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The influence of extraframework cations on the behavior of K-exchanged gonnardite at high pressure. / Seryotkin, Yu V.; Dement’ev, S. N.; Ancharov, A. I.
в: Journal of Structural Chemistry, Том 57, № 7, 01.12.2016, стр. 1386-1391.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - The influence of extraframework cations on the behavior of K-exchanged gonnardite at high pressure
AU - Seryotkin, Yu V.
AU - Dement’ev, S. N.
AU - Ancharov, A. I.
PY - 2016/12/1
Y1 - 2016/12/1
N2 - The behavior of K-exchanged gonnardite K2.18Na0.04Ca0.02(H2O)2.2[Al2.26Si2.74O10] at compression in penetrating water-containing medium was studied by synchrotron powder diffraction in diamond anvil cell. In contrast to the initial gonnardite, which exhibits the transition to high-hydrated paranatrolite at elevated humidity, its K-exchanged form is not capable of over-hydration even at high pressure. Within the whole studied pressure range (up to 4.8 GPa) the sample experiences the compression. At 3.5-4 GPa the compression anomaly is observed, which is interpreted as a phase transition accompanied by the symmetry lowering from tetragonal to monoclinic. The high-pressure structure evolution of K-exchanged forms of gonnardite and natrolite is compared; the difference in their behavior is explained by distinct configuration of the framework water-cation subsystem.
AB - The behavior of K-exchanged gonnardite K2.18Na0.04Ca0.02(H2O)2.2[Al2.26Si2.74O10] at compression in penetrating water-containing medium was studied by synchrotron powder diffraction in diamond anvil cell. In contrast to the initial gonnardite, which exhibits the transition to high-hydrated paranatrolite at elevated humidity, its K-exchanged form is not capable of over-hydration even at high pressure. Within the whole studied pressure range (up to 4.8 GPa) the sample experiences the compression. At 3.5-4 GPa the compression anomaly is observed, which is interpreted as a phase transition accompanied by the symmetry lowering from tetragonal to monoclinic. The high-pressure structure evolution of K-exchanged forms of gonnardite and natrolite is compared; the difference in their behavior is explained by distinct configuration of the framework water-cation subsystem.
KW - high pressure
KW - K-gonnardite
KW - K-natrolite
KW - over-hydration
KW - zeolites
UR - http://www.scopus.com/inward/record.url?scp=85009948995&partnerID=8YFLogxK
U2 - 10.1134/S002247661607012X
DO - 10.1134/S002247661607012X
M3 - Article
AN - SCOPUS:85009948995
VL - 57
SP - 1386
EP - 1391
JO - Journal of Structural Chemistry
JF - Journal of Structural Chemistry
SN - 0022-4766
IS - 7
ER -
ID: 25758296