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Lithium is the chemical element with symbol Li and atomic number 3. It is in group 1 of the periodic table, among the alkali metals and is the lightest solid element. Lithium in its pure form is a soft, silver white metal that tarnishes and oxidizes very rapidly in air and water. It is used primarily in heat-transfer alloys and batteries, and also in some mood stabilizing drugs. Lithium is one of only three elements - and the only metal - created in the first moments of the Big Bang. (The other two elements are hydrogen and helium, which according to cosmologists, were created in much greater abundance than lithium.)
Basic featuresLithium is a soft, silvery metal, so soft that it can be cut with a sharp knife. It is the lightest of all metals and has a density only half that of water. Though in group 1, lithium also exhibits properties of the alkali Earth metals in group 2. Like all alkali metals, it has a single valence electron, and will readily lose this electron to become a positive ion without a full shell, or set of electrons at an energy level. Because of this, lithium reacts easily with water and does not occur freely in nature. Nevertheless, it is less reactive than the chemically similar sodium. When placed over a flame, lithium gives off a striking crimson color but when it burns strongly, the flame becomes a brilliant white. Lithium will ignite and burn when exposed to oxygen and water. It is the only metal that reacts with nitrogen at room temperature. Lithium has a high specific heat capacity, 3582 J/(kg·K), and a great temperature range in its liquid form, which makes it a useful chemical. Lithium in its pure form is highly flammable and slightly explosive when exposed to air and especially water. Lithium fires are difficult to extinguish, requiring special chemicals designed to smother them. Lithium metal is also corrosive and requires special handling to avoid skin contact. Lithium should be stored in a non-reactive compound such as naphtha or a hydrocarbon. Lithium compounds play no natural biological role and are considered to be slightly toxic. When used as a drug, blood concentrations of Li+ must be carefully monitored. ApplicationsBecause of its specific heat, the largest of any solid, lithium is used in heat transfer applications. It is also an important battery anode material due to its high electrochemical potential. In addition to being lighter than the standard dry cell, these batteries produce a higher voltage (3 volts versus 1.5 volts). Other uses:
HistoryPetalite, which contains lithium, was first discovered by the Brazilian scientist José Bonifácio de Andrada e Silva toward the end of the 1700s on a trip to Sweden. Lithium was discovered by Johann Arfvedson in 1817. Arfvedson found the new element within the minerals spodumene and lepidolite in a petalite ore, LiAl(Si2O5)2, he was analyzing during a routine investigation of some minerals from a mine on the island Utö in Sweden. In 1818 Christian Gmelin was the first to observe that lithium salts give a bright red color in flame. Both men tried and failed to isolate the element from its salts. The element was not isolated until William Thomas Brande and Sir Humphrey Davy later used electrolysis on lithium oxide in 1818. Bunsen and Matiessen isolated larger quantities of the metal by electrolysis of lithium chloride in 1855. Commercial production of lithium metal was achieved in 1923 by the German company Metallgesellschaft through using electrolysis of molten lithium chloride and potassium chloride. It was apparently given the name "lithium" (Greek λιθοσ (lithos), meaning "stone") because it was discovered from a mineral while other common alkali metals were first discovered from plant tissue. OccurrenceLithium pellets (covered in white lithium hydroxide)Lithium is widely distributed but does not occur in nature in its free form. Because of its reactivity, it is always found bound with one or more other elements or compounds. It forms a minor part of almost all igneous rocks and is also found in many natural brines. Lithium is the thirty-first most abundant element, contained in trace amounts in the minerals spodumene, lepidolite, and amblygonite. The Earth's crust contains 65 parts per million (ppm) of lithium. Along with hydrogen, helium, and beryllium, some lithium was created in the big bang. Since the end of World War II, lithium production has greatly increased. The metal is separated from other elements in igneous rocks, and is also extracted from the water of mineral springs. Lepidolite, spodumene, petalite, and amblygonite are the more important minerals containing it. In the United States lithium is recovered from brine pools in Nevada.[1] Today, most commercial lithium is recovered from brine sources in Argentina and Chile. The metal, which is silvery in appearance like sodium, potassium and other members of the alkali metal series, is produced electrolytically from a mixture of fused lithium and potassium chloride. There is little market for lithium in its pure metal form and price information is scarce. In 1998 it was about US$ 43 per pound ($95 per kg). [2] Chile is currently the leading pure metal lithium producer in the world. See also Lithium minerals. RegulationSince lithium metal can act as a catalyst in amateur methamphetamine production, some jurisdictions limit the sale of lithium batteries, which are the most readily available source of lithium metal for ordinary consumers. However, the effectiveness of such restrictions in controlling illegal production of methamphetamine remains indeterminate and controversial. Carriage and shipment of some kinds of lithium batteries may be prohibited aboard certain types of transportation (particularly aircraft), because of the ability of most types of lithium batteries to fully discharge very rapidly when short-circuited, leading to overheating and possible explosion. However, most consumer lithium batteries have thermal overload protection built-in to prevent this type of incident, or their design inherently limits short-circuit currents. IsotopesNaturally occurring lithium is composed of 2 stable isotopes 6Li and 7Li with 7Li being the most abundant (92.5% natural abundance). Seven radioisotopes have been characterized with the most stable being 8Li with a half-life of 838 ms and 9Li with a half-life of 178.3 ms. All of the remaining radioactive isotopes have half-lifes that are less than 8.6 ms. The shortest-lived isotope of lithium is 4Li which decays through proton emission and has a half-life of 7.58043x10-23 s. 7Li is one of the primordial elements (produced in Big Bang nucleosynthesis). Lithium isotopes fractionate substantially during a wide variety of natural processes, including mineral formation (chemical precipitation), metabolism, ion exchange (Li substitutes for magnesium and iron in octahedral sites in clay minerals, where 6Li is preferential over 7Li), hyperfiltration, and rock alteration. See also
References
External linksLook up Lithium in Wiktionary, the free dictionary Wikimedia Commons has media related to: Lithium
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