Colloidal precipitates
Precipitate Formation and Particle Size Control
Shape and Texture of Coarse Aggregate
The Colloidal State
Porosity and Absorption of Aggregate
Gravimetry: Inorganic And Organic Precipitating Agents
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Laboratory Drop Towers for the Experimental Simulation of Dust-aggregate Collisions in the Early Solar System
Published on: June 5, 2014
Vishal Gupta1, Marc A Hampton, Jason R Stokes
1Department of Metallurgical Engineering, College of Mines and Earth Sciences, University of Utah, 135 South 1460 East, Room 412, Salt Lake City, UT 84112, USA. Vishal.Gupta@utah.edu
Kaolinite particle aggregation depends on pH-driven surface charges. At low pH, silica-alumina face interactions dominate, promoting aggregation, while high pH leads to dispersion and stable suspensions.
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