तरल-पदार्थ-का-बहना इसके अंग्रेजी अर्थ का उदाहरण

Canadian culture In fluid dynamics, stagnation pressure (or pitot pressure) is the static pressure at a stagnation point in a fluid flow.

Expatriates of the Ottoman Empire in the United States Direct Simulation Monte Carlo (DSMC) method uses probabilistic Monte Carlo simulation to solve the Boltzmann equation for finite Knudsen number fluid flows.

The DSMC method models fluid flows using simulation molecules which represent a large number of real molecules in a probabilistic simulation to solve the Boltzmann equation.

where bold symbols denote vectors, \mathbf{u} is the fluid flow velocity, \mathbf{v} is the spherical particle velocity, \rho_\mathrm{c} is the mass density of the fluid (continuous phase), V_\mathrm{p} is the volume of the particle, and D/Dt denotes the material derivative.

It is used to characterize fluid flows where there is simultaneous heat and mass transfer.

Combustion Schmidt number (Sc) is a dimensionless number defined as the ratio of momentum diffusivity (kinematic viscosity) and mass diffusivity, and is used to characterize fluid flows in which there are simultaneous momentum and mass diffusion convection processes.

A special class of advancing front techniques creates thin boundary layers of elements for fluid flow.

This has serious ramifications for the fluid dynamics of inward fluid flow.

The Navier–Stokes equations govern the velocity and pressure of a fluid flow.

Laminar flow, (or streamline flow) occurs when a fluid flows in parallel layers, with no disruption between the layers.

Computational fluid dynamics and other fluid flow techniques are being used extensively in the design of new continuous casting operations, especially in the tundish, to ensure that inclusions and turbulence are removed from the hot metal, yet ensure that all the metal reaches the mould before it cools too much.

Flux lines of the magnetic field are then advected with the fluid flow, until such time as gradients are concentrated into regions of short enough length scale that diffusion can balance advection.