VOLUME 82, NUMBER 11 PHYSICAL REVIEW LETTERS 15 MARCH 1999 Molecular Dynamics in Confining Space: From the Single Molecule to the Liquid State A. Huwe and F. Kremer* Department of Physics, University of Leipzig, D-04103 Leipzig, Germany P. Behrens Department of Chemistry, University of Hannover, D-30167 Hannover, Germany W. Schwieger Department of Chemistry, Martin-Luther-University Halle–Wittenberg, D-06108 Halle, Germany (Received 15 September 1998) The transition from the dynamics of isolated molecules to that of a bulk liquid is observed for the first time by analyzing the dielectric relaxation 10 22 10 9 Hzof ethylene glycol (EG) guest molecules confined to zeolitic host systems of different topology. Beyond a threshold channel size the liquid character is lost, indicated by a dramatically increased relaxation rate and an Arrhenius-like temperature dependence. Computer simulations of the molecular arrangement in a confining space prove that an ensemble as small as six molecules is sufficient to exhibit the dynamics of a bulk liquid. [S0031-9007(99)08701-3] PACS numbers: 64.70.Pf, 77.22.Gm The nature of glassy liquids is still not well understood and is the focus of worldwide scientific discussion [1–6]. Central questions are the length scale on which the mo- lecular fluctuations of a liquid take place, and under what conditions the transition from a single molecule behav- ior to that of a liquid occurs [7–17]. Guest molecules [e.g., ethylene glycol (EG) HO-CH 2 -CH 2 -OH] being con- fined to zeolitic host systems offer a unique possibility of studying this: While in sodalite—because of steric rea- sons—only one molecule of EG is present per zeolitic cage, other zeolites (e.g., silicalite and zeolite beta) pos- sess inner channel structures in which guest molecules can interact with each other. In measuring the dynamics of the (dielectrically active) guest molecules in (dielectrically in- active) host systems over a frequency range from 10 22 to 10 9 Hz, broadband dielectric spectroscopy proves to be an ideal experimental tool for these studies [14–19]. Silica sodalite is a clathrasil compound built from identical, so-called b cages, with a free inner diameter of 0.6 nm. Ethylene glycol is one of the structure-directing agents which controls the formation of silica sodalite [20,21]. The EG molecules become occluded during synthesis and cannot escape from the cages (unless they are thermally decomposed) [21]. Besides silica sodalite, silicalite-I and zeolite beta were used as zeolitic host systems with three-dimensional pore systems. Silicalite consists of pure silica and has two different types of elliptical channels with cross sections of 0.56 nm 3 0.53 nm and 0.55 nm 3 0.51 nm [22]. In zeolite beta, an aluminosilicate with a Si:Al ratio of 40, the channels in [100] and [010] directions have a diameter of 0.76 nm 3 0.64 nm, whereas the channels in the [001] direction have smaller pores 0.55 nm 3 0.55 nm[23]. Silicalite and zeolite beta are filled with guest molecules after synthesis and calcination. These nanoporous hosts are heated to 330 ± C with a temperature increase of 20 ± Ch and evacuated at 10 25 mbar for 36 h to remove water and other volatile impurities. Afterwards they are filled with EG from the vapor phase in a closed vacuum chamber at 175 ± C. The samples are cooled to room temperature and remain in the vacuum chamber for 24 h before the dielectric measurements are carried out. The dielectric measurements were performed using two different systems based on different measurement prin- ciples: Between 10 22 and 10 7 Hz, frequency response analysis is carried out (Solatron–Schlumberger frequency response analyzer FRA 1260 with a Novocontrol ac- tive sample cell BDC–S). From 10 6 to 1.8 3 10 9 Hz a Hewlett-Packard impedance analyzer (HP 4291A) is employed. The sample temperatures are controlled by means of a nitrogen gas jet having a stability better than 60.05 K. Details of the setup may be found in Ref. [24]. For the analysis of the dielectric measurements the imagi- nary part e 00 of the dielectric function is fitted using a superposition of a conductivity contribution and a gen- eralized relaxation function according to Havriliak and Negami [25], e 00 s 0 e 0 a v s 2 Im " De 1 1 i vt a g # . (1) In this notation, e 0 is the vacuum permittivity, s 0 is the dc conductivity, and De is the dielectric strength. a and g describe the symmetric and asymmetric broadening of the relaxation time distribution function. From the fits according to Eq. (1), the mean relaxation rate 1t max can be deduced which is given at the frequency of maximum dielectric loss e 00 for a certain temperature. It is shown (Fig. 1) that the relaxation rates for EG in zeolite beta and silicalite are separated by several orders of magnitude and that the relaxation strength of EG in sodalite is 2338 0031-900799 82(11) 2338(4)$15.00 © 1999 The American Physical Society