described as
lead(II,IV) oxide, or structurally 2PbO·PbO2, and is the best-known mixed valence lead compound.
Lead dioxide is a strong oxidizing agent, capable of oxidizing hydrochloric acid to chlorine gas. This is because the expected PbCl4 that would be produced is unstable and spontaneously decomposes to PbCl2 and Cl2. Analogously to
lead monoxide, lead dioxide is capable of forming
plumbate anions.
Lead disulfide and lead diselenide are only stable at high pressures.
Lead tetrafluoride, a yellow crystalline powder, is stable, but less so than the
difluoride.
Lead tetrachloride (a yellow oil) decomposes at room temperature, lead tetrabromide is less stable still, and the existence of lead tetraiodide is questionable.
Other oxidation states anion [Pb9]4− from [K(18-crown-6)]2K2Pb9·(en)1.5|alt=Nine dark gray spheres connected by cylinders of the same color forming a convex shape Some lead compounds exist in formal oxidation states other than +4 or +2. Lead(III) may be obtained, as an intermediate between lead(II) and lead(IV), in larger organolead complexes; this oxidation state is not stable, as both the lead(III) ion and the larger complexes containing it are
radicals. The same applies for lead(I), which can be found in such radical species. Numerous mixed lead(II,IV) oxides are known. When PbO2 is heated in air, it becomes Pb12O19 at 293 °C, Pb12O17 at 351 °C, Pb3O4 at 374 °C, and finally PbO at 605 °C. A further
sesquioxide, Pb2O3, can be obtained at high pressure, along with several non-stoichiometric phases. Many of them show defective
fluorite structures in which some oxygen atoms are replaced by vacancies: PbO can be considered as having such a structure, with every alternate layer of oxygen atoms absent. Negative oxidation states can occur as
Zintl phases, as either free lead anions, as in Ba2Pb, with lead formally being lead(−IV), or in oxygen-sensitive ring-shaped or polyhedral cluster ions such as the
trigonal bipyramidal Pb52− ion, where two lead atoms are lead(−I) and three are lead(0). In such anions, each atom is at a polyhedral vertex and contributes two electrons to each covalent bond along an edge from their sp3 hybrid orbitals, the other two being an external
lone pair. They may be made in
liquid ammonia via the reduction of lead by
sodium.
Organolead molecule:
Carbon Hydrogen Lead|alt=A gray-green sphere linked to four black spheres, each, in turn, linked also to three white ones Lead can form
multiply-bonded chains, a property it shares with its lighter
homologs in the carbon group. Its capacity to do so is much less because the Pb–Pb
bond energy is over three and a half times lower than that of the
C–C bond. With itself, lead can build metal–metal bonds of an order up to three. With carbon, lead forms organolead compounds similar to, but generally less stable than, typical organic compounds (due to the Pb–C bond being rather weak). This makes the
organometallic chemistry of lead far less wide-ranging than that of tin. Lead predominantly forms organolead(IV) compounds, even when starting with inorganic lead(II) reactants; very few organolead(II) compounds are known. The most well-characterized exceptions are Pb[CH(SiMe3)2]2 and
plumbocene. The lead analog of the simplest
organic compound,
methane, is
plumbane. Plumbane may be obtained in a reaction between metallic lead and atomic hydrogen. Two simple derivatives,
tetramethyllead and
tetraethyllead, are the best-known
organolead compounds. These compounds are relatively stable: tetraethyllead only starts to decompose if heated or if exposed to sunlight or ultraviolet light. With sodium metal, lead readily forms an equimolar alloy that reacts with
alkyl halides to form
organometallic compounds such as tetraethyllead. The oxidizing nature of many organolead compounds is usefully exploited:
lead tetraacetate is an important laboratory reagent for oxidation in organic synthesis. Tetraethyllead, once added to automotive gasoline, was produced in larger quantities than any other organometallic compound, and is still widely used in
fuel for small aircraft. Other organolead compounds are less chemically stable. For many organic compounds, a lead analog does not exist. == Origin and occurrence ==