Difference between revisions of "Salts of oxoacids"

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== Silicates (& Quartz) ==
 
== Silicates (& Quartz) ==
  
Not exactly a salt but related ...
+
Silicates typically have pretty good mechanical properties. <br>
 +
Typically Mohs 5-6 sometimes up to almost ~8.
 +
 
 +
Of interest as base materials may be the pure end members of the mixing series of
 +
[http://en.wikipedia.org/wiki/Olivine olivine (wikipedia)] / [http://en.wikipedia.org/wiki/Peridot peridot (wikipedia)] <br>
 +
From Mg<sub>2</sub>SiO<sub>4</sub> forsterite to Fe<sub>2</sub>SiO<sub>4</sub> fayalite. <br> 
 +
And especially the associated high pressure modifications. <br>
 +
'''High pressure modifications tend to have higher crystal symmetries and mechanical strength at the cots of a bit of thermal stability.'''
 +
 
 +
=== Olivin/Peridot end-members and their low pressure stable stable high pressure modifications ===
 +
 
 +
Low pressure magnesium endmember forsterite:
 +
* Mg<sub>2</sub>SiO<sub>4</sub> [http://en.wikipedia.org/wiki/Forsterite Forsterite] – orthorhombic dipyramidal – Mohs 7
 +
High pressure modifications of fortserite:
 +
* Mg<sub>2</sub>SiO<sub>4</sub> [http://en.wikipedia.org/wiki/Wadsleyite wadseylite (wikipedia)] – sorosilicate – ortorhombic – dipyramidal – Mohs ?? – mid pressure crystal structure
 +
* Mg<sub>2</sub>SiO<sub>4</sub> '''[http://en.wikipedia.org/wiki/Ringwoodite ringwoodite (wikipedia)]''' – nesosilicate – '''cubic''' – Mohs ?? – 3.9g/ccm – high pressure crystal structure – [https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Ringwoodite 3D structure (de)]
 +
Low pressure iron endmember fayalite:
 +
* Fe<sub>2</sub>SiO<sub>4</sub> [http://en.wikipedia.org/wiki/Fayalite Fayalite] – orthorhombic dipyramidal – Mohs 6.5-7.0 – 4.39g/ccm – [https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Fayalite 3D structure (de)]
 +
High pressure modifications of fayalite:
 +
* γ-Fe<sub>2</sub>SiO<sub>4</sub> '''ahrensite''' – '''cubic''' – 4.85g/ccm – high pressure crystal structure of fayalite – [https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Ahrensite 3D structure (de)]
 +
 
 +
==== Neo-polymorphic transitions ====
 +
 
 +
The low pressure modifications forsterite and fayalite (and tephroite, ... see further below) are all isostructural (atoms at the same places). <br>
 +
This allows for [[neo-polymorph]]s spanning the natural mixing series. Just checkerpatterned as deisred. <br>
 +
{{wikitodo|Magnesium and iron are pretty far apart in the periodic table – find out why they behave so similar electronically in these minerals}}
 +
 
 +
'''Q:''' Is there an iron analog to wadseylite?
 +
 
 +
Ringwoodite (Mg) and ahrensite (Fe), while both cubic, have quite different structure. No [[neo-polymorph]]s here. <br>
 +
But Maybe unnatural iron-ringwoodite and magnesium-ahrensite can be [[piezosynthesized]]. <br>
 +
At least a little bit of substitution should work if electronic similarity still holds in these high pressure modifications
 +
 
 +
=== Silicates of further rather common elements ===
 +
 
 +
'''Calcium:'''
 +
* γ-Ca<sub>2</sub>SiO<sub>4</sub> Calcio-Olivine – Mohs 4.5 – orthorhombic
 +
* β-Ca<sub>2</sub>SiO<sub>4</sub> [https://en.wikipedia.org/wiki/Larnite Larnite] – Mohs 6 – monoclinic (?)
 +
----
 +
* Ni<sub>2</sub>SiO<sub>4</sub> [https://de.wikipedia.org/wiki/Liebenbergit Liebenbergite (de)] – (Mohs 6-6.5 or 4.5?) -- orthorhombic
 +
* Mn<sub>2</sub>SiO<sub>4</sub> [http://en.wikipedia.org/wiki/Tephroite Tephroite] (maybe less interesting since Mn is more scarce) – orthorhombic dipyramidal – Mohs 6
 +
* TiSiO<sub>4</sub> Titanium Silicate (no natural mineral here?) [https://www.chemspider.com/Chemical-Structure.4954356.html] [http://www.americanelements.com/titanium-silicate-nanopowder.html (broken)]
 +
----
 +
 
 +
Beyond that adding one more element there are an innumerable amount of natural silicates around.
 +
 
 +
=== Some semi random picks of other silicates ===
 +
 
 +
Misc, Not exactly a salt but related ...
 
* PbCa<sub>3</sub>Zn<sub>4</sub>'''(SiO<sub>4</sub>)<sub>4</sub>''' esperite [https://en.wikipedia.org/wiki/Esperite] Mohs 5-5.5 (unabundant zinc | exceptionally hard lead mineral) Specific gravity: 4.28-4.42
 
* PbCa<sub>3</sub>Zn<sub>4</sub>'''(SiO<sub>4</sub>)<sub>4</sub>''' esperite [https://en.wikipedia.org/wiki/Esperite] Mohs 5-5.5 (unabundant zinc | exceptionally hard lead mineral) Specific gravity: 4.28-4.42
 +
----
 +
 +
=== Other pages listing silicates of interest ===
 +
 +
Context specific silicates are also listed on these pages:
 +
* [[Ternary and higher gem-like compounds]]
 +
* [[s-block metals]] – lists some alkali and earth alkali silicates (among other compounds)
 +
* [[Iron]] – lists a few iron silicates
  
 
== Phosphate minerals ==
 
== Phosphate minerals ==
Line 17: Line 73:
 
[http://en.wikipedia.org/wiki/Phosphate_minerals (wikipedia)]
 
[http://en.wikipedia.org/wiki/Phosphate_minerals (wikipedia)]
  
 +
Calciumphosphates (bone biominaeral):
 
* Especially interesting: Hydoxy- Fluor- & Clorapatite Ca<sub>5</sub>'''(PO<sub>4</sub>)<sub>3</sub>'''(F,Cl,OH) - (Mohs 5 defining mineral) - '''a biomineral''' [https://en.wikipedia.org/wiki/Apatite]
 
* Especially interesting: Hydoxy- Fluor- & Clorapatite Ca<sub>5</sub>'''(PO<sub>4</sub>)<sub>3</sub>'''(F,Cl,OH) - (Mohs 5 defining mineral) - '''a biomineral''' [https://en.wikipedia.org/wiki/Apatite]
* Lazulite [http://en.wikipedia.org/wiki/Lazulite (wikipedia)] & Scorzalite [http://en.wikipedia.org/wiki/Scorzalite (wikipedia)] magnesium iron aluminium phosphates - (Mohs 5.5-6)
+
 
* Phosphophyllite [http://en.wikipedia.org/wiki/Phosphophyllite (wikipedia)] - zinc iron phosphate - rather soft (Mohs 3.5)
+
Magnesium and iron (aluminium) phosphates lazulite, scorcalite, wagnerite (naturally 75%iron 25%magnesium) (anhydrous low pressure modifications):
* Pb<sub>5</sub>'''(PO<sub>4</sub>)<sub>3</sub>'''Cl pyromorphite [http://en.wikipedia.org/wiki/Pyromorphite (wikipedia)] - relatively hard for a lead mineral (Mohs 3.5)
+
* FeAl2'''(PO<sub>4</sub>)<sub>2</sub>''' iron-lazulite [http://en.wikipedia.org/wiki/Lazulite (wikipedia)] – monoclinic – Mohs 6
* Y'''(PO<sub>4</sub>)''' Xenotime [http://en.wikipedia.org/wiki/Xenotime (wikipedia)] - rare yttrium - high symmetry (tetragonal) - (Mohs 4.5)
+
* MgAl2'''(PO<sub>4</sub>)<sub>2</sub>''' magnesium-lazulite
* Al<sub>2</sub>'''(PO<sub>4</sub>)'''(OH)<sub>3</sub> augelite [https://en.wikipedia.org/wiki/Augelite] Mohs 4-4.5
+
* FeAl2'''(PO<sub>4</sub>)<sub>2</sub>''' iron-scorzalite [http://en.wikipedia.org/wiki/Scorzalite (wikipedia)] – monoclinic (does not look so) – (Mohs 5.5-6.0)
* Fe'''PO<sub>4</sub>''' heterosite [https://de.wikipedia.org/wiki/Heterosit Wikipedia:Heterosit(de)] Mohs 4-4.5
+
* MgAl2'''(PO<sub>4</sub>)<sub>2</sub>''' magnesium-scorcalite
* Mn'''PO<sub>4</sub>''' purpurite [https://en.wikipedia.org/wiki/Purpurite] Mohs 4-5 (unabundant manganese)
+
* Fe2'''PO4'''F iron-wagnerite [https://en.wikipedia.org/wiki/Wagnerite] – monoclinic – Mohs 5.0-5.5
* (MgFe)2'''PO4'''F magnesium and iron wagnerite [https://en.wikipedia.org/wiki/Wagnerite] Mohs (?)
+
* Mg2'''PO4'''F magnesium wagnerite
* FeAl2'''(PO<sub>4</sub>)<sub>2</sub>''' anhydous iron scorzalite [https://en.wikipedia.org/wiki/Scorzalite] Mohs 6
+
----
* MgAl2'''(PO<sub>4</sub>)<sub>2</sub>''' anhydous magnesium scorzalite Mohs 6
+
* Al<sub>2</sub>'''(PO<sub>4</sub>)'''(OH)<sub>3</sub> augelite [https://en.wikipedia.org/wiki/Augelite] – monoclinic – Mohs 4-4.5
* Zn<sub>2</sub>Fe'''(PO<sub>4</sub>)<sub>2</sub>'''•4H<sub>2</sub>O phosphophyllite [https://en.wikipedia.org/wiki/Phosphophyllite] Mohs 3.5 (soft)
+
* Fe'''PO<sub>4</sub>''' heterosite [https://de.wikipedia.org/wiki/Heterosit Wikipedia:Heterosit(de)] – '''orthorhombic dipyramidal''' – Mohs 4-4.5
 +
----
 +
* Mn'''PO<sub>4</sub>''' purpurite [https://en.wikipedia.org/wiki/Purpurite] – '''ortorhombic dipyramidal''' – Mohs 4-5 (manganese is not too abundant) – (is that impressive color material inherent rather due to impurities?)
 +
* Zn<sub>2</sub>Fe(PO<sub>4</sub>)<sub>2</sub>•4H<sub>2</sub>O Phosphophyllite [http://en.wikipedia.org/wiki/Phosphophyllite (wikipedia)] – monoclinic – zinc iron phosphate - rather soft (Mohs 3.5) – rather soft
 +
* Pb<sub>5</sub>'''(PO<sub>4</sub>)<sub>3</sub>'''Cl pyromorphite [http://en.wikipedia.org/wiki/Pyromorphite (wikipedia)] '''hexahonal dipyramidal''' Mohs 3.5 – (relatively hard for a lead mineral)
 +
* Y'''(PO<sub>4</sub>)''' Xenotime [http://en.wikipedia.org/wiki/Xenotime (wikipedia)] – '''tetragonal dipyramidal''' – Mohs 4.5 (yttrium is not too abundant)
  
 
== Carbonate minerals ==
 
== Carbonate minerals ==
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[http://en.wikipedia.org/wiki/Template:Carbonates (wikipedia - artificial)]
 
[http://en.wikipedia.org/wiki/Template:Carbonates (wikipedia - artificial)]
  
* Calcite Mohs 3 (defining mineral) & Aragonite Mohs 3.5-4 - calcium
+
Many may be isostructural and amenable to making [[neo-polymorph]]s (to check). <br>
* Magnesite Mohs 3.5-4.5 - magnesium
+
The relatively low symmetry crystal structure may be a bit annoying. <br>
* Dolomite -- CaMg(CO<sub>3</sub>)<sub>2</sub> [https://en.wikipedia.org/wiki/Dolomite] Mohs 3.5-4
+
Degradability solubility properties when exposed to the weather as spill may be decent. <br>
* Siderite - iron
+
(Only relevant if that is the design goal).
* Smithsonite - zinc
+
 
* Malachite & Azurite - copper
+
Calcium:
* Rhodochrosite - manganese (rare)
+
* CaCO<sub>3</sub> [[Calcite]] Mohs 3 (defining mineral)
* ...
+
* CaCO<sub>3</sub> Aragonite Mohs 3.5-4  
* Mg<sub>3</sub>Ca'''(CO<sub>3</sub>)<sub>4</sub>''' huntite [https://en.wikipedia.org/wiki/Huntite] Mohs 1-2 (very soft!)
+
 
* Pb'''CO<sub>3</sub>''' cerussite [https://en.wikipedia.org/wiki/Cerussite] Mohs 3-3.5 (soft)
+
Magnesium:
 +
* MgCO<sub>3</sub> Magnesite [https://en.wikipedia.org/wiki/Magnesite] – trigonal – Mohs 3.5-4.5
 +
 
 +
Both:
 +
* CaMg'''(CO<sub>3</sub>)<sub>2</sub>''' Dolomite [https://en.wikipedia.org/wiki/Dolomite_(mineral)] – trigonal rhombohedral – Mohs 3.5-4
 +
* Mg<sub>3</sub>Ca'''(CO<sub>3</sub>)<sub>4</sub>''' Huntite [https://en.wikipedia.org/wiki/Huntite] – trigonal – '''Mohs 1-2 (way too soft!)'''
 +
 
 +
Copper:
 +
* Cu2CO3(OH)2 malachite [https://en.wikipedia.org/wiki/Malachite] – Monoclinic – Mohs 3.5-4.0
 +
* Cu3(CO3)2(OH)2 azurite – Monoclinic – Mohs 3.5-4.0 – (complex structure)
 +
 
 +
Iron, zinc, manganese, lead:
 +
* FeCO<sub>3</sub> Siderite [https://en.wikipedia.org/wiki/Siderite] – Trigonal – Mohs MgCO<sub>3</sub>
 +
* ZnCO<sub>3</sub> Smithsonite [https://www.mindat.org/min-3688.html (mindat)] – trigonal – Mohs 4.0-4.5 – 4.44g/ccm
 +
* MnCO<sub>3</sub> Rhodochrosite – trional – Mohs 3.5-4.0 – manganese is not too abundant
 +
* Pb'''CO<sub>3</sub>''' Cerussite [https://en.wikipedia.org/wiki/Cerussite] – '''orthorhombic dipyramidal''' – Mohs 3.0-3.5 (soft) – 6.57g/ccm
  
 
== Sulfate minerals ==
 
== Sulfate minerals ==
Line 53: Line 130:
 
One of the harder ones is brochantite [http://en.wikipedia.org/wiki/Brochantite (wikipedia)] - (Mohs 3.5-4)
 
One of the harder ones is brochantite [http://en.wikipedia.org/wiki/Brochantite (wikipedia)] - (Mohs 3.5-4)
 
* CaSO<sub>4</sub> anhydrite [https://en.wikipedia.org/wiki/Anhydrite] (decomposes slowly to hydroxyde gypsum)
 
* CaSO<sub>4</sub> anhydrite [https://en.wikipedia.org/wiki/Anhydrite] (decomposes slowly to hydroxyde gypsum)
 +
-----
 +
Very common chemical. Not at all useful as structural material though:
 +
* [https://en.wikipedia.org/wiki/Copper(II)_sulfate Copper(II) sulfate] – copper sulfate pentahydrate [https://en.wikipedia.org/wiki/Chalcanthite Chalcanthite] – Mohs 2.5 – very soft
  
 
== Borate minerals ==
 
== Borate minerals ==
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* ...
 
* ...
  
== Nitrate Aluminate and other minerals ==
+
== Nitrate and Aluminates ==
  
All rather water soluble. See: [http://en.wikipedia.org/wiki/Category:Nitrate_minerals (wikipedia - minerals)]  
+
Nitrates are typically rather water soluble. <br>
[http://en.wikipedia.org/wiki/Template:Nitrates (wikipedia - artificial)]
+
While that migh be desired for intentional degradability of inner normally sealed structures <br>
 +
nitrates are also typically extremely soft, strongly limiting their applicability for mechanical purposes. <br>
 +
See: [http://en.wikipedia.org/wiki/Category:Nitrate_minerals (wikipedia - natural nitrate minerals)] and [http://en.wikipedia.org/wiki/Template:Nitrates (wikipedia - artificial nitrates)]
  
Aluminates: [http://en.wikipedia.org/wiki/Aluminate (wikipedia)]
+
----
 +
 
 +
Aluminates: <br>
 +
[http://en.wikipedia.org/wiki/Aluminate (wikipedia)]
 +
 
 +
== Salts of metal oxoacids ==
 +
 
 +
* [https://en.wikipedia.org/wiki/Category:Transition_metal_oxoacids Category:Transition_metal_oxoacids]
 +
* [https://en.wikipedia.org/wiki/Category:Oxyanions Category:Oxyanions]
 +
* [https://en.wikipedia.org/wiki/Germanate Germanate]
 +
 
 +
=== Titanates (salts of titanic acid) ===
 +
 
 +
* [https://en.wikipedia.org/wiki/Titanic_acid titanic acid]
 +
* [https://en.wikipedia.org/wiki/Titanate titanate]
 +
----
 +
Trigonal structure:
 +
* MgTiO<sub>3</sub> – [https://de.wikipedia.org/wiki/Magnesiumtitanoxid Magnesium titanate (de)] – [https://en.wikipedia.org/wiki/Geikielite geikelite] – trigonal rhombohedral – Mohs5-6 – 1610°C
 +
* FeTiO<sub>3</sub> – [https://en.wikipedia.org/wiki/Ilmenite ilmenite] – trigonal rhombohedral (like sapphire) – Mohs 5-6
 +
* MnTiO<sub>3</sub> – [https://en.wikipedia.org/wiki/Pyrophanite pyrophanite]
 +
----
 +
Perovskite structure:
 +
* CaTiO<sub>3</sub> – [https://en.wikipedia.org/wiki/Calcium_titanate Calcium titanate] – [https://en.wikipedia.org/wiki/Perovskite perovskite] – orthorhombic – Mohs 5.0-5.5 – 1975°C
 +
* SrTiO<sub>3</sub> – [https://en.wikipedia.org/wiki/Strontium_titanate Strontium titanate] [https://en.wikipedia.org/wiki/Tausonite tausonite] – cubic – Mohs6.0-6.5 – 4.88g/ccm – n=2.4
 +
* BaTiO<sub>3</sub> – [https://en.wikipedia.org/wiki/Barium_titanate Barium titanate] [https://www.mineralienatlas.de/lexikon/index.php/MineralData?lang=en&language=english&mineral=Barioperowskit Barioperowskit (mineralienatlas)] – ([https://en.wikipedia.org/wiki/Barium_orthotitanate Barium orthotitanate] – electroceranic – hygroscopic)
 +
* PbTiO<sub>3</sub> – [https://en.wikipedia.org/wiki/Lead_titanate Lead titanate] – [https://www.mineralienatlas.de/lexikon/index.php/MineralData?lang=en&language=english&mineral=Macedonit macedonite (mineralienatlas)] – Mohs 5.5-6.0
 +
* Other more complex structure: [https://en.wikipedia.org/wiki/Bismuth_titanate Bismuth_titanate]
 +
----
 +
* Al<sub>2</sub>TiO<sub>5</sub> [https://de.wikipedia.org/wiki/Aluminiumtitanat aluminium titanate (de)] – decays to rutile and sapphire on heating
 +
* [https://en.wikipedia.org/wiki/Lead_zirconate_titanate Lead zirconate titanate]
 +
* [https://en.wikipedia.org/wiki/Calcium_copper_titanate Calcium copper titanate]
  
 
== Related ==
 
== Related ==
  
 
* [[Oxygen]]
 
* [[Oxygen]]
 +
* [[Gemstone like compounds]]
 +
* [[Gemstone like compounds with high potential]]
  
 
== External links ==
 
== External links ==
  
 +
Wikipedia:
 
* Solubility chart: https://en.wikipedia.org/wiki/Solubility_chart
 
* Solubility chart: https://en.wikipedia.org/wiki/Solubility_chart
 +
* [https://en.wikipedia.org/wiki/Oxyacid Oxoacid]
 +
* [https://en.wikipedia.org/wiki/Category:Oxoacids Category:Oxoacids]

Latest revision as of 21:57, 1 July 2021

This article is a stub. It needs to be expanded.

The X-O-X bonds present in those compounds increase the space between the spacially linking X atoms. This lead to a lower density of bonds in cross sections inclusion of bigger voids thus higher porousity. Due to the porousness of these compounds it is harder to get the surfaces flat - figuratively like the surface of a pumice stone. It's impossible to get them as smooth as passivated diamond. [todo: investigate wheter superlubricating bearings can be constructed from these types of diamondoid compounds]

(wikipedia:oxoacid)

Silicates (& Quartz)

Silicates typically have pretty good mechanical properties.
Typically Mohs 5-6 sometimes up to almost ~8.

Of interest as base materials may be the pure end members of the mixing series of olivine (wikipedia) / peridot (wikipedia)
From Mg2SiO4 forsterite to Fe2SiO4 fayalite.
And especially the associated high pressure modifications.
High pressure modifications tend to have higher crystal symmetries and mechanical strength at the cots of a bit of thermal stability.

Olivin/Peridot end-members and their low pressure stable stable high pressure modifications

Low pressure magnesium endmember forsterite:

  • Mg2SiO4 Forsterite – orthorhombic dipyramidal – Mohs 7

High pressure modifications of fortserite:

Low pressure iron endmember fayalite:

High pressure modifications of fayalite:

  • γ-Fe2SiO4 ahrensitecubic – 4.85g/ccm – high pressure crystal structure of fayalite – 3D structure (de)

Neo-polymorphic transitions

The low pressure modifications forsterite and fayalite (and tephroite, ... see further below) are all isostructural (atoms at the same places).
This allows for neo-polymorphs spanning the natural mixing series. Just checkerpatterned as deisred.
(wiki-TODO: Magnesium and iron are pretty far apart in the periodic table – find out why they behave so similar electronically in these minerals)

Q: Is there an iron analog to wadseylite?

Ringwoodite (Mg) and ahrensite (Fe), while both cubic, have quite different structure. No neo-polymorphs here.
But Maybe unnatural iron-ringwoodite and magnesium-ahrensite can be piezosynthesized.
At least a little bit of substitution should work if electronic similarity still holds in these high pressure modifications

Silicates of further rather common elements

Calcium:

  • γ-Ca2SiO4 Calcio-Olivine – Mohs 4.5 – orthorhombic
  • β-Ca2SiO4 Larnite – Mohs 6 – monoclinic (?)

  • Ni2SiO4 Liebenbergite (de) – (Mohs 6-6.5 or 4.5?) -- orthorhombic
  • Mn2SiO4 Tephroite (maybe less interesting since Mn is more scarce) – orthorhombic dipyramidal – Mohs 6
  • TiSiO4 Titanium Silicate (no natural mineral here?) [1] (broken)

Beyond that adding one more element there are an innumerable amount of natural silicates around.

Some semi random picks of other silicates

Misc, Not exactly a salt but related ...

  • PbCa3Zn4(SiO4)4 esperite [2] Mohs 5-5.5 (unabundant zinc | exceptionally hard lead mineral) Specific gravity: 4.28-4.42

Other pages listing silicates of interest

Context specific silicates are also listed on these pages:

Phosphate minerals

(wikipedia)

Calciumphosphates (bone biominaeral):

  • Especially interesting: Hydoxy- Fluor- & Clorapatite Ca5(PO4)3(F,Cl,OH) - (Mohs 5 defining mineral) - a biomineral [3]

Magnesium and iron (aluminium) phosphates lazulite, scorcalite, wagnerite (naturally 75%iron 25%magnesium) (anhydrous low pressure modifications):

  • FeAl2(PO4)2 iron-lazulite (wikipedia) – monoclinic – Mohs 6
  • MgAl2(PO4)2 magnesium-lazulite
  • FeAl2(PO4)2 iron-scorzalite (wikipedia) – monoclinic (does not look so) – (Mohs 5.5-6.0)
  • MgAl2(PO4)2 magnesium-scorcalite
  • Fe2PO4F iron-wagnerite [4] – monoclinic – Mohs 5.0-5.5
  • Mg2PO4F magnesium wagnerite

  • Al2(PO4)(OH)3 augelite [5] – monoclinic – Mohs 4-4.5
  • FePO4 heterosite Wikipedia:Heterosit(de)orthorhombic dipyramidal – Mohs 4-4.5

  • MnPO4 purpurite [6]ortorhombic dipyramidal – Mohs 4-5 (manganese is not too abundant) – (is that impressive color material inherent rather due to impurities?)
  • Zn2Fe(PO4)2•4H2O Phosphophyllite (wikipedia) – monoclinic – zinc iron phosphate - rather soft (Mohs 3.5) – rather soft
  • Pb5(PO4)3Cl pyromorphite (wikipedia)hexahonal dipyramidal – Mohs 3.5 – (relatively hard for a lead mineral)
  • Y(PO4) Xenotime (wikipedia)tetragonal dipyramidal – Mohs 4.5 – (yttrium is not too abundant)

Carbonate minerals

(wikipedia - minerals) (wikipedia - artificial)

Many may be isostructural and amenable to making neo-polymorphs (to check).
The relatively low symmetry crystal structure may be a bit annoying.
Degradability solubility properties when exposed to the weather as spill may be decent.
(Only relevant if that is the design goal).

Calcium:

  • CaCO3 Calcite Mohs 3 (defining mineral)
  • CaCO3 Aragonite Mohs 3.5-4

Magnesium:

  • MgCO3 Magnesite [7] – trigonal – Mohs 3.5-4.5

Both:

  • CaMg(CO3)2 Dolomite [8] – trigonal rhombohedral – Mohs 3.5-4
  • Mg3Ca(CO3)4 Huntite [9] – trigonal – Mohs 1-2 (way too soft!)

Copper:

  • Cu2CO3(OH)2 malachite [10] – Monoclinic – Mohs 3.5-4.0
  • Cu3(CO3)2(OH)2 azurite – Monoclinic – Mohs 3.5-4.0 – (complex structure)

Iron, zinc, manganese, lead:

  • FeCO3 Siderite [11] – Trigonal – Mohs MgCO3
  • ZnCO3 Smithsonite (mindat) – trigonal – Mohs 4.0-4.5 – 4.44g/ccm
  • MnCO3 Rhodochrosite – trional – Mohs 3.5-4.0 – manganese is not too abundant
  • PbCO3 Cerussite [12]orthorhombic dipyramidal – Mohs 3.0-3.5 (soft) – 6.57g/ccm

Sulfate minerals

(wikipedia)

Sulfate minerals are generally rather soft with few exceptions.
One of the harder ones is brochantite (wikipedia) - (Mohs 3.5-4)

  • CaSO4 anhydrite [13] (decomposes slowly to hydroxyde gypsum)

Very common chemical. Not at all useful as structural material though:

Borate minerals

(wikipedia)


  • Al6B5O15(F,OH)3 Jeremejevite (wikipedia) - (Mohs 6.5-7.5)
  • Mg7(BO3)3(OH)4Cl Karlite (wikipedia) - (Mohs 5½)
  • Ca2B5SiO9(OH)5 Howlite (wikipedia) - soft (Mohs 3.5)
  • MnSn(BO3)2 Tusionite (wikipedia) - (Mohs 5-6) - tin
  • CaZrAl9O15(BO3) Painite (wikipedia) - rare zirconium (Mohs 8)
  • ...

Nitrate and Aluminates

Nitrates are typically rather water soluble.
While that migh be desired for intentional degradability of inner normally sealed structures
nitrates are also typically extremely soft, strongly limiting their applicability for mechanical purposes.
See: (wikipedia - natural nitrate minerals) and (wikipedia - artificial nitrates)


Aluminates:
(wikipedia)

Salts of metal oxoacids

Titanates (salts of titanic acid)


Trigonal structure:


Perovskite structure:


Related

External links

Wikipedia: