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Uganda Atlas of Our Changing Environment - GRID-Arendal

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Soils: Changes . Classification and Nomenclature<br />

Soils Types<br />

Soil Type Sub Type Area (Km 2 )<br />

Andosols Leptic/Skeletic 5,751<br />

Table 4: Soil Types and Productivity status in <strong>Uganda</strong><br />

Changes<br />

Melanic 63<br />

Arenosols 5,579<br />

Calcisols 204<br />

Ferralsols Acric 43,180<br />

Lixic 24,392<br />

Gleysols 24,019<br />

Histosols 580<br />

Leptosols 22,086<br />

Luvisols 5,275<br />

Nitisols 3,907<br />

Planosols 1,735<br />

Plinthosols Petric 35,205<br />

Regosols Dystric 5,072<br />

Eutric 8,085<br />

Vertisols 19,066<br />

Over the years, food production has been characterized<br />

by subsistence farming. A subsistence production<br />

system usually focuses on maximizing short term pr<strong>of</strong>it<br />

which promotes consuming and depleting natural stocks<br />

<strong>of</strong> plant nutrients. Such a farming system has resulted<br />

in soil fertility degradation through nutrient mining.<br />

In the past, when <strong>Uganda</strong>’s population was still low,<br />

lost soil fertility was restored through long periods <strong>of</strong><br />

fallows. With an average land holding <strong>of</strong> about 2 ha<br />

per household today, fallows are no longer practical.<br />

Research has demonstrated that fertilizer inputs and<br />

appropriate land management practices are important<br />

components <strong>of</strong> technology required to maintain or<br />

improve soil fertility in <strong>Uganda</strong> (P. Ndeki et al).<br />

Severe soil erosion on Mt. Elgon slopes in Kapchorwa District, resulting from<br />

loss <strong>of</strong> vegetation cover and leading to heavy siltation <strong>of</strong> River Ngenge (2005)<br />

Classification and Nomenclature<br />

The major criteria in soil classification are the physical<br />

and chemical characteristics. Physical characteristics<br />

include factors such as parent rock, texture, structure,<br />

location, depth, colour, and topography, while chemical<br />

characteristics include pH, base composition, base<br />

saturation, and Cation Exchange Capacity (CEC). Going by<br />

those criteria, 13 major classes (some with sub classes)<br />

have been identified at national level (see Table 4).<br />

The earlier nomenclature <strong>of</strong> soils in <strong>Uganda</strong> was based on<br />

the catena system, in which units were assigned names <strong>of</strong><br />

the most prominent town or centre in the area. This <strong>Atlas</strong><br />

however uses reclassified soils based on the standard FAO<br />

nomenclature.<br />

The high productivity soils cover only 8% <strong>of</strong> the area <strong>of</strong><br />

<strong>Uganda</strong>. This is indeed a small area. Therefore, moderate<br />

and fair productivity categories form the bulk <strong>of</strong> the<br />

soils and must be effectively managed in order to sustain<br />

<strong>Uganda</strong>’s agriculture. Furthermore, through intensive<br />

but sustainable agricultural practices, yields on low<br />

productivity soils can be enhanced.<br />

45<br />

NEMA 2005

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