Part of the book series: Mechanical Engineering Series ((MES))

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Abstract

This chapter begins with a description of thermodynamic equilibrium and its relationship to static equilibrium, defines a global equilibrium state as an idealized actual quasi-equilibrium state. Also a local equilibrium state is described together with the principle of local equilibrium, namely that in a thermodynamic process in which system properties vary in space and time the local equilibrium state equations remain valid. The chapter continues with a review of the mathematics of curves and surfaces needed later and describes a methodology for solving all subsequent thermodynamic problems. This methodology is modified in later chapters to include additional features, but the basic principle remains the same throughout. Finally there is an explanation of how the mechanical equation of state can be written as a differential equation in terms of its measurable first partial derivatives and then integrated to obtain the equation. This idea is then applied to obtain mechanical equations of state for liquids, vaporizable liquids, ideal gases, condensible gases, and mixtures, which includes mixtures of ideal gases such as air and moist air, and most importantly liquid-vapor phase equilibrium mixtures.

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Notes

  1. 1.

    A simple example is x = x(y) = y 2, which cannot be inverted uniquely, and there are two possibilities \(y=y_1(x)=\sqrt {x}\) and \(y=y_2(x)=-\sqrt {x}\).

  2. 2.

    Each partial derivative is done holding the other variable constant, but we will not represent this explicitly, as we did in Sects. 1.3.10 and 1.3.11, as long as there can be no confusion.

  3. 3.

    A solid in a general state of stress is not a simple compressible substance because its state is not determined by 2 independent variables.

  4. 4.

    The range of validity of Eq. (2.36), , is small, not large, in the vicinity of the critical point, which will be discussed later, because β c = ∞ (α c = ∞ also).

  5. 5.

    The data in Table A.3 for the liquid phase of water shows that the pressure correction to Eq. (2.36) is less than 1% up to pressures of 2000 psi (15 MPa in Appendix B.3). In Tables A.5 and B.5 for R-12, all the liquid data given is the saturated value.

  6. 6.

    An elementary entity may be an atom, a molecule, or any other particle or specified group of particles.

  7. 7.

    The range 40 to 60% is comfortable. At higher levels the air feels too wet and at lower ones, too dry.

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Whitman, A.M. (2023). Equilibrium. In: Thermodynamics: Basic Principles and Engineering Applications. Mechanical Engineering Series. Springer, Cham. https://doi.org/10.1007/978-3-031-19538-9_2

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  • DOI: https://doi.org/10.1007/978-3-031-19538-9_2

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  • Publisher Name: Springer, Cham

  • Print ISBN: 978-3-031-19537-2

  • Online ISBN: 978-3-031-19538-9

  • eBook Packages: EngineeringEngineering (R0)

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