Strontium

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Strontium is a chemical element in the periodic table that has the symbol Sr and the atomic number 38. An alkaline earth metal, strontium is a soft silver-white or yellowish metallic element that is highly reactive chemically. This metal turns yellow when exposed to air and occurs in celestite and strontianite. Sr-90 is present in radioactive fallout and has a half-life of 28 years.

Properties
General
Name, Symbol, NumberStrontium, Sr, 38
Seriesalkaline earth metal
Group, Period, Block2 (II), 5, s
Density, Hardness2630 kg/m3, 1.5
Appearancesilvery white metalic
Atomic
Atomic weight87.62 amu
Atomic radius219 pm
Covalent radius192 pm
van der Waals radiusno information
Electron configuration [Kr]5s2
e- 's per energy level2, 8, 18, 8, 2
Oxidation states (Oxide)2 (strong base)
Crystal structureCubic face centered
Physical
State of mattersolid (nonmagnetic)
Melting point1050 K (1431 °F)
Boiling point1655 K (2520 °F)
Molar volume33.94 ×10-3 m3/mol
Heat of vaporization 144 kJ/mol
Heat of fusion8.3 kJ/mol
Vapor pressure246 Pa at 1042 K
Velocity of sounddata not available
Miscellaneous
Electronegativity0.95 (Pauling scale)
Specific heat capacity300 J/kg-K
Electrical conductivity7.62 106/m ohm
Thermal conductivity 35.3 W/m-K
1st ionization potential 549.5 kJ/mol
2nd ionization potential1064.2 kJ/mol
3rd ionization potential4138 kJ/mol
Most Stable Isotopes
isoNAhalf-life DMDE MeV DP
84Sr0.56%Strontium is stable with 46 neutrons
86Sr9.86%Sr is stable with 48 neutrons
87Sr7.0%Sr is stable with 49 neutrons
88Sr82.58%Sr is stable with 50 neutrons
90Sr{syn.}28.78 ybeta-0.54690Y
SI units & STP are used except where noted.

Notable Characteristics
Always naturally occurring combined, as in the minerals strontianite, celestite, etc. It is isolated as a yellowish metal and is somewhat malleable. It is chiefly employed (as in the nitrate) to color pyrotechnic flames red.

Strontium is a bright silvery metal that is softer than calcium and even more reactive in water; strontium will decompose on contact to produce strontium hydroxide and hydrogen gas. It burns in air to produce both strontium oxide and strontium nitride, but since it does not react with nitrogen below 380°C it will only form the oxide spontaneously at room temperature. It should be kept under kerosene to prevent oxidation; freshly exposed strontium metal rapidly turns a yellowish color with the formation of the oxide. Finely powdered strontium metal will ignite spontaneously in air. Volatile strontium salts impart a beautiful crimson color to flames, and these salts are used in pyrotechnics and in the production of flares. Natural strontium is a mixture of four stable isotopes.


Uses
The major use for strontium at present is in producing glass for color television cathode ray tubes. It has also found use in producing ferrite magnets and in refining zinc. Strontium titanate is an interesting optical material as it has an extremely high refractive index and an optical dispersion greater than that of diamond. It has been used as a gemstone, but is very soft and so scratches easily. It does not occur naturally. Strontium is also used in fireworks.

History
Adair Crawford recognized the mineral strontianite, named after the Scottish town of Strontian, as differing from other barium minerals in 1790. However, Klaproth and Hope discovered strontium itself in 1798 and metallic strontium was first isolated by Sir Humphry Davy in 1808 using electrolysis.

Sources
Strontium is found chiefly as the form of the sulfate mineral celestite (SrSO4) and the carbonate strontianite (SrCO3). The metal can be prepared by electrolysis of the melted chloride mixed with potassium chloride, or is made by reducing strontium oxide with aluminum in a vacuum at a temperature at which strontium distills off. Three allotropes of the metal exist, with transition points at 235 and 540°C. Strontium metal (98% pure) in January 1990 cost about $5/oz. The largest commercially exploited deposits are found in England.

Isotopes
The alkali earth metal strontium has four stable, naturally occurring isotopes: 84Sr (0.56%), 86Sr (9.86%), 81Sr (7.0%) and 88Sr (82.58%). Only 87Sr is radiogenic; it is produced by decay from the radioactive alkali metal 87Rb, which has a half-life of 48,800,000 years. Thus, there are two sources of 87Sr in any material: that formed during primordial nucleo-synthesis along with 84Sr, 86Sr and 88Sr, as well as that formed by radioactive decay of 87Rb. The ratio 87Sr/86Sr is the parameter typically reported in geologic investigations. Because strontium has an atomic radius similar to that of Ca, it readily substitutes for Ca in minerals. 87Sr/86Sr ratios in minerals and rocks have values ranging from about 0.7 to greater than 4.0.

Sixteen unstable isotopes are known to exist. Of greatest importance is 90Sr with a half-life of 29 years. It is a product of nuclear fallout and presents a health problem since it substitutes for calcium in bone, preventing expulsion from the body. This isotope is one of the best long-lived high-energy beta emitters known, and is used in SNAP (Systems for Nuclear Auxilliary Power) devices. These devices hold promise for use in spacecraft, remote weather stations, navigational buoys, etc., where a lightweight, long-lived, nuclear-electric power source is needed.

Precautions

Sources and external links
Los Alamos National Laboratory - Strontium
WebElements.com - Strontium
EnvironmentalChemistry.com - Strontium