2017
DOI: 10.1088/1742-6596/906/1/012010
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Hydrodynamic modeling of electron transport in silicon quantum wires

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Cited by 4 publications
(3 citation statements)
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“…The variables T The number of the unknowns present in the evolution equations is greater than the number of the equations, therefore one needs constitutive equations for the extravariables. A physically well sound method to get these constitutive equations is based on the exploitation of MEP [30][31][32][33][34][35]. This principle states that the occupation number can be approximated by that which maximizes the total entropy under the constraints that it reproduces the moments which have been chosen to describe the phonon state.…”
Section: Macroscopic Modelsmentioning
confidence: 99%
“…The variables T The number of the unknowns present in the evolution equations is greater than the number of the equations, therefore one needs constitutive equations for the extravariables. A physically well sound method to get these constitutive equations is based on the exploitation of MEP [30][31][32][33][34][35]. This principle states that the occupation number can be approximated by that which maximizes the total entropy under the constraints that it reproduces the moments which have been chosen to describe the phonon state.…”
Section: Macroscopic Modelsmentioning
confidence: 99%
“…Macroscopic models can be derived from the kinetic one [ 17 , 19 , 30 ] by taking suitable moments of the distribution functions as state variables. Here, we present in some detail only the evolution equations of the phonon variables, and refer the interested reader to [ 17 ] for a complete treatment of the problem.…”
Section: A Macroscopic Model and The Definition Of The Second Local Temperaturementioning
confidence: 99%
“…A new finite-difference method with an improved accuracy was proposed by the author and Russo in [18,20,17] for elliptic equations and extended to thermo-poroelastic Cauchy-Navier equations for elastic deformation [15], Euler equations for gas dynamics [11,19], electron transport in semiconductors [44,45], fluid flow in porous media for water-rock interaction [16,14]. In this approach, the ghost point values are eventually coupled each other, resulting in a bigger linear system with non-eliminated boundary conditions, solved by a multigrid approach suitably designed for ghost-point methods.…”
Section: Introductionmentioning
confidence: 99%