4.2 Review

Zentropy Theory for Positive and Negative Thermal Expansion

期刊

JOURNAL OF PHASE EQUILIBRIA AND DIFFUSION
卷 43, 期 6, 页码 598-605

出版社

SPRINGER
DOI: 10.1007/s11669-022-00942-z

关键词

entropy; negative thermal expansion; partition function; thermal expansion; thermal contraction; thermodynamics; zentropy

资金

  1. National Science Foundation (NSF) [CMMI-1825538, CMMI-2050069]
  2. Department of Energy [DE-FE0031553, DE-NE0008945, DE-EE0008456, DE-SC0020147, DE-AR0001435]
  3. NASA Space Technology Research Fellowship [80NSSC18K1168]
  4. Army Research Lab [W911NF-14-2-0084]
  5. Office of Naval Research [N00014-21-1-2608]
  6. Wright Patterson AirForce Base
  7. National Institute of Standards and Technology [0433033, 0541674/8, 1034965/8]
  8. Office of Science of the U.S. Department of Energy [DE-AC02-05CH11231]
  9. NSF [ACI-1053575]
  10. Endowed Dorothy Pate Enright Professorship at The Pennsylvania State University
  11. NASA Jet Propulsion Laboratory
  12. U.S. Department of Energy (DOE) [DE-SC0020147] Funding Source: U.S. Department of Energy (DOE)

向作者/读者索取更多资源

The study introduces a general theory based on multiscale entropy to explain why volume sometimes decreases with increasing temperature. It is found that a phase at high temperatures is a statistical representation of the ground-state stable and multiple nonground-state metastable configurations. The theory provides a new understanding of the behavior of phase volume changes with temperature.
It has been observed in both natural and man-made materials that volume sometimes decreases with increasing temperature. Though mechanistic understanding has been gained for some individual materials, a general answer to the question Why does volume sometimes decrease with the increase of temperature? remains lacking. Based on the thermodynamic relation that the derivative of volume with respect to temperature, i.e., thermal expansion, is equal to the negative derivative of entropy with respect to pressure, we developed a general theory in terms of multiscale entropy to understand and predict the change of volume as a function of temperature, which is termed as zentropy theory in the present work. It is shown that a phase at high temperatures is a statistical representation of the ground-state stable and multiple nonground-state metastable configurations. It is demonstrated that when the volumes of the nonground-state configurations with high probabilities are smaller than that of the ground-state configuration, the volume of the phase may decrease with the increase of temperature in certain ranges of temperature-pressure combinations, depicting the negative divergency of thermal expansion at the critical point. As examples, positive and negative divergencies of thermal expansion are predicted at the critical points of Ce and Fe3Pt, respectively, along with the temperature and pressure ranges for abnormally positive and negative thermal expansions. The authors believe that the zentropy theory is applicable to predict anomalies of other physical properties of phases because the change of entropy drives the responses of a system to external stimuli.

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