Source:http://linkedlifedata.com/resource/pubmed/id/14564003
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Predicate | Object |
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rdf:type | |
lifeskim:mentions | |
pubmed:issue |
5644
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pubmed:dateCreated |
2003-10-17
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pubmed:abstractText |
Compressed under ambient temperature, graphite undergoes a transition at approximately 17 gigapascals. The near K-edge spectroscopy of carbon using synchrotron x-ray inelastic scattering reveals that half of the pi-bonds between graphite layers convert to sigma-bonds, whereas the other half remain as pi-bonds in the high-pressure form. The x-ray diffraction pattern of the high-pressure form is consistent with a distorted graphite structure in which bridging carbon atoms between graphite layers pair and form sigma-bonds, whereas the nonbridging carbon atoms remain unpaired with pi-bonds. The high-pressure form is superhard, capable of indenting cubic-diamond single crystals.
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pubmed:language |
eng
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pubmed:journal | |
pubmed:status |
PubMed-not-MEDLINE
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pubmed:month |
Oct
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pubmed:issn |
1095-9203
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pubmed:author | |
pubmed:issnType |
Electronic
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pubmed:day |
17
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pubmed:volume |
302
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pubmed:owner |
NLM
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pubmed:authorsComplete |
Y
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pubmed:pagination |
425-7
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pubmed:dateRevised |
2007-3-19
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pubmed:year |
2003
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pubmed:articleTitle |
Bonding changes in compressed superhard graphite.
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pubmed:affiliation |
Department of the Geophysical Sciences, University of Chicago, Chicago, IL 60637, USA. wmao@chicago.edu
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pubmed:publicationType |
Journal Article
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