dc.contributor.author |
Ovsyannikov A. |
|
dc.contributor.author |
Ferlay S. |
|
dc.contributor.author |
Solovieva S. |
|
dc.contributor.author |
Antipin I. |
|
dc.contributor.author |
Konovalov A. |
|
dc.contributor.author |
Kyritsakas N. |
|
dc.contributor.author |
Hosseini M. |
|
dc.date.accessioned |
2018-09-18T20:35:57Z |
|
dc.date.available |
2018-09-18T20:35:57Z |
|
dc.date.issued |
2014 |
|
dc.identifier.uri |
https://dspace.kpfu.ru/xmlui/handle/net/141548 |
|
dc.description.abstract |
Combinations of neutral tetrakis meta-pyridyl appended calix[4]arene derivatives in 1,3-A conformation as tectons 3 (tetrakis-meta-pyridyl- tetrathiacalix[4]arene) and 4 (tetrakis-meta- pyridyltetrathiatetramercaptocalix[4]arene) with MX2, behaving as a neutral metallatecton, lead to the formation of 2- and 3-D neutral coordination networks. In all cases, the metal centre adopts a distorted octahedral geometry with the two anions occupying the two apical positions. For compound 3-CdX 2 (X = Cl or Br), 4-CdBr2 and 4-FeCl2 similar porous diamondoid 3D networks, resulting from the tetrakis monodentate behaviour of the organic tectons, are formed. In marked contrast, for 4-CoX2 (X = Cl or Br), only two out of the four pyridyl units take part in the connectivity pattern leading thus to the formation of 2D grid type architectures. This journal is © the Partner Organisations 2014. |
|
dc.title |
Molecular tectonics: Generation of grid and porous diamondoid coordination networks by calixarene based tectons |
|
dc.type |
Article |
|
dc.relation.ispartofseries-issue |
18 |
|
dc.relation.ispartofseries-volume |
16 |
|
dc.collection |
Публикации сотрудников КФУ |
|
dc.relation.startpage |
3765 |
|
dc.source.id |
SCOPUS-2014-16-18-SID84898039178 |
|