Book contents
- Frontmatter
- Contents
- Preface
- 1 What is thermodynamics?
- 2 Defining our terms
- 3 The first law of thermodynamics
- 4 The second law of thermodynamics
- 5 Getting data
- 6 Some simple applications
- 7 Ideal solutions
- 8 Fugacity and activity
- 9 The equilibrium constant
- 10 Real solutions
- 11 The phase rule
- 12 Redox reactions
- 13 Equations of state
- 14 Solid solutions
- 15 Electrolyte solutions
- 16 Rock–water systems
- 17 Phase diagrams
- 18 Process modeling
- Appendices
- References
- Index
1 - What is thermodynamics?
- Frontmatter
- Contents
- Preface
- 1 What is thermodynamics?
- 2 Defining our terms
- 3 The first law of thermodynamics
- 4 The second law of thermodynamics
- 5 Getting data
- 6 Some simple applications
- 7 Ideal solutions
- 8 Fugacity and activity
- 9 The equilibrium constant
- 10 Real solutions
- 11 The phase rule
- 12 Redox reactions
- 13 Equations of state
- 14 Solid solutions
- 15 Electrolyte solutions
- 16 Rock–water systems
- 17 Phase diagrams
- 18 Process modeling
- Appendices
- References
- Index
Summary
Introduction
Thermodynamics is the branch of science that deals with relative energy levels and transfers of energy between systems and between different states of matter. Because these subjects arise in virtually every other branch of science, thermodynamics is one of the cornerstones of scientific training. Various scientific specialties place varying degrees of emphasis on the subject areas covered by thermodynamics – a text on thermodynamics for physicists can look quite different from one for chemists, or one for mechanical engineers. For chemists, biologists, geologists, and environmental scientists of various types, the thermodynamics of chemical reactions is of course a central concern, and that is the emphasis to be found in this book. Let us start by considering a few simple reactions and the questions that arise in doing this.
What is the problem?
Some simple chemical reactions
A chemical reaction involves the rearrangement of atoms from one structure or configuration to another, normally accompanied by an energy change. Let's consider some simple examples.
Take an ice cube from the freezer of your refrigerator and place it in a cup on the counter. After a few minutes, the ice begins to melt, and it soon is completely changed to water. When the water has warmed up to room temperature, no further change can be observed, even if you watch for hours. If you put the water back in the freezer, it changes back to ice within a few minutes, and again there is no further change. […]
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- Thermodynamics of Natural Systems , pp. 1 - 7Publisher: Cambridge University PressPrint publication year: 2005