Book contents
- Frontmatter
- Contents
- Preface
- Prelude
- 1 The Earth-atmosphere system
- 2 Thermodynamics of gases
- 3 The Second Law and its implications
- 4 Heterogeneous systems
- 5 Transformations of moist air
- 6 Hydrostatic equilibrium
- 7 Static stability
- 8 Radiative transfer
- 9 Aerosol and cloud
- 10 Atmospheric motion
- 11 Atmospheric equations of motion
- 12 Large-scale motion
- 13 The planetary boundary layer
- 14 Wave propagation
- 15 The general circulation
- 16 Dynamic stability
- 17 Influence of the ocean
- 18 Interaction with the stratosphere
- Appendix A Conversion to SI units
- Appendix B Thermodynamic properties of air and water
- Appendix C Physical constants
- Appendix D Vector identities
- Appendix E Curvilinear coordinates
- Appendix F Pseudo-adiabatic chart
- Appendix G Acronyms
- Answers to selected problems
- References
- Index
- Plate section
4 - Heterogeneous systems
Published online by Cambridge University Press: 05 June 2012
- Frontmatter
- Contents
- Preface
- Prelude
- 1 The Earth-atmosphere system
- 2 Thermodynamics of gases
- 3 The Second Law and its implications
- 4 Heterogeneous systems
- 5 Transformations of moist air
- 6 Hydrostatic equilibrium
- 7 Static stability
- 8 Radiative transfer
- 9 Aerosol and cloud
- 10 Atmospheric motion
- 11 Atmospheric equations of motion
- 12 Large-scale motion
- 13 The planetary boundary layer
- 14 Wave propagation
- 15 The general circulation
- 16 Dynamic stability
- 17 Influence of the ocean
- 18 Interaction with the stratosphere
- Appendix A Conversion to SI units
- Appendix B Thermodynamic properties of air and water
- Appendix C Physical constants
- Appendix D Vector identities
- Appendix E Curvilinear coordinates
- Appendix F Pseudo-adiabatic chart
- Appendix G Acronyms
- Answers to selected problems
- References
- Index
- Plate section
Summary
The thermodynamic principles developed in Chaps. 2 and 3 apply to a homogeneous system, which can involve only a single phase. For it to be in thermodynamic equilibrium, a homogeneous system must be in thermal equilibrium: At most, an infinitesimal temperature difference exists between the system and its environment. It must also be in mechanical equilibrium: At most, an infinitesimal pressure difference exists between the system and its environment.
A heterogeneous system can involve more than one phase. For such a system, thermodynamic equilibrium imposes an additional constraint. The system must also be in chemical equilibrium: No conversion of mass occurs from one phase to another. Analogous to thermal and mechanical equilibrium, chemical equilibrium requires a certain state variable to have, at most, an infinitesimal difference between the phases present.
DESCRIPTION OF A HETEROGENEOUS SYSTEM
For a homogeneous system, two intensive properties describe the thermodynamic state. Conversely, only two state variables may be varied independently. A homogeneous system therefore has two thermodynamic degrees of freedom. For a heterogeneous system, each phase may be regarded as a homogeneous subsystem, one that is “open” due to exchanges with the other phases present. Consequently, the number of intensive properties that describe the thermodynamic state of a heterogeneous system is proportional to the number of phases present. Were they independent, those properties would constitute additional degrees of freedom for a heterogeneous system. However, thermodynamic equilibrium between phases introduces additional constraints.
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- Physics of the Atmosphere and Climate , pp. 112 - 126Publisher: Cambridge University PressPrint publication year: 2012