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Vertical flow constructed wetlands for the treatment of inorganic ...

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shown that anammox bacteria belong to a deep branching planctomycete (Strous et al.,<br />

1999).<br />

1NH4 + + 1.3NO2 - � 1.02N2 +0.26NO3 - + 2H2O (2.21)<br />

Because <strong>of</strong> <strong>the</strong> reduced carbon and oxygen requirements, less than half <strong>the</strong><br />

oxygen and no carbon, as compared to conventional routes, anammox is particularly<br />

suited to <strong>the</strong> <strong>treatment</strong> <strong>of</strong> high strength industrial wastewaters in which <strong>the</strong><br />

ammonium content is high and <strong>the</strong> organic carbon content very low (Mulder et al.,<br />

1995). The discovery <strong>of</strong> this alternative route has led to <strong>the</strong> development <strong>of</strong> o<strong>the</strong>r<br />

processes that make use <strong>of</strong> anammox such as SHARON-anammox (Single reactor High<br />

Activity Ammonia Removal Over Nitrite), CANON (complete autotrophic nitrogen<br />

removal over nitrate) and OLAND (Oxygen Limited Autotrophic Nitrification-<br />

Denitrification). In <strong>the</strong> SHARON-Anammox process partial nitritation is achieved in one<br />

vessel by washing out NOB with high temperatures and short residence times (< 1 day)<br />

and anaerobic elimination <strong>of</strong> nitrite by ammonia is achieved in a second vessel<br />

(Hellinga et al., 1998). The CANON process per<strong>for</strong>ms both partial nitritation and<br />

anammox in a single reactor simultaneously, under oxygen-limitation. The process<br />

relies on <strong>the</strong> simultaneous interaction <strong>of</strong> aerobic and anaerobic ammonium oxidisers<br />

(Third, 2003). The OLAND process makes use <strong>of</strong> <strong>the</strong> ability <strong>of</strong> Nitrosomonas to denitrify<br />

using ammonium as <strong>the</strong> electron donor and nitrite as <strong>the</strong> electron acceptor, toge<strong>the</strong>r<br />

with <strong>the</strong>ir ability to per<strong>for</strong>m anaerobic ammonium oxidation in <strong>the</strong> presence <strong>of</strong> gaseous<br />

NO2 (Schmidt and Bock, 1997).<br />

Macrophyte uptake <strong>of</strong> ammonium and nitrate represents an important nitrogen<br />

removal process <strong>for</strong> many wetland systems. The majority <strong>of</strong> <strong>the</strong> assimilated nitrogen is<br />

subsequently released in <strong>the</strong> water during <strong>the</strong> death and decay cycles, providing a<br />

“flywheel” effect in a nitrogen removal time series (Kadlec and Wallace, 2009). A small<br />

part <strong>of</strong> <strong>the</strong> nitrogen containing residues is permanently stored as part <strong>of</strong> <strong>the</strong> creation <strong>of</strong><br />

new soil and sediment, hence accretion represents a burial process <strong>for</strong> nitrogen.<br />

Accretion (ammonia net removal in <strong>the</strong> order <strong>of</strong> 10gN/m 2 /yr) is only <strong>of</strong> importance in<br />

lightly loaded systems but has no importance in heavy loaded <strong>wetlands</strong> (Kadlec and<br />

Wallace, 2009). Plant harvesting with <strong>the</strong> objective to remove nitrogen from <strong>the</strong> system<br />

does not represent a cost effective solution, proving to be expensive and labour<br />

24

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