The mineralogy of Silicon
General Properties | |
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Symbol: | Si |
Atomic Number: | 14 |
Standard atomic weight (Ar): | 28.0855(3) |
Electron configuration: | [Ne] 3s2 3p2 |
Photos | ||
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< | Ultrapure silicon chunks | > |
Atomic Properties | |
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Electronegativity (Pauling scale): | 1.9 |
Atomic Radius: | 111 pm |
Ionic Radius: | 40 pm (+4) |
Van der Waals Radius: | 210 pm |
1st Ionization energy: | 787 kJ/mol |
1st Electron affinity: | -134 kJ/mol |
Oxidation States: | -4,-3,-2,-1,1,2,3,4 |
Physical Properties | |
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Standard State: | solid |
Bonding Type: | metallic |
Melting Point: | 1687 K |
Boiling Point: | 3173 K |
Density: | 2.33 g/cm3 |
Metal/Non-Metal: | metalloid |
Main isotopes of Silicon | ||||
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Isotope | % in Nature | Half Life | Decay type | Decay product |
28Si | 92.23% | stable | ||
29Si | 4.67% | stable | ||
30Si | 3.1% | stable | ||
32Si | trace | 153y | β− | 32P |
Other Information | |
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Year Discovered: | 1854 |
Discovered By: | |
Year Predicted: | 1787 |
Named For: | From the Latin silex, silicis for flint. |
CPK color coding: | #F0C8A0 |
External Links: | WikipediaWebElementsLos Alamos National LaboratoryTheodore Gray's PeriodicTable.com |
Simple Compounds and Mineral Names | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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Nitrides | trisilicon tetranitride | Si3N4 | +4 | Nierite | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Sulfides | silicon sulphide | SiS2 | +4 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Hydrides | silane | SiH4 | +4 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
disilicon hexahydride | Si2H6 | +3 | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Fluorides | silicon tetrafluoride | SiF4 | +4 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Chlorides | silicon tetrachloride | SiCl4 | +4 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Iodides | silicon tetraiodide | SiI4 | +4 | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Oxides | silicon oxide | SiO2 | +4 | Quartz, Coesite, Cristobalite, Mogánite, Seifertite, Stishovite, Tridymite |
Mineral Diversity of Silicon | |
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1. Elements | 22 valid mineral species |
2. Sulfides And Sulfosalts | 1 valid mineral species |
3. Halides | 9 valid mineral species |
4. Oxides | 22 valid mineral species |
5. Carbonates | 3 valid mineral species |
6. Borates | 5 valid mineral species |
7. Sulfates | 14 valid mineral species |
8. Phosphates, Arsenates, Vanadates | 19 valid mineral species |
9. Silicates | 1600 valid mineral species |
Total: | 1695 valid species containing essential Silicon |
Minerals with the greatest weight % of Silicon | ||
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Silicon | Si | 100.00 % |
Moissanite | SiC | 70.05 % |
Luanshiweiite | KLiAl1.5(Si3.5Al0.5)O10(OH)2 | 61.21 % |
Fluorluanshiweiite | KLiAl1.5(Si3.5Al0.5)O10F2 | 60.85 % |
Nierite | Si3N4 | 60.06 % |
Sinoite | Si2N2O | 56.07 % |
Luobusaite | Fe0.84Si2 | 54.49 % |
Zhiqinite | TiSi2 | 53.99 % |
Linzhiite | FeSi2 | 50.15 % |
Xiexiandeite | SiO2 | 46.74 % |
Geochemistry of Silicon | |
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Goldschmidt classification: | Lithophile |
Si4+ was one of the ions least depleted from the mantle in the formation of the crust. | |
Si4+ enters early-forming phases in igneous rocks. | |
Si4+ is commonly concentrated in residual soils and sediments. | |
Si4+ is one of the eight most abundant solutes in average river water. | |
Si4+ solute can be a limiting nutrient in the oceans. | |
Si4+ is essential to nutrition of at least some vertebrates ('essential minerals'). |
Elemental Silicon in Nature | ||
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Found as native element: | Silicon | Si |
Elemental Abundance for Silicon | ||
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Crust (CRC Handbook) | 2.82 x 10-1 | mass fraction, kg/kg |
Crust (Kaye & Laby) | 2.7 x 10-1 | mass fraction, kg/kg |
Crust (Greenwood) | 2.72000 x 10-1 | mass fraction, kg/kg |
Crust (Ahrens/Taylor) | 2.677 x 10-1 | mass fraction, kg/kg |
Crust (Ahrens/Wänke) | 2.81 x 10-1 | mass fraction, kg/kg |
Crust (Ahrens/Weaver) | 2.95 x 10-1 | mass fraction, kg/kg |
Upper Crust (Ahrens/Taylor) | 3.08 x 10-1 | mass fraction, kg/kg |
Upper Crust (Ahrens/Shaw) | 3.04 x 10-1 | mass fraction, kg/kg |
Sea Water (CRC Handbook) | 2.2 x 10-6 | mass per volume fraction, kg/L |
Sea Water (Kaye & Laby) | 2.9 x 10-6 | mass per volume fraction, kg/L |
The Sun (Kaye & Laby) | 1.0 x 100 | atom mole fraction relative to Si=1 |
Solar System (Kaye & Laby) | 1.0 x 100 | atom mole fraction relative to Si=1 |
Solar System (Ahrens) | 1.0 x 100 (4.4%) | atom mole fraction relative to Si=1 (% uncertainty) |
Element association of Silicon in the Mineral World | |||
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This table compares the known valid mineral species listed listed with Silicon and the other elements listed based on the official IMA formula. Note that unlike other sections on this page this includes non-essential elements. The first data column contains the total number of minerals listed with Silicon and the element listed for that row. The second data column lists this number as a percentage of all minerals listed with Silicon. The final data column compares this percentage against the percentage of all minerals that contain the element listed in each row. Click on a heading to sort. |
Periodic Table | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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Aluminium << Silicon >> Phosphorus |