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Motion of a fluid subjected to unbalanced forces or stresses. The motion continues
as long as unbalanced forces are applied. For example, in the pouring of
water from a pitcher the water velocity is very high over the lip, moderately
high approaching the lip, and very low near the bottom of the pitcher.
The unbalanced force is gravity, that is, the weight of the tilted water
particles near the surface. The flow continues as long as water is available
and the pitcher remains tilted.
A fluid may be a liquid, vapor, or gas. The term vapor denotes a gaseous substance
interacting with its own liquid phase, for example, steam above water.
If this phase interaction is not important, the vapor is simply termed
a gas.
Gases have weak intermolecular forces and expand to fill any
container. Left free, gases expand and form the atmosphere of the Earth.
Gases are highly compressible; doubling the pressure at constant temperature
doubles the density.
Liquids, in contrast, have strong intermolecular forces and
tend to retain constant volume. Placed in a container, a liquid occupies
only its own volume and forms a free surface which is at the same pressure
as any gas touching it. Liquids are nearly incompressible; doubling the
pressure of water at room temperature, for example, increases its density
by only 0.005%.
Liquids and vapors can flow together as a mixture, such as
steam condensing in a pipe flow with cold walls. This constitutes a special
branch of fluid mechanics, covering two-phase-flow.
The physical properties of a fluid are essential to formulating
theories and developing designs for fluid flow. Especially important
are pressure, density, and temperature.
Since shear stresses cause motion in a fluid and result in
differences in normal stresses at a point, it follows that a fluid at
rest must have zero shear and uniform pressure at a point. This is the
hydrostatic condition. The fluid pressure increases deeper in the fluid
to balance the increased weight of fluid above. For liquids, and for
gases over short vertical distances, the fluid density can be assumed
to be constant.
When a fluid is subjected to shear stress, it flows and resists
the shear through molecular momentum transfer. The macroscopic effect
of this molecular action, for most common fluids, is the physical property
called viscosity. Shear stress results in a gradient in fluid velocity;
the converse is also true.
The common fluids for which the linear relationship of flow
velocity and sheer stress holds are called newtonian viscous fluids.
More complex fluids, such as paints, pastes, greases, and slurries, exhibit
nonlinear or non-newtonian behavior and require more complex theories
to account for their behavior.
A common characteristic of all fluids, whether newtonian or
not, is that they do not slip at a solid boundary. No matter how fast
they flow away from the boundary, fluid particles at a solid surface
become entrapped by the surface structure. The macroscopic effect is
that the fluid velocity equals the solid velocity at a boundary. This
is called the no-slip condition where the solid is fixed, so that the
fluid velocity drops to zero there. No-slip sets up a slow-moving shear
layer or boundary layer when fluid flows near a solid surface. The theory
of boundary-layer flow is well developed and explains many effects involving
viscous flow past immersed bodies or within passages.
All fluids are at least slightly compressible, that is, their
density increases as pressure is applied. In many flows, however, compressibility
effects may be neglected.
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