Viscosity
黏滯係數
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What's Viscosity?
wiki
The viscosity of a fluid is a measure of its
resistance to deformation at a given rate.
Viscosity can be conceptualized as quantifying the frictional
force that arises between adjacent layers of fluid that are in
relative motion
Newton's law of viscosity is not a fundamental law of nature,
but rather a constitutive equation (like Hooke's law, Fick's
law, and Ohm's law) which serves to define the viscosity
μ .
Its form is motivated by experiments which show that for a wide
range of fluids,
μ
is independent of strain rate. Such fluids
are called Newtonian. Gases, water, and many common liquids can
be considered Newtonian in ordinary conditions and contexts.
Only
a small group of fluids exhibit such constant viscosity. The
large class of fluids whose viscosity changes with the strain
rate (the relative flow velocity) are called non-Newtonian
fluids.
For example:
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Shear-thickening liquids, whose viscosity increases with the
rate of shear strain.
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Shear-thinning liquids, whose viscosity decreases with the rate
of shear strain.
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Thixotropic liquids, that become less viscous over time when
shaken, agitated, or otherwise stressed.
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Rheopectic (dilatant) liquids, that become more viscous over
time when shaken, agitated, or otherwise stressed.
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Bingham plastics that behave as a solid at low stresses but flow
as a viscous fluid at high stresses.
Rheology
generally accounts for the behavior of non-Newtonian
fluids, by characterizing the minimum number of functions that
are needed to relate stresses with rate of change of strain or
strain rates.
The term rheology was coined by Eugene C. Bingham, a professor
at Lafayette College, in 1920, from a suggestion by a colleague,
Markus Reiner.
液體的粘滯性 Visocity
如何使用
Thomas-Stormer viscometer
溫度對粘滯係數的影響
Rheology
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