Thermodynamics: Introduction and Basic Concepts Study Notes

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29 Terms

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Thermodynamics

The science of energy and its transformations, particularly between heat, work, and the properties of matter.

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First Law of Thermodynamics

The principle of conservation of energy stating that energy cannot be created or destroyed, only changed in form (ΔE=Ein−Eout\Delta E = E_{\text{in}} - E_{\text{out}}).

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Second Law of Thermodynamics

The law asserting that energy possesses quality as well as quantity, and natural processes proceed only in the direction of decreasing quality of energy.

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Zeroth Law of Thermodynamics

States that if two bodies are each in thermal equilibrium with a third body, they are in thermal equilibrium with each other; serves as the basis of temperature measurement.

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Classical Thermodynamics

A macroscopic approach that evaluates the overall behavior of a system without requiring detailed knowledge of individual particles.

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Statistical Thermodynamics

A microscopic approach based on evaluating the average statistical behavior of large groups of individual atoms or molecules.

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Closed System (Control Mass)

A thermodynamic system with a fixed amount of mass where no mass can cross the boundary, though energy may cross as heat or work.

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Open System (Control Volume)

A selected region in space where both mass and energy can flow across the boundary surface.

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Isolated System

A system whose boundary prevents any exchange of mass or energy with its surroundings.

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Intensive Property

A system characteristic that is independent of system size or mass, such as temperature (TT), pressure (PP), or density (ρ\rho).

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Extensive Property

A system characteristic that depends directly on the size or extent of the system, such as total mass (mm), total volume (VV), or total energy (EE).

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Specific Property

An extensive property expressed per unit mass, converting it into an intensive value (e.g., specific volume v=Vmv = \frac{V}{m}).

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Continuum

The idealization of matter as continuous and evenly distributed rather than empty space with tiny molecules, valid for ordinary engineering scales.

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Specific Gravity (SGSG)

The dimensionless ratio of a substance's density to that of pure water at 4∘C4^\circ\text{C} (ρH2O=1000 kg/m3\rho_{\text{H}_2\text{O}} = 1000\,\text{kg/m}^3): SG=ρρH2OSG = \frac{\rho}{\rho_{\text{H}_2\text{O}}}. Substances with SG<1SG < 1 float in water.

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Thermodynamic Equilibrium

A state of balance where no driving forces exist, requiring simultaneous thermal, mechanical, phase, and chemical equilibrium.

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State Postulate

The principle stating that the thermodynamic state of a simple compressible system is completely specified by two independent, intensive properties.

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Quasi-equilibrium Process

An idealized process occurring slowly enough that the system remains infinitesimally close to thermodynamic equilibrium at all points, providing the maximum theoretical work output.

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Isothermal Process

A thermodynamic process during which temperature remains constant (T=constantT = \text{constant}).

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Isobaric Process

A thermodynamic process during which pressure remains constant (P=constantP = \text{constant}).

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Isochoric (Isometric) Process

A thermodynamic process during which specific volume remains constant (v=constantv = \text{constant}).

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Steady-Flow Process

A process in which a fluid flows steadily through a control volume such that conditions at any fixed position do not change with time.

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Absolute Pressure (PabsP_{\text{abs}})

The actual pressure measured relative to absolute vacuum (0 Pa0\,\text{Pa}).

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Gage Pressure (PgageP_{\text{gage}})

The pressure relative to local atmospheric pressure: Pgage=Pabs−PatmP_{\text{gage}} = P_{\text{abs}} - P_{\text{atm}}. Most measurement gages read zero at atmospheric pressure.

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Vacuum Pressure (PvacP_{\text{vac}})

The pressure measured below atmospheric pressure: Pvac=Patm−PabsP_{\text{vac}} = P_{\text{atm}} - P_{\text{abs}}.

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Hydrostatic Pressure with Depth

The linear increase of pressure with fluid depth due to fluid weight above: P=Patm+ρghP = P_{\text{atm}} + \rho g h.

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Pascal's Principle

The principle stating that an externally applied pressure is transmitted equally throughout an entire confined fluid: F1A1=F2A2\frac{F_1}{A_1} = \frac{F_2}{A_2}.

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Barometer

An instrument used to measure atmospheric pressure by balancing it against an inverted column of fluid: Patm=ρghP_{\text{atm}} = \rho g h.

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Manometer

A U-tube containing one or more dense fluids used to measure small to moderate pressure differences.