Introduction
- Soil and water are two very important natural resources in farming.
- They should therefore be well maintained and used efficiently without wastage to sustain continuous agricultural production.
- Water loss during the rainy season should be prevented, and excess water conserved for use during periods of scarcity.
- Soil erosion must be controlled at all costs if soil is to be conserved effectively.
Soil Erosion
- Soil erosion is the removal and carrying away of the topsoil by the action of water or wind.
Factors Influencing Soil Erosion
- Amount and intensity of rainfall
- The steeper the land, the higher the velocity of surface runoff.
- The higher the velocity of surface runoff, the greater its erosive power and effect.
- Type of soil – for example, sandy soils are more easily detached and carried away than clayey soils.
- Soil depth – the deeper the soil, the longer it takes to become saturated with water.
- Land use:
- Overstocking leads to bareness of the land and looseness of the soil.
- Deforestation – indiscriminate removal of trees exposes soil to heavy rainfall and high temperatures.
- Indiscriminate burning of vegetation exposes the soil to erosive agents.
- Clean weeding leaves the soil bare and vulnerable to erosion.
- Ploughing along the slopes increases erosion risk.
- Monoculture or continuous cultivation reduces soil cover and increases erosion.
- Ground cover:
- Trees act as windbreakers, reducing wind erosion.
- Roots of vegetation hold soil particles together, preventing detachment.
- Leaf fall acts as mulch, reducing erosion by protecting the soil surface.
- Leaves of vegetation intercept raindrops, reducing their erosive power.
Agents of Erosion
- Water – moving water has strong erosive power.
- Wind – wind carries away loose soil particles.
- Human beings – through activities such as cultivation and mining that disturb the soil.
- Animals – overgrazing and creation of footpaths contribute to soil erosion.
Types of Erosion
- Raindrop (splash) – displacement of soil caused by the impact of raindrops.
- Sheet – uniform removal of soil in thin layers from flat or gently sloping areas.
- Rill – removal of soil from small but well-defined channels or rills.
- Gulley – removal of soil from channels that become progressively deeper and wider.
- Riverbank erosion – removal of soil along river banks by flowing river water.
- Solifluction – gravitational flow of soil saturated with water down a slope.
- Landslides – mass movement of rock debris and soil down a slope:
- Slip movement of earth or rock masses for a short distance.
- Debris slide – materials move at a greater speed.
- Debris fall – movement of materials or debris along a vertical cliff.
- Rock fall – movement of rock down a very steep slope.
- Rock slides – mass of rock materials sliding along a bedding plane, joint, or fault face.
Soil Erosion Control Measures
Soil conservation measures can be classified into:
- Biological or cultural control
- Physical or structural control
Biological or Cultural Control Measures
These measures are applicable where the land slope is between 2–12%.
- Grass strips/filter strips:
- Narrow uncultivated strips along the contour left between cultivated strips to reduce runoff velocity and trap soil.
- Cover cropping:
- Establishment of a crop that spreads over the soil surface to provide protective cover.
- Contour farming:
- Carrying out all land operations along the contour lines to reduce runoff and erosion.
- Mulching:
- Covering the soil with organic or synthetic materials to protect it from erosion and conserve moisture.
- Proper cropping systems such as:
- Crop rotation
- Correct spacing
- Intercropping
- Ridging or furrowing
- Strip cropping
- Controlled grazing:
- Maintaining proper stocking rates and rotational grazing to prevent overgrazing and soil exposure.
- Strip cropping:
- Growing crops with little ground cover in alternate strips with crops such as beans that provide good ground cover.
- Afforestation and re-afforestation:
- Afforestation – planting trees where none existed before.
- Re-afforestation – planting trees where they have been cut down.
- Agroforestry – land use involving growing trees in combination with crops and pastures on the same piece of land.
Physical or Structural Control Measures
- These are soil and water conservation measures involving mechanical constructions on the land.
- They are used in areas with moderate slopes between 13–55%.
They include:
- Trash or stone lines:
- Rows of heaped crop residues or stones made along the contours to reduce runoff velocity.
- Filter strips:
- Growing an open crop on the upper side of the slope followed by a dense crop to reduce water speed and increase infiltration.
- Terraces:
- Structures constructed across a slope to reduce its length and thus reduce runoff.
- Bench terraces:
- Constructed where the slope is 35–55%.
- Tree crops are suitable for such areas.
- Importance of a Bench Terrace:
- Reduces the slope of the land.
- Conserves soil moisture.
- Improves retention of soil fertility.
- Narrow-based terraces – cannot allow cultivation by machines.
- Broad-based terraces – wide enough to allow cultivation by machines.
- Graded terraces:
- Have a drainage channel to lead off excess water to a vegetated area.
- They should be about 100 meters in length.
- Level terraces:
- Have no outlet channels.
- The aim is to allow water infiltration so no water flows from the ends of the terrace.
- Fanya juu:
- A ridge made by digging a channel and throwing the soil uphill.
- Fanya chini:
- Soil is heaped on the lower side of the channel.
- Bunds: heaps of soil (earth) made along the contour to reduce runoff.
- Cutoff drains:
- An open trench with an embankment on the lower side into which water from the farm drains.
Water from the trench should be discharged into:
- Natural waterways,
- Artificial waterways,
- Rocky ground,
- Grassland.
- Gabion/Porous dams:
- Galvanized wire mesh boxes filled with stones, built across slopes and gullies to reduce erosion.
- Dams and reservoirs:
- Dams are barriers built across rivers or waterways to hold and store water, reducing runoff speed.
- Reservoirs are large storage tanks for water.
- Ridging – heaps of soil constructed to reduce the speed of water and retain it for some time.
Water Harvesting Methods
- Water harvesting and storage should be done during the rainy seasons to avoid wastage and ensure availability during dry periods.
This should be done using the following methods:
- Roof catchment – trapping and collecting rainwater from rooftops.
- Rock catchment – harvesting water by constructing a barrier on the lower side of a large impervious rock to trap surface runoff.
- Weirs and dams – structures to hold and manage water flow.
- Dam – a barrier constructed across a river or dry valley to hold water.
- Weirs – barriers constructed across rivers or streams to raise the water level while allowing water to flow over them.
- Ponds – excavations made to hold excess surface water.
- Retention ditches/level terraces – terraces constructed with blocked ends to retain water.
Micro-Catchments
- A system of harvesting limited rainfall and storing water in the ground for use by planted crops.
Types of Microcatchments:
- Triangular/V-shaped/Negarims:
- V-shaped bunds measuring 25 cm, built with soil from excavated planting holes to direct runoff water towards the basin area around each plant.
- Semi-circular bunds:
- Formed around growing plants to hold water near the roots.
- Trapezoidal bunds:
- Trapezoidal-shaped bunds enclosing a large area where crops are grown.
- Contour bunds/furrows:
- Furrows made along contours between rows of crops where agroforestry trees are intercropped with annual crops.
- Planting holes/pits:
- Extra-large planting holes filled with dry plant materials before filling with soil to improve water retention.
Use of Micro-Catchments
- Slow down the speed of surface runoff, reducing erosion.
- Used in landscaping of compounds, parks, and roadside nesting areas.
- Assist in reclamation of land for food crops in dry areas.
- Water collected and stored can be used for irrigation.
- Support afforestation efforts in dry areas.

