Generated by DeepSeek V3.2| silver | |
|---|---|
| Name | silver |
| Number | 47 |
| Category | transition metal |
| Group | 11 |
| Appearance | lustrous white metal |
| Standard atomic weight | 107.8682 |
| Electron configuration | [Kr] 4d10 5s1 |
| Phase | solid |
| Melting point degC | 961.78 |
| Boiling point degC | 2162 |
| Density g per cm3 | 10.49 |
| Atomic radius empirical | 144 pm |
| Crystal structure | face-centered cubic |
| Oxidation states | −2, −1, +1, +2, +3 |
| Electronegativity | 1.93 |
| Ionization energies | 731.0 kJ/mol, 2070 kJ/mol, 3361 kJ/mol |
silver. A chemical element with the symbol Ag and atomic number 47, it is a soft, white, lustrous transition metal. It exhibits the highest electrical conductivity, thermal conductivity, and reflectivity of any metal, making it invaluable in numerous industrial and artistic applications. Historically, it has been used for coinage, jewelry, and ornamentation for millennia, alongside its more precious counterpart gold.
It possesses the highest electrical conductivity of any element and the highest thermal conductivity of any metal, properties critical to its use in electronics. The metal is very ductile and malleable, slightly harder than gold, and is stable in pure air and water but tarnishes when exposed to ozone, hydrogen sulfide, or air containing sulfur. Its most common oxidation state is +1, as in compounds like silver nitrate and silver chloride. It forms a variety of coordination complexes, such as those used in photographic film, and has a single stable isotope, 107Ag.
Native metal is found in the Earth's crust in its pure, free form, often alloyed with gold or other metals, and as a constituent in various ores like argentite and chlorargyrite. Major deposits have been historically mined in locations such as Potosí in Bolivia, Kongsberg in Norway, and the Comstock Lode in Nevada. Today, primary production often comes as a byproduct of refining copper, gold, lead, and zinc ores. The leading producers include Mexico, Peru, and China, with significant refining also occurring in India and the United States.
Evidence of smelting from lead ores dates to around 3000 BCE in Anatolia and the Aegean region. It was highly valued by ancient civilizations, including the Minoans, who used it in Crete, and the Lydians, who are credited with some of the first coinage. The Athenian Laurium mines helped finance the city-state's fleet during the Peloponnesian War. The Spanish Empire's exploitation of Potosí and Mexico flooded the global market in the 16th and 17th centuries. The United States experienced rushes like the Comstock Lode discovery, while the demonetization of the metal in standards like the Coinage Act of 1873 marked a major economic shift.
Its primary industrial use is in electrical contacts and conductors, found in everything from printed circuit boards to automotive components. It is essential in specialized batteries like silver-oxide batteries and in soldering alloys. The photography industry relied heavily on its light-sensitive halide salts, such as those in Kodak film. Other significant uses include mirrors, optical instruments, and as a catalyst in chemical production, such as for ethylene oxide. It is widely used in jewelry, sterling silverware, and coinage, and its compounds have antimicrobial properties applied in wound dressings and water purification.
It has no known natural biological role in humans, but ionic compounds are toxic to many lower organisms, a property exploited for antimicrobial uses. Chronic exposure or ingestion, such as in argyria, can lead to permanent blue-gray skin discoloration, as historically seen in workers from the silvering industry. While colloidal preparations have been marketed as alternative medicines, agencies like the Food and Drug Administration have taken action against fraudulent health claims. Environmental release, particularly from mining operations like those historically in the Rio Tinto, can be toxic to aquatic life.
Category:Chemical elements Category:Transition metals Category:Precious metals