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Prior to the peak of urbanisation being experienced now,

these two systems had a wide coverage of wetlands and

around them a buffer of thick forests. Citizens in 1960s

would use boats to cross over from Kamwokya along the

stream through the present Centenary Park to Luzira.

The streams even had a lot of water then.

This has seen most of the water in these places drained

and lowering the water tables temporailiry during the

dry seasons.

The shrinkage of Nsooba-Lubigi wetland system in the

upper catchments due to settlements has increased the

retention time of the water in the lower reaches during

rains resulting into flooding. It should be noted that the

gradient of this system is quite low making the water

meander at a slow rate as it finds its level. This process

has greatly increased on the wetland coverage down-

stream around the Kampala-Wakiso border and beyond.

Areas of Namungoona have seen land that was dry being

reclaimed by the wetland overtime.

There has been contionous shrinkage of the Nakivubo

wetland system. The gradient of this drainage system is

a bit steeper than that of Nsooba-Lubigi wetland system

and so water in this system has less time to reticulate

and claim some areas. The situation was worsened by

the widening of Nakivubo Channel which saw a lot of

water being drained from these areas. This has greatly

lowered the water table in these areas leading to further

encroachment of the remaing strectches for agriculture.

Water Quality

In the 1960s Kampala had clear water in the streams and

good drinking water in the natural springs.

Overtime, the city has had the water quality

deteriorating due to:

Contamination of water from pit latrines and

poorly constructed ‘hanging’ latrines that

are opened into the channels during rains

Frequent flooding that ends up draining the pit

latrines directly into the water tables

Currently, more than 85% of the spring wells in Kampala

are polluted with

E-coli

- a sign of faecal contamination.

Industries that have been constructed close to

water ways, releasing their effluents into the

water.

The silt which is being eroded from the opened

up areas and during the rains is swept down into

the water sources. Overtime, Lake Victoria has

become more turbid and this has a negative

impact on the fish industry since it leads

to silting up of the breeding grounds for fish.

Flooding in Bwaise, a Kampala surbub after a heavy down pour (2008)

NEMA 2008

Effects of the Northern By-pass during the rainy season (2007)

NEMA 2007

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