14-2 WATER AND WASTEWATER ENGINEERING
14-1 INTRODUCTION
The focus of the previous chapters has been on removal of broad classes of constituents: turbid-
ity, color, hardness, and pathogens. The focus of this chapter is a selected list of specific constitu-
ents that are not addressed in the previous chapters. They were selected
because of their impact
on the potability and palatability of water. These include arsenic, iron and manganese, fluoride,
nitrate, NOM, pharmaceuticals, radionuclides, taste and odor (T&O), synthetic organic chemicals
(SOCs) and volatile organic compounds (VOCs). In addition, becaus
e of its economic impact on
the softening process, treatment to remove carbon dioxide is included.
14-2 ARSENIC
A r senic is almost exclusively a groundwater contaminant. Therefore, this discussion is limited to
a few selected processes deemed reasonable for treating groundwater at a centralized facility. A
more thorough discussion may be found in the Arsenic Treatment Technology Handbook (U.S.
EPA, 2003).
Arseni
c can occur in four oxidation states in water: 5, 3, 0, 3. The most common states
are trivalent arsenite [As(III)] and pentavalent arsenate [As(V)]. Most As(III)-containing water in
the pH range of 6 to 9 will have As in the form of H
3
A sO
3
. Arsenate will be in the form HAsO
4
2
in the pH range 7 to 11.5. At pH values less than 7.0, arsenate will be in the form H
2
A sO
4
.
Treatment Strategies
Preoxidation Processes. Reduced inorganic arsenite cannot be removed effectively. Preoxida-
tion to form As(V) at the head end of all of the unit processes described in the following para-
graphs is essential. Chlorine, permanganate, and ozone are highly effective. Chlorine dioxide,
monochloramine, and UV are ineffective as stand-alone oxidants for As(III).
Side reactions with iron,
manganese, and sulfide must be accounted for in determining the
dose for oxidation (Ghurye and Clifford, 2001).
The oxidation-reduction reaction with chlorine is
HAsOOCl
HAsO
HCl
33
24
→ (14-1)
This reaction is relatively independent of pH in the range 6.3 to 8.3. In a laboratory study, at an
excess of three times the stoichiometric amount of chlorine, 95 percent of the As(III) was con-
verted to As(V) in 42 seconds (Ghurye and Clifford, 2001).
The oxidation-reduction reaction with permanganate is
3
2 3
2
33
424
22
HAsO
MnO H AsO
HMnOHO
→
(14-2)
Like the chlorine reaction, this reaction is relatively independent of pH in the range 6.3 to 8.3.
At a similar threefold stoichiometric excess, 95 percent of the As(III) was converted to As(V) in
36 seconds. As with chlorine oxidation, side reactions with iron, manganese, and sulfide must be
accounted
for in determining the dose (Ghurye and Clifford, 2001).
Permanganate is difficult to handle. It is commercially available as a crystal that is corrosive
and stains nearly everything purple. Manganese particles are produced as a result of permanga-
nate oxidation reactions. Therefore, postoxidation filtration is essential to prevent a
ccumulation
of deposits in the distribution system.