The Effects of Ore Properties on the Characterization of Suspension in Settling and Compression

Many studies have considered the effects of suspens ion properties on the dewatering process but few have focused on ore properties. Thus, the present w ork studied the effects of ore properties (density, particle size, mineralogy) on the dewatering proces s based on lab and pilot experiments. A hydrocyclon e was used to prepare the required samples for the ex periments. To study the effects of mineralogical properties, the sedimentation behaviour of hydrocyc lone feed and underflow samples were compared. It was observed that the free-settling velocity of fee d (2 to 6mm/sec) was less than in the underflow sample (2 to 7mm/sec) and the final concentration of under flow sample (0.45 to 0.48t/m 3 ) was more than the feed sample (0.44 to 0.47t/m 3 ). Additionally, to study the effects of particle s ize and density, the sedimentation behaviour of hydrocyclone overflow and feed samples were compared. The settling velocity and final concentration of overflow sample were obtained at 0.15 to 0.4mm/sec and 0.32t/m 3 , respectively, which was significantly less than the feed sample. This was due to the amount of clay reduction in the underflow sample and particle size and density reduction in the overflow sample. Following on, the pilot experiments were carried ou t. It was observed that the bed formation of the fe ed sample tended to overflow in the sample at low flux (10t/m 2 /day) and tended to underflow in the sample at high flux (28.5t/m 2 /day). This meant that the long time at lower flux created an opportunity for fine particles to settle easily, similar to coarser part icles and as such, ore properties did not play a de cisive role in bed formation, but their effects appeared i nstead at higher flux. Furthermore, it was observed that the underflow concentration increased by decreasing the flux from 28.5 to 10t/m 2 /day. These increasing amounts were 0.05t/m 3 and 0.12t/m 3 in hydrocyclone overflow and underflow samples, respectively, at a height of 2.5 metres. This meant that the compressi bility and permeability of the hydrocyclone underflow sample was much better than in the hydrocyclone overflow sample, which was clearly a result of the ore properties (density, particle size, mine ralogy).