THE METAL-RICH PART OF THE CO-NI-P SYSTEM AT 800 °C
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dc.contributor.author | Drábek M. | |
dc.date.accessioned | 2024-10-18T08:57:30Z | |
dc.date.available | 2024-10-18T08:57:30Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=15406828 | |
dc.identifier.citation | European Journal of Mineralogy, 2006, 18, 5, 545-550 | |
dc.identifier.issn | 0935-1221 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/45945 | |
dc.description.abstract | The metal-rich portion of the Co-Ni-P system was studied experimentally at 800 °C by means of evacuated silica glass tube technique. Five binary phases: Co2P, Ni2P, Ni12P2 Ni 5 Ni3P and ive ternary phosphides solid solutions: (Co1-x,NixP,λ (Ni1-xCox) 2P (hexagonal), λ-(Co1-xNix) 2P (orthorhombic), (Co1-xNix)12 P5and (Co1-xNix)5P2 were found to be stable in the system. Cobalt has a significant influence on the structure of (Ni,Co)2P solid solutions and, therefore, cobalt contents might change the crystal structure of naturally occurring phosphides with the Ni/P = 2:1 ratio. Ni-rich, cobalt-containing phosphides with the Ni/P ratio = 3:1 and 2:1, isotypic with minerals schreibersite and barringerite, could possibly be found in meteorites. Likewise, phosphides with Ni/P ratio = 12:5 and 5:2 may possibly be found, but in close association with natural Ni-rich phosphides. © 2006 E. Schweizcrbart'schc Verlagsbuchhandlung. | |
dc.subject | CO | |
dc.subject | NI | |
dc.subject | PHASE RELATIONS | |
dc.subject | PHOSPHIDES | |
dc.title | THE METAL-RICH PART OF THE CO-NI-P SYSTEM AT 800 °C | |
dc.type | Статья | |
dc.identifier.doi | 10.1127/0935-1221/2006/0018-0545 |
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