WATER PLANT RESIDUALS MANAGEMENT 15-35
is low as shown in this example. A typical occurrence is when rains bring high turbidity.
Thus, the sludge production goes up while the rains reduce the net evaporation.
3. In climates where there is a season with little or no evaporation, either storage is pro-
vided or sufficient beds are provided to store the sludge until evaporative drying c
an take
place. These climates may be cold enough to take advantage of additional dewatering by
freezing and thawing of the sludge.
Freeze Treatment. Dewatering sludge by either of the nonmechanical methods may be en-
hanced by physical conditioning of the sludge through alternate natural freezing and thawing
cycles. The freeze-thaw process dehyd
rates the sludge particles by freezing the water that is
closely associated with the particles. The dewatering process takes place in two stages. The first
stage reduces sludge volume by selectively freezing the water molecules. Next, the solids are
dehydrated when they become frozen. When thawed, the solid
mass forms granular-shaped par-
ticles. This coarse material readily settles and retains its new size and shape. This residue sludge
dewaters rapidly and makes suitable landfill material.
The supernatant liquid from this process can be decante
d, leaving the solids to dewater by
natural drainage and evaporation. Pilot-scale systems can be utilized to evaluate this method’s
effectiveness and to establish design parameters. Elimination of rain and snow from the dewater-
ing system by the provision of a roof will enhance the process considerably.
The potential advantages of a freeze-thaw
system are
1 . Insensitivity to variations in sludge quality.
2. No conditioning required.
3. Minimum operator attention.
4. Natural process in cold climates (winter).
5. Solids cake more acceptable at landfills.
6. Sludge easily worked with conventional equipment.
Several natural freeze-thaw installation
s are located in New York state. At the alum coagula-
tion plant of the Metropolitan Water Board of Oswego County, SFBW is discharged to lagoons
that act as dec ant basins. Thickened sludge is pumped from the lagoons to special freeze-thaw
basins in layers about 450 mm thick. The slud ge has never been deeper than 3
00 mm during
freezing because of additional water losses. The 300 mm sludge layer reduces to about 75 mm of
dried material after freeze-thaw (Davis and Cornwell, 2008).
Solar Drying Beds. These beds are similar in construction and operation to conventional sand
drying beds. They differ in that they are constructed with sealed bottoms. Th
us, there is no provi-
sion for water to be removed through drainage. Because they rely primarily on evaporation, they
typically have lower solids loading rates and filling depths of liquid sludge are less. These beds
are cheaper to build and operate than conventional sand drying beds because there is no cost for
und
erdrains and cleaning with front-end loaders is quicker without incurring sand loss. Most
solar beds are located in the southern and southwestern parts of the United States where evapora-
tion rates are high (Cornwell, 1999).