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longitudinal dispersion in nonuniform isotropic porous media

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48<br />

CHAPTER 3<br />

A THEORETICAL MODEL FOR PERMEABILITY AND LONGITUDINAL DISPERSION<br />

IN NONUNIFORM POROUS MEDIA<br />

In this chapter, a theoretical method is developed for comput<strong>in</strong>g<br />

permeability and <strong>longitud<strong>in</strong>al</strong> <strong>dispersion</strong> <strong>in</strong> <strong>isotropic</strong>, <strong>nonuniform</strong><br />

<strong>porous</strong> <strong>media</strong> based on structural features of the medium. As discussed<br />

<strong>in</strong> Chapter 2, the spectrum of length scales present <strong>in</strong> a <strong>nonuniform</strong><br />

medium is important <strong>in</strong> determ<strong>in</strong><strong>in</strong>g the transport behavior of miscible<br />

solutes. Because of additional variables describ<strong>in</strong>g the distribution<br />

of length scales, there are more dimensionless groups to correlate<br />

through experimentation. S<strong>in</strong>ce the range of parameters is large, it<br />

would be helpful to have reliable models. Of the models presented <strong>in</strong><br />

Chapter 2, the network model, statistical capillary tube model, and the<br />

volume-averag<strong>in</strong>g model are capable of be<strong>in</strong>g extended to <strong>nonuniform</strong><br />

<strong>media</strong>. The model to be developed here is an extension of the random<br />

capillary tube model proposed by Saffman (1959). No extensions were<br />

attempted with the network model or the volume-averag<strong>in</strong>g model.<br />

As for the orig<strong>in</strong>al model for uniform <strong>media</strong> (Saffman, 1959), the<br />

extended model is also limited to high Pec1et number flows. The model<br />

follows the orig<strong>in</strong>al Saffman (1959) model closely, and is similar <strong>in</strong><br />

some respects to the <strong>nonuniform</strong> <strong>media</strong> model proposed by Har<strong>in</strong>g and<br />

Greenkorn (1970); however, there are some important differences:<br />

1. Molecular diffusion is <strong>in</strong>cluded as <strong>in</strong> the Saffman (1959) model such<br />

that an asymptotic <strong>longitud<strong>in</strong>al</strong> <strong>dispersion</strong> coefficient may be obta<strong>in</strong>ed,<br />

<strong>in</strong> contrast to the Har<strong>in</strong>g and Greenkorn (1970) model.

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