Standard

Cation and anion sublattices in a series of typical cristal structures. / Borisov, S.; Magarill, S. A.; Pervukhina, N.

в: Journal of Structural Chemistry, Том 61, № 10, 10.2020, стр. 1585-1593.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Borisov, S, Magarill, SA & Pervukhina, N 2020, 'Cation and anion sublattices in a series of typical cristal structures', Journal of Structural Chemistry, Том. 61, № 10, стр. 1585-1593. https://doi.org/10.1134/S0022476620100108

APA

Borisov, S., Magarill, S. A., & Pervukhina, N. (2020). Cation and anion sublattices in a series of typical cristal structures. Journal of Structural Chemistry, 61(10), 1585-1593. https://doi.org/10.1134/S0022476620100108

Vancouver

Borisov S, Magarill SA, Pervukhina N. Cation and anion sublattices in a series of typical cristal structures. Journal of Structural Chemistry. 2020 окт.;61(10):1585-1593. doi: 10.1134/S0022476620100108

Author

Borisov, S. ; Magarill, S. A. ; Pervukhina, N. / Cation and anion sublattices in a series of typical cristal structures. в: Journal of Structural Chemistry. 2020 ; Том 61, № 10. стр. 1585-1593.

BibTeX

@article{0a9da05a419d4b5ba6dab3a683e2472c,
title = "Cation and anion sublattices in a series of typical cristal structures",
abstract = "Abstract: The crystallographic analysis of Rb 2NaAlF 6(Fd(Formula presented.)m) and (Al,V) 4(P 4O 12) 3((Formula presented.)3d) cubic structures and the trigonal structure of phenakite Be 2SiO4 R(Formula presented.) is performed. In Rb 2NaAlF 6 a large and heavy Rb cation stabilizes cation and anion sublattices, promoting their maximum symmetry. In the structure of cyclic tetraphosphate, the core is formed by the cation sublattice with a noticeable deviation of P cations from its nodes. The anion arrangement ordered by pseudo-cubic and hexagonal sublattices with pseudo-symmetry features dominates in the trigonal structure of phenakite. ",
keywords = "crystallographic analysis, {"}skeletal{"} sublattices, anion and cation sublattices, pseudo-symmetry, symmetry-stability, CRYSTAL-STRUCTURE, CRYSTALLOGRAPHIC ANALYSIS, FRAMEWORK, “skeletal” sublattices, symmetry–stability",
author = "S. Borisov and Magarill, {S. A.} and N. Pervukhina",
note = "Publisher Copyright: {\textcopyright} 2020, Pleiades Publishing, Ltd. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.",
year = "2020",
month = oct,
doi = "10.1134/S0022476620100108",
language = "English",
volume = "61",
pages = "1585--1593",
journal = "Journal of Structural Chemistry",
issn = "0022-4766",
publisher = "Springer GmbH & Co, Auslieferungs-Gesellschaf",
number = "10",

}

RIS

TY - JOUR

T1 - Cation and anion sublattices in a series of typical cristal structures

AU - Borisov, S.

AU - Magarill, S. A.

AU - Pervukhina, N.

N1 - Publisher Copyright: © 2020, Pleiades Publishing, Ltd. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.

PY - 2020/10

Y1 - 2020/10

N2 - Abstract: The crystallographic analysis of Rb 2NaAlF 6(Fd(Formula presented.)m) and (Al,V) 4(P 4O 12) 3((Formula presented.)3d) cubic structures and the trigonal structure of phenakite Be 2SiO4 R(Formula presented.) is performed. In Rb 2NaAlF 6 a large and heavy Rb cation stabilizes cation and anion sublattices, promoting their maximum symmetry. In the structure of cyclic tetraphosphate, the core is formed by the cation sublattice with a noticeable deviation of P cations from its nodes. The anion arrangement ordered by pseudo-cubic and hexagonal sublattices with pseudo-symmetry features dominates in the trigonal structure of phenakite.

AB - Abstract: The crystallographic analysis of Rb 2NaAlF 6(Fd(Formula presented.)m) and (Al,V) 4(P 4O 12) 3((Formula presented.)3d) cubic structures and the trigonal structure of phenakite Be 2SiO4 R(Formula presented.) is performed. In Rb 2NaAlF 6 a large and heavy Rb cation stabilizes cation and anion sublattices, promoting their maximum symmetry. In the structure of cyclic tetraphosphate, the core is formed by the cation sublattice with a noticeable deviation of P cations from its nodes. The anion arrangement ordered by pseudo-cubic and hexagonal sublattices with pseudo-symmetry features dominates in the trigonal structure of phenakite.

KW - crystallographic analysis

KW - "skeletal" sublattices

KW - anion and cation sublattices

KW - pseudo-symmetry

KW - symmetry-stability

KW - CRYSTAL-STRUCTURE

KW - CRYSTALLOGRAPHIC ANALYSIS

KW - FRAMEWORK

KW - “skeletal” sublattices

KW - symmetry–stability

UR - http://www.scopus.com/inward/record.url?scp=85106817688&partnerID=8YFLogxK

U2 - 10.1134/S0022476620100108

DO - 10.1134/S0022476620100108

M3 - Article

VL - 61

SP - 1585

EP - 1593

JO - Journal of Structural Chemistry

JF - Journal of Structural Chemistry

SN - 0022-4766

IS - 10

ER -

ID: 27359737