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dc.contributor.author | Kristavchuk A. | |
dc.contributor.author | Vymazalova A. | |
dc.contributor.author | Osadchii E. | |
dc.contributor.author | Vikentyev I. | |
dc.contributor.author | Chareev D. | |
dc.contributor.author | Bortnikov N. | |
dc.date.accessioned | 2020-01-21T20:45:19Z | |
dc.date.available | 2020-01-21T20:45:19Z | |
dc.date.issued | 2019 | |
dc.identifier.issn | 1028-334X | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/157729 | |
dc.description.abstract | © 2019, Pleiades Publishing, Ltd. Abstract: The reactions of 6Ag(cr) + 3PdSe2(cr) = 2Ag2Se(cr) + Ag2Pd3Se4(cr) and 12Ag(cr) + 5PtSe2(cr) = 6Ag2Se(cr) + Pt5Se4(cr) were studied with the EMF method in a completely solid-state galvanic cell with an Ag ion-conducting solid electrolyte with overall gas space (argon under atmospheric pressure). The EMF vs. temperature dependencies were obtained in the temperature ranges of Т = 425–648 K and 501–713 K, respectively. Then, they were recalculated for gaseous Se fugacity in dependence on the temperature for nonvariant equilibriums of Ag2Pd3Se4 (chrisstanleyite)–β-PdSe2 (the phase, which transforms into verbeekite under low temperatures)–Ag2Se (naumannite) and Pt5Se4 (luberoite)–PtSe2 (sudovikovite): logf Se2(gas) (Ag2Pd3Se4/Ag2Se/PdSe2) = 7.710 ± 0.050 – 8.524 ± 0.026(1000/T), logfSe2(gas) (Pt5Se4/PtSe2) = 7.135 ± 0.027 – 12.274 ± 0.016(1000/T). | |
dc.relation.ispartofseries | Doklady Earth Sciences | |
dc.title | The Se<inf>2</inf> (Gas) Fugacity in Systems with Noble Metals: Chrisstanleyite Ag<inf>2</inf>Pd<inf>3</inf>Se<inf>4</inf> – Naumannite Ag<inf>2</inf>Se–β-PdSe<inf>2</inf> and Luberoite Pt<inf>5</inf>Se<inf>4</inf>–Sudovikovite PtSe<inf>2</inf> | |
dc.type | Article | |
dc.relation.ispartofseries-issue | 2 | |
dc.relation.ispartofseries-volume | 485 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 439 | |
dc.source.id | SCOPUS1028334X-2019-485-2-SID85066947751 |