Difference between revisions of "Polymorphs of silicon dioxide"
From apm
(basic page) |
(added link to page: Neo-polymorphs) |
||
| (3 intermediate revisions by the same user not shown) | |||
| Line 4: | Line 4: | ||
* Common [[Quartz]] | * Common [[Quartz]] | ||
| − | * amorphous forms (properties similar to: chalcedon, opal, | + | * amorphous forms (properties similar to: chalcedon, opal, obsidian, ...) <br>[[mechanosynthesis]] would allow for synthesis of '''pseudo amorphous configurations''' <br> [[Neo-polymorph]]s |
== Especially interesting since unusually hard and dense == | == Especially interesting since unusually hard and dense == | ||
| Line 20: | Line 20: | ||
* [[Silicon]], [[Oxygen]] | * [[Silicon]], [[Oxygen]] | ||
| + | * [[Gemstone like compound]] | ||
| + | * [[Neo-polymorphs]] | ||
Latest revision as of 08:41, 25 April 2021
More commonly known SiO2 gemstones
- Common Quartz
- amorphous forms (properties similar to: chalcedon, opal, obsidian, ...)
mechanosynthesis would allow for synthesis of pseudo amorphous configurations
Neo-polymorphs
Especially interesting since unusually hard and dense
- Stishovite –– may be transitionable into other gemstomes with the same rutile structure forming pseudo phase diagrams
- Seifertite –– (scrutinyte structure)
Both are metastable very hard and very dense.
They may not be very resilient against high temperatures.
Other polymorphs of SiO2
- (wiki-TODO: add some known ones)
