creeping flow technical
creeping motion technical

Even though his heart raced, time ceased to be a river running and became a creeping flow of mud.

Note that the equation for creeping flow results when the left side is assumed zero.

And it's being carried in the creeping flow of black blood - Wither's rain.

The creeping flow of light halted at the edge of the stone, did not reach her.

Time reversibility means that it is difficult to mix two fluids using creeping flow.

The analytical solution for the creeping flow around a sphere was first given by Stokes in 1851.

Creeping flow was first studied to understand lubrication.

The ellipsoid is the most general shape for which it has been possible to calculate the creeping flow of fluid around the solid shape.

He developed a solution for the internal and external flow field using a streamfunction approach similar to that of creeping flow past a sphere.

Kropinski (1999) Integral equation methods for particle simulations in creeping flows, Comput.

Creeping Flow Specialist A better way of applying mathematics to problems in fluid dynamics results in faster, more accurate answers.

An arbitrary lagrangian-eulerian formulation for creeping flows and its applications in tectonic models, Geophysical Journal International, 120, 1-23.

In some cases, such as one-dimensional flow and Stokes flow (or creeping flow), the equations can be simplified to linear equations.

In principle one doesn't know beforehand whether to apply the creeping flow solution, or what coefficient of drag to use, because the coefficient depends on the speed.

When the value of is substituted in the equation (5), we obtain the expression for terminal velocity of a spherical object moving under creeping flow conditions:

In our approach this is an Arbitrary Lagrangian-Eulerian implicit finite element thermal-mechanical model for creeping flows with viscous and plastic/frictional material properties.

There are three regimes: creeping flow, intermediate-Reynolds number Newton's Law (almost constant drag coefficient), and a high-Reynolds number regime.

References Fullsack, P., 1995, An arbitrary Lagrangian-Eulerian formulation for creeping flows and applications in tectonic models, Geophys.

Issue 1 Mining the Human Genone (Pio) Creeping Flow Specialist (Kropinski)

The creeping flow results can be applied in order to study the settling of sediment particles near the ocean bottom and the fall of moisture drops in the atmosphere.

Convective acceleration is present in most flows (exceptions include one-dimensional incompressible flow), but its dynamic effect is disregarded in creeping flow (also called Stokes flow).

Such flows are called creeping flows and the condition to be satisfied for the flows to be creeping flows is the Reynolds number, .

If the Reynolds number is very small, much less than 1, then the fluid will exhibit Stokes or creeping flow, where the viscous forces of the fluid dominate the inertial forces.

In fluid dynamics, Faxén's laws relate a sphere's velocity and angular velocity to the forces, torque, stresslet and flow it experiences under low Reynolds number (creeping flow) conditions.

His initial fluid mechanics interests included hypersonic aerodynamics, creeping flow, sloshing and channel flows and leading to flows in porous media, ship hydrodynamics and models for flow separation.

My apparel was in slow, creeping motion all around me, repairing extensive damage.

Small, brownish, undefined shape; they move with a creeping motion.

It was a creeping motion behind The Shadow's back.

Hence, when a long streak of blackness appeared upon the cracked marble floor, there was no one present to view its strange, creeping motion.

When the Reynolds number is much less than 1, Creeping motion or Stokes flow occurs.

Mantle convection is the slow creeping motion of Earth's rocky mantle caused by convection currents carrying heat from the interior of the earth to the surface.

Stokes flow (named after George Gabriel Stokes), also named creeping flow or creeping motion, is a type of fluid flow where advective inertial forces are small compared with viscous forces.

But then he began to add the creeping motions he had observed in smaller, younger strata creatures, keeping the area around the central depression motionless, however, and hoping that with the pumping motions of the stomachs he was giving the impression of a living organism.