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Thermal Properties I - Coggle Diagram
Thermal Properties I
Heat Capacity
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The heat capacity of such a system is defined as the amount of heat absorbed by a system per unit change in temperature
The experimental measurements of specific heat for solids are normally done at constant (atmospheric) pressure, yielding CP.
However, theory calculates CV since constant internuclear distances are used. From the equation, we can relate CV to CP by easily measurable quantities
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Classical Results
The heat capacity at constant volume, CV as a function of temperature for solid
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At room temperature, in most cases, the value of the heat capacity is 3Nk = 3R per mole = 25 J mol−1 deg−1. This result, derived from data is called the Dulong and Petit law
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CV of free particles
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This is just the classical result that each particle has an energy of kBT/2 for each degree of freedom
If we have Ν free particles in three dimensions, at thermal equilibrium the thermal average energy can be written out just as the preceding
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