• No results found

Engineered Clay Barriers

N/A
N/A
Protected

Academic year: 2021

Share "Engineered Clay Barriers"

Copied!
7
0
0

Loading.... (view fulltext now)

Full text

(1)

Developments

Clay

Natural and

Engineered Clay

Barriers

Edited

by

Christophe

Tournassat

Water, Environment and

Ecotechnology

Division, French

Geological

Survey

(BRGM),

Orleans,

France

Earth Sciences

Division,

Lawrence

Berkeley

National

Laboratory,

Berkeley,

CA, USA

Carl

I.

Steefel

Earth Sciences

Division,

Lawrence

Berkeley

National

Laboratory,

Berkeley,

CA, USA

Ian C.

Bourg

Department

of Civil and Environmental

Engineering,

Princeton

University,

Princeton, NJ, USA

Earth Sciences

Division,

Lawrence

Berkeley

National

Laboratory,

Berkeley,

CA, USA

FaYza

Bergaya

Centrede Recherche sur la Matiere

Divisee,

Centre National de la

Recherche

Scientifique (CNRS), Orleans,

France

AMSTERDAM•BOSTON• HEIDELBERG•LONDON•NEW YORK•OXFORD

(2)

List of Contributors xi

Acknowledgments

xiii

Introduction 1

1. Surface

Properties

of

Clay

Minerals 5

Christophe

Tournassat, Ian C. Bourg, Carl I.Steefeland

Fa'fzaBergaya

1.1 From Sheetsto

Clay

Mineral Layers 6 1.1.1 Structure of

Clay

Mineral Layers 6

1.1.2 Layer

Charge

and

Charge Compensation

Mechanisms 8

1.1.3 Aspect Ratio and

Morphology

of

Clay

Mineral

Particles 8

1.2 From Layersto Particles and

Aggregates

9 1.2.1 Layer

Stacking

and

Hydration

9 1.2.2

Mixed-Layer Clay

Minerals 10 1.2.3 Particle SSA 10

1.2.4 Nature of theExternal Basal Surfaces of

Clay

Mineral Particles 13

1.2.5

Charge

Balanceatthe Scale ofa

Clay

Mineral Particle 15 1.2.6 From Particlesto Aggregatesand Porous Media 15 1.3 Surface

Properties

of Basal Surfaces 17

1.3.1 Cation

Exchange

and Cation

Exchange Capacity

17

1.3.2 Protonation and

Deprotonation

of

Oxygen

Atoms

on Basal Surfaces 19

1.3.3 Electrostatic Potential, Cation Condensation, and

Anion Exclusion 19

1.4 Surface

Properties

of

Edges

23 1.4.1 Structureof

Edges

23 1.4.2

Protonation/Deprotonation,

Edge

Surface

Charge,

and Electrostatic Potential 23

1.4.3 Surface

Complexation,

Cation andAnion

Exchange

24 1.5 Summary 25

References 25

(3)

2.

Adsorption

of

Inorganic

and

Organic

Solutes

by Clay

Minerals 33

Mikhail Borisover and JamesA. Davis

2.1 Introduction 34

2.2

Clay

Minerals and Surface Functional Croups 34

2.3

Inorganic

Solute Adsorption—DesorptionMechanisms 35 2.3.1

Interlayer Adsorption

36

2.3.2

Edge

Site

Adsorption

37

2.3.3 Surface

Precipitation

and Metal Substitution

Reactions inthe

Clay

Mineral Layer 45 2.4

Organic

Solute

Adsorption

Mechanisms 46

2.4.1

Adsorption

of Organic Molecules

by Clay

Mineral

Surfaces 46

2.4.2

Adsorption

of

Charged

Organic Species

by Clay

Mineral Surfaces 52

2.5 Interactions of

Clay

Mineral Surfaces in Soils and Sediments with NOM and Natural Nanoparticles of

Other Minerals 55

2.6

Adsorption

Processeson

Clays

in Natural and

Engineered

Environments 56 2.6.1 Interactionsof Metal and MetalloidIonswith

Clays

in Natural and

Engineered

Environments 57 2.6.2 Interactionsof

Organic Compounds

with

Clays

in

Natural and

Engineered

Environments 59

2.7

Summary

62

References 64

3. Chemical Conditions in

Clay-Rocks

71

Christophe

Tournassat,Agnes Vinsot, Eric C. Gaucher and Scott Altmann

3.1 Introduction 72

3.2

Clay-Rock Mineralogy,

WaterContent and Porosity 73 3.3 InvestigationMethods for Pore-Water Chemical

Composition

Characterization 75 3.3.1 In Situ

Techniques:

Piezometers and Instrumented

Boreholes 75

3.3.2 Pore-Water Extraction from Core

Samples by

Squeezing 78 3.3.3 Alternative

Techniques

79

3.3.4

Examples

of Pore-Water

Compositions

80 3.3.5 Indirect Characterization ofPore-Water

Chemistry

80 3.4

Modeling

Pore-Water

Composition

86

3.4.1

Modeling Hypotheses,

Strategies,and

(4)

3.4.2

Modeling

the Pore-WaterComposition in Pristine

Rock 91

3.4.3 Additional Model Controls 92

3.4.4

Significance

ofPore-Water Composition 92 3.5 Conclusion:Achievements and Future

Challenges

93

References 93

4. Dissolution Kinetics of

Clay

Minerals 101

JordiCama andJiwchar Ganor

4.1 Introduction 102

4.2 Theoretical

Background: Clay

Mineral Dissolution

Kinetics 103

4.2.1

pH Dependence

105

4.2.2 T

Dependence

107 4.2.3

Catalytic/inhibitor

Effect 107

4.2.4 Effect ofDeviationfrom

Equilibrium

(ACrEffect) 108 4.2.5 Surface Area and Surface

Reactivity

109 4.2.6 Ionic

Strength

Effect 109

4.3

Experimental Methodology

109

4.3.1

Aqueous Chemistry:

Chemical Reactors 110 4.3.2 Solid

Sample

Surface

Topography:

AFM, VSI, PSI,

and LCM-DIM 111

4.4 Kaolinite 112

4.4.1 pH andT

Dependence

113 4.4.2 EffectofDeviation from

Equilibrium

(ACr Effect) 115 4.4.3

Catalytic/Inhibition

Effect 116 4.4.4 Ionic

Strength

Effect 117 4.4.5 Surface Area Effect 117

4.5 Smectite 118

4.5.1

pH

andT

Dependence

118 4.5.2 Effect ofDeviation from

Equilibrium

(ACrEffect) 121

4.5.3

Catalytic/Inhibition

Effect 122 4.5.4 Ionic

Strength

Effect 124

4.5.5 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 137

4.9

Summary

and Conclusions 141

Appendix

143

(5)

5.

Stability

of

Clay

Barriers Under

Chemical

Perturbations

155 Olivier Bildstein andFrancis Claret

5.1 Introduction 155

5.2

Perturbing

the

Physicochemical

Conditions inthe

Subsurface: Desaturation and Oxidation 157 5.3

Introducing

Allochthonous Solid Materials in the

Geological

Environment 160

5.3.1

Concrete/Clay

Interactions 160 5.3.2 Steel Corrosion in

Clay

165 5.4 Chemical Perturbations dueto Allochthonous Gas 170 5.4.1 H2

Injection/Production

171 5.4.2

Injection

ofC02 172 5.5 Conclusion: What Is Known andWhat Needsto Be

Improved

175

References 176

6.

Self-Diffusion

of Water and Ions in

Clay

Barriers

189

Ian C. Bourgand

Christophe

Tournassat

6.1 Introduction 189

6.2 MacroscopicScale Diffusion Coefficients: Definition

and Measurement 191 6.2.1 Fickian

Expressions

191 6.2.2

Experimental Techniques

192

6.2.3

Experimental Challenges

195

6.3

Conceptual

Models ofDaand De 197 6.4 SummaryofMeasured Daand DeValues 199

6.4.1 Parametersthat Influence Diffusion in

Clay

Barriers 199

6.4.2

Compilation

of Diffusion Data 201

6.4.3 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. Maes

7A Introduction 228

7.2 Diffusive

Transport

of Gas in Solution 230 7.2.1 Theoretical

Background

230 7.2.2 Literature Review 232

7.3 Advective Flow 235

7.3.1 Theoretical

Background

235 7.3.2 Literature Review 241

(6)

7.4 Experiments 245 7.4.1 Diffusion

Experiments

245 7.4.2 Two-Phase Flow

Experiments

246 7.4.3

Examples

247 7.5 Final Remarks and Conclusions 257

Symbols

and Abbreviations 258

References 259

8.

Semipermeable

Membrane

Properties

and

Chemomechanical

Coupling

in

Clay

Barriers 269

Julio Gonqalves,Pierre M.

Adler,

Philippe Cosenza,

Aliaksei Pazdniakou and Ghislain de

Marsily

Table of Notation 270

8.1 Introduction 273

8.2

Transport

Processes in

Clay-Rock

Formations 274 8.2.1 Reevaluation of Darcy's Lawfor

Clay-Rocks

274 8.2.2

Experimental

Evidence for aLimited

Validity

of

Darcy's

Law in

Clay-Rocks

276 8.2.3 Standard

Hydrogeological Approach: Nondiagonal

Terms areAssumed

Negligible

279

8.2.4 When

Off-Diagonal

Terms Are Not

Negligible:

Formalism and

Experimental

Evidence 287 8.2.5 Importanceof

Coupled

Terms in

Transport Equations

296 8.3 PredictiveModels for

Hydrodynamical Coupling

Terms

Using

Continuous and/or Granular Media

Physics

300 8.3.1 Chemical OsmoticModels 300 8.3.2 Electroosmosis 302 8.3.3 Thermoosmosis: From Molecular

Concepts

to a

Macroscopic

Model 306 8.4

Coupled Hydro-Chemo-Mechanical

Behavior in

Clay-Rocks

308 8.4.1 Surface Forcesand Disjunction Pressure 308 8.4.2

Implication

of the

Disjunction

Pressure Term for

the

Storativity:

The Electrochemical

Specific

StorageCoefficient 311

8.5 Conclusion 319

References 320

9.

Coupled Thermo-Hydro-Mechanical

Behavior of

Natural and

Engineered Clay

Barriers 329

Jonny Rutqvist

9.1 Introduction 329

9.2 THM Behavior of Buffer and Backfill Material 333

9.3 THM Behavior of

Clay

HostRocks 343 9.4

Coupled

THM Evolution of

Engineered

and Natural

Clay

Barriers in aNuclearWasteRepository 346

9.5 Links ofTHM to

Geochemistry

350 9.6

Concluding

Remarks 352

(7)

10.

Transport Properties through

Partially

Saturated

Charged

Membranes and

Geophysical

Approaches

357

A. Revil

10.1 Introduction 358

10.2 Notations 359

10.3 Electrokinetic Phenomena withoutFiltration 360

10.3.1

Summary

of the

Theory

360 10.3.2

Application

to Electrical

Conductivity

365 10.3.3

Application

tothe

Streaming

Potential

Coupling

Coefficient 366 10.3.4

Application

totheElectroosmotic

Permeability

371

10.4 Filtration

Efficiency

372 10.4.1

Summary

of the

Theory

373 10.4.2 Determination of the Osmotic

Efficiency

374 10.4.3 Filtration

Efficiency

inSaturated Conditions 377

10.4.4 Filtration

Efficiency

in Unsaturated Conditions 379

10.4.5 DiffusionCoefficient 380

10.5 Useof

Geophysical

Methods 382

10.5.1 The Self-Potential Method 382 10.5.2 The DirectCurrent (DC)

Resistivity

Method 383

10.5.3 The Induced PolarizationMethod 383

10.6 Conclusions 384

Glossary

384

Appendix

A:

Cation-Dependent

CEC 386

Appendix B: Osmotic Pressure with theDonnan and

Revil Models 387

Appendix

C: Osmotic Coefficient, Reverse Osmosis,

and Salt

Diffusivity

391

References 394

11.

Upscaling Strategies

for

Modeling Clay-Rock

Properties

399

Virginie

MarryandBenjamin

Rotenberg

11.1 Introduction 399

11.2 From theAtomic Scale tothe Mesoscale 400

11.2.1

Interlayer

Porosity 400

11.2.2

Clay

Mineral Particle in Contactwith a Reservoir 403

11.3 From the Mesoscopicto the

Macroscopic

Scale 406

11.3.1

Representative Elementary

Volume 407 11.3.2

Upscaling

from the Particle and PoreScales

tothe

Sample

Scale 408

11.4 Conclusion 411

References 411

Summary

and

Perspective

419

References

Related documents

Make  changes  to  section  on  agreements  to   reflect  emphasis  of  agreements  in  new

The government co ll ect s revenue f rom taxes on capital and labour income and value-added taxes on fina l demand , production taxes on intermediate inputs, and...

The subsequent chapters deal with particular problems occurring in this context: the sovereignty of states and the development of competition law in the globalization era (Chapter

investment advice (for the relevant information requirement, see Article 24(3) of the MiFID II draft). Only then is it actually possible for banks to offer this service without

Furthermore, on a methodological front, empirical studies that analyse export venture modes have not always measured mode choice and performance at the same

Meets expectations -- student demonstrates sufficient knowledge, skills, and abilities or does what is expected of students in collegiate business programs.. Does not meet

• Our goal is to make Pittsburgh Public Schools First Choice by offering a portfolio of quality school options that promote high student achievement in the most equitable and

Comments This can be a real eye-opener to learn what team members believe are requirements to succeed on your team. Teams often incorporate things into their “perfect team