Subsurface Iron and Arsenic Removal
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<strong>Subsurface</strong> iron <strong>and</strong> arsenic removal for drinking water treatment in Bangladesh<br />
2<br />
Oasen Drinking Water Company<br />
The three locations in the west of the Netherl<strong>and</strong>s,<br />
WTP Lekkerkerk (since 1998), WTP De Put (1981-<br />
1988, <strong>and</strong> 1996-current) <strong>and</strong> WTP ‘t Kromme Gat<br />
(1983-2010), are operated by Oasen Drinking Water<br />
Company. Oasen operates subsurface aeration, a less<br />
intensive form of subsurface iron removal, since 1980.<br />
The operation of the injection-abstraction wells are not<br />
optimized to target iron removal, but the purpose of<br />
1. Aalten<br />
2. Corle<br />
3. De Pol<br />
4. Dinxperlo<br />
5. Gorssel<br />
6. Noordijk<br />
7. ‘Klooster<br />
8. Vorden<br />
9. Zutphen<br />
10. Eerbeek<br />
11. Lekkerkerk<br />
12. ’t Kromme Gat<br />
13. De Put<br />
subsurface aeration is the enhancement of nitrification<br />
in the dry biofilters (de Vet, 2011). After subsurface<br />
aeration the water is mixed with other sources before<br />
treatment. The total amount of injection water is only<br />
1% of the total abstracted raw water. The retention of<br />
iron, arsenic <strong>and</strong> phosphate is, in this case, a side effect<br />
observed during subsurface treatment for enhanced<br />
nitrification. As iron <strong>and</strong> other constituents are allowed<br />
to arrive at elevated concentrations in the well, the<br />
measurements at these locations provide information<br />
on the constituent behaviour during an injectionabstraction<br />
cycle.<br />
Influence of pH<br />
The pH of the groundwater influences the efficiency<br />
of subsurface iron removal both during injection<br />
(oxidation) <strong>and</strong> abstraction (adsorption). During<br />
injection the heterogeneous oxidation reaction is<br />
catalyzed at higher pH ranges (Tamura et al., 1980;<br />
Sung <strong>and</strong> Morgan, 1980):<br />
d<br />
[ Fe ]<br />
dt<br />
Equation 2.3<br />
[ S − OH ][ Fe ][ O ]<br />
[ H ]<br />
0 2+<br />
2+<br />
2<br />
hetero<br />
= − k<br />
2<br />
+<br />
Figure 2.4 Geographical locations of subsurface iron removal<br />
WTPs in the Netherl<strong>and</strong>s (Gorssel has been shut<br />
down)<br />
The value of k 2<br />
depends on the type of mineral<br />
structure, being lowest for the more crystalline iron<br />
(oxy)hydroxides (goethite, lepidocrocite). When<br />
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