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Large-scale inhomogeneous thermodynamics : and application for atmospheric energetics /
Annotation There are large-scale fluid systems in the gravity field, such as the Earth's atmosphere and oceans, which posses some features different from those of classical thermodynamic systems. For example, the oceans and atmosphere possess in homogeneous melt equilibrium states with the same...
| Clasificación: | Libro Electrónico |
|---|---|
| Autor principal: | |
| Formato: | Electrónico eBook |
| Idioma: | Inglés |
| Publicado: |
Cambridge :
Cambridge International Science Pub.,
2004.
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| Temas: | |
| Acceso en línea: | Texto completo |
Tabla de Contenidos:
- Contents
- Introduction
- Two classical physical systems
- Introduction
- The Newtonian systems
- Principle of friction
- Dynamic entropy
- Simple thermodynamic systems
- Mole-number and molecular mass
- Thermodynamic variables
- Pressure of monatomic gas
- The first law of thermodynamics
- State equation of gases
- State equation of ideal gases
- Ideal-gas equation
- More features of ideal gases
- Kelvin temperature
- Mixing ratio of water vapor
- Thermodynamic energy law of ideal gases
- Internal energy and heat exchange
- Polytropic processMolecular transport processes
- Introduction
- Diffusion velocity and partial velocities
- Diffusion element and diffusion velocity
- Partial velocities
- Diffusion velocity in non-uniform ideal gases
- Self-diffusion of ideal gases
- Diffusive mass flux
- Coefficient of self-diffusion
- Viscosity of ideal gases
- Diffusive momentum flux
- Momentum conduction
- Coefficient of viscosity
- Relation to self-diffusion
- Heat conduction of ideal gases
- Conductive heat flux
- Heat conductivity
- Modified Eucken formula
- Collisional heat capacityComparison with experiments
- Predictability and thermodynamic entropy
- Introduction
- Change rate in diffusion processes
- Mass conservation law
- Mass diffusion equation
- Mass conservation
- Diffusive transport equation
- Unpredictability in classical thermodynamics
- Thermodynamic entropy law for uniform states
- Thermodynamic entropy change of non-uniform state
- Inadditive and scale-dependent features
- Thermodynamic entropy balance equation
- Relation to dynamic entropy
- Calculations for ideal gases
- Newtonian-thermodynamic systemIntroduction
- Field variables
- Parcel and parcel velocity
- Mass and heat transport equations
- Continuity equations
- Integrated variations in a system
- General continuity equation
- Heat flux equation
- Heat conduction equation
- Inhomogeneous thermodynamic system
- Adiabatic and transport processes
- Inhomogeneous thermodynamics
- Momentum equation of atmosphere
- Pressure gradient force
- Navier-Stokes equation
- Momentum equation of atmosphere
- Shallow water dynamics
- Newtonian-thermodynamic systemTurbulent entropy and universal principle
- Introduction
- Thermodynamic entropy of turbulent system
- Simple turbulent process
- Thermodynamic entropy changes
- Grid thermometers
- Turbulent thermodynamic entropy
- Turbulent entropy law
- Difference from classical thermodynamic entropy
- General discussion
- Example
- Turbulent entropy and disorderliness
- Universal principle
- The principle
- Applications
- Partition functions
- Heat capacity and van der Waals equation
- Einstein function