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1 
CHAPTER 1 
Copyrighted Material 
Introduction 
1.1 SOIL BEHAVIOR IN CIVIL AND 
ENVIRONMENTAL ENGINEERING 
Civil and environmental engineering includes the con-ception, 
analysis, design, construction, operation, and 
maintenance of a diversity of structures, facilities, and 
systems. All are built on, in, or with soil or rock. The 
properties and behavior of these materials have major 
influences on the success, economy, and safety of the 
work. Geoengineers play a vital role in these projects 
and are also concerned with virtually all aspects of 
environmental control, including water resources, wa-ter 
pollution control, waste disposal and containment, 
and the mitigation of such natural disasters as floods, 
earthquakes, landslides, and volcanoes. Soils and their 
interactions with the environment are major consider-ations. 
Furthermore, detailed understanding of the be-havior 
of earth materials is essential for mining, for 
energy resources development and recovery, and for 
scientific studies in virtually all the geosciences. 
To deal properly with the earth materials associated 
with any problem and project requires knowledge, 
understanding, and appreciation of the importance 
of geology, materials science, materials testing, and 
mechanics. Geotechnical engineering is concerned 
with all of these. Environmental concerns—especially 
those related to groundwater, the safe disposal and con-tainment 
of wastes, and the cleanup of contaminated 
sites—has spawned yet another area of specialization; 
namely, environmental geotechnics, wherein chemistry 
and biological science are important. Geochemical and 
microbiological phenomena impact the composition, 
properties, and stability of soils and rocks to degrees 
only recently beginning to be appreciated. 
Students in civil engineering are often quite sur-prised, 
and sometimes quite confused, by their first 
course in engineering with soils. After studying statics, 
mechanics, and structural analysis and design, wherein 
problems are usually quite clear-cut and well defined, 
they are suddenly confronted with situations where this 
is no longer the case. A first course in soil mechanics 
may not, at least for the first half to two-thirds of the 
course, be mechanics at all. The reason for this is sim-ple: 
Analyses and designs are useless if the boundary 
conditions and material properties are improperly de-fined. 
Acquisition of the data needed for analysis and de-sign 
on, in, and with soils and rocks can be far more 
difficult and uncertain than when dealing with other 
engineering materials and aboveground construction. 
There are at least three important reasons for this. 
1. No Clearly Defined Boundaries. An embank-ment 
resting on a soil foundation is shown in Fig. 
1.1a, and a cantilever beam fixed at one end is 
shown in Fig. 1.1b. The free body of the canti-lever 
beam, Fig. 1.1c, is readily analyzed for re-actions, 
shears, moments, and deflections using 
standard methods of structural analysis. However, 
what are the boundary conditions, and what is the 
free body for the embankment foundation? 
2. Variable and Unknown Material Properties. 
The properties of most construction materials 
(e.g., steel, plastics, concrete, aluminum, and 
wood) are ordinarily known within rather narrow 
limits and usually can be specified to meet certain 
needs. Although this may be the case in construc-tion 
using earth and rock fills, at least part of 
every geotechnical problem involves interactions 
with in situ soil and rock. No matter how exten-sive 
(and expensive) any boring and sampling 
program, only a very small percentage of the sub-surface 
material is available for observation and 
testing. In most cases, more than one stratum is 
Copyright © 2005 John Wiley & Sons Retrieved from: www.knovel.com
2 1 INTRODUCTION 
Copyrighted Material 
Figure 1.1 The problem of boundary conditions in geo-technical 
problems: (a) embankment on soil foundation, (b) 
cantilever beam, and (c) free body diagram for analysis of 
propped cantilever beam. 
present, and conditions are nonhomogeneous and 
anisotropic. 
3. Stress and Time-Dependent Material Proper-ties. 
Soils, and also some rocks, have mechan-ical 
properties that depend on both the stress 
history and the present stress state. This is be-cause 
the volume change, stress–strain, and 
strength properties depend on stress transmission 
between particles and particle groups. These 
stresses are, for the most part, generated by body 
forces and boundary stresses and not by internal 
forces of cohesion, as is the case for many other 
materials. In addition, the properties of most soils 
change with time after placement, exposure, and 
loading. Because of these stress and time de-pendencies, 
any given geotechnical problem may 
involve not just one or two but an almost infinite 
number of different materials. 
Add to the above three factors the facts that soil and 
rock properties may be susceptible to influences from 
changes in temperature, pressure, water availability, 
and chemical and biological environment, and one 
might conclude that successful application of mechan-ics 
to earth materials is an almost hopeless proposition. 
It has been amply demonstrated, of course, that such 
is not the case; in fact, it is for these very reasons that 
geotechnical engineering offers such a great challenge 
for imaginative and creative work. 
Modern theories of soil mechanics, the capabilities 
of modern computers and numerical analysis methods, 
and our improved knowledge of soil physics and chem-istry 
make possible the solution of a great diversity of 
static and dynamic problems of stress deformation and 
stability, the transient and steady-state flow of fluids 
through the ground, and the long-term performance of 
earth systems. Nonetheless, our ability to analyze and 
compute often exceeds considerably our ability to un-derstand, 
measure, and characterize a problem or 
process. Thus, understanding and the ability to con-ceptualize 
soil and rock behavior become all the more 
important. 
The objectives of this book are to provide a basis 
for the understanding of the engineering properties and 
behavior of soils and the factors controlling changes 
with time and to indicate why this knowledge is im-portant 
and how it is used in the solution of geotech-nical 
and geoenvironmental problems. 
It is easier to state what this book is not, rather than 
what it is. It is not a book on soil or rock mechanics; 
it is not a book on soil exploration or testing; it is not 
a book that teaches analysis or design; and it is not a 
book on geotechnical engineering practice. Excellent 
books and references dealing with each of these im-portant 
areas are available. It is a book on the com-position, 
structure, and behavior of soils as engineering 
materials. It is intended for students, researchers, and 
practicing engineers who seek a more in-depth knowl-edge 
of the nature and behavior of soils than is pro-vided 
by classical and conventional treatments of soil 
mechanics and geotechnical engineering. 
Here are some examples of the types of questions 
that are addressed in this book: 
• What are soils composed of? Why? 
• How does geological history influence soil prop-erties? 
• How are engineering properties and behavior re-lated 
to composition? 
• What is clay? 
• Why are clays plastic? 
• What are friction and cohesion? 
• What is effective stress? Why is it important? 
• Why do soils creep and exhibit stress relaxation? 
• Why do some soils swell while others do not? 
• Why does stability failure sometimes occur at 
stresses less than the measured strength? 
• Why and how are soil properties changed by dis-turbance? 
Copyright © 2005 John Wiley & Sons Retrieved from: www.knovel.com
GETTING STARTED 3 
• How do changes in environmental conditions 
change properties? 
• What are some practical consequences of the pro-longed 
exposure of clay containment barriers to 
waste chemicals? 
• What controls the rate of flow of water, heat, 
chemicals, and electricity through soils? 
• How are the different types of flows through soil 
interrelated? 
• Why is the residual strength of a soil often much 
less than its peak strength? 
• How do soil properties change with time after dep-osition 
Copyrighted Material 
or densification and why? 
• How do temperature changes influence the me-chanical 
properties of soils? 
• What is soil liquefaction, and why is it important? 
• What causes frost heave, and how can it be pre-vented? 
• What clay types are best suited for sealing waste 
repositories? 
• What biological processes can occur in soils and 
why are they important in engineering problems? 
Developing answers to questions such as these re-quires 
application of concepts from chemistry, geol-ogy, 
biology, materials science, and physics. Principles 
from these disciplines are introduced as necessary to 
develop background for the phenomena under study. It 
is assumed that the reader has a basic knowledge of 
applied mechanics and soil mechanics, as well as a 
general familiarity with the commonly used engineer-ing 
properties of soils and their determination. 
1.2 SCOPE AND ORGANIZATION 
The topics covered in this book begin with consider-ation 
of soil formation in Chapter 2 and soil mineral-ogy 
and compositional analysis of soil in Chapter 3. 
Relationships between soil composition and engineer-ing 
properties are developed in Chapter 4. Soil com-position 
by itself is insufficient for quantification of 
soil properties for specific situations, because the soil 
fabric, that is, the arrangements of particles, particle 
groups, and pores, may play an equally important role. 
This topic is covered in Chapter 5. 
Water may make up more than half the volume of 
a soil mass, it is attracted to soil particles, and the 
interactions between water and the soil surfaces influ-ence 
the behavior. In addition, owing to the colloidal 
nature of clay particles, the types and concentrations 
of chemicals in a soil can influence significantly its 
behavior in a variety of ways. Soil water and the clay– 
water–electrolyte system are then analyzed in Chapter 
6. An analysis of interparticle forces and total and ef-fective 
stresses, with a discussion of why they are im-portant, 
is given in Chapter 7. 
The remaining chapters draw on the preceding de-velopments 
for explanations of phenomena and soil 
properties of interest in geotechnical and geoenviron-mental 
engineering. The formation of soil deposits, 
their resulting structures and relationships to geotech-nical 
properties and stability are covered in Chapter 8. 
The next three chapters deal with those soil properties 
that are of primary importance to the solution of most 
geoengineering problems: the flows of fluids, chemi-cals, 
electricity, and heat and their consequences in 
Chapter 9; volume change behavior in Chapter 10; and 
deformation and strength and deformation behavior in 
Chapter 11. Finally, Chapter 12 on time effects on 
strength and deformation recognizes that soils are not 
inert, static materials, but rather how a given soil re-sponds 
under different rates of loading or at some time 
in the future may be quite different than how it re-sponds 
today. 
1.3 GETTING STARTED 
Find an article about a problem, a project, or issue that 
involves some aspect of geotechnical soil behavior as 
an important component. The article can be from the 
popular press, from a technical journal or magazine, 
such as the Journal of Geotechnical and Geoenviron-mental 
Engineering of the American Society of Civil 
Engineers, Ge´otechnique, The Canadian Geotechnical 
Journal, Soils and Foundations, ENR, or elsewhere. 
1. Read the article and prepare a one-page infor-mative 
abstract. (An informative abstract sum-marizes 
the important ideas and conclusions. A 
descriptive abstract, on the other hand, simply 
states the article contents.) 
2. Summarize the important geotechnical issues that 
are found in the article and write down what you 
believe you should know about to understand 
them well enough to solve the problem, resolve 
the issue, advise a client, and the like. In other 
words, what is in the article that you believe the 
subject matter in this book should prepare you to 
deal with? Do not exceed two pages. 
Copyright © 2005 John Wiley & Sons Retrieved from: www.knovel.com

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63027 01

  • 1. 1 CHAPTER 1 Copyrighted Material Introduction 1.1 SOIL BEHAVIOR IN CIVIL AND ENVIRONMENTAL ENGINEERING Civil and environmental engineering includes the con-ception, analysis, design, construction, operation, and maintenance of a diversity of structures, facilities, and systems. All are built on, in, or with soil or rock. The properties and behavior of these materials have major influences on the success, economy, and safety of the work. Geoengineers play a vital role in these projects and are also concerned with virtually all aspects of environmental control, including water resources, wa-ter pollution control, waste disposal and containment, and the mitigation of such natural disasters as floods, earthquakes, landslides, and volcanoes. Soils and their interactions with the environment are major consider-ations. Furthermore, detailed understanding of the be-havior of earth materials is essential for mining, for energy resources development and recovery, and for scientific studies in virtually all the geosciences. To deal properly with the earth materials associated with any problem and project requires knowledge, understanding, and appreciation of the importance of geology, materials science, materials testing, and mechanics. Geotechnical engineering is concerned with all of these. Environmental concerns—especially those related to groundwater, the safe disposal and con-tainment of wastes, and the cleanup of contaminated sites—has spawned yet another area of specialization; namely, environmental geotechnics, wherein chemistry and biological science are important. Geochemical and microbiological phenomena impact the composition, properties, and stability of soils and rocks to degrees only recently beginning to be appreciated. Students in civil engineering are often quite sur-prised, and sometimes quite confused, by their first course in engineering with soils. After studying statics, mechanics, and structural analysis and design, wherein problems are usually quite clear-cut and well defined, they are suddenly confronted with situations where this is no longer the case. A first course in soil mechanics may not, at least for the first half to two-thirds of the course, be mechanics at all. The reason for this is sim-ple: Analyses and designs are useless if the boundary conditions and material properties are improperly de-fined. Acquisition of the data needed for analysis and de-sign on, in, and with soils and rocks can be far more difficult and uncertain than when dealing with other engineering materials and aboveground construction. There are at least three important reasons for this. 1. No Clearly Defined Boundaries. An embank-ment resting on a soil foundation is shown in Fig. 1.1a, and a cantilever beam fixed at one end is shown in Fig. 1.1b. The free body of the canti-lever beam, Fig. 1.1c, is readily analyzed for re-actions, shears, moments, and deflections using standard methods of structural analysis. However, what are the boundary conditions, and what is the free body for the embankment foundation? 2. Variable and Unknown Material Properties. The properties of most construction materials (e.g., steel, plastics, concrete, aluminum, and wood) are ordinarily known within rather narrow limits and usually can be specified to meet certain needs. Although this may be the case in construc-tion using earth and rock fills, at least part of every geotechnical problem involves interactions with in situ soil and rock. No matter how exten-sive (and expensive) any boring and sampling program, only a very small percentage of the sub-surface material is available for observation and testing. In most cases, more than one stratum is Copyright © 2005 John Wiley & Sons Retrieved from: www.knovel.com
  • 2. 2 1 INTRODUCTION Copyrighted Material Figure 1.1 The problem of boundary conditions in geo-technical problems: (a) embankment on soil foundation, (b) cantilever beam, and (c) free body diagram for analysis of propped cantilever beam. present, and conditions are nonhomogeneous and anisotropic. 3. Stress and Time-Dependent Material Proper-ties. Soils, and also some rocks, have mechan-ical properties that depend on both the stress history and the present stress state. This is be-cause the volume change, stress–strain, and strength properties depend on stress transmission between particles and particle groups. These stresses are, for the most part, generated by body forces and boundary stresses and not by internal forces of cohesion, as is the case for many other materials. In addition, the properties of most soils change with time after placement, exposure, and loading. Because of these stress and time de-pendencies, any given geotechnical problem may involve not just one or two but an almost infinite number of different materials. Add to the above three factors the facts that soil and rock properties may be susceptible to influences from changes in temperature, pressure, water availability, and chemical and biological environment, and one might conclude that successful application of mechan-ics to earth materials is an almost hopeless proposition. It has been amply demonstrated, of course, that such is not the case; in fact, it is for these very reasons that geotechnical engineering offers such a great challenge for imaginative and creative work. Modern theories of soil mechanics, the capabilities of modern computers and numerical analysis methods, and our improved knowledge of soil physics and chem-istry make possible the solution of a great diversity of static and dynamic problems of stress deformation and stability, the transient and steady-state flow of fluids through the ground, and the long-term performance of earth systems. Nonetheless, our ability to analyze and compute often exceeds considerably our ability to un-derstand, measure, and characterize a problem or process. Thus, understanding and the ability to con-ceptualize soil and rock behavior become all the more important. The objectives of this book are to provide a basis for the understanding of the engineering properties and behavior of soils and the factors controlling changes with time and to indicate why this knowledge is im-portant and how it is used in the solution of geotech-nical and geoenvironmental problems. It is easier to state what this book is not, rather than what it is. It is not a book on soil or rock mechanics; it is not a book on soil exploration or testing; it is not a book that teaches analysis or design; and it is not a book on geotechnical engineering practice. Excellent books and references dealing with each of these im-portant areas are available. It is a book on the com-position, structure, and behavior of soils as engineering materials. It is intended for students, researchers, and practicing engineers who seek a more in-depth knowl-edge of the nature and behavior of soils than is pro-vided by classical and conventional treatments of soil mechanics and geotechnical engineering. Here are some examples of the types of questions that are addressed in this book: • What are soils composed of? Why? • How does geological history influence soil prop-erties? • How are engineering properties and behavior re-lated to composition? • What is clay? • Why are clays plastic? • What are friction and cohesion? • What is effective stress? Why is it important? • Why do soils creep and exhibit stress relaxation? • Why do some soils swell while others do not? • Why does stability failure sometimes occur at stresses less than the measured strength? • Why and how are soil properties changed by dis-turbance? Copyright © 2005 John Wiley & Sons Retrieved from: www.knovel.com
  • 3. GETTING STARTED 3 • How do changes in environmental conditions change properties? • What are some practical consequences of the pro-longed exposure of clay containment barriers to waste chemicals? • What controls the rate of flow of water, heat, chemicals, and electricity through soils? • How are the different types of flows through soil interrelated? • Why is the residual strength of a soil often much less than its peak strength? • How do soil properties change with time after dep-osition Copyrighted Material or densification and why? • How do temperature changes influence the me-chanical properties of soils? • What is soil liquefaction, and why is it important? • What causes frost heave, and how can it be pre-vented? • What clay types are best suited for sealing waste repositories? • What biological processes can occur in soils and why are they important in engineering problems? Developing answers to questions such as these re-quires application of concepts from chemistry, geol-ogy, biology, materials science, and physics. Principles from these disciplines are introduced as necessary to develop background for the phenomena under study. It is assumed that the reader has a basic knowledge of applied mechanics and soil mechanics, as well as a general familiarity with the commonly used engineer-ing properties of soils and their determination. 1.2 SCOPE AND ORGANIZATION The topics covered in this book begin with consider-ation of soil formation in Chapter 2 and soil mineral-ogy and compositional analysis of soil in Chapter 3. Relationships between soil composition and engineer-ing properties are developed in Chapter 4. Soil com-position by itself is insufficient for quantification of soil properties for specific situations, because the soil fabric, that is, the arrangements of particles, particle groups, and pores, may play an equally important role. This topic is covered in Chapter 5. Water may make up more than half the volume of a soil mass, it is attracted to soil particles, and the interactions between water and the soil surfaces influ-ence the behavior. In addition, owing to the colloidal nature of clay particles, the types and concentrations of chemicals in a soil can influence significantly its behavior in a variety of ways. Soil water and the clay– water–electrolyte system are then analyzed in Chapter 6. An analysis of interparticle forces and total and ef-fective stresses, with a discussion of why they are im-portant, is given in Chapter 7. The remaining chapters draw on the preceding de-velopments for explanations of phenomena and soil properties of interest in geotechnical and geoenviron-mental engineering. The formation of soil deposits, their resulting structures and relationships to geotech-nical properties and stability are covered in Chapter 8. The next three chapters deal with those soil properties that are of primary importance to the solution of most geoengineering problems: the flows of fluids, chemi-cals, electricity, and heat and their consequences in Chapter 9; volume change behavior in Chapter 10; and deformation and strength and deformation behavior in Chapter 11. Finally, Chapter 12 on time effects on strength and deformation recognizes that soils are not inert, static materials, but rather how a given soil re-sponds under different rates of loading or at some time in the future may be quite different than how it re-sponds today. 1.3 GETTING STARTED Find an article about a problem, a project, or issue that involves some aspect of geotechnical soil behavior as an important component. The article can be from the popular press, from a technical journal or magazine, such as the Journal of Geotechnical and Geoenviron-mental Engineering of the American Society of Civil Engineers, Ge´otechnique, The Canadian Geotechnical Journal, Soils and Foundations, ENR, or elsewhere. 1. Read the article and prepare a one-page infor-mative abstract. (An informative abstract sum-marizes the important ideas and conclusions. A descriptive abstract, on the other hand, simply states the article contents.) 2. Summarize the important geotechnical issues that are found in the article and write down what you believe you should know about to understand them well enough to solve the problem, resolve the issue, advise a client, and the like. In other words, what is in the article that you believe the subject matter in this book should prepare you to deal with? Do not exceed two pages. Copyright © 2005 John Wiley & Sons Retrieved from: www.knovel.com