Everything about Viscous totally explained
Viscosity is a measure of the
resistance of a
fluid which is being deformed by either
shear stress or
extensional stress. It is commonly perceived as "thickness", or resistance to flow. Viscosity describes a fluid's internal resistance to flow and may be thought of as a measure of fluid
friction. Thus,
water is "thin", having a lower viscosity, while
vegetable oil is "thick" having a higher viscosity. All real fluids (except
superfluids) have some resistance to
stress, but a fluid which has no resistance to shear stress is known as an
ideal fluid or
inviscid fluid. The study of viscosity is known as
rheology.
Etymology
The word "viscosity" derives from the
Latin word "" for
mistletoe. A viscous glue was made from mistletoe berries and used for lime-twigs to catch birds.
Viscosity coefficients
When looking at a value for viscosity, the number that one most often sees is the coefficient of viscosity. There are several different viscosity coefficients depending on the nature of applied stress and nature of the fluid. They are introduced in the main books on
hydrodynamics and
rheology.
Shear viscosity and
dynamic viscosity are much better known than the others. That is why they're often referred to as simply
viscosity.
Simply put, this quantity is the ratio between the pressure exerted on the surface of a fluid, in the lateral or horizontal direction, to the change in velocity of the fluid as you move down in the fluid (this is what is referred to as a velocity
gradient). For example, at room temperature, water has a nominal viscosity of 1.0 × 10
-3 Pa∙s and motor oil has a nominal apparent viscosity of 250 × 10
-3 Pa∙s.
» Extensional viscosity is widely used for characterizing polymers.
Volume viscosity is essential for
Acoustics in fluids, see
Stokes' law (sound attenuation)
Newton's theory
In general, in any flow, layers move at different
velocities and the fluid's viscosity 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.
»
Further Information
Get more info on 'Viscous'.
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