WATER
TREATMENT: IRON AND MANGANESE REMOVAL
Iron and manganese in
well waters occur as soluble ferrous and manganous bicarbonates. In the
aeration process, the water is saturated with oxygen to promote the following
reactions:
4Fe(HCO3)2
+ O2 + 2H2O = 4Fe(OH)3 + 8CO2
ferrous bicarbonate + oxygen + water = ferric hydroxide +
carbon dioxide
2Mn(HCO3)2
+ O2 = 2MnO2 + 4CO2 + 2H2O
manganese bicarbonate +
oxygen = manganese dioxide + carbon dioxide + water
The oxidation products, ferric hydroxide and
manganese dioxide, are insoluble. After aeration, they are removed by
clarification or filtration.
Occasionally, strong chemical oxidants such as
chlorine (Cl2) or potassium permanganate (KMnO4) may be
used following aeration to ensure complete oxidation.
Dissolved
Gas Reduction
Gases dissolved in water follow the principle that
the solubility of a gas in a liquid (water) is directly proportional to the
partial pressure of the gas above the liquid at equilibrium. This is known as
Henry's Law and may be expressed as follows:
Ctotal = kP
Where
Ctotal = total
concentration of the gas in solution
P = partial
pressure of the gas above the solution
k = a
proportionality constant known as Henry's Law Constant
However, the gases frequently encountered in water
treatment (with the exception of oxygen) do not behave in accordance with
Henry's Law because they ionize when dissolved in water. For example:
H2O + CO2 =
H+ + HCO3
water + carbon dioxide = hydrogen ion + bicarbonate ion
H2S = H+
+ HS-
hydrogen sulfide = hydrogen ion + hydrosulfide ion
H2O + NH3 = NH4+
+ OH-
waterammonia =
ammonium ion + hydroxide ion
Carbon dioxide, hydrogen sulfide, and ammonia are
soluble in water under certain conditions to the extent of 1,700, 3,900, and
531,000 ppm, respectively. Rarely are these concentrations encountered except
in certain process condensates. In a normal atmosphere, the partial pressure of
each of these gases is practically zero. Consequently, the establishment of a
state of equilibrium between water and air by means of aeration results in
saturation of the water with nitrogen and oxygen and nearly complete removal of
other gases.
As the equations above show, ionization of the gases
in water is a reversible reaction. The common ion effect may be used to obtain
almost complete removal of these gases by aeration. If the concentration of one
of the ions on the right side of the equation is increased, the reaction is
driven to the left, forming the gas. In the case of carbon dioxide and hydrogen
sulfide, hydrogen ion concentration may be increased by the addition of an
acid. Bicarbonate and carbonate ions in the water will form carbon dioxide,
which can be removed by aeration.
In a similar manner, an increase in hydroxyl ion
concentration through the addition of caustic soda aids in the removal of
ammonia.
Gas removal by aeration
is achieved as the level of gas in the water approaches equilibrium with the
level of the gas in the surrounding atmosphere. The process is improved by an
increase in temperature, aeration time, the volume of air in contact with the
water, and the surface area of water exposed to the air. As previously
indicated, pH is an important consideration. The efficiency of aeration is
greater where the concentration of the gas to be removed is high in the water
and low in the atmosphere.
LIMITATIONS
Temperature
significantly affects the efficiency of air stripping processes. Therefore,
these processes may not be suitable for use in colder climates. Theoretically,
at 68 o F the carbon dioxide content of the water can be reduced to 0.5 ppm by
aeration to equilibrium conditions. This is not always practical from an
economic standpoint, and reduction of carbon dioxide to 10 ppm is normally
considered satisfactory.
Although removal of free carbon dioxide increases
the pH of the water and renders it less corrosive from this standpoint,
aeration also results in the saturation of water with dissolved oxygen. This
does not generally present a problem when original oxygen content is already
high. However, in the case of a well water supply that is high in carbon
dioxide but devoid of oxygen, aeration simply exchanges one corrosive gas for
another.
The efficiency of aeration increases as the initial
concentration of the gas to be removed increases above its equilibrium value.
Therefore, with waters containing only a small amount of carbon dioxide,
neutralization by alkali addition is usually more cost-effective.
The complete removal of hydrogen sulfide must be
combined with pH reduction or chemical oxidation.
Nonvolatile organic compounds cannot be removed by
air stripping. For example, phenols and creosols are unaffected by the aeration
process alone.
Suspended matter in raw water supplies is removed by
various methods to provide a water suitable for domestic purposes and most
industrial requirements. The suspended matter can consist of large solids,
settable by gravity alone without any external aids, and nonsettleable
material, often colloidal in nature. Removal is generally accomplished by
coagulation, flocculation, and sedimentation. The combination of these three
processes is referred to as conventional clarification.
Coagulation is the process of destabilization by
charge neutralization. Once neutralized, particles no longer repel each other
and can be brought together. Coagulation is necessary for the removal of the
colloidal-sized suspended matter.
Flocculation is the process of bringing together the
destabilized, or "coagulated," particles to form a larger
agglomeration, or "floc."
Sedimentation refers to the physical removal from
suspension, or settling, that occurs once the particles have been coagulated
and flocculated. Sedimentation or subsidence alone, without prior coagulation,
results in the removal of only relatively coarse suspended solids.
Steps
of Clarification
Finely divided particles suspended in surface water
repel each other because most of the surfaces are negatively charged. The following
steps in clarification are necessary for particle agglomeration:
Coagulation.
Coagulation can be accomplished through the addition of inorganic salts of aluminum
or iron. These inorganic salts neutralize the charge on the particles causing
raw water turbidity, and also hydrolyze to form insoluble precipitates, which
entrap particles.
Coagulation can also be effected by the addition of
water-soluble organic polymers with numerous ionized sites for particle charge
neutralization.
· Flocculation.
Flocculation, the agglomeration of destabilized particles into large particles,
can be enhanced by the addition of high-molecular-weight, water-soluble organic
polymers. These polymers increase floc size by charged site binding and by
molecular bridging.
Therefore, coagulation involves neutralizing charged
particles to destabilize suspended solids. In most clarification processes, a
flocculation step then follows. Flocculation starts when neutralized or
entrapped particles begin to collide and fuse to form larger particles. This
process can occur naturally or can be enhanced by the addition of polymeric
flocculant aids.
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