Dynamics of supercooled water in highly compacted clays studied by neutron scattering

Beitrag in einer Fachzeitschrift

Details zur Publikation

Autorinnen und Autoren: González Sánchez F, Juranyi F, Gimmi T, Van Loon LR, Seydel T, Unruh T
Zeitschrift: Journal of Physics: Condensed Matter
Jahr der Veröffentlichung: 2008
Band: 20
Heftnummer: 41
ISSN: 0953-8984
eISSN: 1361-648X


The freezing behavior of water confined in compacted charged and uncharged clays (montmorillonite in Na-and Ca-forms, illite in Na-and Ca-forms, kaolinite and pyrophyllite) was investigated by neutron scattering. Firstly, the amount of frozen (immobile) water was measured as a function of temperature at the IN16 backscattering spectrometer, Institute Laue-Langevin (ILL). Water in uncharged, partly hydrophobic (kaolinite) and fully hydrophobic (pyrophyllite) clays exhibited a similar freezing and melting behavior to that of bulk water. In contrast, water in charged clays which are hydrophilic could be significantly supercooled. To observe the water dynamics in these clays, further experiments were performed using quasielastic neutron scattering. At temperatures of 250, 260 and 270 K the diffusive motion of water could still be observed, but with a strong reduction in the water mobility as compared with the values obtained above 273 K. The diffusion coefficients followed a non-Arrhenius temperature dependence well described by the Vogel-Fulcher-Tammann and the fractional power relations. The fits revealed that Na-and Ca-montmorillonite and Ca-illite have similar Vogel-Fulcher-Tammann temperatures (T-VFT, often referred to as the glass transition temperature) of similar to 120 K and similar temperatures at which the water undergoes the 'strong-fragile' transition, T-s similar to 210 K. On the other hand, Na-illite had significantly larger values of T-VFT similar to 180 K and T-s similar to 240 K. Surprisingly, Ca-illite has a similar freezing behavior of water to that of montmorillonites, even though it has a rather different structure. We attribute this to the stronger hydration of Ca ions as compared with the Na ions occurring in the illite clays.

FAU-Autorinnen und Autoren / FAU-Herausgeberinnen und Herausgeber

Unruh, Tobias Prof. Dr.
Professur für Nanomaterialcharakterisierung (Streumethoden)

Einrichtungen weiterer Autorinnen und Autoren

Institute Laue-Langevin (ILL)
Paul Scherrer Institute (PSI)


González Sánchez, F., Juranyi, F., Gimmi, T., Van Loon, L.R., Seydel, T., & Unruh, T. (2008). Dynamics of supercooled water in highly compacted clays studied by neutron scattering. Journal of Physics: Condensed Matter, 20(41). https://dx.doi.org/10.1088/0953-8984/20/41/415102

González Sánchez, Fátima, et al. "Dynamics of supercooled water in highly compacted clays studied by neutron scattering." Journal of Physics: Condensed Matter 20.41 (2008).


Zuletzt aktualisiert 2018-10-08 um 15:39