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lead

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Article Genealogy
Parent: BCS theory Hop 4
Expansion Funnel Raw 82 → Dedup 0 → NER 0 → Enqueued 0
1. Extracted82
2. After dedup0 (None)
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lead
Namelead
Number82
Categorypost-transition metal
Group14
Appearancemetallic gray
Standard atomic weight207.2
Electron configuration[Xe] 4f14 5d10 6s2 6p2
Phasesolid
Melting point327.46 °C
Boiling point1749 °C
Density11.34 g/cm3
Atomic radius175 pm
Crystal structureface-centered cubic

lead. A dense, malleable post-transition metal with the atomic number 82 and symbol Pb, derived from the Latin *plumbum*. It is a relatively unreactive element with a low melting point, known for its high density and resistance to corrosion. Historically, its ease of extraction and workability made it one of the first metals used by human civilizations, but its toxicity to biological systems has led to significant public health and environmental regulations in the modern era.

Properties

Lead is a bluish-white, lustrous metal with a bright sheen that tarnishes to a dull gray upon exposure to air. It is very soft, highly malleable, ductile, and has relatively low tensile strength. The element has a face-centered cubic crystal structure and is a poor conductor of electricity compared to other metals like copper or aluminum. Chemically, it exhibits oxidation states of +2 and +4, with the +2 state being more stable, a characteristic of the heavier members of the carbon group. Lead compounds, such as lead(II) oxide and lead(IV) oxide, are common, and it forms a protective layer of lead carbonate or lead sulfate when exposed to air or water, which inhibits further corrosion. Its low melting point makes it easy to cast and alloy with other metals like tin and antimony.

Occurrence and production

Lead is rarely found in its native metallic state; it primarily occurs in the mineral galena (lead sulfide), which is the most important ore worldwide. Other significant minerals include cerussite (lead carbonate) and anglesite (lead sulfate). Major deposits are found in association with zinc, silver, and copper ores in regions like the Mississippi Valley in the United States, the Broken Hill deposit in Australia, and the Sullivan Mine in Canada. Global production is dominated by China, followed by Australia, the United States, Peru, and Mexico. The extraction process typically involves mining the ore, concentrating it via froth flotation, and then smelting in a blast furnace or Imperial Smelting Process to produce bullion lead, which is often refined electrolytically to remove impurities like bismuth.

Applications

Historically, lead was used extensively in aqueducts, plumbing, roofing, and stained glass windows. Its high density and ability to absorb radiation make it invaluable for radiation shielding in nuclear reactors, X-ray machines, and for containing radioactive materials. The largest historical use was in lead-acid batteries for automotive and industrial storage, a market that continues to dominate consumption. Other applications include use as a solder in electronics, as an additive in certain types of crystal glass (lead glass), and in weights for scuba diving and fishing. Compounds like tetraethyllead were once critical antiknock agents in gasoline, but this use has been phased out globally due to toxicity.

Biological and environmental effects

Lead and its compounds are potent neurotoxins that accumulate in soft tissues and bones, causing lead poisoning. Exposure, even at low levels, can cause irreversible neurological damage, particularly in children, affecting cognitive development and leading to conditions like anemia and encephalopathy. Major exposure pathways include ingestion of contaminated dust, water from lead pipes, and paint chips from older buildings containing lead paint. Environmental contamination stems from historical mining activities, industrial emissions, and the past use of leaded fuels. Efforts to mitigate effects include regulations like the Clean Air Act in the United States, the global phase-out of leaded gasoline championed by the United Nations Environment Programme, and remediation of sites like the Bunker Hill Superfund Site.

History

Lead use dates to antiquity, with artifacts found at Çatalhöyük in Turkey from around 6500 BCE. The Romans were extensive users, employing it for water pipes, cooking pots, cosmetics, and as a sweetener in wine (sapa), practices now understood to have caused widespread poisoning. Alchemists associated lead with the planet Saturn and believed it could be transmuted into gold. During the Industrial Revolution, demand surged for piping, paint, and later, ammunition. The 20th century saw its integration into petroleum additives and electronics, followed by a dramatic reassessment after the work of researchers like Clair Cameron Patterson on lead contamination and its health impacts, leading to major public health reforms and the rise of substitute materials.

Category:Chemical elements Category:Post-transition metals Category:Neurotoxins