Lead (Pb)
Stable isotopes of lead available from ISOFLEX
Isotope | Z(p) | N(n) | Atomic Mass | Natural Abundance | Enrichment Level | Chemical Form |
Pb-204 | 82 | 122 | 203.973028 | 1.40% | 99.90% | Metal |
Pb-204 | 82 | 122 | 203.973028 | 1.40% | 99.90% | Oxide |
Pb-206 | 82 | 124 | 205.974449 | 24.10% | >99.00% | Metal |
Pb-206 | 82 | 124 | 205.974449 | 24.10% | >99.00% | Oxide |
Pb-207 | 82 | 125 | 206.975880 | 22.10% | 72.00->99.00% | Metal |
Pb-207 | 82 | 125 | 206.975880 | 22.10% | 72.00->99.00% | Oxide |
Pb-208 | 82 | 126 | 207.976636 | 52.40% | 97.80->99.50% | Metal |
Pb-208 | 82 | 126 | 207.976636 | 52.40% | 97.80->99.50% | Oxide |
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Lead has been known and used throughout history — ancient alchemists believed it was the world's oldest metal and devoted a great deal of time attempting to transmute it into gold. Its name originates with the Anglo-Saxon word lead, and its symbol — Pb — with the Latin word plumbum, meaning “liquid silver.”
Lead is a heavy, very soft, malleable, ductile solid with face-centered cubic crystals. It is soluble in dilute nitric acid and insoluble in water (but dissolves slowly in water containing a weak acid). It resists corrosion and is relatively impenetrable to radiation. It is a poor electrical conductor. Lead forms amphoteric compounds in +2 and +4 valence states, forming plumbous and plumbic salts, as well as plumbites and plumbates. Its divalent compounds are far more numerous than its tetravalent compounds. In its very finely divided form, lead is pyrophoric. The metal is not attacked by hot water; in hard water, however, the presence of small amounts of carbonate, sulfate or silicate ions forms a protective film on the metal's surface. Lead does not evolve hydrogen readily with acids. At ordinary temperatures, it is not readily attacked by sulfuric acid. Hydrofluoric acid also has little action on the metal. Organic acids in the presence of oxygen react slowly with lead, forming their soluble salts; thus acetic acid in the presence of oxygen forms lead(II) acetate. Lead combines with fluorine, chlorine and bromine, forming bivalent lead halides.
There are numerous applications for lead in all its forms: metal, alloys and compounds. It is useful in the construction of pipelines, plumbing fixtures, wires, ammunition, containers for corrosive acids, and as a shield against short-wavelength radiation. Both the metal and its dioxide are used in storage batteries. Several lead compounds — such as lead chromate, lead sulfate, lead tetroxide and the basic carbonate — have been used in paint.
Considered an acute and chronic toxicant, lead can cause acute ataxia, headache, vomiting, stupor, hallucination, tremors and convulsions, along with chronic symptoms including weight loss, anemia, kidney damage, memory loss and brain damage.
Properties of Lead
Name | Lead |
Symbol | Pb |
Atomic number | 82 |
Atomic weight | 207.2 |
Standard state | Solid at 298 °K |
CAS Registry ID | 7439-92-1 |
Group in periodic table | 14 |
Group name | None |
Period in periodic table | 6 |
Block in periodic table | p-block |
Color | Bluish white |
Classification | Metallic |
Melting point | 327.46 °C |
Boiling point | 1740 °C |
Thermal conductivity | 35.3 W/(m·K) at 298.2 °K |
Electrical resistivity | 20.65 µΩ·cm at 20 °C |
Electronegativity | 1.8 |
Specific heat | 0.128 J/(g·K) at 20 °C |
Heat of vaporization | 178 kJ·mol-1 at 1740 °C |
Heat of fusion | 4.77 kJ·mol-1 |
Density of liquid | 10.66 g/cm3 at 327.46 °C |
Density of solid | 11.3 g/cm3 |
Mohs hardness scale | 1 |
Electron configuration | [Xe]4f145d106s26p2 |
Atomic radius | 1.75 Å |
Covalent radius (sp3) | 1.44 Å |
Ionic radius | Pb2+: 1.18 Å; Pb4+: 0.70 Å |
Oxidation states | +2, +4 |
Research
- Stable isotopes of lead and strontium as tracers of sources of airborne particulate matter in Kyrgyzstan
- A lead isotope perspective on urban development in ancient Naples
- Trace elements and Pb isotopes in soils and sediments impacted by uranium mining
- Direct evidence of octupole deformation in neutron-rich 144Ba
- Measurement of several β-delayed neutron emitting isotopes beyond N = 126
- Isotope geochemistry and revised geochronology of the Purrido Ophiolite (Cabo Ortegal Complex, NW Iberian Massif): Devonian magmatism with mixed sources and involved Mesoproterozoic basement
- Nanogeochronology of discordant zircon measured by atom probe microscopy of Pb-enriched dislocation loops
- B isotopes of Carboniferous-Permian volcanic rocks in the Tuha basin mirror a transition from subduction to intraplate setting in Central Asian Orogenic Belt
- Confirmation of the new isotope 178Pb
- Isotopic data for Late Cretaceous intrusions and associated altered and mineralized rocks in the Big Belt Mountains, Montana
- Geochemical, isotopic, and zircon (U-Pb, O, Hf isotopes) evidence for the magmatic sources of the volcano-plutonic Ollo de Sapo Formation, Central Iberia
- Multi-isotope proveniencing of human remains from a Bronze Age battlefield in the Tollense Valley in northeast Germany
- Geochemical markers of human occupation in the lower Argens valley (Fréjus, France): from protohistory to Roman times
- Targeted Alpha Therapy, an Emerging Class of Cancer Agents: A Review
- Accelerated burial of petroleum hydrocarbons in Arabian Gulf blue carbon repositories
- Isotope systematics and chemical composition of tin ingots from Mochlos (Crete) and other Late Bronze Age sites in the eastern Mediterranean Sea: An ultimate key to tin provenance?
- Patterns of camelid management in Wari Empire reconstructed using multiple stable isotope analysis: evidence from Castillo de Huarmey, northern coast of Peru
- The Isotopic Ecology of Fossil Vertebrates and Conservation Paleobiology