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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 />

28

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