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Author: Subject: Diamond synthesis
Nicodem
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[*] posted on 21-11-2015 at 02:16


I noticed this thread a bit late, but nevertheless, since it is not about organic chemistry (at least by product) and since it is mainly just a some idle talk, I'm moving it to the Miscellaneous section.

Quote: Originally posted by morsagh  
Think about intermediate, that can be C(CBr3)4 because of better reactivity of substituted carbon no?

There is no way something that monstrous could exist at normal conditions. Just consider the thermodynamic instability of anything crowded like that.
Besides, the reduction of CX4 with metals or electroreduction is known to give graphite (or the corresponding carbides where applicable). In protic environment the reduction gives partially reduced products like CH2X2. (for a short review, see: Carbyne and Carbynoid Structures, 1999, pages 198-199).
The closest reduction that gives tetrahedral carbon-based polymeric materials, is the reduction of CHX3 with some alkali and alkaline earth metals based reducing reagents to give polycarbynes of the structure [HC]n (the carbon is sp3). If allowed to go wildly speculative, I would say that this material might be a suitable starting material for growing diamond crystals at not particularly high pressures, if made soluble or volatile and a suitable oxidation system could be applied. Too bad I can't think of any such.




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Nicodem
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[*] posted on 4-12-2015 at 08:52


Didn't Moissan in the 1800s create very small diamonds by mixing charcoal in melted iron and then cooling in a water bath? The idea was that the contracting iron upon cooling created tremendous pressure upon the trapped carbon.
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[*] posted on 4-12-2015 at 09:00



Quote:

The contraction generated by the cooling supposedly produced the high pressure required to transform graphite into diamond. Moissan published his work in a series of articles in the 1890s.[7]
Many other scientists tried to replicate his experiments. Sir William Crookes claimed success in 1909.[8] Otto Ruff claimed in 1917 to have produced diamonds up to 7 mm in diameter,[9] but later retracted his statement.[10] In 1926, Dr. J Willard Hershey of McPherson College replicated Moissan's and Ruff's experiments,[11][12] producing a synthetic diamond; that specimen is on display at the McPherson Museum in Kansas.[13] Despite the claims of Moissan, Ruff, and Hershey, other experimenters were unable to reproduce their synthesis




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[*] posted on 10-1-2016 at 13:21


Even natural diamonds are slowly changing back to graphite(extremly slowly ) becouse diamond is only high temperature allotrope of carbon.
-Diamonds are "unstable" at normal temperature and pressure and they also can be produced only in conditions which are natural for diamonds (high temp. and pressure).

[Edited on 10-1-2016 by crystal grower]




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[*] posted on 10-1-2016 at 18:59


Quote: Originally posted by crystal grower  
Even natural diamonds are slowly changing back to graphite(extremly slowly ) becouse diamond is only high temperature allotrope of carbon.
[Edited on 10-1-2016 by crystal grower]


They are thermodynamically unstable, in that graphite is a lower energy form - but diamonds are not changing to graphite.

Natural diamonds are over one billion years old (dated in a range of 1.2-2.7 billion years old) and clearly are not converting to graphite, despite the fact that a lot of them spent a lot of their time deep in the crust where it is hot.

This should be placed in the same category as claims of glass flowing at room temperature, i.e. the atomic arrangement is actually stable - unable to rearrange itself no matter how thermodynamically favored.

See:
http://www.gia.edu/gems-gemology/WN13-advances-diamond-geolo...
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[*] posted on 11-1-2016 at 07:37


Quote: Originally posted by careysub  
Quote: Originally posted by crystal grower  
Even natural diamonds are slowly changing back to graphite(extremly slowly ) becouse diamond is only high temperature allotrope of carbon.
[Edited on 10-1-2016 by crystal grower]


They are thermodynamically unstable, in that graphite is a lower energy form - but diamonds are not changing to graphite.

Natural diamonds are over one billion years old (dated in a range of 1.2-2.7 billion years old) and clearly are not converting to graphite, despite the fact that a lot of them spent a lot of their time deep in the crust where it is hot.

This should be placed in the same category as claims of glass flowing at room temperature, i.e. the atomic arrangement is actually stable - unable to rearrange itself no matter how thermodynamically favored.

See:
http://www.gia.edu/gems-gemology/WN13-advances-diamond-geolo...


Ive heard some scientist saying that diamonds are changing but in extreme time period (but what u re saying makes sense too)
Main thing I wanted to explain was that diamonds cant be produced in normal conditions according thermodynamical stability of diamond.




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[*] posted on 14-1-2016 at 06:16


Why start a new tread when one already exists?

Growing synthetic diamonds at home




PH Z (PHILOU Zrealone)

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