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Preface to the Second Edition xiii
Preface to the First Edition: Why Thermodynamics? xv
Acknowledgments xxi
Notes for Instructors xxiii
List of Variables xxv
I Historical Roots: From Heat Engines to Cosmology
1 Basic Concepts and the Laws of Gases 3
Introduction 3
1.1 Thermodynamic Systems 4
1.2 Equilibrium and Nonequilibrium Systems 6
1.3 Biological and Other Open Systems 8
1.4 Temperature, Heat and Quantitative Laws of Gases 9
1.5 States of Matter and the van der Waals Equation 17
1.6 An Introduction to the Kinetic Theory of Gases 24
Appendix 1.1 Partial Derivatives 32
Appendix 1.2 Elementary Concepts in Probability Theory 33
Appendix 1.3 Mathematica Codes 34
References 39
Examples 39
Exercises 41
2 The First Law of Thermodynamics 45
The Idea of Energy Conservation Amidst New Discoveries 45
2.1 The Nature of Heat 46
2.2 The First Law of Thermodynamics: The Conservation of Energy 50
2.3 Elementary Applications of the First Law 57
2.4 Thermochemistry: Conservation of Energy in Chemical Reactions 61
2.5 Extent of Reaction: A State Variable for Chemical Systems 68
2.6 Conservation of Energy in Nuclear Reactions and Some General Remarks 69
2.7 Energy Flows and Organized States 71
Appendix 2.1 Mathematica Codes 79
Appendix 2.2 Energy Flow in the USA for the Year 2013 79
References 82
Examples 82
Exercises 85
3 The Second Law of Thermodynamics and the Arrow of Time 89
3.1 The Birth of the Second Law 89
3.2 The Absolute Scale of Temperature 96
3.3 The Second Law and the Concept of Entropy 99
3.4 Modern Formulation of the Second Law 104
3.5 Examples of Entropy Changes due to Irreversible Processes 112
3.6 Entropy Changes Associated with Phase Transformations 114
3.7 Entropy of an Ideal Gas 115
3.8 Remarks about the Second Law and Irreversible Processes 116
Appendix 3.1 The Hurricane as a Heat Engine 117
Appendix 3.2 Entropy Production in Continuous Systems 120
References 121
Examples 122
Exercises 123
4 Entropy in the Realm of Chemical Reactions 125
4.1 Chemical Potential and Affinity: The Thermodynamic Force for Chemical Reactions 125
4.2 General Properties of Affinity 132
4.3 Entropy Production Due to Diffusion 135
4.4 General Properties of Entropy 136
Appendix 4.1 Thermodynamics Description of Diffusion 138
References 139
Example 139
Exercises 140
II Equilibrium Thermodynamics
5 Extremum Principles and General Thermodynamic Relations 145
Extremum Principles in Nature 145
5.1 Extremum Principles Associated with the Second Law 145
5.2 General Thermodynamic Relations 153
5.3 Gibbs Energy of Formation and Chemical Potential 156
5.4 Maxwell Relations 159
5.5 Extensivity with Respect to N and Partial Molar Quantities 160
5.6 Surface Tension 162
References 165
Examples 165
Exercises 166
6 Basic Thermodynamics of Gases, Liquids and Solids 169
Introduction 169
6.1 Thermodynamics of Ideal Gases 169
6.2 Thermodynamics of Real Gases 172
6.3 Thermodynamics Quantities for Pure Liquids and Solids 180
Reference 183
Examples 183
Exercises 184
7 Thermodynamics of Phase Change 187
Introduction 187
7.1 Phase Equilibrium and Phase Diagrams 187
7.2 The Gibbs Phase Rule and Duhem's Theorem 192
7.3 Binary and Ternary Systems 194
7.4 Maxwell's Construction and the Lever Rule 198
7.5 Phase Transitions 201
References 203
Examples 203
Exercises 204
8 Thermodynamics of Solutions 207
8.1 Ideal and Nonideal Solutions 207
8.2 Colligative Properties 211
8.3 Solubility Equilibrium 217
8.4 Thermodynamic Mixing and Excess Functions 222
8.5 Azeotropy 225
References 225
Examples 225
Exercises 227
9 Thermodynamics of Chemical Transformations 231
9.1 Transformations of Matter 231
9.2 Chemical Reaction Rates 232
9.3 Chemical Equilibrium and the Law of Mass Action 239
9.4 The Principle of Detailed Balance 243
9.5 Entropy Production due to Chemical Reactions 245
9.6 Elementary Theory of Chemical Reaction Rates 248
9.7 Coupled Reactions and Flow Reactors 251
Appendix 9.1 Mathematica Codes 256
References 260
Examples 260
Exercises 261
10 Fields and Internal Degrees of Freedom 265
The Many Faces of Chemical Potential 265
10.1 Chemical Potential in a Field 265
10.2 Membranes and Electrochemical Cells 270
10.3 Isothermal Diffusion 277
10.4 Chemical Potential for an Internal Degree of Freedom 281
References 284
Examples 284
Exercises 285
11 Thermodynamics of Radiation 287
Introduction 287
11.1 Energy Density and Intensity of Thermal Radiation 287
11.2 The Equation of State 291
11.3 Entropy and Adiabatic Processes 293
11.4 Wien's Theorem 295
11.5 Chemical Potential of Thermal Radiation 296
11.6 Matter-Antimatter in Equilibrium with Thermal Radiation: The State of Zero Chemical Potential 297
11.7 Chemical Potential of Radiation not in Thermal Equilibrium with Matter 299
11.8 Entropy of Nonequilibrium Radiation 300
References 302
Example 302
Exercises 302
III Fluctuations and Stability
12 The Gibbs Stability Theory 307
12.1 Classical Stability Theory 307
12.2 Thermal Stability 308
12.3 Mechanical Stability 309
12.4 Stability and Fluctuations in Nk 310
References 313
Exercises 313
13 Critical Phenomena and Configurational Heat Capacity 315
Introduction 315
13.1 Stability and Critical Phenomena 315
13.2 Stability and Critical Phenomena in Binary Solutions 317
13.3 Configurational Heat Capacity 320
Further Reading 321
Exercises 321
14 Entropy Production, Fluctuations and Small Systems 323
14.1 Stability and Entropy Production 323
14.2 Thermodynamic Theory of Fluctuations 326
14.3 Small Systems 331
14.4 Size-Dependent Properties 333
14.5 Nucleation 336
References 339
Example 339
Exercises 340
IV Linear Nonequilibrium Thermodynamics
15 Nonequilibrium Thermodynamics: The Foundations 343
15.1 Local Equilibrium 343
15.2 Local Entropy Production 345
15.3 Balance Equation for Concentration 346
15.4 Energy Conservation in Open Systems 348
15.5 The Entropy Balance Equation 351
Appendix 15.1 Entropy Production 354
References 356
Exercises 356
16 Nonequilibrium Thermodynamics: The Linear Regime 357
16.1 Linear Phenomenological Laws 357
16.2 Onsager Reciprocal Relations and the Symmetry Principle 359
16.3 Thermoelectric Phenomena 363
16.4 Diffusion 366
16.5 Chemical Reactions 371
16.6 Heat Conduction in Anisotropic Solids 375
16.7 Electrokinetic Phenomena and the Saxen Relations 377
16.8 Thermal Diffusion 379
References 382
Further Reading 382
Exercises 383
17 Nonequilibrium Stationary States and Their Stability: Linear Regime 385
17.1 Stationary States under Nonequilibrium Conditions 385
17.2 The Theorem of Minimum Entropy Production 391
17.3 Time Variation of Entropy Production and the Stability of Stationary States 398
References 400
Exercises 400
V Order Through Fluctuations
18 Nonlinear Thermodynamics 405
18.1 Far-from-Equilibrium Systems 405
18.2 General Properties of Entropy Production 405
18.3 Stability of Nonequilibrium Stationary States 407
18.4 Linear Stability Analysis 411
Appendix 18.1 A General Property of dFP/dt 415
Appendix 18.2 General Expression for the Time Derivative of ¿¿¿¿ 2S 416
References 418
Exercises 418
19 Dissipative Structures 421
19.1 The Constructive Role of Irreversible Processes 421
19.2 Loss of Stability, Bifurcation and Symmetry Breaking 421
19.3 Chiral Symmetry Breaking and Life 424
19.4 Chemical Oscillations 431
19.5 Turing Structures and Propagating Waves 436
19.6 Dissipative Structures and Machines 440
19.7 Structural Instability and Biochemical Evolution 441
Appendix 19.1 Mathematica Codes 442
References 447
Further Reading 448
Exercises 449
20 Elements of Statistical Thermodynamics 451
Introduction 451
20.1 Fundamentals and Overview 452
20.2 Partition Function Factorization 454
20.3 The Boltzmann Probability Distribution and Average Values 456
20.4 Microstates, Entropy and the Canonical Ensemble 457
20.5 Canonical Partition Function and Thermodynamic Quantities 460
20.6 Calculating Partition Functions 461
20.7 Equilibrium Constants 467
20.8 Heat Capacities of Solids 469
20.9 Planck's Distribution Law for Thermal Radiation 472
Appendix 20.1 Approximations and Integrals 474
Reference 475
Example 475
Exercises 475
21 Self-Organization and Dissipative Structures in Nature 477
21.1 Dissipative Structures in Diverse Disciplines 477
21.2 Towards a Thermodynamic Theory of Organisms 483
References 485
Epilogue 487
Physical Constants and Data 489
Standard Thermodynamic Properties 491
Energy Units and Conversions 501
Answers to Exercises 503
Author Index 511
Subject Index 513
Since half a century ago, our view of Nature has changed drastically. Classical science emphasized equilibrium and stability. Now we see fluctuations, instability, evolutionary processes on all levels from chemistry and biology to cosmology. Everywhere we observe irreversible processes in which time symmetry is broken. The distinction between reversible and irreversible processes was first introduced in thermodynamics through the concept of 'entropy', the arrow of time, as Arthur Eddington called it. Therefore our new view of Nature leads to an increased interest in thermodynamics. Unfortunately, most introductory texts are limited to the study of equilibrium states, restricting thermodynamics to idealized, infinitely slow reversible processes. The student does not see the relationship between irreversible processes that naturally occur, such as chemical reactions and heat conduction, and the rate of increase of entropy. In this text, we present a modern formulation of thermodynamics in which the relation between the rate of increase of entropy and irreversible processes is made clear from the very outset. Equilibrium remains an interesting field of inquiry but in the present state of science, it appears essential to include irreversible processes as well.
It is the aim of this book to give a readable introduction to present-day thermodynamics, starting with its historical roots as associated with heat engines but including also the thermodynamic description of far-from-equilibrium situations. As is well known today, far-from-equilibrium situations lead to new space-time structures. For this reason the restriction to equilibrium situations hides, in our opinion, some essential features of the behavior of matter and energy. An example is the role of fluctuations. The atomic structure of matter leads to fluctuations. However, at equilibrium or near equilibrium, these fluctuations are inconsequential.
Indeed a characteristic feature of equilibrium thermodynamics is the existence of extremum principles. For isolated systems entropy increases and is therefore maximum at equilibrium. In other situations (such as constant temperature) there exist functions called thermodynamic potentials which are also extrema (that is maximum or minimum) at equilibrium. This has important consequences. A fluctuation that leads to a temporal deviation from equilibrium is followed by a response that brings back the system to the extremum of the thermodynamic potential. The equilibrium world is also a stable world. This is no longer so in far-from-equilibrium situations. Here fluctuations may be amplified by irreversible dissipative processes and lead to new space-time structures which one of us (I. Prigogine) has called 'dissipative structures' to distinguish them from 'equilibrium' structures such as crystals. Therefore distance from equilibrium becomes a parameter somewhat similar to temperature. When we lower the temperature, we go from the gaseous state to a liquid and then a solid. As we shall see, here the variety is even greater. Take the example of chemical reactions. Increasing the distance from equilibrium we may obtain in succession oscillatory reactions, new spatial periodic structures and chaotic situations in which the time behavior becomes so irregular that initially close trajectories diverge exponentially.
One aspect is common to all these nonequilibrium situations, the appearance of long-range coherence. Macroscopically distinct parts become correlated. This is in contrast to equilibrium situations where the range of correlations is determined by short-range intermolecular forces. As a result, situations that are impossible to realize at equilibrium become possible in far-from-equilibrium situations. This leads to important applications in a variety of fields. We can produce new materials in nonequilibrium situations where we escape from the restrictions imposed by the phase rule. Also, nonequilibrium structures appear at all levels in biology. We give some simple examples in Chapters 19 and the postface. It is now generally admitted that biological evolution is the combined result of Darwin's natural selection as well as of self-organization, which results from irreversible processes.
Since Ludwig Boltzmann (1844-1906) introduced a statistical definition of entropy in 1872, entropy is associated with disorder. The increase of entropy is then described as an increase of disorder, as the destruction of any coherence that may be present in the initial state. This has unfortunately led to the view that the consequences of the Second Law are self-evident, are trivial. This is, however, not true even for equilibrium thermodynamics, which leads to highly nontrivial predictions. Anyway, equilibrium thermodynamics covers only a small fraction of our everyday experience. We now understand that we cannot describe Nature around us without an appeal to nonequilibrium situations. The biosphere is maintained in nonequilibrium through the flow of energy coming from the Sun and this flow is itself the result of the nonequilibrium situation of our present state of the universe.
It is true that the information obtained from thermodynamics both for equilibrium and nonequilibrium situations is limited to a few general statements. We have to supplement them by the equation of state at equilibrium or the rate laws, such as chemical reaction rates. Still the information we obtain from thermodynamics is quite valuable precisely because of its generality.
Our book is subdivided into five parts. The first, Chapters 1 to 4, deals with the basic principles. The systems considered in thermodynamics are large systems (the number of particles N is a typical Avogadro number). Such systems are described by two types of variables, variables such as pressure or temperature, which are independent of the size of the system and are called 'intensive' variables, and variables such as the total energy, which are proportional to the number of particles ('extensive variables'). Historically thermodynamics started with empirical observations concerning the relation between these variables (e.g. the relation between pressure and volume). This is the main subject of Chapter 1. However, the two conceptual innovations of thermodynamics are the formulation of the 'First Law' expressing conservation of energy (Chapter 2) and of the 'Second Law' introducing entropy (Chapter 3).
Ignis mutat res. Fire transforms matter; fire leads to chemical reactions, to processes such as melting and evaporation. Fire makes fuel burn and release heat. Out of all this common knowledge, nineteenth century science concentrated on the single fact that combustion produces heat and that heat may lead to an increase in volume; as a result, combustion produces work. Fire leads, therefore, to a new kind of machine, the heat engine, the technological innovation on which industrial society has been founded.
What is then the link between 'heat' and 'work'? This question was at the origin of the formulation of the principle of energy conservation. Heat is of the same nature as energy. In the heat engine, heat is transferred into work but energy is conserved.
However, there was more. In 1811 Baron Jean-Joseph Fourier, the Prefect of Isère, won the prize of the French Academy of Sciences for his mathematical description of the propagation of heat in solids. The result stated by Fourier was surprisingly simple and elegant: heat flow is proportional to the gradient of temperature. It is remarkable that this simple law applies to matter, whether its state is solid, liquid or gaseous. Moreover, it remains valid whatever the chemical composition of the body, whether it is iron or gold. It is only the coefficient of proportionality between the heat flow and the gradient of temperature that is specific to each substance.
Fourier's law was the first example describing an irreversible process. There is a privileged direction of time as heat flows according to Fourier's law, from higher to lower temperature. This is in contrast with the laws of Newtonian dynamics in which the past and future play the same role (time enters only in Newton's law through a second derivative, so Newton's law is invariant in respect to time inversion). As already mentioned, it is the Second Law of thermodynamics that expresses the difference between 'reversible' and irreversible processes through the introduction of entropy. Irreversible processes produce entropy.
The history of the two principles of thermodynamics is a most curious one. Born in the middle of technological questions, they acquired rapidly a cosmological status. Let us indeed state the two principles as formulated by Rudolph Clausius (1822-1888) in the year 1865:
The energy of the universe is constant.
The entropy of the universe approaches a maximum.
It was the first evolutionary formulation of cosmology. This was a revolutionary statement as the existence of irreversible processes (and therefore of entropy) conflicts with the time-reversible view of dynamics. Of course, classical dynamics has been superseded by quantum theory and relativity. However, this conflict remains because, in both quantum theory and relativity, the basic dynamical laws are time-reversible.
The traditional answer to this question is to emphasize that the systems...
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