BEHAVIOUR OF BEDS OF DENSE PARTICLES IN A HORIZONTALLY OSCILLATING LIQUID.
Abstract
WHEN A BED OF DENSE SOLID PARTICLES IN A HORIZONTAL TUBE IS SUBJECT TO AN OSCILLATORY LIQUID FLOW, FIVE DIFFERENT 'FLOW REGIMES' CAN BE IDENTIFIED, RANGING FROM A STATIONARY BED REGIME TO A COMPLETE SUSPENSION OF THE PA%TICLES IN THE LIQUID.IN THIS INVESTIGATION, THE TRANSITIONS BETWEEN THESE REGIMES HAVE BEEN MEASURED AS A FUNCTION OF THE FOLLOWING VARIABLES: ANGULAR FREQUENCY GW %2.5 TO 9 RAD/S<, AMPLITUDE A %UP TO 41 CM<, PARTICLE DIAMETER D %100 TO 1100 MM<, THE RATIO GG OF THE DENSITY DIFFERENCE BETWEEN PARTICLES AND LIQUID TO THE DENSITY OF THE LIQUID %0.26 TO 4.1< AND THE KINEMATIC VISCOSITY OF THE LIQUID V %0.89 TO 80.6 CST<.TWO FURTHER CONDITIONS WERE CONSTANT, NAMELY THE VOLUME CONCENTRATION OF SOLIDS %2 PERCENT< AND THE DIAMETER OF THE TUBE %5.08 CM<.LTHE AMPLITUDE-FREQUENCY THRESHOLD AT WHICH GENERAL SURFACE MOTION OF THE PARTICLES FOR PART OF THE OSCILLATION CYCLE WWAS FIRST OBSERVED COULD BE CORRELATED AS FOLLOWS:LAGW/SUP 1.5///SUB %/GG/SUB G0.75/SUB D/0.25 EQUALS 0.37LTHE LEFT-HAND SIDE OF THE CORRELATING EQUATION CAN BE OBTAINED FROM A MODIFIED FORM OF A THEORY BASED ON AN OSCILLATING LAMINAR BOUNDARY LAYER NEAR THE SURFACE OF THE PARTICLE BED.ONCE GENERAL SURFACE MOTION OF PARTICLES HAS BEEN ESTABLISHED, THE BEDS TEND TO FORM REGULARLY SPACED DUNES.THE DUNE WAVELENGTH CAN BE CORRELATED APPROXIMATELY AS FOLLOWS: GL EQUALS 18(%A-A/SUB 23/
Authors
CHAN KW; BAIRD MHI; ROUND GF
Journal
Proc Roy Soc London Series A, Vol. 330, No. 1583 (1972), pp. 537–559