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The Potential Energy Landscape and Mechanisms of Diffusion in Liquids

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 Added by Tom Keyes
 Publication date 2001
  fields Physics
and research's language is English




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The mechanism of diffusion in supercooled liquids is investigated from the potential energy landscape point of view, with emphasis on the crossover from high- to low-T dynamics. Molecular dynamics simulations with a time dependent mapping to the associated local mininum or inherent structure (IS) are performed on unit-density Lennard-Jones (LJ). New dynamical quantities introduced include r2_{is}(t), the mean-square displacement (MSD) within a basin of attraction of an IS, R2(t), the MSD of the IS itself, and g_{loc}(t) the mean waiting time in a cooperative region. At intermediate T, r2_{is}(t) posesses an interval of linear t-dependence allowing calculation of an intrabasin diffusion constant D_{is}. Near T_{c} diffusion is intrabasin dominated with D = D_{is}. Below T_{c} the local waiting time tau_{loc} exceeds the time, tau_{pl}, needed for the system to explore the basin, indicating the action of barriers. The distinction between motion among the IS below T_{c} and saddle, or border dynamics above T_{c} is discussed.

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149 - T. Keyes , J. Chowdhary 2003
The inherent structures ({it IS}) are the local minima of the potential energy surface or landscape, $U({bf r})$, of an {it N} atom system. Stillinger has given an exact {it IS} formulation of thermodynamics. Here the implications for the equation of state are investigated. It is shown that the van der Waals ({it vdW}) equation, with density-dependent $a$ and $b$ coefficients, holds on the high-temperature plateau of the averaged {it IS} energy. However, an additional ``landscape contribution to the pressure is found at lower $T$. The resulting extended {it vdW} equation, unlike the original, is capable of yielding a water-like density anomaly, flat isotherms in the coexistence region {it vs} {it vdW} loops, and several other desirable features. The plateau energy, the width of the distribution of {it IS}, and the ``top of the landscape temperature are simulated over a broad reduced density range, $2.0 ge rho ge 0.20$, in the Lennard-Jones fluid. Fits to the data yield an explicit equation of state, which is argued to be useful at high density; it nevertheless reproduces the known values of $a$ and $b$ at the critical point.
68 - T. Keyes , J. Chowdhary 2000
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