Thermodynamic principles and empirical studies confirm that the change in entropy of a system is dependent on temperature, often calculated via heat capacity integrals over temperature ranges.
Evidence for · 3
Magnetic cooling near Curie temperatures above 300 K
1984 · cited by 840
Discusses predicting entropy changes as a function of temperature near magnetic ordering temperatures.
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More for · 2
Thermodynamic parameters in the Earth as determined from seismic profiles
1981 · cited by 613
Calculates mineral entropies and temperature profiles using thermodynamic models.
Extended Regression Analysis for Debye–Einstein Models Describing Low Temperature Heat Capacity Data of Solids
2024 · cited by 2
Derives entropy as a function of temperature from heat capacity data of solids.