Phase Interactions--Definitions

 
bacterial floc
Aggregated bacterial particles--these flocs remove a substantial portion of the organic carbon from wastewater
bridging compounds
Compounds which bridge between two colloidal particles, binding them together in a larger mass, a floc
cation exchange capacity (CEC)
The quantity of cationic material which can be sorbed  by a given quantity of solid. It is generally expressed in milliequivalents per 100 g of solid. This varies with pH and salt concentration.
coagulation
Coalescence of colloidal particles, brought about by the reduction of the surface charges on the particles, thus overcoming the interparticle repulsion
colloidal surface charge
Colloids will collect ions on their surfaces, leading to a charged double layer. For instance, in an acid solution, an oxide particle will sorb H+ ions, and have a positive charge. At high pH, H+ ions are lost, and a negatively charged colloid results. The point at which the charge changes from positive to negative, is the zero point of charge. 
double layer
A colloidal particles generally has a surface charge which attracts a second layer of ions of opposite charge, producing a charged surface. This electrical double layer prevents particles from adhering to each other until it is disrupted.
double layer compression
Ions in the solution neutralize the surface double layer and allow the particles to adhere to each other. This is a particularly important mechanism for the production of river deltas. Colloidal particles travel down the river, and are coagulated and deposited on contact with seawater.
exchangeable cations
Cations which can be exchanged between a solid surface and the surrounding solution.
flocculation
Coalescence of colloidal particles by bridging compounds which join the particles together.
Henry's law
The solubility of a gas in a liquid can be calculated by Henry's law which states that the solubility of the gas is proportional to the partial pressure of the gas in contact with the liquid.
Henry's law constant
The constant in Henry's law which depends on the solvent, the gas being dissolved and the temperature.
hydrophobic colloid
A colloid which does not interact strongly with water, and which is stabilized by formation of an ionic double layer
hydrophyllic colloid
A colloid, usually a macromolecule, which interacts strongly with water and is less apt to coagulate when salts are added to the solution. Proteins and some synthetic polymers form hydrophobic colloids.
hydrous mica
A clay mineral of the formula KAl2(OH)2(AlSi3)O10
interstitial gases
Gases dissolved in pore water. The pore gases are usually different from the gases dissolved in the overlying water.
interstitial water or pore water
This is the water which exists between the particles of sediments
kaolinite
A clay mineral of the formula Al2(OH)4Si2O5
micelle
A colloidal particle composed of a group of surfactant molecules. In water the inside of the micelle holds the hydrophobic, oily ends of the molecules, while the outer surface is covered with the hydrophyllic groups at the other ends of the molecules. Micelles enable the solublization of hydrophobic compounds in water.
montmorillonite
A clay mineral of the formula Al2(OH)2Si4O10
nontronite
A clay mineral of the formula Fe2(OH)2Si4O10
polyelectrolyte
A high molecular weight polymeric molecule with ionizable functional groups, which can act as a bridging compound and cause flocculation. Often these have anionic functional groups, and  negatively charged colloids can be joined by bridging through metal ions.
sediment
Soild particles which have settled out of suspension in water
sedimentary rock
Rock formed from the coagulation and precipitation of colloidal particles and dissolved minerals from water
solubility product
The equilibrium constant for the solution process, solid -> ions
zero point of charge (ZPC)
Condition of pH where the colloidal particles have a neutral surface charge and can readily coagulate.
 

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