longitudinal dispersion in nonuniform isotropic porous media

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154 number flows since the advection time scale for mass transfer becomes shorter while the diffusion time scale remains constant. The conclusions are summarized in the next chapter, and suggestions for future work are presented.
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LONGITUDINAL DISPERSION IN NONUNIFO
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ii ACKNOWLEDGEMENTS This research p
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iv ABSTRACT A theoretical and exper
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ACKNOWLEDGEMENTS ABSTRACT LIST OF F
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viii TABLE OF CONTENTS (continued)
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4.2 4.3 4.4 4.5 4.6 4.7 4.8 4.9 4.1
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Table 3.1 3.2 4.1 4.2 4.3 4.4 4.5 5
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o en -o ::J o CD FLOW .. Solute Con
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porous medium and an unconsolidated
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20 CHAPTER 2 LITERATURE REVIEW Tran
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(1/2) V yd s From experiments, they
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39 governed by an effective advecti
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2.4 SUmmary 46 Several different cl
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48 CHAPTER 3 A THEORETICAL MODEL FO
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Q = 52 (3.1) where P'cos8 is the pr
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I 1 FLOW 3 PORE • JUNCTION 57 CAP
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shows a histogram of 10000 particle
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This expression gives the frequency
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PERMEABILITY where 82 TABLE 3.1 Sum
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LITER RESERVOIR (FRESH OR SALINE) O
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100 screens are needed to character
Page 120 and 121: VQ!gme-W@ight@d pistripgtiop(a) Gra
Page 123: 108 space in the medium, while the
Page 135: 120 When one fluid displaces anothe
Page 141: 126 medium type. This deviation of
Page 149: D v 134 Table 4.5 Longitudinal Disp
Page 152 and 153: 137 Monte Carlo integration techniq
Page 160 and 161: 145 Table 5.3 Computed Results for
Page 166 and 167: where a m £ m total porosity 151 =
Page 170: 155 CHAPTER 6 SUMMARY AND CONCLUSIO
Page 176: 161 4. Experimental and theoretical
Page 188: 173 times this number. It is possib
Page 191 and 192: 176 Table A.1 Ko1mogorov-Smirnov Te
Page 193: Dual Linear Congruential Generator:
Page 200 and 201: 185 For a finite medium of length L
Page 208 and 209: 193 max1mum error). The breakthroug
Page 212: 197 APPENDIX C SHEAR DISPERSION AND
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longitudinal dispersion in nonuniform isotropic porous media

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