HAL Id: jpa-00222501
https://hal.archives-ouvertes.fr/jpa-00222501
Submitted on 1 Jan 1982
HAL is a multi-disciplinary open access archive for the deposit and dissemination of sci- entific research documents, whether they are pub- lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.
L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.
COMPUTER SIMULATION STUDIES OF
MIGRATION MECHANISMS IN IONIC GLASSES AND LIQUIDS
C. Angell, P. Cheeseman, S. Tamaddon
To cite this version:
C. Angell, P. Cheeseman, S. Tamaddon. COMPUTER SIMULATION STUDIES OF MIGRATION
MECHANISMS IN IONIC GLASSES AND LIQUIDS. Journal de Physique Colloques, 1982, 43 (C9),
pp.C9-381-C9-385. �10.1051/jphyscol:1982972�. �jpa-00222501�
Colloque C9, supplément au n°12, Tome 43, décembre 1982 page C9-381
COMPUTER SIMULATION STUDIES OF MIGRATION MECHANISMS IN IONIC GLASSES AND LIQUIDS
C.A. A n g e l l , P.A. Cheeseman and S. Tamaddon
Department of Chemistvy Thωue University, West Lafayette, Indiana 47907, U.S.A.
Résumé.- Les mécanismes de m i g r a t i o n des c a t i o n s e t d e s a n i o n s dans l e s v e r r e s e t l i q u i d e s du type s i l i c a t e e t f l u o r u r e s i m u l é s o n t é t é é t u d i é s p a r des méthodes de dynamique m o l é c u l a i r e à l ' o r d i n a t e u r . On donne des exemples m o n t r a n t l a p u i s s a n c e de l a m é t h o d e . On montre l ' e x i s t e n c e d ' u n minimum de v i s c o s i t é aux p r e s s i o n s é l e - v é e s pour des a l u m i n o s i l i c a t e s f o n d u s .
Abstract. - Ion dynamics computer simulations of the migration of cation and anions in "computer glasses" and liquids of silicate and fluoride types are reported, and examples of the diagnostic power of the simulation method are given. The existence of high pressure minima in the viscosity of molten aluminosilicates is indicated.
Introduction. - In this paper we will review briefly the way in which the use of ion dynamics computer simulation studies can help develop concepts for, and models of, ionic motion in both rigid glasses and high-temperature ionic liquids. The descrip- tion will cover (1) cases in which the physical properties of the normal substance are directly simulated, and (2) cases in which the special ability of the simulation programs to introduce changes in the system (for instance, a change of mass without change of interionic potential) which cannot be introduced in laboratory experiments, is used to reveal features of the migration mechanism which otherwise might be diffi- cult to recognize.
Considering migration in solid glasses first, we reproduce in Fig. 1 the a.c.
conductivity (or absorptivity) over a wide frequency range for a well-studied system, Na20'3Si02 glass, in order to draw attention to those features of the observed be- havior which the simulation should help to explain. Fig. 1 shows the electrical conductivity over a wide frequency range from 10~1-10 Hz based on data from a num- ber of different studies to which reference can be found in Ref. 1. We see, firstly, a frequency-independent but strongly temperature-dependent part of the conductivity response which is related directly to the diffusivity of the alkali cation in this material. Secondly, we see a frequency-dependent region with a maximum at M0*--> Hz in which the conductivity is comparatively independent of temperature. This is ob- served experimentally using far infra-red spectroscopy. Thirdly, we see a more or less temperature independent, constant slope, regime which connects the high fre- quency and low frequency extremes. This frequency-dependent regime conforms to the simple relation
a(f) = kf
a(1)
where a = 1.0.
The simulation, then, should show features which correspond with each of these regions and hopefully will provide a mechanistic interpretation of their existence.
Simulations of the cases of alkali migration in silicate glasses, and also for fluoride anion conduction in fluorozirconate glasses, were performed using a multi- component ion dynamics program described in previous publications (2). The potential of interaction for the various possible pairs of ions in the simulated stretches is assumed to be a simple two term function (coulomb + exponential repulsion)
U. .(r) = e z.z./r.. + b.. exp [(a. + a. - r..)/p] (2) ij 1 3 1 0 13 ^ 1 : 13
Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphyscol:1982972
C9-382 JOURNAL DE PHYSIQUE
The p a r a m e t e r s u s e d i n Eq. ( 2 ) i n t h i s s t u d y a r e c o l l e c t e d i n T a b l e 1 below.
The number of i o n s i n t h e p r i m a r y c o m p u t a t i o n a l box was of o r d e r 200, and d e t a i l s of t h e c a l c u l a t i o n and of l i m i t a t i o n s on i t s a c c u r a c y a r e g i v e n i n e a r l i e r p u b l i c a - t i o n s (2,7)
T a b l e 1
A l k a l i S i l i c a t e and Alumino S i l i c a t e Barium F l u o r o z i r c o n a t e
S p e c i e s a b . ( 10-13erg)
~j p
=0.29 S p e c i e s a bi . ( l o a 1 3 e r g )
S i 0 Na A1 2 r Ba F
S i 1 . 3 3 3.42 2 r 1 . 2 8 3.80
0 1 . 4 2 2.117 0.814 Ba 1 . 4 9 3.325 2.85
Na 1.252 2.898 1 . 5 9 5 2.375 F 1 . 3 3 2.613 2.138 1.425
A1 1.358 3.372 2.070 2.850 3.325
cm-'
1 10 I00 KXX) 'uDlo RAD1u M I ~ R O' ~ l k Ik
-
- 'E
1000-0
a
Q) 10-
Z