Neo-polymorph: Difference between revisions

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{{wikitodo|There was a significant mixup with '''neo-isotypes''' here. Do some more cleanup & checks if transition succeeded.}}
{{site specific term}}
{{site specific term}}
A '''neo-polymorphic compound''' (or neo-isomorphic compound) is a highly stable non equilibrium polymorph of a material with a certain fixed stoichiometry that is exclusively accessible through [[mechanosynthesis]].


This includes patterns where specifically ordered states are thermodynamically not more attractive than disordered (or in other undesired form ordered) states but where a (sufficiently) high activation energy lies between the ordered and unordered states.
A '''neo-polymorphic compound''' (or neo-isomorphic compound) is a highly (meta)stable non equilibrium polymorph <br>
of a material with a certain fixed stoichiometry that is exclusively accessible through [[mechanosynthesis]]. <br>
If just one element is involved the term '''[[neo-allotrope]]''' can be applied too/instead.
 
This includes patterns where specifically ordered states are thermodynamically not more attractive <br>
than disordered (or in other undesired form ordered) states but <br>
where a (sufficiently) high activation energy lies between the ordered and unordered states <br>
making the via conventional means inacessible states highly kinetically metastable. <br>


The patterns can be:
The patterns can be:
* different atom types (elements) ... specific example: A crossover gemstone between Rutile (polymorph of TiO<sub>2</sub>) and stishovite (polymorph of SiO<sub>2</sub>). The pattern making elements are Ti & Si. Oxygen atoms stay at their places.
* different stacking geometry, specific example: <br>A crossover between Diamond (cubic stacking) and lonsdaleite (hexagonal stacking). <br>(When pointing up a tetrapod of carbon bonds there are two ways one can orient the up facing three bonds in a six direction hexagon).
* different stacking geometry or ... specific example: A crossover between Diamond (cubic stacking) and lonsdaleite (hexagonal stacking). (When pointing up a tetrapod of carbon bonds there are two ways one can orient the up facing three bonds in a six direction hexagon).
* changes between different crystal structures of the same composition (adn stoichometry) so long nigh seamless covalent transitions are possible
* ...
Excluded here:
* changes of atom types and stoichometry falls under [[neo-isotypes]] instead: <br>specific example: A crossover gemstone between Rutile (polymorph of TiO<sub>2</sub>) and stishovite (polymorph of SiO<sub>2</sub>). <br>The pattern making elements are Ti & Si. Oxygen atoms stay at their places.


Patterns:
Stacking order patterns:
* ABABBABBBBAABABAABAA – unwanted unordered state – may be the only one that is thermodynamically accessible
* ABABBABBBBAABABAABAA – unwanted unordered state – may be the only one that is thermodynamically accessible
* ABABABABABABABABABAB – unwanted ordered state – may be the only one that is thermodynamically accessible
* ABABABABABABABABABAB – unwanted ordered state – may be the only one that is thermodynamically accessible
* AABBAABBAABBAABBAABB – '''neo-polymorph''' – wanted peculiarly ordered state – not thermodynamically accessible - but accessible via [[mechanosynthesis]]
* ABBAABBAABBAABBAABB – '''neo-polymorph''' – wanted peculiarly ordered state – not thermodynamically accessible - but accessible via [[mechanosynthesis]]
Note: in the case of SiC ([[moissanite]]) there is the constraint of no two same letters following adjacently. Above examples for simplicity.


Of course arbitrary many elements/layertypes/... are allowed. A,B,C,D,...
Also '''[[neo-polymorphs]] and [[neo-isotypes]] can intermix here to [[neo gemstones like compounds]]''' or '''neo-gems''' for short. <br>
All sorts of II-IV semiconductor compounds have fitting structure stacking order variations in {111} directions. <br>
So structural stacking order can be augmented with material type stacking order. <br>
Material stacking order not being constrained to the by {111} directions but by lattice strain. <br>


Note: '''Thermodynamic accessibility''' refers to all the crude processes available today (2017) that only allow to handle matter in statistical quantities: melting, mixing, cooling, pressurizing, irradiating, ... This explicitly excludes advanced [[mechanosynthesis]].
Note: '''Thermodynamic accessibility''' refers to all the crude processes available today (2025) <br>
that only allow to handle matter in statistical quantities: <br<
melting, mixing, cooling, pressurizing, irradiating, ([[cook mix and stir thermodynamic synthesis]]) ... <br>
This explicitly excludes advanced [[mechanosynthesis]].


== Examples ==
== Examples ==


'''The rutile stishovite neopolymorphic transition:''' <br>
See: [[pseudo phase diagrams]] for more details on this.
The common mineral [[rutile]] and the rare mineral [[stishovite]] (made out of the two most common elements in earth crust) share the same crystal structure. The rutile structure.
 
Albeit rutile not drawing silicon into its structure naturally (meaning it's thermodynamically unfavourable)
* [[Dialondeite]] cubic to hexagonal series
(as can be seen with rutile occuring embedded in quartz https://commons.wikimedia.org/wiki/File:Rutile@quartz.jpg)
* [[Moissanite]] cubic to hexagonal series
a forced substitution (at least to some degree) may very well be possible via [[mechanosynthesis|mechanosyntheic]] means
* genrally: cubic zincblende structure to hexagonal wurzite structure series (for all applicable compounds respectively, mostly III-V semiconductors)
and the resulting product [[base material]] may very well be highly (meta) stable at room temperature.
----
Other patternd back and forth transitions between small chunks of highly compatible crystal structures:
* [[withe sapphire]] to [[deltalumide]] (unclear if transitionable)
* [[silicon nitride]] trigonal alpha to hexagonal beta & (unclear) to cubic gamma
* SiO<sub>2</sub> low pressure modification transitions - see page: [[Quartz]]
* … {{wikitodo|Find more examples to put here}}


== Related ==
== Related ==


* [[pseudo phase diagram]]
* [[Neo-gems]]
* [[diamondoid compound]]
* '''[[Neo-isotypes]]'''
* [[binary diamondoid compound]]
----
* [[Classifications for gemstone like compounds]]
----
* '''[[Pseudo phase diagram]]''' - mapping out neo-polymorphs
* [[Simple crystal structures of especial interest]] - browse there as a starting point
-----
* [[Diamondoid compound]]
* [[Binary diamondoid compound]]
----
* [[Kaehler bracket]]s
----
'''Examples:'''
* [[Dialondeite]]


== External links ==
== External links ==


* Wikipedia: [https://en.wikipedia.org/wiki/Polymorphism_(materials_science) Polymorphism (materials science)]
Wikipedia pages:
* Wikipedia: [https://en.wikipedia.org/wiki/Polymorphs_of_silicon_carbide Polymorphs of silicon carbide]
* [https://en.wikipedia.org/wiki/Polymorphism_(materials_science) Polymorphism (materials science)]
* Wikipedia: [https://en.wikipedia.org/wiki/Isomer isomer], [https://en.wikipedia.org/wiki/Stereoisomerism stereoisomer], [https://en.wikipedia.org/wiki/Conformational_isomerism conformational isomer]
* [https://en.wikipedia.org/wiki/Polymorphs_of_silicon_carbide Polymorphs of silicon carbide]
* Wikipedia: [https://en.wikipedia.org/wiki/Superstructure_(condensed_matter) Superstructure (condensed matter)]
* [https://en.wikipedia.org/wiki/Isomer isomer], [https://en.wikipedia.org/wiki/Stereoisomerism stereoisomer], [https://en.wikipedia.org/wiki/Conformational_isomerism conformational isomer]
* [https://en.wikipedia.org/wiki/Superstructure_(condensed_matter) Superstructure (condensed matter)]
* [https://en.wikipedia.org/wiki/Isomorphism_(crystallography) Isomorphism_(crystallography)]
----
* Isotype: [https://www.mineralienatlas.de/lexikon/index.php/isotyp?lang=de (de)] Translated citation: "Minerals of the same structural type are called isotypes. They crystallize in the same class of crystals and form similar crystal forms. "
* Isotype: [https://de.wikipedia.org/wiki/Isotyp (wikipedia de) Isotyp]
----
* [https://www.mineralienatlas.de/ www.mineralienatlas.de] <br>lists minerals with equal or similar structures for any given mineral <br> so thhis can serve as a possible starting point to find potential neo-polymorphs
 
[[Category:Far term target]]

Latest revision as of 19:10, 29 March 2026

(wiki-TODO: There was a significant mixup with neo-isotypes here. Do some more cleanup & checks if transition succeeded.)

This article defines a novel term (that is hopefully sensibly chosen). The term is introduced to make a concept more concrete and understand its interrelationship with other topics related to atomically precise manufacturing. For details go to the page: Neologism.


A neo-polymorphic compound (or neo-isomorphic compound) is a highly (meta)stable non equilibrium polymorph
of a material with a certain fixed stoichiometry that is exclusively accessible through mechanosynthesis.
If just one element is involved the term neo-allotrope can be applied too/instead.

This includes patterns where specifically ordered states are thermodynamically not more attractive
than disordered (or in other undesired form ordered) states but
where a (sufficiently) high activation energy lies between the ordered and unordered states
making the via conventional means inacessible states highly kinetically metastable.

The patterns can be:

  • different stacking geometry, specific example:
    A crossover between Diamond (cubic stacking) and lonsdaleite (hexagonal stacking).
    (When pointing up a tetrapod of carbon bonds there are two ways one can orient the up facing three bonds in a six direction hexagon).
  • changes between different crystal structures of the same composition (adn stoichometry) so long nigh seamless covalent transitions are possible

Excluded here:

  • changes of atom types and stoichometry falls under neo-isotypes instead:
    specific example: A crossover gemstone between Rutile (polymorph of TiO2) and stishovite (polymorph of SiO2).
    The pattern making elements are Ti & Si. Oxygen atoms stay at their places.

Stacking order patterns:

  • ABABBABBBBAABABAABAA – unwanted unordered state – may be the only one that is thermodynamically accessible
  • ABABABABABABABABABAB – unwanted ordered state – may be the only one that is thermodynamically accessible
  • ABBAABBAABBAABBAABB – neo-polymorph – wanted peculiarly ordered state – not thermodynamically accessible - but accessible via mechanosynthesis

Note: in the case of SiC (moissanite) there is the constraint of no two same letters following adjacently. Above examples for simplicity.

Also neo-polymorphs and neo-isotypes can intermix here to neo gemstones like compounds or neo-gems for short.
All sorts of II-IV semiconductor compounds have fitting structure stacking order variations in {111} directions.
So structural stacking order can be augmented with material type stacking order.
Material stacking order not being constrained to the by {111} directions but by lattice strain.

Note: Thermodynamic accessibility refers to all the crude processes available today (2025)
that only allow to handle matter in statistical quantities: <br< melting, mixing, cooling, pressurizing, irradiating, (cook mix and stir thermodynamic synthesis) ...
This explicitly excludes advanced mechanosynthesis.

Examples

See: pseudo phase diagrams for more details on this.

  • Dialondeite cubic to hexagonal series
  • Moissanite cubic to hexagonal series
  • genrally: cubic zincblende structure to hexagonal wurzite structure series (for all applicable compounds respectively, mostly III-V semiconductors)

Other patternd back and forth transitions between small chunks of highly compatible crystal structures:

  • withe sapphire to deltalumide (unclear if transitionable)
  • silicon nitride trigonal alpha to hexagonal beta & (unclear) to cubic gamma
  • SiO2 low pressure modification transitions - see page: Quartz
  • (wiki-TODO: Find more examples to put here)

Related






Examples:

External links

Wikipedia pages:


  • Isotype: (de) Translated citation: "Minerals of the same structural type are called isotypes. They crystallize in the same class of crystals and form similar crystal forms. "
  • Isotype: (wikipedia de) Isotyp

  • www.mineralienatlas.de
    lists minerals with equal or similar structures for any given mineral
    so thhis can serve as a possible starting point to find potential neo-polymorphs