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Polonium is a chemical element with symbol Po and atomic number 84, discovered in 1898 by Marie Curie and Pierre Curie. A rare and highly radioactive element with no stable isotopes, polonium is chemically similar to bismuth and tellurium, and it occurs in uranium ores. Applications of polonium are few. They include heaters in space probes, antistatic devices, and sources of neutrons and alpha particles. Because of its position in the periodic table, polonium is sometimes classified as a metalloid. [3] Other sources say that on the basis of its properties and behavior, it is "unambiguously a metal." Also tentatively called "radium F", polonium was discovered by Marie and Pierre Curie in 1898, and was named after Marie Curie's native land of Poland (Latin: Polonia). Polonium may be the first element named to highlight a political controversy. This element was the first one discovered by the Curies while they were investigating the cause of pitchblende radioactivity. Pitchblende, after removal of the radioactive elements uranium and thorium, was more radioactive than the uranium and thorium combined. This spurred the Curies to search for additional radioactive elements. They first separated out polonium from pitchblende in July 1898, and five months later, also isolated radium. The Atomic Energy Commission and the Manhattan Project funded human experiments using polonium on 5 people at the University of Rochester between 1943 and 1947. The people were administered between 9 and 22 microcuries (330 and 810 kBq) of polonium to study its excretion. Polonium has 33 known isotopes, all of which are radioactive. They have atomic masses that range from 188 to 220 u. 210 Po (half- life 138.376 days) is the most widely available. The longer-lived 209 Po (half-life 125.2 ± 3.3 years, longest-lived of all polonium isotopes) [2] and 208 Po (half-life 2.9 years) can be made through the alpha, proton, or deuteron bombardment of lead or bismuth in a cyclotron. [5]

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Polonium is a chemical element with symbol Po and atomic number 84, discovered in 1898 by Marie Curie and Pierre Curie. A rare and highly radioactive element with no stable isotopes, polonium is chemically similar to bismuth and tellurium, and it occurs in uranium ores. Applications of polonium are few. They include heaters in space probes, antistatic devices, and sources of neutrons and alpha particles. Because of its position in the periodic table, polonium is sometimes classified as a metalloid.[3] Other sources say that on the basis of its properties and behavior, it is "unambiguously a metal."Also tentatively called "radium F", polonium was discovered by Marie and Pierre Curie in 1898, and was named after Marie Curie's native land of Poland (Latin: Polonia). Polonium may be the first element named to highlight a political controversy.This element was the first one discovered by the Curies while they were investigating the cause of pitchblende radioactivity. Pitchblende, after removal of the radioactive elements uranium and thorium, was more radioactive than the uranium and thorium combined. This spurred the Curies to search for additional radioactive elements. They first separated out polonium from pitchblende in July 1898, and five months later, also isolated radium. The Atomic Energy Commission and the Manhattan Project funded human experiments using polonium on 5 people at the University of Rochester between 1943 and 1947. The people were administered between 9 and 22 microcuries (330 and 810kBq) of polonium to study its excretion. Polonium has 33 known isotopes, all of which are radioactive. They have atomic masses that range from 188 to 220 u. 210Po (half-life 138.376days) is the most widely available. The longer-lived 209Po (half-life 125.2 3.3 years, longest-lived of all polonium isotopes)[2] and 208Po (half-life 2.9years) can be made through the alpha, proton, or deuteron bombardment of lead or bismuth in a cyclotron.[5]210Po is an alpha emitter that has a half-life of 138.4days; it decays directly to its stable daughter isotope, 206Pb. A milligram (5curies) of 210Po emits about as many alpha particles per second as 5grams of 226Ra.[6] A few curies (1curie equals 37gigabecquerels, 1Ci = 37GBq) of 210Po emit a blue glow which is caused by excitation of surrounding air.About one in 100,000alpha emissions causes an excitation in the nucleus which then results in the emission of a gamma ray with a maximum energy of 803keVPolonium is a radioactive element that exists in two metallic allotropes. The alpha form is the only known example of a simple cubic crystal structure in a single atom basis, with an edge length of 335.2 picometers; the beta form is rhombohedral.[9][10][11] The structure of polonium has been characterized by X-ray diffraction[12][13] and electron diffraction.[14]210Po (in common with 238Pu) has the ability to become airborne with ease: if a sample is heated in air to 55C (131F), 50% of it is vaporized in 45 hours to form diatomic Po2 molecules, even though the melting point of polonium is 254C (489F) and its boiling point is 962C (1,764F).[15][16][1] More than one hypothesis exists for how polonium does this; one suggestion is that small clusters of polonium atoms are spalled off by the alpha decay.ChemistryThe chemistry of polonium is similar to that of tellurium and bismuth. Polonium dissolves readily in dilute acids, but is only slightly soluble in alkalis. Polonium solutions are first colored in pink by the Po2+ ions, but then rapidly become yellow because alpha radiation from polonium ionizes the solvent and converts Po2+ into Po4+. This process is accompanied by bubbling and emission of heat and light by glassware due to the absorbed alpha particles; as a result, polonium solutions are volatile and will evaporate within days unless sealed.[17][18]CompoundsPolonium has no common compounds, and almost all of its compounds are synthetically created; more than 50 of those are known.[19] The most stable class of polonium compounds are polonides, which are prepared by direct reaction of two elements. Na2Po has the antifluorite structure, the polonides of Ca, Ba, Hg, Pb and lanthanides form a NaCl lattice, BePo and CdPo have the wurtzite and MgPo the nickel arsenide structure. Most polonides decompose upon heating to about 600C, except for HgPo that decomposes at ~300C and the lanthanide polonides, which do not decompose but melt at temperatures above 1000C. For example PrPo melts at 1250C and TmPo at 2200C.[20] PbPo is one of the very few naturally occurring polonium compounds, as polonium alpha decays to form lead.[21]Polonium hydride (PoH2) is a volatile liquid at room temperature prone to dissociation.[20] The two oxides PoO2 and PoO3 are the products of oxidation of polonium.[22]Halides of the structure PoX2, PoX4 and PoX6 are known. They are soluble in the corresponding hydrogen halides, i.e., PoClX in HCl, PoBrX in HBr and PoI4 in HI.[23] Polonium dihalides are formed by direct reaction of the elements or by reduction of PoCl4 with SO2 and with PoBr4 with H2S at room temperature. Tetrahalides can be obtained by reacting polonium dioxide with HCl, HBr or HI.[24]Other polonium compounds include acetate, bromate, carbonate, citrate, chromate, cyanide, formate, hydroxide, nitrate, selenate, monosulfide, sulfate and disulfate.Krypton (from Greek: kryptos "the hidden one") is a chemical element with symbolKr and atomic number36. It is a member of group 18 (noble gases) elements. A colorless, odorless, tasteless noble gas, krypton occurs in trace amounts in the atmosphere, is isolated by fractionally distilling liquefied air, and is often used with other rare gases in fluorescent lamps. Krypton is inert for most practical purposes.A whitish, largely inert gaseous element used chiefly in gas discharge lamps and fluorescent lamps. Solid krypton is a white crystalline substance with a face-centered cubic structure which is common to all the 'rare gases'. The Atomic Number of this element is 36 and the Element Symbol is Kr.Krypton, like the other noble gases, can be used in lighting and photography. Krypton light has a large number of spectral lines, and krypton's high light output in plasmas allows it to play an important role in many high-powered gas lasers (krypton ion and excimer lasers), which pick out one of the many spectral lines to amplify. There is also a specific krypton fluoride laser. The high power and relative ease of operation of krypton discharge tubes caused (from 1960 to 1983) the official length of a meter to be defined in terms of the wavelength of the 605nm (orange) spectral line of krypton-86.Krypton was discovered in Britain in 1898 by Sir William Ramsay, a Scottish chemist, and Morris Travers, an English chemist, in residue left from evaporating nearly all components of liquid air. Neon was discovered by a similar procedure by the same workers just a few weeks later.[5] William Ramsay was awarded the 1904 Nobel Prize in Chemistry for discovery of a series of noble gases, including krypton.In 1960, the International Conference on Weights and Measures defined the meter as 1,650,763.73 wavelengths of light emitted by the krypton-86 isotope.[6][7] This agreement replaced the 1889 international prototype meter located in Paris, which was a metal bar made of a platinum-iridium alloy (one of a series of standard meter bars, originally constructed to be one ten-millionth of a quadrant of the Earth's polar circumference). This also obsoleted the 1927 definition of the ngstrm based on the red cadmium spectral line,[8] replacing it with 1 = 1010m. The krypton-86 definition lasted until the October 1983 conference, which redefined the meter as the distance that light travels in a vacuum during 1/299,792,458s.[9][10][11]CharacteristicsKrypton is characterized by several sharp emission lines (spectral signatures) the strongest being green and yellow.[12] It is one of the products of uranium fission.[13] Solidified krypton is white and crystalline with a face-centered cubic crystal structure, which is a common property of all noble gases (except helium, with a hexagonal close-packed crystal structure).IsotopesMain article: Isotopes of kryptonNaturally occurring krypton is made of six stable isotopes. In addition, about thirty unstable isotopes and isomers are known.[14] 81Kr, the product of atmospheric reactions, is produced with the other naturally occurring isotopes of krypton. Being radioactive, it has a half-life of 230,000 years. Krypton is highly volatile when it is near surface waters but 81Kr has been used for dating old (50,000800,000 years) groundwater.[15]85Kr is an inert radioactive noble gas with a half-life of 10.76 years. It is produced by the fission of uranium and plutonium, such as in nuclear bomb testing and nuclear reactors. 85Kr is released during the reprocessing of fuel rods from nuclear reactors. Concentrations at the North Pole are 30% higher than at the South Pole due to convective mixing.[16]ChemistryLike the other noble gases, krypton is highly chemically unreactive. However, following the first successful synthesis of xenon compounds in 1962, synthesis of krypton difluoride (KrF2) was reported in 1963. In fact, before the 1960s, no noble gas compounds had been discovered.[17] Under extreme conditions, krypton reacts with fluorine to form KrF2 according to the following equation:Kr + F2 KrF2In the same year, KrF4 was reported by Grosse, et al.,[18] but was subsequently shown to be a mistaken identification.[19] There are also unverified reports of a barium salt of a krypton oxoacid.[20] ArKr+ and KrH+ polyatomic ions have been investigated and there is evidence for KrXe or KrXe+.[21]Compounds with krypton bonded to atoms other than fluorine have also been discovered. The reaction of KrF2 with B(OTeF5)3 produces an unstable compound, Kr(OTeF5)2, that contains a krypton-oxygen bond. A krypton-nitrogen bond is found in the cation [HCNKrF]+, produced by the reaction of KrF2 with [HCNH]+[AsF6] below 50C.[22][23] HKrCN and HKrCCH (krypton hydride-cyanide and hydrokryptoacetylene) were reported to be stable up to 40 K.Lead (/ld/) is a chemical element in the carbon group with symbolPb (from Latin: plumbum) and atomic number82. Lead is a soft, malleable and heavy post-transition metal. Metallic lead has a bluish-white color after being freshly cut, but it soon tarnishes to a dull grayish color when exposed to air. Lead has a shiny chrome-silver luster when it is melted into a liquid. It is also one of the heaviest non-radioactive elements.Lead is used in building construction, lead-acid batteries, bullets and shot, weights, as part of solders, pewters, fusible alloys, and as a radiation shield. Lead has the highest atomic number of all of the stable elements, although the next higher element, bismuth, has one isotope with a half-life that is so long (over one billion times the estimated age of the universe) that it can be considered stable. Lead's four stable isotopes have 82 protons, a magic number in the nuclear shell model of atomic nuclei. The isotope lead-208 also has 126 neutrons, another magic number, and is hence double magic, a property that grants it enhanced stability: lead-208 is the heaviest known stable isotope.If ingested, lead is poisonous to animals and humans, damaging the nervous system and causing brain disorders. Excessive lead also causes blood disorders in mammals. Like the element mercury, another heavy metal, lead is a neurotoxin that accumulates both in soft tissues and the bones. Lead poisoning has been documented from ancient Rome, ancient Greece, and ancient China.

CharacteristicsLead is a bright and silvery metal with a very slight shade of blue in a dry atmosphere.[1] Upon contact with air, it begins to tarnish by forming a complex mixture of compounds depending on the conditions. The color of the compounds can vary. The tarnish layer can contain significant amounts of carbonates and hydroxycarbonates.[2][3] Lead's characteristic properties include high density, softness, ductility and malleability, poor electrical conductivity compared to other metals, high corrosion resistance, and ability to react with organic chemicals.[1]Various traces of other metals change its properties significantly: the addition of small amounts of antimony or copper to lead increases the alloy's hardness and improves corrosion resistance to sulfuric acid.[1] Some other metals, such as cadmium, tin, and tellurium, also improve hardness and fight metal fatigue. Sodium and calcium also have this ability, but they reduce the alloy's chemical stability.[1] Finally, zinc and bismuth simply impair the corrosion resistance (0.1% bismuth content is the industrial usage threshold).[1] Conversely, lead impurities mostly worsen the quality of industrial materials, although there are exceptions: for example, small amounts of lead improve the ductility of steel.[1]Lead has only one common allotrope, which is face-centered cubic, with the leadlead distance being 349pm.[4] At 327.5C (621.5F),[5] lead melts; the melting point is above that of tin (232C, 449.5F),[5] but significantly below that of germanium (938C, 1721F).[6] The boiling point of lead is 1749C (3180F),[7] which is below those of both tin (2602C, 4716F)[5] and germanium (2833C, 5131F).[6] Densities increase down the group: the Ge and Sn values (5.23[8] and 7.29gcm3,[9] respectively) are significantly below that of lead: 11.32gcm3.[8]A lead atom has 82 electrons, having an electronic configuration of [Xe]4f145d106s26p2. In its compounds, lead (unlike the other group 14 elements) most commonly loses its two and not four outermost electrons, becoming lead(II) ions, Pb2+. Such unusual behavior is rationalized by considering the inert pair effect, which occurs because of the stabilization of the 6s-orbital due to relativistic effects, which are stronger closer to the bottom of the periodic table.[10] Tin shows a weaker such effect: tin(II) is still a reducer.[10]The figures for electrode potential show that lead is only slightly easier to oxidize than hydrogen. Lead thus can dissolve in acids, but this is often impossible due to specific problems (such as the formation of insoluble salts).[11] Powdered lead burns with a bluish-white flame. As with many metals, finely divided powdered lead exhibits pyrophoricity.[12] Toxic fumes are released when lead is burned.Isotopes[edit]Main article: Isotopes of leadLead occurs naturally on Earth exclusively in the form of four isotopes: lead-204, -206, -207, and -208.[13] All four can be radioactive as the hypothetical alpha decay of any would be exothermic, but the lower half-life limit has been put only for lead-204: over 1.41017years.[14] This effect is, however, so weak that natural lead poses no radiation hazard. Three isotopes are also found in three of the four major decay chains: lead-206, -207 and -208 are final decay products of uranium-238, uranium-235, and thorium-232, respectively. Since the amounts of them in nature depend also on other elements' presence, the isotopic composition of natural lead varies by sample: in particular, the relative amount of lead-206 varies between 20.84% and 27.78%.[13]Aside from the stable ones, thirty-four radioisotopes have been synthesized: they have mass numbers of 178215.[14] Lead-205 is the most stable radioisotope of lead, with a half-life of over 107years. 47 nuclear isomers (long-lived excited nuclear states), corresponding to 24 lead isotopes, have been characterized. The most long-lived isomer is lead-204m2 (half-life of about 1.1hours).[14]Chemical reactivity[edit]Lead is classified as a post-transition metal and is also a member of the carbon group. Massive lead forms a protective oxide layer, but finely powdered highly purified lead can ignite in air. Melted lead is oxidized in air to lead monoxide. All chalcogens oxidize lead upon heating.[15]Fluorine does not oxidize cold lead. Hot lead can be oxidized, but the formation of a protective halide layer lowers the intensity of the reaction above 100C (210F). The reaction with chlorine is similar: thanks to the chloride layer, lead persistence against chlorine surpasses that of copper or steel up to 300C (570F).[15]Water in the presence of oxygen attacks lead to start an accelerating reaction. The presence of carbonates or sulfates results in the formation of insoluble lead salts, which protect the metal from corrosion. So does carbon dioxide, as the insoluble lead carbonate is formed; however, an excess of the gas leads to the formation of the soluble bicarbonate, which makes the use of lead pipes dangerous.[11] Lead dissolves in organic acids (in the presence of oxygen) and concentrated (80%) sulfuric acid thanks to complexation; however, it is only weakly affected by hydrochloric acid and is stable against hydrofluoric acid, as the corresponding halides are weakly soluble. Lead also dissolves in quite concentrated alkalis (10%) because of the amphoteric character and solubility of plumbites.[11]Compounds[edit]Lead compounds exist mainly in two main oxidation states, +2 and +4. The former is more common. Inorganic lead(IV) compounds are typically strong oxidants or exist only in highly acidic solutions.[