The Inertial number I {\displaystyle I} is a dimensionless quantity which quantifies the significance of dynamic effects on the flow of a granular material. It measures the ratio of inertial forces of grains to imposed forces: a small value corresponds to the quasi-static state, while a high value corresponds to the inertial state or even the "dynamic" state. It is given by:
where γ ˙ {\displaystyle {\dot {\gamma }}} is the shear rate, d {\displaystyle d} the average particle diameter, P {\displaystyle P} is the pressure and ρ {\displaystyle \rho } is the density. Generally three regimes are distinguished:
I < 10 − 3 {\displaystyle I<10^{-3}} : quasi static flow
10 − 3 < I < 10 − 1 {\displaystyle 10^{-3}<I<10^{-1}} : dense flow
I > 10 − 1 {\displaystyle I>10^{-1}} : collisional flow One model of dense granular flows, the μ(I) rheology, asserts that the coefficient of friction μ of a granular material is a function of the inertial number only.
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