Difference between revisions of "Base materials with high potential"
From apm
(→Simple salt structures: restructuring) |
(→Simple salt structures: simple -> simple cubic) |
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Other: MnO<sub>2</sub>, FeSbO<sub>4</sub> | Other: MnO<sub>2</sub>, FeSbO<sub>4</sub> | ||
− | == Simple salt structures == | + | == Simple cubic salt structures == |
* MgO [[periclase]] | * MgO [[periclase]] |
Revision as of 09:19, 14 April 2021
Very good materials
Best of the best
- diamond and its polymorphs including hexagonal diamond aka lonsdaleite
- moissanite - SiC - high heat resistance
- stishovite and seifertite - metastable ultrahard and dense SiO2 polymorphs
- simple titanium gemstones including: TiN TiP TiC TiSi2 TiB2 TiO2 Ti2O3
Simple rutile structure & hard
- rutile TiO2
- stishovite - metastable SiO2 polymorph - rutile structure & very hard and dense
Neo-polymorphs with rutile structure
See: the stishovite continuum on the page about silicon
Silicon group: GeO2, SnO2, β-PbO2
Other: MnO2, FeSbO4
Simple cubic salt structures
- MgO periclase
Some transition metal monoxides (Typical: Max 1300-1900°C - Mohs 5-6)
- TiO hongquiite
- MnO Manganosite - (Mn is less abundant)
- FeO wüstite
- NiO brommelite - (Ni is not too abundant on earth but very abundant on metallic asteroids)
V vanadium, Cr chromium, Co cobalt do that too but
these elements are more scarce thus not included as pure high volume base materials here
Other
- spinell MgAl2O4 - very hard and cubic
Materials with some weakness
Con: low crystal structure symmetry
- leukosapphire - very hard
- quartz - and other low density polymorphs of SiO2
Con: Rather soft materials
- calcite and aragonite
Others
- garnets - hard and cubic (but big unit cell)
- brommelite BeO - very hard but beryllium is scarce and poisonous