Sciact
  • EN
  • RU

Water Dynamics in Bulk and Dispersed in Silica CaCl2 Hydrates Studied by 2H NMR Full article

Journal The Journal of Physical Chemistry C
ISSN: 1932-7447 , E-ISSN: 1932-7455
Output data Year: 2008, Volume: 112, Number: 33, Pages: 12853-12860 Pages count : 8 DOI: 10.1021/jp801223c
Tags DEUTERON MAGNETIC-RESONANCE; SPIN-LATTICE-RELAXATION; CALCIUM DICHLORIDE; PHASE-TRANSITIONS; LINE-SHAPES; MOLECULES; DIFFUSION; ROTATION; HALIDES; ICE
Authors Kolokolov Daniil I. 1,2 , Glaznev Ivan S. 1 , Aristov Yurii I. 1 , Stepanov Alexander G. 1 , Jobic Herve 2
Affiliations
1 BoreskoV Institute of Catalysis, Siberian Branch of the Russian Academy of Sciences, Prospekt Akademika LaVrentieVa 5, NoVosibirsk 630090, Russia
2 Institut de Recherches sur la Catalyse et l’EnVironnement de Lyon, CNRS, UniVersite de Lyon, 2 aVenue Albert Einstein, 69626 Villeurbanne, France

Funding (1)

1 Russian Foundation for Basic Research 05-03-34762

Abstract: The mobility of water in deuterated analogues of CaCl2·nH2O (n = 2, 4, 6) hydrates has been studied by solid-state 2H NMR spectroscopy. Dynamics of water molecules in hydrates dispersed in the mesopores of silica are compared with those in the bulk state. Analysis of the 2H NMR line shape and T1 and T2 relaxation times allowed us to characterize the water mobility in a wide temperature range (120−493 K). In both crystalline and melted hydrates, the mobility of water molecules is governed by O−D···Cl hydrogen bonding. Both bulk and dispersed hydrates have been found to exhibit three types of molecular motion. Two of these represent fast internal and local motions performed on a time scale of 10−10−10−11 s. The third, slow isotropic reorientation occurs on a time of 10−6−10−7 s. Dispersed hydrates become involved in the slow isotropic motion at temperatures 50−130 K lower than the corresponding bulk hydrates. The temperature TNMR at which dispersed hydrates are involved in isotropic motion represents the melting point of the hydrates located in the silica pores. The decrease of the melting point for the dispersed hydrates is in good accordance with the Gibbs−Thompson effect for dispersed materials. In dispersed hydrates, water molecules reorient isotropically 1 order of magnitude faster in the temperature range 230−490 K; that is, water is more mobile in the dispersed hydrates. The slow isotropic reorientation of water molecules is influenced by both the quantity of water in the hydrate and the dispersibility of the hydrates. In the case of the hydrate with n = 4, the activation energy of this motion decreases by ca. 3 times when the hydrate becomes dispersed in the silica pores.
Cite: Kolokolov D.I. , Glaznev I.S. , Aristov Y.I. , Stepanov A.G. , Jobic H.
Water Dynamics in Bulk and Dispersed in Silica CaCl2 Hydrates Studied by 2H NMR
The Journal of Physical Chemistry C. 2008. V.112. N33. P.12853-12860. DOI: 10.1021/jp801223c WOS Scopus РИНЦ ANCAN OpenAlex
Dates:
Submitted: Feb 11, 2008
Accepted: May 8, 2008
Published online: Jul 26, 2008
Published print: Aug 1, 2008
Identifiers:
Web of science: WOS:000258443000039
Scopus: 2-s2.0-51049104048
Elibrary: 13572125
Chemical Abstracts: 2008:899872
Chemical Abstracts (print): 149:275999
OpenAlex: W2002979438
Citing:
DB Citing
Web of science 22
Scopus 21
Elibrary 22
OpenAlex 22
Altmetrics: