| THEORY & FORMULAE |
Processes for the collection and recovery of particles in a fluid stream are based on the movement of particle in the fluid stream. An important characteristic of particle movement is the settling or terminal velocity. This is the constant velocity reached when all forces (gravity, bouyancy, drag, etc) acting on the particle balance. To computer the settling velocity, one must first determine the applicable flow-regime via the K-factor:
     K = dp[gρpρg/μ2]1/3
For K < 3.3, flow-regime is laminar and Stoke's law applies:
     vt= gdp2ρp/18μ
For 3.3 <= K < 43.6, flow-regime is transitional and the Intermediate law applies:
     vt= 1.53g0.71dp1.14ρp0.71/
μ0.43ρg0.43
For K > 43.6, flow-regime is turbulent and Newton's law applies:
     vt= 1.74√[gdpρp/ρg]
where
     vt= settling velocity
     dp= effective diameter of particle
     ρp= density of particle
     ρg= density of fluid
     μp= fluid viscosity
     g = acceleration due to gravity = 981 cm/sec2
◊ Use link
EXAMPLE Of Input/Output
to demo data entry expectations and results; you may edit & use it as starting point