1994
DOI: 10.1016/0378-4371(94)90329-8
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Brownian motion in the presence of a temperature gradient

Abstract: By considering an ensemble of Brownian particles suspended in a heat bath as a thermodynamic system with an internal degree of freedom it is possible to obtain the Fokker-Planck equation for Brownian motion in a temperature gradient, by applying the scheme of non-equilibrium thermodynamics. We recover explicitely the equations derived in particular by Zubarev and Bashkirov using statistical mechanical and kinetic methods. In addition when the temperature gradient does not have an externally imposed magnitude w… Show more

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Cited by 91 publications
(86 citation statements)
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“…28,29 Although both the flashing and the thermal ratchet are characterized by a multiplicative noise, their different physical origin is at the basis of this different response. For the thermal ratchet the spatial inhomogeneity affects both the amplitude of the fluctuations and the local equilibrium distribution while for the flashing ratchet the noise amplitude is regarded as an effective coarse-graining of a molecular mechanism that is decoupled from the underlying equilibrium properties of the Brownian particle.…”
Section: Thermal Ratchetmentioning
confidence: 99%
“…28,29 Although both the flashing and the thermal ratchet are characterized by a multiplicative noise, their different physical origin is at the basis of this different response. For the thermal ratchet the spatial inhomogeneity affects both the amplitude of the fluctuations and the local equilibrium distribution while for the flashing ratchet the noise amplitude is regarded as an effective coarse-graining of a molecular mechanism that is decoupled from the underlying equilibrium properties of the Brownian particle.…”
Section: Thermal Ratchetmentioning
confidence: 99%
“…Thermophoretic forces caused by a temperature gradient give rise to dust structures, are of central interest in the scavenging of aerosol particles in clouds, when droplets and/or ice crystals grow or evaporate, during the fall of hydrometeors, 1,2 and have been discussed in the context of nonequilibrium thermodynamics, 3,4 and in terms of a kinetic description, leading to a stochastic differential equation for a tracer particle in a solvent. 5 In contrast to thermophoretic forces, barophoretic effects caused by pressure gradients 6 and rheophoretic forces caused by velocity field gradients have been considered less frequently and not yet elaborated in an extensive, complete, or unifying fashion.…”
Section: Introductionmentioning
confidence: 99%
“…1 Thermophoretic forces caused by a temperature gradient induce dust structures, are of central interest in the scavenging of aerosol particles in clouds, when droplets and/or ice crystals grow or evaporate, during the fall of hydrometeors, 2,3 influence the velocity measurements in particle image velocimetry measurements, 4 and have been discussed in the context of nonequilibrium thermodynamics, 1,5,6 and in terms of a kinetic description, [7][8][9][10] leading to a stochastic differential equation for a tracer particle in a solvent. 1,11 In contrast to thermophoretic forces, barophoretic effects caused by pressure gradients, 12,13 and rheophoretic forces caused by velocity field gradients have been considered less frequently and not yet elaborated in an extensive, complete, or unifying fashion for nonspherical tracers.…”
Section: Introductionmentioning
confidence: 99%