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longitudinal dispersion in nonuniform isotropic porous media

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iv<br />

ABSTRACT<br />

A theoretical and experimental <strong>in</strong>vestigation has been made of the<br />

<strong>longitud<strong>in</strong>al</strong> <strong>dispersion</strong> of chemically and dynamically passive solutes<br />

dur<strong>in</strong>g flow through <strong>nonuniform</strong>, <strong>isotropic</strong> <strong>porous</strong> <strong>media</strong>. Both<br />

theoretical and experimental results are limited to the high Pee let<br />

number, low Reynolds number flow regime. The goal of the theoretical<br />

<strong>in</strong>vestigation is to provide a quantitative method for calculat<strong>in</strong>g the<br />

coefficient of <strong>longitud<strong>in</strong>al</strong> <strong>dispersion</strong> us<strong>in</strong>g only measurable structural<br />

features of the <strong>porous</strong> medium and the characteristics of the carry<strong>in</strong>g<br />

fluid and solute. A <strong>nonuniform</strong> <strong>porous</strong> medium conta<strong>in</strong>s variations Ln<br />

gra<strong>in</strong> scale pore structure, but is homogeneous at the macroscopic level<br />

for quantities such as the permeability or porosity.<br />

A random capillary tube network model of <strong>nonuniform</strong> <strong>porous</strong> <strong>media</strong><br />

is developed which uses a pore radius distribution and pore length<br />

distribution to characterize the gra<strong>in</strong> scale structure of <strong>porous</strong> <strong>media</strong>.<br />

The analysis gives the asymptotic <strong>longitud<strong>in</strong>al</strong> <strong>dispersion</strong> coefficient<br />

<strong>in</strong> terms of <strong>in</strong>tegrals of k<strong>in</strong>ematic properties of solute particles<br />

flow<strong>in</strong>g through <strong>in</strong>dividual, random capillary tubes. However, shear<br />

<strong>dispersion</strong> with<strong>in</strong> <strong>in</strong>dividual capillary tubes is found to have<br />

negligible impact on the overall <strong>longitud<strong>in</strong>al</strong> <strong>dispersion</strong> <strong>in</strong> <strong>porous</strong><br />

<strong>media</strong>. The <strong>dispersion</strong> <strong>in</strong>tegrals are evaluated us<strong>in</strong>g a Monte Carlo<br />

<strong>in</strong>tegration technique. An analysis of the permeability <strong>in</strong> <strong>nonuniform</strong><br />

<strong>porous</strong> <strong>media</strong> is used to establish a proper flow field for the analysis<br />

of <strong>longitud<strong>in</strong>al</strong> <strong>dispersion</strong>.

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