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Uganda Atlas of Our Changing Environment - GRID-Arendal

Uganda Atlas of Our Changing Environment - GRID-Arendal

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Effects <strong>of</strong> the Northern By-pass during the rainy season (2007)<br />

Prior to the peak <strong>of</strong> urbanisation being experienced now,<br />

these two systems had a wide coverage <strong>of</strong> wetlands and<br />

around them a buffer <strong>of</strong> thick forests. Citizens in 1960s<br />

would use boats to cross over from Kamwokya along the<br />

stream through the present Centenary Park to Luzira.<br />

The streams even had a lot <strong>of</strong> water then.<br />

This has seen most <strong>of</strong> the water in these places drained<br />

and lowering the water tables temporailiry during the<br />

dry seasons.<br />

The shrinkage <strong>of</strong> Nsooba-Lubigi wetland system in the<br />

upper catchments due to settlements has increased the<br />

retention time <strong>of</strong> the water in the lower reaches during<br />

rains resulting into flooding. It should be noted that the<br />

gradient <strong>of</strong> this system is quite low making the water<br />

meander at a slow rate as it finds its level. This process<br />

has greatly increased on the wetland coverage downstream<br />

around the Kampala-Wakiso border and beyond.<br />

Areas <strong>of</strong> Namungoona have seen land that was dry being<br />

reclaimed by the wetland overtime.<br />

There has been contionous shrinkage <strong>of</strong> the Nakivubo<br />

wetland system. The gradient <strong>of</strong> this drainage system is<br />

a bit steeper than that <strong>of</strong> Nsooba-Lubigi wetland system<br />

and so water in this system has less time to reticulate<br />

and claim some areas. The situation was worsened by<br />

the widening <strong>of</strong> Nakivubo Channel which saw a lot <strong>of</strong><br />

NEMA 2007<br />

Flooding in Bwaise, a Kampala surbub after a heavy down pour (2008)<br />

water being drained from these areas. This has greatly<br />

lowered the water table in these areas leading to further<br />

encroachment <strong>of</strong> the remaing strectches for agriculture.<br />

Water Quality<br />

In the 1960s Kampala had clear water in the streams and<br />

good drinking water in the natural springs.<br />

Overtime, the city has had the water quality<br />

deteriorating due to:<br />

• Contamination <strong>of</strong> water from pit latrines and<br />

poorly constructed ‘hanging’ latrines that<br />

are opened into the channels during rains<br />

• Frequent flooding that ends up draining the pit<br />

latrines directly into the water tables<br />

Currently, more than 85% <strong>of</strong> the spring wells in Kampala<br />

are polluted with E-coli- a sign <strong>of</strong> faecal contamination.<br />

• Industries that have been constructed close to<br />

water ways, releasing their effluents into the<br />

water.<br />

• The silt which is being eroded from the opened<br />

up areas and during the rains is swept down into<br />

the water sources. Overtime, Lake Victoria has<br />

become more turbid and this has a negative<br />

impact on the fish industry since it leads<br />

to silting up <strong>of</strong> the breeding grounds for fish.<br />

127<br />

NEMA 2008

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