Base materials with high potential

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Revision as of 10:41, 14 April 2021 by Apm (talk | contribs) (Simple rutile structure & hard: added link to yet unwritten page the stishovite continuum)
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Very good materials

Best of the best

Best diamondoids

Best SiO2 polymorphs

Metastable ultrahard and dense SiO2 polymorphs:

Simple titanium gemstones

  • TiN, TiP, TiC, TiSi2, TiB2, TiO2, Ti2O3

Quite simple rutile structure & Hard

Neo-polymorphs with rutile structure
See: the stishovite continuum currently on the page about silicon
Silicon group: GeO2, SnO2, β-PbO2
Other: MnO2, FeSbO4

Mono metal monoxides (simple cublic NaCl salt structure)

Earth alkali based

  • MgO periclase
  • CaO - questionable - highly reactive with water

Transition metal based

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

Con: Rather soft materials

Others

  • garnets - hard and cubic (but big unit cell)
  • brommelite BeO - very hard but beryllium is scarce and poisonous