Positron Emission Particle Tracking of Near Gravitational Material inside a Dense Media Cyclone

"We present an analysis of trajectory and time averaged data of near gravitational material (NGM) representative coal tracer particles within a magnetite medium passing through a 100mm diameter hydrocyclone imaged with PEPT (positron emission particle tracking) at iThemba labs, Cape Town. The tracking of neutrally buoyant tracers as well as the other NGM allows an empirical study of the approximate dynamical behaviours of both the dense medium as well as the range (size and density) of particles around the separator’s cut size within a partially imaged volume of the cyclone body lying within the field of view of the detector. The study was commissioned as part of a CFD validation study using empirical data from a real-world lab-appropriate system in order to shed light on the inner workings of hydrocyclones and their separation mechanisms. We employ various optimisation and noise reduction techniques within the analysis and follow a detailed investigation of the velocity fields derived from the raw spatial positions with an emphasis on the velocity profile within the forced and free vortex zones. Challenges encountered with this high velocity particle tracking experiment within a highly attenuating environment are also discussed. Various important velocity distributions are shown and compared to theoretical predictions. The power law decay profile of the free vortex and radial velocity scaling with regards to the Froude number are reproduced in line with the static particle approach. INTRODUCTION Cyclones have long been a vital industrial tool for the separation of different classes of particles. These cyclonic separators (with either gas or liquid medium) operate by forcing the solids-bearing fluid at high pressure into a cylindrical vessel causing high tangential velocity fluid rotation as well as, in the case of an “open” (with exit channels open to the atmosphere) cyclone, a central vortex air column spanning from underflow to overflow exit. The fluid is forced to exit the cyclone at two locations, the spigot and the vortex finder, generating the underflow and overflow respectively. The body of the cyclone usually terminates in a conical shape to focus the underflow stream. This geometry and large incident fluid velocity force high density materials toward the wall of the vessel where they are most likely to move along and down the inside wall away from the inlet to exit via the underflow while lower density materials traverse the cyclone body closer to the central vortex and are buffeted by the upward-moving column towards the overflow exit. This separation mechanism is selective of density and size in an interplay between the centrifugal force due to the rotation of the fluid and a drag force acting on the particles."