Opens in a new tab

Flocculation

Flocculation is the process by which fine particles in suspension aggregate to form larger particles or flocs, typically due to the action of chemical agents or changes in water chemistry. This process is important in sedimentation, water treatment, and the study of fine-grained sediment transport in rivers, lakes, and oceans. 

Reference: Van Olphen, H. (1977). An Introduction to Clay Colloid Chemistry. Wiley-Interscience. 

← Back to the Glossary

join.me

Geology made clear, in your inbox.

Get clear, visual explainers on rocks, minerals, deep time, and the most fascinating parts of Earth science from Geoscopy.