Developments
Clay
Natural and
Engineered Clay
Barriers
Edited
by
Christophe
Tournassat
Water, Environment and
Ecotechnology
Division, FrenchGeological
Survey
(BRGM),Orleans,
FranceEarth Sciences
Division,
LawrenceBerkeley
NationalLaboratory,
Berkeley,
CA, USACarl
I.
Steefel
Earth Sciences
Division,
LawrenceBerkeley
NationalLaboratory,
Berkeley,
CA, USAIan C.
Bourg
Department
of Civil and EnvironmentalEngineering,
PrincetonUniversity,
Princeton, NJ, USAEarth Sciences
Division,
LawrenceBerkeley
NationalLaboratory,
Berkeley,
CA, USAFaYza
Bergaya
Centrede Recherche sur la Matiere
Divisee,
Centre National de laRecherche
Scientifique (CNRS), Orleans,
FranceAMSTERDAM•BOSTON• HEIDELBERG•LONDON•NEW YORK•OXFORD
List of Contributors xi
Acknowledgments
xiiiIntroduction 1
1. Surface
Properties
of
Clay
Minerals 5Christophe
Tournassat, Ian C. Bourg, Carl I.SteefelandFa'fzaBergaya
1.1 From Sheetsto
Clay
Mineral Layers 6 1.1.1 Structure ofClay
Mineral Layers 61.1.2 Layer
Charge
andCharge Compensation
Mechanisms 8
1.1.3 Aspect Ratio and
Morphology
ofClay
MineralParticles 8
1.2 From Layersto Particles and
Aggregates
9 1.2.1 LayerStacking
andHydration
9 1.2.2Mixed-Layer Clay
Minerals 10 1.2.3 Particle SSA 101.2.4 Nature of theExternal Basal Surfaces of
Clay
Mineral Particles 13
1.2.5
Charge
Balanceatthe Scale ofaClay
Mineral Particle 15 1.2.6 From Particlesto Aggregatesand Porous Media 15 1.3 Surface
Properties
of Basal Surfaces 171.3.1 Cation
Exchange
and CationExchange Capacity
171.3.2 Protonation and
Deprotonation
ofOxygen
Atomson Basal Surfaces 19
1.3.3 Electrostatic Potential, Cation Condensation, and
Anion Exclusion 19
1.4 Surface
Properties
ofEdges
23 1.4.1 StructureofEdges
23 1.4.2Protonation/Deprotonation,
Edge
SurfaceCharge,
and Electrostatic Potential 23
1.4.3 Surface
Complexation,
Cation andAnionExchange
24 1.5 Summary 25References 25
2.
Adsorption
ofInorganic
andOrganic
Solutes
by Clay
Minerals 33Mikhail Borisover and JamesA. Davis
2.1 Introduction 34
2.2
Clay
Minerals and Surface Functional Croups 342.3
Inorganic
Solute Adsorption—DesorptionMechanisms 35 2.3.1Interlayer Adsorption
362.3.2
Edge
SiteAdsorption
372.3.3 Surface
Precipitation
and Metal SubstitutionReactions inthe
Clay
Mineral Layer 45 2.4Organic
SoluteAdsorption
Mechanisms 462.4.1
Adsorption
of Organic Moleculesby Clay
MineralSurfaces 46
2.4.2
Adsorption
ofCharged
Organic Speciesby Clay
Mineral Surfaces 52
2.5 Interactions of
Clay
Mineral Surfaces in Soils and Sediments with NOM and Natural Nanoparticles ofOther Minerals 55
2.6
Adsorption
ProcessesonClays
in Natural andEngineered
Environments 56 2.6.1 Interactionsof Metal and MetalloidIonswithClays
in Natural andEngineered
Environments 57 2.6.2 InteractionsofOrganic Compounds
withClays
inNatural and
Engineered
Environments 592.7
Summary
62References 64
3. Chemical Conditions in
Clay-Rocks
71Christophe
Tournassat,Agnes Vinsot, Eric C. Gaucher and Scott Altmann3.1 Introduction 72
3.2
Clay-Rock Mineralogy,
WaterContent and Porosity 73 3.3 InvestigationMethods for Pore-Water ChemicalComposition
Characterization 75 3.3.1 In SituTechniques:
Piezometers and InstrumentedBoreholes 75
3.3.2 Pore-Water Extraction from Core
Samples by
Squeezing 78 3.3.3 Alternative
Techniques
793.3.4
Examples
of Pore-WaterCompositions
80 3.3.5 Indirect Characterization ofPore-WaterChemistry
80 3.4Modeling
Pore-WaterComposition
863.4.1
Modeling Hypotheses,
Strategies,and3.4.2
Modeling
the Pore-WaterComposition in PristineRock 91
3.4.3 Additional Model Controls 92
3.4.4
Significance
ofPore-Water Composition 92 3.5 Conclusion:Achievements and FutureChallenges
93References 93
4. Dissolution Kinetics of
Clay
Minerals 101JordiCama andJiwchar Ganor
4.1 Introduction 102
4.2 Theoretical
Background: Clay
Mineral DissolutionKinetics 103
4.2.1
pH Dependence
1054.2.2 T
Dependence
107 4.2.3Catalytic/inhibitor
Effect 1074.2.4 Effect ofDeviationfrom
Equilibrium
(ACrEffect) 108 4.2.5 Surface Area and SurfaceReactivity
109 4.2.6 IonicStrength
Effect 1094.3
Experimental Methodology
1094.3.1
Aqueous Chemistry:
Chemical Reactors 110 4.3.2 SolidSample
SurfaceTopography:
AFM, VSI, PSI,and LCM-DIM 111
4.4 Kaolinite 112
4.4.1 pH andT
Dependence
113 4.4.2 EffectofDeviation fromEquilibrium
(ACr Effect) 115 4.4.3Catalytic/Inhibition
Effect 116 4.4.4 IonicStrength
Effect 117 4.4.5 Surface Area Effect 1174.5 Smectite 118
4.5.1
pH
andTDependence
118 4.5.2 Effect ofDeviation fromEquilibrium
(ACrEffect) 1214.5.3
Catalytic/Inhibition
Effect 122 4.5.4 IonicStrength
Effect 1244.5.5 SurfaceArea Effect 124
4.6 Micas 127 4.6.1 lllite 127 4.6.2 Muscovite 129 4.6.3 Biotite 132 4.6.4
Phlogopite
136 4.7 Vermiculite 137 4.8 Chlorite 1374.9
Summary
and Conclusions 141Appendix
1435.
Stability
of
Clay
Barriers UnderChemical
Perturbations
155 Olivier Bildstein andFrancis Claret5.1 Introduction 155
5.2
Perturbing
thePhysicochemical
Conditions intheSubsurface: Desaturation and Oxidation 157 5.3
Introducing
Allochthonous Solid Materials in theGeological
Environment 1605.3.1
Concrete/Clay
Interactions 160 5.3.2 Steel Corrosion inClay
165 5.4 Chemical Perturbations dueto Allochthonous Gas 170 5.4.1 H2Injection/Production
171 5.4.2Injection
ofC02 172 5.5 Conclusion: What Is Known andWhat Needsto BeImproved
175References 176
6.
Self-Diffusion
of Water and Ions inClay
Barriers
189Ian C. Bourgand
Christophe
Tournassat6.1 Introduction 189
6.2 MacroscopicScale Diffusion Coefficients: Definition
and Measurement 191 6.2.1 Fickian
Expressions
191 6.2.2Experimental Techniques
1926.2.3
Experimental Challenges
1956.3
Conceptual
Models ofDaand De 197 6.4 SummaryofMeasured Daand DeValues 1996.4.1 Parametersthat Influence Diffusion in
Clay
Barriers 1996.4.2
Compilation
of Diffusion Data 2016.4.3 WaterDiffusion 207 6.4.4 Anion Diffusion 209
6.4.5 Cation Diffusion 211
6.5 Future Research Opportunities 216
References 217
7. Gas
Transfer
Through Clay
Barriers 227 A.Amann-Hildenbrand,
B.M. Krooss, J.Harrington,
R. Cuss,C.
Davy,
F.Skoczylas,
E. JacopsandN. Maes7A Introduction 228
7.2 Diffusive
Transport
of Gas in Solution 230 7.2.1 TheoreticalBackground
230 7.2.2 Literature Review 2327.3 Advective Flow 235
7.3.1 Theoretical
Background
235 7.3.2 Literature Review 2417.4 Experiments 245 7.4.1 Diffusion
Experiments
245 7.4.2 Two-Phase FlowExperiments
246 7.4.3Examples
247 7.5 Final Remarks and Conclusions 257Symbols
and Abbreviations 258References 259
8.
Semipermeable
MembraneProperties
andChemomechanical
Coupling
inClay
Barriers 269Julio Gonqalves,Pierre M.
Adler,
Philippe Cosenza,Aliaksei Pazdniakou and Ghislain de
Marsily
Table of Notation 270
8.1 Introduction 273
8.2
Transport
Processes inClay-Rock
Formations 274 8.2.1 Reevaluation of Darcy's LawforClay-Rocks
274 8.2.2Experimental
Evidence for aLimitedValidity
ofDarcy's
Law inClay-Rocks
276 8.2.3 StandardHydrogeological Approach: Nondiagonal
Terms areAssumed
Negligible
2798.2.4 When
Off-Diagonal
Terms Are NotNegligible:
Formalism and
Experimental
Evidence 287 8.2.5 ImportanceofCoupled
Terms inTransport Equations
296 8.3 PredictiveModels forHydrodynamical Coupling
TermsUsing
Continuous and/or Granular MediaPhysics
300 8.3.1 Chemical OsmoticModels 300 8.3.2 Electroosmosis 302 8.3.3 Thermoosmosis: From MolecularConcepts
to aMacroscopic
Model 306 8.4Coupled Hydro-Chemo-Mechanical
Behavior inClay-Rocks
308 8.4.1 Surface Forcesand Disjunction Pressure 308 8.4.2Implication
of theDisjunction
Pressure Term forthe
Storativity:
The ElectrochemicalSpecific
StorageCoefficient 311
8.5 Conclusion 319
References 320
9.
Coupled Thermo-Hydro-Mechanical
Behavior ofNatural and
Engineered Clay
Barriers 329Jonny Rutqvist
9.1 Introduction 329
9.2 THM Behavior of Buffer and Backfill Material 333
9.3 THM Behavior of
Clay
HostRocks 343 9.4Coupled
THM Evolution ofEngineered
and NaturalClay
Barriers in aNuclearWasteRepository 346
9.5 Links ofTHM to
Geochemistry
350 9.6Concluding
Remarks 35210.
Transport Properties through
Partially
SaturatedCharged
Membranes and
Geophysical
Approaches
357A. Revil
10.1 Introduction 358
10.2 Notations 359
10.3 Electrokinetic Phenomena withoutFiltration 360
10.3.1
Summary
of theTheory
360 10.3.2Application
to ElectricalConductivity
365 10.3.3Application
totheStreaming
PotentialCoupling
Coefficient 366 10.3.4Application
totheElectroosmoticPermeability
37110.4 Filtration
Efficiency
372 10.4.1Summary
of theTheory
373 10.4.2 Determination of the OsmoticEfficiency
374 10.4.3 FiltrationEfficiency
inSaturated Conditions 37710.4.4 Filtration
Efficiency
in Unsaturated Conditions 37910.4.5 DiffusionCoefficient 380
10.5 Useof
Geophysical
Methods 38210.5.1 The Self-Potential Method 382 10.5.2 The DirectCurrent (DC)
Resistivity
Method 38310.5.3 The Induced PolarizationMethod 383
10.6 Conclusions 384
Glossary
384Appendix
A:Cation-Dependent
CEC 386Appendix B: Osmotic Pressure with theDonnan and
Revil Models 387
Appendix
C: Osmotic Coefficient, Reverse Osmosis,and Salt
Diffusivity
391References 394
11.
Upscaling Strategies
forModeling Clay-Rock
Properties
399Virginie
MarryandBenjaminRotenberg
11.1 Introduction 399
11.2 From theAtomic Scale tothe Mesoscale 400
11.2.1
Interlayer
Porosity 40011.2.2
Clay
Mineral Particle in Contactwith a Reservoir 40311.3 From the Mesoscopicto the
Macroscopic
Scale 40611.3.1
Representative Elementary
Volume 407 11.3.2Upscaling
from the Particle and PoreScalestothe
Sample
Scale 40811.4 Conclusion 411
References 411