longitudinal dispersion in nonuniform isotropic porous media

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197 APPENDIX C SHEAR DISPERSION AND RESIDENCE TIME FOR LAMINAR FLOW IN CAPILLARY TUBES see Journal of Fluid Mechanics Vol. 142, May 1984, pp. 289-308.
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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
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VQ!gme-W@ight@d pistripgtiop(a) Gra
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108 space in the medium, while the
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120 When one fluid displaces anothe
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126 medium type. This deviation of
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D v 134 Table 4.5 Longitudinal Disp
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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 169 and 170: 154 number flows since the advectio
Page 175 and 176: 160 homogeneous packing is not to b
Page 182: 167 f( £) = probability density fo
Page 190 and 191: 175 to a known distribution functio
Page 192 and 193: 177 Table A.2 Kolmogorov-Smirnov Te
Page 196: 181 a change 1n source strength ove
Page 201: 186 where P = vL/4D L and Ak are th
Page 209: B.3 Summary 194 Solutions for the m
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longitudinal dispersion in nonuniform isotropic porous media

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