Linked from

The 19 pages that link to Newtonian fluid, each with the reason it gives.

• ViscoelasticityCompared with: It represents the purely viscous limit that viscoelastic materials depart from.

• RheologyCompared with: It is the simple-fluid limit against which non-Newtonian responses are distinguished.

• Granular materialCompared with: Granular flow can stop under stress and sustain enduring contact networks.

• Non-Newtonian fluidCompared with: It supplies the constant-viscosity reference that non-Newtonian fluids violate.

• Food rheologyCompared with: Many foods depart from this simple flow model through shear dependence or yield behavior.

• Shear rateCompared with: Its linear stress–rate relation provides the simplest interpretation of shear rate.

• Granular flowCompared with: Granular flow can change resistance with packing and stress, unlike this standard fluid model.

• Mantle viscosityCompared with: Mantle rocks often show stress-dependent creep, unlike an ideal Newtonian fluid.

• Rheology of the mantleCompared with: Mantle convection models often assume Newtonian behavior; real dislocation creep is non-linear.

• Complex fluidsCompared with: It provides the simple-flow benchmark that complex-fluid constitutive behavior departs from.

• Power-law fluidCompared with: The power-law model reduces to Newtonian behavior when its index equals one.