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Temperature inversion of the thermal polarization of water
Author(s) -
Jeff Armstrong,
Fernando Bresme
Publication year - 2015
Publication title -
physical review e
Language(s) - English
Resource type - Journals
eISSN - 1550-2376
pISSN - 1539-3755
DOI - 10.1103/physreve.92.060103
Subject(s) - non equilibrium thermodynamics , thermal , polarization (electrochemistry) , dipole , inversion (geology) , inversion temperature , temperature gradient , materials science , thermal reservoir , condensed matter physics , thermodynamics , chemical physics , physics , chemistry , heat transfer , quantum mechanics , geology , paleontology , atmospheric sciences , structural basin , heat spreader , daytime
Temperature gradients polarize water, a nonequilibrium effect that may result in significant electrostatic fields for strong thermal gradients. Using nonequilibrium molecular dynamics simulations, we show that the thermal polarization features a significant dependence with temperature that ultimately leads to an inversion phenomenon, whereby the polarization field reverses its sign at a specific temperature. Temperature inversion effects have been reported before in the Soret coefficient of aqueous solutions, where the solution changes from thermophobic to thermophilic at specific temperatures. We show that a similar inversion behavior is observed in pure water. Microscopically, the inversion is the result of a balance of dipolar and quadrupolar contributions and the strong temperature dependence of the quadrupolar contribution, which is determined by the thermal expansion of the liquid

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