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  2. Saffman–Taylor instability - Wikipedia

    en.wikipedia.org/wiki/Saffman–Taylor_instability

    A demonstration of the Saffman-Taylor instability is such when a viscous substance, such as PVA glue, is placed on a flat surface (Top), another parallel surface is placed on top and the glue spreads out (Middle), and the surfaces are lifted, air, a less viscous fluid, attempts to invade the space where the glue is located.The interface between ...

  3. Asthenosphere - Wikipedia

    en.wikipedia.org/wiki/Asthenosphere

    The asthenosphere (from Ancient Greek ἀσθενός (asthenós) 'without strength') is the mechanically weak [1] and ductile region of the upper mantle of Earth. It lies below the lithosphere, at a depth between c. 80 and 200 km (50 and 120 mi) below the surface, and extends as deep as 700 km (430 mi). However, the lower boundary of the ...

  4. List of viscosities - Wikipedia

    en.wikipedia.org/wiki/List_of_viscosities

    Here "standard conditions" refers to temperatures of 25 °C and pressures of 1 atmosphere.Where data points are unavailable for 25 °C or 1 atmosphere, values are given at a nearby temperature/pressure.

  5. Viscosity solution - Wikipedia

    en.wikipedia.org/wiki/Viscosity_solution

    Nevertheless, while the theory of viscosity solutions is sometimes considered unrelated to viscous fluids, irrotational fluids can indeed be described by a Hamilton-Jacobi equation. [15] In this case, viscosity corresponds to the bulk viscosity of an irrotational, incompressible fluid.

  6. Derivation of the Navier–Stokes equations - Wikipedia

    en.wikipedia.org/wiki/Derivation_of_the_Navier...

    The general form of the equations of motion is not "ready for use", the stress tensor is still unknown so that more information is needed; this information is normally some knowledge of the viscous behavior of the fluid. For different types of fluid flow this results in specific forms of the Navier–Stokes equations.

  7. Viscoelasticity - Wikipedia

    en.wikipedia.org/wiki/Viscoelasticity

    In materials science and continuum mechanics, viscoelasticity is the property of materials that exhibit both viscous and elastic characteristics when undergoing deformation. Viscous materials, like water, resist both shear flow and strain linearly with time when a stress is applied. Elastic materials strain when stretched and immediately return ...

  8. Temperature dependence of viscosity - Wikipedia

    en.wikipedia.org/wiki/Temperature_dependence_of...

    In liquids, viscous forces are caused by molecules exerting attractive forces on each other across layers of flow. Increasing temperature results in a decrease in viscosity because a larger temperature means particles have greater thermal energy and are more easily able to overcome the attractive forces binding them together.

  9. Inviscid flow - Wikipedia

    en.wikipedia.org/wiki/Inviscid_flow

    The value represents the ratio of inertial forces to viscous forces in a fluid, and is useful in determining the relative importance of viscosity. [6] In inviscid flow, since the viscous forces are zero, the Reynolds number approaches infinity. [1] When viscous forces are negligible, the Reynolds number is much greater than one. [1]