Silicon

Aluminum - Silicon - Phosphorus
C Si Ge
	Full table

General

Name, Symbol, Number

Silicon, Si, 14

Series

metalloid

Group, Period, Block

14 (IVA), 3, p

Density, Hardness

2330 kg/m³, 6.5

Appearance

dark grey, bluish tinge

Atomic Properties

Atomic weight

28.0855 amu

Atomic radius (calc.)

110 (111)pm

Covalent radius

111 pm

van der Waals radius

210 pm

Electron configuration

[Ne]33 s² 3p²

e^- 's per energy level

2, 8, 4

Oxidation states (Oxide)

4 (amphoteric)

Crystal structure

Cubic face centered

Physical Properties

State of matter

solid (nonmagnetic)

Melting point

1687 K (2577 �F)

Boiling point

3173 K (5252 �F)

Molar volume

12.06 ×1010^-3 m³/mol

Heat of vaporization

384.22 kJ/mol

Heat of fusion

50.55 kJ/mol

Vapor pressure

4.77 Pa at 1683 K

Speed of sound

__ m/s at __ K

Miscellaneous

Electronegativity

1.90 (Pauling scale)

Specific heat capacity

700 J/(kg*K)

Electrical conductivity

2.52 10^-4/m ohm

Thermal conductivity

148 W/(m*K)

1^st ionization potential

786.5 kJ/mol

2^nd ionization potential

1577.1 kJ/mol

3^rd ionization potential

3231.6 kJ/mol

4^th ionization potential

4355.5 kJ/mol

5^th ionization potential

16091 kJ/mol

6^th ionization potential

19805 kJ/mol

7^th ionization potential

23780 kJ/mol

8^th ionization potential

29287 kJ/mol

9^th ionization potential

33878 kJ/mol

10^th ionization potential

38726 kJ/mol

Most Stable Isotopes

iso	NA	half-life	DM	DE M eV	DP
²⁸Si	92.23%	Si is stable with 14 neutrons
²⁹Si	4.67%	Si is stable with 15 neutrons
³⁰Si	3.1%	Si is stable with 16 neutrons
³²Si	{syn}	276 y	Beta^-	0.224	³²P

SI units & STP are used except where noted.

Silicon is a chemical element in the periodic table that has the symbol Si and atomic number 14. A tetravalent metalloid, silicon is less reactive than its chemical analog carbon. It is the second most abundant element in the Earth's crust, making up 25.7% of it by weight. It occurs in clay, feldspar, granite, quartz and sand, mainly in the form of silicon dioxide (also known as silica) and silicates (compounds containing silicon, oxygen and metals). Silicon is the principal component of glass, semiconductors, cement, ceramics and silicones, the latter a plastic substance often confused with silicon.

Table of contents

1 Notable Characteristics
2 Applications
3 History
4 Occurrence
5 Production
6 Purification

6.1 Physical methods
6.2 Chemical methods

7 Crystallization
8 Isotopes
9 Precautions
10 Miscellaneous Information
11 External Links

Notable Characteristics

In its crystalline form, silicon has a metallic luster and a grayish color. Even though it is a relatively inert element, silicon still reacts with halogens and dilute alkalis, but most acids, (except for hydrofluoric acid) do not affect it. Elemental silicon transmits more than 95% of all wavelengths of infrared light.

Applications

Silicon is a very useful element that is vital to many human industries. Silicon dioxide in the form of sand and clay is an important ingredient of concrete and brick and is also used to produce Portland cement. Silicon is a very important element for plant and animal life. Diatoms extract silica from water to build their protective cell walls. Other uses:

It is a refractory material used in high-temperature material production and its silicates are used in making enamels and pottery.
Silicon is an important constituent of some steels.
Silica from sand is a principal component of glass. Glass can be made into a great variety of shapes and is used to make window glass, containers, and insulators, among many other uses.
Silicon carbide is one of the most important abrasives.
Ultrapure silicon can be doped with arsenic, boron, gallium, or phosphorus to make silicon more conductive for use in transistors, solar cells and other semiconductor devices which are used in electronics and other high-tech applications.
Silicon can be used in lasers to produce coherent light with a wavelength of 4560 angstroms.
Silicones are flexible compounds containing silicon-oxygen and silicon-carbon bonds; they are widely used in applications such as artificial breast implants and contact lenses.
Hydrogenated amorphous silicon has shown promise in the production of low-cost, large-area electronics and solar cells.
Silica is a major ingredient in bricks because of its low chemical activity.

History

Silicon (Latin silex, silicis meaning flint) was first identified by Antoine Lavoisier in 1787, and was later mistaken by Humphry Davy in 1800 for a compound. In 1811 Gay Lussac and Thenard probably prepared impure amorphous silicon through the heating of potassium with silicon tetrafluoride. In 1824 Berzelius prepared amorphous silicon using approximately the same method of Lussac. Berzelius also purified the product by repeatedly washing it.

Occurrence

Silicon is a principal component of aerolites which are a class of meteoroids and also of tektites which is a natural form of glass.

Measured by weight, silicon makes up 25.7% of the earth's crust and after oxygen is also the second most abundant element. Elemental silicon is not found in nature. It occurrs most often as oxides and as silicates. Sand, amethyst, agate, quartz, rock crystal, flint, jasper, and opal are some of the forms in which the oxide appears. Granite, asbestos, feldspar, clay, hornblende, and mica are a few of the many silicate minerals.

Production

Silicon is commercially prepared by the heating of high-purity silica in an electric arc furnace using carbon electrodes. At temperatures over 1900°C, the carbon reduces the silica to silicon according to the chemical equation

SiO₂ + C → Si + CO₂

Liquid silicon collects in the bottom of the furnace, and is then drained and cooled. The silicon produced via this process is called metallurgical grade silicon and is at least 99% pure. In 1997, metallurgical grade silicon cost about United States dollar 0.50 per g.

Purification

The use of silicon in semiconductor devices demands a much greater purity than afforded by metallurgical grade silicon. Historically, a number of methods have been used to produce high-purity silicon.

Physical methods

Early silicon purification techniques were based on the fact that if silicon is melted and re-solidified, the last parts of the mass to solidify contain most of the impurities. The earliest method of silicon purification, first described in 1919 and used on a limited basis to make radar components during World War II, involved crushing metallurgical grade silicon and then partially dissolving the silcon powder in an acid. When crushed, the silicon cracked so that the weaker impurity-rich regions were on the outside of the resulting grains of silicon. As a result, the impurity-rich silicon was the first to be dissolved when treated with acid, leaving behind a more pure product.

In zone melting, the first silicon purification method to be widely used industrially, rods of metallurgical grade silicon were heated to melt at one end. Then, the heater was slowly moved down the length of the rod, keeping a small length of the rod molten as the silicon cooled and resolidified behind it. Since most impurities tend to remain in the molten region rather than resolidify, when the process was complete, most of the impurities in the rod had been moved into end that was the last to be melted. This end was then cut off and discarded, and the process repeated if a still higher purity was desired.

Chemical methods

Today, silicon is instead purified by converting it to a silicon compound that can be more easily purified than silicon itself, and then converting that silicon compound back into pure silcon. Trichlorosilane is the silicon compound most commonly used as the intermediate, although silicon tetrachloride and silane are also used. When these gases are blown over silicon at high temperature, they decompose to high-purity silicon.

In the Siemens process, high-purity silicon rods are exposed to trichlorosilane at 1150°C. The trichlorosilane gas decomposes and deposits additional silicon onto the rods, enlarging them according to chemical reactions like

2 HSiCl₃ → Si + 2 HCl + SiCl₄

Silicon produced from this and similar processes is called polycrystalline silicon. Polycrystalline silicon typically has impurity levels of 1 part per billion or less.

At one time, DuPont produced ultrapure silicon by reacting silicon tetrachloride with high-purity zinc vapors at 950°C, producing silicon according to the chemical equation

SiCl₄ + 2 Zn → Si + 2 ZnCl₂

However, this technique was plauged with practical problems (such as the zinc chloride byroduct solidifying and clogging lines) and was evenutally abandoned in favor of the Siemens process.

Crystallization

The Czochralski process is often used to make high-purity single silicon crystals for use in solid-state/semiconductor devices.

Isotopes

Silicon has nine isotopes, with mass numbers from 25-33. Si-28 (the most abundant isotope, at 92.23%), Si-29 (4.67%), and Si-30 (3.1%) are stable; Si-32 is a radioactive isotope produced by argon decay. Its half-life, after much argument, has been determined to be approximately 276 years, and it decays by beta emission to P-32 (which has a 14.28 year half-life) and then to S-32.