longitudinal dispersion in nonuniform isotropic porous media

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I 1 FLOW 3 PORE • JUNCTION 57 CAPILLARY TUBES OF CONSTANT LENGTH 2 BUT VARYING RADIUS FIGURE 3.2 Def<strong>in</strong>ition Sketch for the Unit Cell
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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
Page 24: o en -o ::J o CD FLOW .. Solute Con
Page 33 and 34: porous medium and an unconsolidated
Page 35: 20 CHAPTER 2 LITERATURE REVIEW Tran
Page 43: (1/2) V yd s From experiments, they
Page 54: 39 governed by an effective advecti
Page 61 and 62: 2.4 SUmmary 46 Several different cl
Page 63: 48 CHAPTER 3 A THEORETICAL MODEL FO
Page 67: Q = 52 (3.1) where P'cos8 is the pr
Page 78: motion of a single particle. Hence
Page 90: 75 (3.44» involving the pore size
Page 95: 80 FIGURE 3.4 Packing Hodel for a N
Page 102: OVERFLOW 1 380mm 446mm I CONDUCTIVI
Page 108: the sand pack. Constant head is mai
Page 117: 102 cumulative probability distribu
Page 121: 106 Water in the column experiments
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110 deviations for these distributi
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122 proper boundary condition arise
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C 0.6 CO - 0.4 0.2 99.99 132 PECLET
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136 CHAPTER 5 A COMPARISON OF MODEL
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Measured Calculated ( C = 16) (equa
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146 of the required number of steps
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152 effective porosity as compared
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155 CHAPTER 6 SUMMARY AND CONCLUSIO
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161 4. Experimental and theoretical
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173 times this number. It is possib
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176 Table A.1 Ko1mogorov-Smirnov Te
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Dual Linear Congruential Generator:
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185 For a finite medium of length L
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193 max1mum error). The breakthroug
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197 APPENDIX C SHEAR DISPERSION AND
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longitudinal dispersion in nonuniform isotropic porous media

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