|
| |
|
|
|
|
|
|
|
|
|
silica (silicon dioxide) |
|
| |
|
SiO{TAG(tag=>sub)}2{TAG} An abundant material on Earth, being the major constituent of sand. It is a white solid, with a high melting point (1710 °C) due to the structure of the solid, which is a giant covalent lattice with four Si-O covalent bonds arranged tetrahedrally (see the diagram). It forms three polymorphs: quartz, tridymite and cristobalite (all of which can exist in both low- and high-temperature forms). At high temperatures, silicates can be formed by fusion with other substances, as in the formation of slag in a blast furnace. When fused with limestone (CaCO{TAG(tag=>sub)}3{TAG}) and sodium carbonate (Na{TAG(tag=>sub)}2{TAG}CO{TAG(tag=>sub)}3{TAG}) at around 1500 °C and then cooled, a glass is formed.
{img src=show_image.php?name=image_19_13.gif } |
|
|
|
|
Bookmark this page:
|
|
|
|
<< former term |
|
next term >> |
|
|
|
|
|
| |
|
|
| Other Terms : electron | Jacob-Monod theory | Wien's (displacement) law
|
| |
|
Home |
Add new article |
Your List |
Tools |
Become an Editor |
Tell a Friend |
Links |
Awards |
Testimonials |
Press |
News |
About
| Imprint |
|
Copyright ©2009 Globalscience24. All rights reserved. Terms of Use | Privacy Policy | Contact Us
|