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coaltech upper olifants river catchment wetland inventory ...

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3.5.2.4 Water quality<br />

Floodplain <strong>wetland</strong>s are connected systems with the water in different zones<br />

(compartments). These zones include the permanent, seasonal and temporary wet zones. It<br />

is therefore possible that salts previously deposited during a drying out cycle will be<br />

dissolved and leached from the soil during rewetting. This can contribute to a mineral<br />

exchange between floodwater and sediment. Flooding changes the redox potential in the<br />

<strong>wetland</strong> that will in turn increase the solubility of metals such as manganese and iron, and<br />

triggers the release of phosphates. The opposite applies when the <strong>wetland</strong> dries out. The<br />

concentration of nutrients in this <strong>wetland</strong> type is normally low, due to the dilution effect of<br />

water passing through the <strong>wetland</strong>. The wet and dry cycles in a <strong>wetland</strong>, therefore contribute<br />

to the water quality leaving the system. Water leaving the system during a drying out cycle<br />

will have less dissolved salts and will therefore be of a better quality (Palmer et al 2002,<br />

Kotze 2000, Kotze et al 2000).<br />

3.5.2.5 Storage and evaporation of mine water<br />

Wetlands can be used for the storage and evaporation of water, thereby contributing to<br />

potential storage facilities at mine sites. The use of natural <strong>wetland</strong>s in stead of man made<br />

dams is highly detrimental to the <strong>wetland</strong> (Palmer et al 2002, Kotze 2000, Kotze et al 2000,<br />

Limpitlaw 1995, 1996).<br />

3.5.3 Sediment trapping<br />

Wetlands play an important role in the sediment balance of streams and <strong>river</strong>s. Wetlands<br />

generally slow the water flow in a channel, thereby allowing the precipitation of sediments to<br />

take place. However, should the flow velocity increase, the sediment load in the water will<br />

increase as well (Palmer et al 2002, Kotze 2000, Kotze et al 2000, Kitheka 2003, Zierholtz<br />

2001).<br />

The soil losses in the portion of the UORC investigated by Palmer et al (2002) are moderate<br />

to high, at an average of 44 - 47 tons/km 2 /year. The extent to which <strong>wetland</strong>s contribute to<br />

sediment trapping in the <strong>catchment</strong> has not yet been determined. The presence of this<br />

function in <strong>wetland</strong>s depends on the type of <strong>wetland</strong> (Palmer et al 2002, Midgley et al 1994).<br />

Wetland Database for UORC - 38 -

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