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A comprehensive set of vocabulary flashcards covering the fundamental laws, state functions, and spontaneity criteria from the Core Chemistry 2 Thermodynamics lecture.
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Zeroth Law
States that if two systems are each in thermal equilibrium with a third system, they are in thermal equilibrium with each other; systems with different temperatures exchange heat, q, until they reach thermal equilibrium.
1st Law of Thermodynamics
The Conservation of Energy principle which states that internal energy, U, is the sum of a system’s potential and kinetic energies, and an increase in internal energy (ΔU) for a closed system is achieved by heating it (q > 0) and doing work on it (w > 0).
Internal Energy (U)
The sum of a system’s potential and kinetic energies.
Entropy (S)
A state function and measure of the dispersal of energy, thermodynamically defined by dS=Tδqrev. Entropy increases with heat input and accessible volume.
2nd Law of Thermodynamics
States that the entropy of an isolated system increases in a spontaneous process (\Delta S > 0).
Microstate (Ω)
A specific way of distributing the available energy amongst translational, rotational, vibrational, and electronic energy levels.
Clausius Inequality
The relationship defined by dS≥Tδq.
3rd Law of Thermodynamics
States that the entropy of all perfect crystalline substances is 0 at T=0K, consistent with the idea that there is no energy available to disperse.
Zero point energy
Energy that the Uncertainty Principle shows is irremovable and therefore cannot be dispersed.
Enthalpy (H)
Defined as H=U+pV; it is more useful than internal energy at constant pressure because the change in enthalpy is equal to the flow of heat (dH=dqp).
Heat Capacity at Constant Volume (CV)
The partial differential of internal energy with respect to temperature at constant volume: CV=(∂T∂U)V.
Heat Capacity at Constant Pressure (Cp)
The partial differential of enthalpy with respect to temperature at constant pressure: Cp=(∂T∂H)p.
Gibbs Free Energy (G)
Defined as G=H−TS; it represents the amount of energy ‘free’ to do non-expansion work at constant T and p.
Fundamental Equation of Thermodynamics
The equation dG=Vdp−SdT, which shows how Gibbs free energy varies with temperature and pressure for a closed system.
Helmholtz Free Energy (A)
Defined by the relation A=U−TS; it is useful in statistical thermodynamics and must decrease (dA≤0) for a spontaneous process at constant T and V.
Isolated System
A system that has no exchange of energy or matter with the surroundings.
Closed System
A system that exchanges energy with the surroundings but not matter.
Open System
A system that exchanges both energy and matter with the surroundings.
Spontaneity Criteria (Constant T,p)
For a process to occur spontaneously under these conditions, the change in Gibbs Free Energy must be less than or equal to zero (ΔG=ΔH−TΔS≤0).