Quick Answer
Hydrocyclone instability is typically the result of a combination of factors. The most common causes include extreme or fluctuating feed pressure, feed flow, concentration, or particle size; critical geometric imbalances, such as an incorrect apex-to-vortex ratio; and component wear. Feed pressure below 5-6 psi fails to generate sufficient centrifugal force, while excessive pressure collapses the air core. Feed concentration exceeding 20.25% destroys flow field stability. Coarser feed with a small apex causes rapid efficiency deterioration through particle accumulation. The apex-to-vortex ratio is critical—lower ratios produce roping, higher ratios cause flow disorder. Component wear, particularly of the apex, alters internal balance. A systematic approach to troubleshooting—starting with verifying feed pressure and examining the underflow discharge pattern—is essential for identifying and correcting the root cause of instability.