(Àtúnjúwe láti Silicon)

Sílíkọ́nù, a tetravalent metalloid, is a chemical element with the symbol Si and atomic number 14. It is less reactive than its chemical analog carbon, the nonmetal directly above it in the periodic table, but more reactive than germanium, the metalloid directly below it in the table. Controversy about silicon's character dates to its discovery: silicon was first prepared and characterized in pure form in 1823. In 1808, it was given the name silicium (from Látìnì: silicis, flints), with an -ium word-ending to suggest a metal, a name which the element retains in several non-English languages. However, its final English name, first suggested in 1817, reflects the more physically similar elements carbon and boron.

Sílíkọ́nù, 14Si
Àdàkọ:Infobox element/symbol-to-top-image/alt
Ìhànsójúcrystalline, reflective with bluish-tinged faces
Ìwúwo átọ̀mù Ar, std(Si)[28.08428.086] conventional: 28.085
nọ́mbà ìsújọSi:
Sílíkọ́nù ní orí tábìlì àyè
Hydrogen Helium
Lithium Beryllium Boron Carbon Nitrogen Oxygen Fluorine Neon
Sodium Magnesium Aluminium Silicon Phosphorus Sulfur Chlorine Argon
Potassium Calcium Scandium Titanium Vanadium Chromium Manganese Iron Cobalt Nickel Copper Zinc Gallium Germanium Arsenic Selenium Bromine Krypton
Rubidium Strontium Yttrium Zirconium Niobium Molybdenum Technetium Ruthenium Rhodium Palladium Silver Cadmium Indium Tin Antimony Tellurium Iodine Xenon
Caesium Barium Lanthanum Cerium Praseodymium Neodymium Promethium Samarium Europium Gadolinium Terbium Dysprosium Holmium Erbium Thulium Ytterbium Lutetium Hafnium Tantalum Tungsten Rhenium Osmium Iridium Platinum Gold Mercury (element) Thallium Lead Bismuth Polonium Astatine Radon
Francium Radium Actinium Thorium Protactinium Uranium Neptunium Plutonium Americium Curium Berkelium Californium Einsteinium Fermium Mendelevium Nobelium Lawrencium Rutherfordium Dubnium Seaborgium Bohrium Hassium Meitnerium Darmstadtium Roentgenium Copernicium Nihonium Flerovium Moscovium Livermorium Tennessine Oganesson


Nọ́mbà átọ̀mù (Z)14
Ẹgbẹ́group 14 (carbon group)
Àyèàyè 3
Ẹ̀ka ẹ́límẹ́ntìÀdàkọ:Infobox element/category format
Ìtò ẹ̀lẹ́ktrọ́nùÀdàkọ:Infobox element/symbol-to-electron-configuration
Iye ẹ̀lẹ́ktrọ́nù lórí ìpele kọ̀ọ̀kan2, 8, 4
Àwọn ohun ìní ara
Ìfarahàn at STPsolid
Ìgbà ìyọ́1687 K ​(1414 °C, ​2577 °F)
Ígbà ìhó3538 K ​(3265 °C, ​5909 °F)
Kíki (near r.t.)2.3290 g/cm3
when liquid (at m.p.)2.57 g/cm3
Heat of fusion50.21 kJ/mol
Heat of 359 kJ/mol
Molar heat capacity19.789 J/(mol·K)
Atomic properties
Oxidation statesÀdàkọ:Infobox element/symbol-to-oxidation-state
ElectronegativityPauling scale: 1.90
Atomic radiusempirical: 111 pm
Covalent radius111 pm
Van der Waals radius210 pm
Àdàkọ:Infobox element/spectral lines
Other properties
Natural occurrenceÀdàkọ:Infobox element/symbol-to-occurrence
Crystal structureÀdàkọ:Infobox element/crystal structure
Speed of sound thin rod8433 m/s (at 20 °C)
Thermal expansion2.6 µm/(m·K) (at 25 °C)
Thermal conductivity149 W/(m·K)
Electrical resistivity103[1] Ω·m (at 20 °C)
Magnetic orderingdiamagnetic[2]
Young's modulus130-188[3] GPa
Shear modulus51-80[3] GPa
Bulk modulus97.6[3] GPa
Poisson ratio0.064 - 0.28[3]
Mohs hardness7
CAS Number7440-21-3
PredictionAntoine Lavoisier (1787)
DiscoveryJöns Jacob Berzelius[4][5] (1824)
First isolationJöns Jacob Berzelius (1824)
Named byThomas Thomson (1831)
Main isotopes of sílíkọ́nù
Àdàkọ:Infobox element/isotopes table
| references

Silicon is the eighth most common element in the universe by mass, but very rarely occurs as the pure free element in nature. It is most widely distributed in dusts, sands, planetoids, and planets as various forms of silicon dioxide (silica) or silicates. Over 90% of the Earth's crust is composed of silicate minerals, making silicon the second most abundant element in the Earth's crust (about 28% by mass) after oxygen.[7]

Most silicon is used commercially without being separated, and indeed often with little processing of compounds from nature. These include direct industrial building-use of clays, silica sand and stone. Silica is used in ceramic brick. Silicate goes into Portland cement for mortar and stucco, and when combined with silica sand and gravel, to make concrete. Silicates are also in whiteware ceramics such as porcelain, and in traditional quartz-based soda-lime glass. More modern silicon compounds such as silicon carbide form abrasives and high-strength ceramics. Silicon is the basis of the ubiquitous synthetic silicon-based polymers called silicones.

Elemental silicon also has a large impact on the modern world economy. Although most free silicon is used in the steel refining, aluminum-casting, and fine chemical industries (often to make fumed silica), the relatively small portion of very highly purified silicon that is used in semiconductor electronics (< 10%) is perhaps even more critical. Because of wide use of silicon in integrated circuits, the basis of most computers, a great deal of modern technology depends on it.

Silicon is an essential element in biology, although only tiny traces of it appear to be required by animals,[8] however various sea sponges as well as microorganisms like diatoms need silicon in order to have structure. It is much more important to the metabolism of plants, particularly many grasses.


  1. Physical Properties of Silicon. New Semiconductor Materials. Characteristics and Properties. Ioffe Institute
  2. Magnetic susceptibility of the elements and inorganic compounds, in Àdàkọ:RubberBible86th
  3. 3.0 3.1 3.2 3.3 [1] Hopcroft, et al., "What is the Young's Modulus of Silicon?" IEEE Journal of Microelectromechanical Systems, 2010
  4. Weeks, Mary Elvira (1932). "The discovery of the elements: XII. Other elements isolated with the aid of potassium and sodium: beryllium, boron, silicon, and aluminum". Journal of Chemical Education: 1386–1412. 
  5. Voronkov, M. G. (2007). "Silicon era". Russian Journal of Applied Chemistry 80 (12): 2190. doi:10.1134/S1070427207120397. 
  6. Ram, R. S. et al. (1998). "Fourier Transform Emission Spectroscopy of the A2D–X2P Transition of SiH and SiD". J. Mol. Spectr. 190: 341–352. PMID 9668026. http://bernath.uwaterloo.ca/media/184.pdf. 
  7. Nave, R. Abundances of the Elements in the Earth's Crust, Georgia State University
  8. Nielsen, FH (1984). "Ultratrace Elements in Nutrition". Annual Review of Nutrition 4: 21–41. doi:10.1146/annurev.nu.04.070184.000321. PMID 6087860.