<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>G. Dagan</dc:contributor>
  <dc:contributor>A.M. Shapiro</dc:contributor>
  <dc:creator>V.D. Cvetkovic</dc:creator>
  <dc:date>1991</dc:date>
  <dc:description>The problem of one-dimensional transport of passive solute by a random steady velocity field is investigated. This problem is representative of solute movement in porous media, for example, in vertical flow through a horizontally stratified formation of variable porosity with a constant flux at the soil surface. Relating moments of particle travel time and displacement, exact expressions for the advection and dispersion coefficients in the Focker-Planck equation are compared with the perturbation results for large distances. The first- and second-order approximations for the dispersion coefficient are robust for a lognormal velocity field. The mean Lagrangian velocity is the harmonic mean of the Eulerian velocity for large distances. This is an artifact of one-dimensional flow where the continuity equation provides for a divergence free fluid flux, rather than a divergence free fluid velocity. ?? 1991 Springer-Verlag.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/BF01544177</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>An exact solution of solute transport by one-dimensional random velocity fields</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>