The dispersed-air flotation of polystyrene particles of size 4-20 qr has been studied under conditions in which the effect of particle dieter on the rate of flotation could be analysed. The particle charge was controlled by electrolyte addition. The particle charge had a drastic effect on the flotat
The Limits of Fine and Coarse Particle Flotation
β Scribed by Carlos De F. Gontijo; Daniel Fornasiero; John Ralston
- Publisher
- John Wiley and Sons
- Year
- 2008
- Tongue
- English
- Weight
- 440 KB
- Volume
- 85
- Category
- Article
- ISSN
- 0008-4034
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β¦ Synopsis
Abstract
The flotation behaviour of quartz particles was studied over the particle size range from 0.5 Β΅m to 1000 Β΅m and for advancing water contact angles between 0Β° and 83Β°. Flotation was performed in a column and in a Rushton turbine cell. Particle contact angle threshold values, below which the particles could not be floated, were identified for the particle size range 0.5β1000 Β΅m, under different hydrodynamic conditions. The flotation response of the particles, either in a column or in a mechanically agitated cell with a similar bubble size, was comparable. Turbulence plays a role, as does bubbleβparticle aggregate velocity and bubble size. The stability of the bubbleβparticle aggregate controls the maximum floatable particle size of coarse particles. For fine particles, the flotation limit is dictated by the energy required to rupture the intervening liquid film between the particle and bubble. Flotation of very fine and large particles is facilitated with small bubbles and high contact angles. These results greatly extend our earlier observations and theoretical predictions.
π SIMILAR VOLUMES
Abstrae-Expenments have been conducted III wluch the charges on parkles and bubbles m a flotation process have been measured The partxles were polystyrene latlces of dmmeters between 4 and 20 v The bubbles were of mean dmmeter 53 m A catmmc sutfactant was used to promote ilotatmn, and the charge on
## Abstract Three coarseβtextured soils were amended with pulverised fuel ash and two similar fineβparticle materials, fluidised combustor ash and ground silica sand. Incorporation of the amendments to the Ap horizon of the soils increased available water retention by up to 70%. The additional wate
The pax of partial differential equations conventionally used to descrrbe the dynanucal behavior of a porous catalyst pellet 1s approplate only m the hnutmg case when all pore diameters are small compared with mean free path lengths m the reactIon mutture It IS here shown that, at the opposite hnut,