Generated by DeepSeek V3.2| polonium | |
|---|---|
| Name | polonium |
| Number | 84 |
| Category | post-transition metal |
| Group | 16 |
| Appearance | silvery |
| Atomic weight | [209] |
| Electron configuration | [Xe] 4f14 5d10 6s2 6p4 |
| Phase | solid |
| Melting point | 254 °C |
| Boiling point | 962 °C |
| Density | 9.196 g/cm3 |
| Oxidation states | −2, +2, +4, +6 |
| Crystal structure | monoclinic |
polonium is a rare, highly radioactive chemical element with no stable isotopes. It was discovered in 1898 by Marie Curie and Pierre Curie during their pioneering research on pitchblende from the Joachimsthal mines. The element was named in honor of Marie Curie's native land of Poland, which was then partitioned between the Russian Empire, the Kingdom of Prussia, and the Austro-Hungarian Empire. All of its isotopes are unstable and decay into other elements, primarily through alpha decay, making it both a significant scientific curiosity and a potent hazard.
Polonium is a volatile, silvery-gray metal that exhibits characteristics of both metals and nonmetals, sharing some chemical similarities with its periodic table neighbors tellurium and bismuth. It is uniquely radioactive, generating considerable heat from its own decay; a single gram can reach temperatures over 500 °C. The element readily dissolves in dilute acids and forms compounds such as polonium dioxide and polonium tetrachloride. Its intense radioactivity causes rapid damage to its own crystal lattice and induces a blue glow in surrounding air from excitation of nitrogen molecules. Studies at institutions like the Lawrence Berkeley National Laboratory have detailed its complex allotropic forms and electrochemical behavior.
The discovery followed the isolation of uranium and thorium, when the Curies noticed residual radioactivity in processed ore samples from Bohemia. Using meticulous fractional crystallization techniques at the École supérieure de physique et de chimie industrielles de la Ville de Paris, they separated a new element, which Marie Curie named in a covert act of political defiance. Its first isolation in metallic form was achieved in 1910 by Curie and the French chemist André-Louis Debierne. Later, during the Manhattan Project, its potential as a neutron initiator in atomic bomb designs was explored at facilities like Los Alamos National Laboratory. Its notoriety increased dramatically in 2006 when it was used in the poisoning of Alexander Litvinenko in London.
Naturally, it is found only in trace amounts as a decay product in uranium-238 and thorium-232 mineral chains, with concentrations rarely exceeding 0.1 milligrams per ton of uraninite ore. Minute quantities exist in tobacco plants due to uptake from soil and phosphate fertilizers containing radium-226. For practical use, it is produced artificially by irradiating bismuth-209 with neutrons in nuclear reactors, a process pioneered at sites like the Oak Ridge National Laboratory. The resulting bismuth-210 decays via beta decay into the most commonly used isotope. Subsequent chemical separation, often via dry distillation or ion exchange, is required due to the extreme radiation hazards.
All known isotopes are radioactive, with mass numbers ranging from 186 to 227. The most readily available isotope, with a half-life of 138.376 days, decays to stable lead-206 by emitting a 5.3 MeV alpha particle. Another isotope, with a half-life of just 0.15 seconds, is used in research for its short-lived properties. The isotope, produced in reactors, is a common alpha source. Studies of its decay chains have been crucial for understanding nuclear structure and were integral to early work at the Cavendish Laboratory under Ernest Rutherford.
Its primary use is as a compact, potent source of alpha particles in industrial and research settings. It was historically used in devices such as antistatic brushes for neutralizing dust on photographic film and in textile mills. In space exploration, it served as a heat source in radioisotope thermoelectric generators for early Soviet Lunokhod rovers. Its ability to induce radioluminescence when alloyed with beryllium made it a component in some nuclear weapon initiators. More recently, its applications have shifted to specialized laboratory instruments for calibrating particle detectors and in studies of chemical bonding under extreme conditions.
It is exceptionally hazardous, with a specific activity orders of magnitude greater than plutonium or radium. Ingestion, inhalation, or absorption of even microgram quantities can be fatal due to intense ionizing radiation that causes severe damage to soft tissue and bone marrow. The 2006 incident involving Alexander Litvinenko demonstrated its potency as a poison. Handling requires stringent radiation protection protocols, specialized gloveboxes, and constant air monitoring, as practiced at facilities like the Institut Laue-Langevin. Its environmental mobility is low, but contamination events necessitate complex decontamination procedures overseen by bodies such as the International Atomic Energy Agency.
Category:Chemical elements Category:Post-transition metals Category:Radioactive elements