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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 />

An introduction to subsurface<br />

iron removal<br />

<strong>Iron</strong> removal in the Netherl<strong>and</strong>s<br />

In the Netherl<strong>and</strong>s there has been a long history of<br />

groundwater treatment, either above-ground or below<br />

the surface. Since the start of drinking water supply in<br />

the Netherl<strong>and</strong>s, the preferred source has always been<br />

microbiologically safe groundwater (in the Netherl<strong>and</strong>s<br />

this source can be found in confined s<strong>and</strong>y aquifers<br />

in most parts of the country; Smeets et al., 2009).<br />

Conventional above-ground treatment consists in<br />

general of the combination of aeration, e.g., cascade<br />

or plate aeration, <strong>and</strong> subsequent s<strong>and</strong> filtration. Prechlorination<br />

of the groundwater is not applied, as<br />

iron removal can also be achieved with the (slower)<br />

oxidation kinetics as obtained by aeration. <strong>Iron</strong> removal<br />

processes can be approached from a chemical <strong>and</strong><br />

biological perspective, with the latter being considered<br />

only since several decades (Mouchet, 1992; Czekalla et<br />

al., 1985). Chemical iron removal can be subdivided<br />

into oxidation-flocculation <strong>and</strong> adsorptive-oxidation.<br />

The formation of flocs results in faster clogging of the<br />

filter bed, whereas adsorptive iron removal produces a<br />

neatly ordered coating onto the s<strong>and</strong> grains (Sharma<br />

et al., 2001). Biological iron removal relies on the<br />

presence of iron oxidizing bacteria, such as Gallionella<br />

spp., to immobilize iron in the filter bed. An additional<br />

advantage of the bios<strong>and</strong> filters is that nitrification of<br />

ammonium-containing anaerobic groundwater can<br />

be obtained as well. Apart from aeration-filtration,<br />

also nanofiltration, reverse osmosis, activated carbon<br />

filtration <strong>and</strong> pellet softening reactors are sometimes<br />

practised to treat groundwater in the Netherl<strong>and</strong>s.<br />

After treatment, the groundwater is usually biologically<br />

stable <strong>and</strong>, therefore, post-chlorination of the water to<br />

prevent bacterial growth is not needed (Smeets et al.,<br />

2009).<br />

The principle of SIR<br />

For groundwater treatment a new iron removal<br />

technology was introduced in the 1970s, based on<br />

similar oxidation-adsorption principles as s<strong>and</strong><br />

filtration, but utilizing the natural treatment capacity of<br />

the aquifer. The principle of <strong>Subsurface</strong> <strong>Iron</strong> <strong>Removal</strong><br />

(SIR), or in-situ iron removal, is that aerated water is<br />

A<br />

B<br />

1.0<br />

C<br />

C 0<br />

Injection Oxygen front<br />

C<br />

C 0<br />

0.5<br />

0<br />

1.0<br />

0.5<br />

0<br />

Injection<br />

front<br />

distance from the well<br />

Fe 2+ front Fe 2+ front<br />

Abstraction<br />

t 2<br />

t 1<br />

distance from the well<br />

Figure 2.1 Behaviour of injection water, oxygen <strong>and</strong> iron front<br />

at a distance from the well (obtained from van Beek,<br />

1983)<br />

24

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