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Viscosity is a property of a fluid that characterises its perceived
"thickness" or resistance to pouring. It describes a fluid's internal resistance to flow
and may be thought of as a measure of fluid friction. Thus, methanol is "thin", having a low viscosity, while vegetable oil is "thick" having a high viscosity.
Newton's theory
When a shear stress is applied to a solid body, the body deforms until the deformation results in an opposing force to balance that applied, an equilibrium. However, when a shear
stress is applied to a fluid, such as a wind
blowing over the surface of the ocean, the fluid
flows, and continues to flow while the stress is applied. When the stress is removed, in general, the flow decays due to internal
dissipation of energy. The "thicker" the fluid,
the greater its resistance to shear stress and the more rapid the decay of
its flow.
In general, in any flow, layers move at different velocities and the fluid's "thickness" arises from the shear
stress between the layers that ultimately opposes any applied force.
Isaac Newton postulated that, for straight, parallel and uniform flow, the shear stress, τ,
between layers is proportional to the velocity gradient, ∂u/∂y, in the direction perpendicular to the layers, in other words, the relative motion of the layers.
- .
Here, the constant μ is known as the coefficient of viscosity, viscosity or dynamic viscosity.
Many fluids, such as water and most gases, satisfy Newton's criterion and are known as Newtonian fluids. Non-Newtonian fluids
exhibit a more complicated relationship between shear stress and velocity gradient than simple linearity.
In many situations, we are concerned with the ratio of the viscous force to the inertial force, the latter characterised by the fluid density ρ. This ratio is characterised by the kinematic viscosity:
- .
James Clerk Maxwell called viscosity fugitive
elasticity because of the analogy that, elastic deformation opposes shear stress in solids, while in viscous
fluids, shear stress is opposed by
rate of deformation.
Viscosity is the principle means by which energy is dissipated in fluid motion, typically as heat.
Measurement of viscosity
Viscosity is measured with various types of viscometer, typically at 25°C
(standard state).
Units
Dynamic viscosity
The SI physical unit of dynamic
viscosity is the Pascal-second (Pa·s), which
is identical to 1 N·s/m2 or 1 kg/m·s). In France there have been some attempts to establish the poiseuille (Pl) as a name for
the Pa·s but without international success.
Care must be taken in not confusing the poiseuille with the poise!
The cgs physical unit for dynamic
viscosity is the poise (P) named after Jean Louis Marie Poiseuille. It is more commonly
expressed, particularly in ASTM standards, as
centipoise (cP).
1 poise = 100 centipoise = 1 g/cm·s = 0.1 Pa·s.
Kinematic viscosity
The SI physical unit of kinematic
viscosity is the (m2/s). The
cgs physical unit for kinematic
viscosity is the stokes (abbreviated S or St), named after George Gabriel Stokes . It is sometimes expressed in terms of centistokes (cS). US usage is the stoke.
1 stokes = 100 centistokes = 1 cm2/s = 0.0001 m2/s.
Molecular origins
It seems natural to see the origin of viscosity in terms of the attractive and repulsive forces between molecules. However, gases have substantial viscosity
even though their inter-molecular forces are weak suggesting some other mechanism.
Gases
Viscosity in gases arises principally from the molecular diffusion that transports momentum between layers of flow. The
kinetic theory of gases allows accurate prediction of
the behaviour of gaseous viscosity, in particular that, within the regime where the theory is
applicable:
Liquids
In liquids, the additional forces between molecules become important. This leads to
an additional contribution to the shear stress though the exact mechanics
of this are still controversial. Thus, in liquids:
Viscosity of some common materials
Some dynamic viscosities of Newtonian fluids are listed below:
Gases (at 0 °C):
Liquids (at 20 °C):
Many fluids such as honey have a wide range of
viscosities.
Can solids have a viscosity?
It is commonly asserted that amorphous solids, such as glass have viscosity, arguing on the basis that all solids flow, to some possibly
minuscule extent, in response to shear stress. Advocates of such a view
hold that the distinction bewteen solids and liquids is unlcear and that solids are simply liquids with a very high viscosity, typically greater than 1012 Pa·s. This position is often adopted by
supporters of the widely held urban myth that glass flow can be observed in old buildings.
However, others argue that solids are, in general, elastic for small stresses while fluids are not. Even if solids flow at higher stresses, they are characterised by their low-stress behaviour. Viscosity
may be an appropriate characteristic for solids in a plastic regime. The situation becomes somewhat confused as the
term viscosity is sometimes used for solid materials, for example Maxwell materials, to describe the relationship between stress and the rate of change of strain, rather
than rate of shear.
Eddy viscosity
In the study of turbulence in fluids, a common practical strategy for calculation is to ignore the small-scale vortices (or
eddies) in the motion and to calculate a large-scale motion with an eddy viscosity that characterises the
transport and dissipation of energy in the smaller-scale flow. Typical values of eddy
viscosity used in modelling ocean circulation are in excess of 107 Pa·s.
Fluidity
The reciprocal of viscosity is fluidity, usually symbolised by φ (=1/μ), measured in reciprocal
poise (cm·s/g), sometimes called the rhe. Fluidity is seldom used in
engineering practice.
Bibliography
- Massey, B S (1983) Mechanics of Fluids, fifth edition, ISBN 0442305524
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