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Self diffusion constants experimental results

Fig. 5.3. Log-log plot of the self-diffusion constant D of polymer melts vs. chain length N. D is normalized by the diffusion constant of the Rouse limit, DRoUse> which is reached for short chain lengths. N is normalized by Ne, which is estimated from the kink in the log-log plot of the mean-square displacement of inner monomers vs. time [gi (t) vs. t]. Molecular dynamics results [177] and experimental data on PE [178] are compared with the MC results [40] for the athermal bond fluctuation model. From [40]... Fig. 5.3. Log-log plot of the self-diffusion constant D of polymer melts vs. chain length N. D is normalized by the diffusion constant of the Rouse limit, DRoUse> which is reached for short chain lengths. N is normalized by Ne, which is estimated from the kink in the log-log plot of the mean-square displacement of inner monomers vs. time [gi (t) vs. t]. Molecular dynamics results [177] and experimental data on PE [178] are compared with the MC results [40] for the athermal bond fluctuation model. From [40]...
We review Monte Carlo calculations of phase transitions and ordering behavior in lattice gas models of adsorbed layers on surfaces. The technical aspects of Monte Carlo methods are briefly summarized and results for a wide variety of models are described. Included are calculations of internal energies and order parameters for these models as a function of temperature and coverage along with adsorption isotherms and dynamic quantities such as self-diffusion constants. We also show results which are applicable to the interpretation of experimental data on physical systems such as H on Pd(lOO) and H on Fe(110). Other studies which are presented address fundamental theoretical questions about the nature of phase transitions in a two-dimensional geometry such as the existence of Kosterlitz-Thouless transitions or the nature of dynamic critical exponents. Lastly, we briefly mention multilayer adsorption and wetting phenomena and touch on the kinetics of domain growth at surfaces. [Pg.92]

Table 9 The self-diffusion constant for water and the ubiquitin molecule D p in aqueous solutions as calculated with different force fields for the water. In addition, i and T2 are rotational relaxation times for the ubiquitin molecule. Where possible, the results are compared with experimental values. All results are from ref. 36... [Pg.80]

When quantitatively comparing simulation results with experimental data, the choice of force field is crucial. Because our focus is the dynamics of hydration water, we use the widely familiar TlP4P-Ew model. It has a computed self-diffusion constant that agrees well with experimental values and with the T scale (its density maximum is at 274K, only 3K below the correct value) down to 230K. Thus, we... [Pg.283]

FIGURE 7.6. Plots of self-diffusion constants versus the reciprocal temperature in three discotic liquid crystals. The circles and squares correspond to diffusion along z and x, respectively, while the triangles refer to the isotropic liquid. The open and filled symbols refer to different experimental runs. The vertical bars represent the uncertainty in the result for the single measurements (after Ref. [7.65]). [Pg.205]

Our previous study (J 6) of self diffusion in compressed supercritical water compared the experimental results to the predictions of the dilute polar gas model of Monchick and Mason (39). The model, using a Stockmayer potential for the evaluation of the collision integrals and a temperature dependent hard sphere diameters, gave a good description of the temperature and pressure dependence of the diffusion. Unfortunately, a similar detailed analysis of the self diffusion of supercritical toluene is prevented by the lack of density data at supercritical conditions. Viscosities of toluene from 320°C to 470°C at constant volumes corresponding to densities from p/pQ - 0.5 to 1.8 have been reported ( 4 ). However, without PVT data, we cannot calculate the corresponding values of the pressure. [Pg.22]

Self-diffusion of ions in silica has been measured both experimentally and computationally. Experimentally, Mikkelsen (Mikkelsen Jr. 1984) used SIMS (secondary ion mass spectroscopy) to measure the concentration profiles of labeled O deposited on silica to obtain the diffusion coefficient. Brebec et al (Brebec et al. 1980) used labeled Si and SIMS analysis for determining Si diffusion. Hetherington (Hetherington et al. 1964) used viscosity measurements of commercial silica to determine diffusion constants. Their experimental data are shown in Table 1, along with results from several computational studies. [Pg.142]

Figure 2. Plot of the self- Figure 2. Plot of the self-<liffusion constant D of silicon atoms (Si) and oxygen atoms (O) in molten SiC j as a function of inverse temperature. The symbols in the upper left part are the results from molecular dynamics simulations and the data in the lower right part stems from experiments [SO, SI]. The thin straight lines show simple Arrhenius behavior (D exp(— a/( B ))) with various choices of the activation energy En, as indicated in the figure. The vertical broken lines indicate the experimental glass transition temperature, Tg = 14S0 K, as well as values for Tg that one obtains if one extrapolates the data from the simulations to low temperatures and then estimates Tg from the experimental value of the O diffusion constant Dq(T = Tg ) = 10 cm /sec 7 = 1381 K) or the Si diffusion constant, respectively (Dsi( = Tg ) = 5.10 cm /sec Tg = 1303 K). From Horbach andKob[13],...

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