[Rockhounds] "Hexagonal" Diamond and other mineral structures,
was: Another extinction impact-13 KYA
R. Peter Richards
rpr at heidelberg.edu
Fri Jan 2 16:56:23 PST 2009
We always push "Send" too soon...
Two clarifications: I meant to say "once you lay ouT the first
layer" but you probably figured that out. The other relates to the
change from one carbon structure to the other - I started out talking
about changing lonsdaleite into diamond, but wound up pondering the
fact that diamonds survive the trip to the surface of the earth
without being converted to graphite (in fact some are converted,
apparently, but not all).
The point is that all three structures are quite different, so
changing one into another is a disruptive, or "reconstructive" phase
change. This is in contrast, for example, to the change from high-
temperature beta quartz to standard low-temperature alpha quartz,
which only involves a kinking of the structure. This happens almost
immediately when the right temperature is reached, and can be undone
and done again just by appropriate heating and cooling. By contrast,
the change from tridymite or crystobalite to quartz is
reconstructive, and is slow to happen if it happens at all. As a
consequence, we find crystals of tridymite and cristobalite at earth
surface conditions with their structures basically intact, but quartz
that started out as high quartz is invariably found as complexly
twinned low quartz.
There, now I'm done!
Pete Richards
On Jan 2, 2009, at 7:40 PM, R. Peter Richards wrote:
...snip...
>
> To get really technical, the difference between the cubic and
> hexagonal closest packed structures is that, if you form layers of
> spheres (pennies work OK for this analogy), once you lay our the
> first layer....
...snip again...
>
> 2. It must be really destructive (in terms of disturbing strong
> chemical bonds) to try to change an ABABABAB layering sequence into
> an ABCABCABC layering sequence. How can this happen? Does it ever
> happen? Is this part of the reason that diamond can get shot up
> from the depths of the earth and not get changed in to graphite?
>
___________________________________
R. Peter Richards
rpr at heidelberg.edu
Morphological crystallographer
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