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Free Surface Flow in a Microfluidic Corner and in an Unconfined Aquifer with Accretion: The Signorini and Saint-Venant Analytical Techniques Revisited© 2016, Springer Science+Business Media Dordrecht.Steady, laminar, fully developed flows of a

О термокапиллярной неустойчивости жидкого цилиндра, обдуваемого потоком газаThe thermocapillary flows and their stability in an infinite liquid column surrounded by a co

Quadratic mixed convective nanofluid flow past a moving yawed cylinder in the presence of thermal radiation and diffusive liquidsThe fluid flow around a yawed cylinder helps to understand the practical implications for undersea

Three-dimensional numerical simulation of tsunami waves based on the navier-stokes equations to simulate free surface waves and flows with gravity is presented. The main problem here is to ensure

Geochemical modeling with the use of vertical and horizontal relative concentrations of oil compounds for the heavy oil fields gradients of relative concentrations of compounds presented in oil, which allows assessing potential

Continuum regime motion of a growing droplet in opposing thermo-diffusiophoretic and gravitational fields of a thermal diffusion cloud chamberA model for the motion of aerosol particles by Stefan flow, thermo-diffusiophoresis and gravity

COVID-19 entropic characteristics the interaction proceeds along the potential gradient (positive work), the re-sultant potential energy is found

Estimation of the effective coefficient of viscosity within the quasi-viscous mechanism of mass transferWithin the quasi-viscous mechanism of plastic deformation by flows of nonequilibrium point defects

The model of the positive column of a glow discharge with the influence of the acoustic oscillations convective flow caused by the acoustic streaming leads to a redistribution of the gas temperature

Hybridized schemes of the discontinuous Galerkin method for stationary convection–diffusion problems in the leading part and are stated via approximations to the solution of the problem, its gradient, the flow

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