Defaults: u = 10 mm/s, dp = 2.0 mm, eps = 0.40, mu = 1.0 x 10^-3 Pa.s (water at 20 C), with fluid density rho = 1000 kg/m^3 fixed. The minimum fluidisation velocity u_mf assumes a particle density rho_p = 2500 kg/m^3 (sand).
Side view of a cylindrical packed bed. Many spherical particles (diameter d_p) are packed at voidage eps, and fluid flows upward at superficial velocity u. Particle size and density mirror the current d_p and eps values.
Horizontal axis: u (mm/s, log10). Vertical axis: dP/L (Pa/m, log10). Low velocities follow a slope-1 laminar regime, high velocities a slope-2 turbulent regime. The yellow marker shows the current (u, dP/L) and the dashed lines are the laminar and inertial asymptotes.
For a bed of spherical particles, the pressure drop per unit length is the sum of a laminar and an inertial contribution:
$$\frac{\Delta P}{L} = \frac{150\,\mu\,u\,(1-\varepsilon)^2}{\varepsilon^3\,d_p^2} + \frac{1.75\,\rho\,u^2\,(1-\varepsilon)}{\varepsilon^3\,d_p}$$$u$ is the superficial velocity (m/s), $d_p$ the spherical particle diameter (m), $\varepsilon$ the voidage, $\mu$ the dynamic viscosity (Pa.s) and $\rho$ the fluid density (kg/m^3). The first term is the Carman-Kozeny laminar flow contribution; the second is the Burke-Plummer inertial contribution. The particle Reynolds number is:
$$\mathrm{Re}_p = \frac{\rho\,u\,d_p}{\mu\,(1-\varepsilon)}$$The laminar-approximation minimum fluidisation velocity (with particle density $\rho_p$) follows from the first term alone:
$$u_{mf} = \frac{\varepsilon^3\,d_p^2\,(\rho_p-\rho)\,g}{150\,\mu\,(1-\varepsilon)}$$This tool fixes $\rho = 1000$ kg/m^3, $\rho_p = 2500$ kg/m^3 and $g = 9.81$ m/s^2.