Chapter 8: Water Treatment Flashcards
Physical characteristics of water (6)
Color, turbidity, temperature, particulars, taste, odor
Characteristics of groundwater (5)
- Constant composition
- High mineral content (Fe, Mn)
- Low turbidity
- Low or no DO
- High hardness
Characteristics of surface water (5)
- Variable composition
- Low mineral content
- High turbidity
- DO present
- Low hardness
Colloids
Discrete particles that are separated by a dispersal medium (fluid). (EX: milk, fog, butter, blood, paint)
Properties of colloids
- Negative electrostatic surface charges
- 1 nm to 1,000 nm (1µm)
- High surface to volume ratios
- Called “stable ” when colloidal particles remain in suspension without coagulation and flocculation.
Rapid sand filtration/conventional treatment steps (3)
- Pre-sedimentation (removes easily settleable material)
- Pre-chlorination (Cl added at rapid mix stage)
- Direct filtration (coagulation, flocculation, filtration, disinfection)
Coagulation (rapid mixing)
Destabilization and initial coalescing of colloidal pollutant particles. Particles stick to each other.
Flocculation (slow mixing)
Formation of loosely attached larger aggregates of pollutant particles (flocs) via the addition of coagulants.
How does coagulation and flocculation occur? (3)
- Brownian motion of particles (particles < 0.5 µm)
- Stirring
- Differential settlement
Coagulants for water treatment (6)
Alum or ferric iron salts, ferric chloride, polymers, slaked lime, ferric sulfate, ferrous sulfate
Sedimentation
Gravity separates particles from water.
Reynold’s Number
Ratio of inertial forces to viscous forces
Type 1 sedimentation
Particles that settle discretely at a constant velocity. Occurs in dilute suspensions
Type II Sedimentation
Particles that flocculate during sedimentation. Changing size and settling velocity due to flocculation.
Type III/Zone, Sedimentation
High concentration of particles (>1000 mg/L) settle as a mass, a distinct clear zone and sludge zone are present.
Type IV/Compression Settling
Setting of particles that are of such concentration that the settling can occur only by compression of the mass.