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Soil and water conservation

Rainfall is becoming more unreliable and yet most farmers in Africa highly depend on it to grow crops and raise animals. Unexpected droughts are experienced everywhere, leading to reduced or no yields at all in some cases. Sometimes when the rain comes, it is quite heavy and washes away the soil, destroys plants and causes floods or landslides. The extent of damage is usually greater on croplands along hilly slopes. Depending on the extent of damage, the productivity of the land is instantly or gradually reduced, because either all or part of the topsoil that is rich in organic matter and nutrients is lost to the lowlands, leaving behind the less productive part of the soil.
The implication of such scenarios is that farmers need to protect the entire landscape in order to protect the soil and conserve water needed for sustainable production of crops and animals. Whereas fl at and well-drained land is good for farming, sloping lands can only be used under proper soil conservation. Steeper lands should not be used for growing annual crops, but kept under grass, perennial tree crops or put under controlled grazing. Very steep land with shallow soil should rather be left in its natural state and also as home for wildlife.
The two main aims of soil conservation on cultivated lands are, therefore,

  1. to maintain the soil covered with dead plant materials or living plants or trees as much as possible to hold the soil and break the wind force, and
  2. to reduce the movement of surface water, encourage water infiltration and storage in the soil.

Soil conservation is achieved by controlling soil erosion (the extent of soil and organic matter loss) and regulating tillage practices. Proper soil conservation is the foundation for effective organic production of crops and animals.

Soil erosion

Soil erosion is the physical movement of soil particles and organic matter from a given site by the action of raindrops, runoff or wind. Soil erosion accounts for bout 80 per cent of land degradation in Africa.
How to recognise soil erosion: First signs of the soil’s disposition to erosion are recognized by the separation of soil particles that often have a different colour. The extent of soil erosion will advance from sheet erosion (uniform removal of a thin layer of topsoil), rill erosion (small channels formed in the field) to a more destructive stage, gully erosion (large channels formed in the field). Exposed root systems of plants are also a sign of erosion.
Loss of soil organic matter from upper soil layers destroys the physical properties of the soil, its structure, aeration, water-holding capacity and biological activity, and involves loss of soil nutrients, which leads to nutrient deficiencies and poor plant growth. The amount of erosion on a farm land depends on the slope of land, nature of plant or vegetation cover, land use, erodibility (the estimate of the ability of the land to resist erosion), erosivity of eroding agent (i.e. the ability of wind or water to cause erosion).

  • Slope of land: Naturally, the steeper the slope of a field, the greater the amount of soil loss from erosion by water.
  • Vegetation: Soil erosion potential is increased if the soil has no or very little vegetative cover of plants and/or crop residues. Plant and residue cover protects the soil from raindrop impact and splash, tends to slow down the movement of surface runoff and allows excess surface water to infiltrate.
  • Land use: Certain land management and cropping practices (tillage, strip cropping, terracing) can directly affect the overall soil erosion problem and solutions on a farm.
  • Soil erodibility: Soil erodibility is an estimate of the ability of soils to resist erosion, based on the physical characteristics of each soil. Generally, soils with faster infiltration rates, higher levels of organic matter and improved soil structure have a greater resistance to erosion. Sandy loam and loam textured soils tend to be less erodible than silt and certain clay textured soils.

Causes of soil erosion

Soil erosion occurs naturally. Human intervention can, however, accelerate these natural processes, for example, through:

Overgrazing of rangelands that reduces plant cover, exposing the soil surface to rain and animal stamping impacts, which in turn loosens the topsoil making it susceptible to erosion. As the stocking rates increase and new animal species such as sheep and goats are introduced, the grazing land will eventually be cleaned to bare ground.

Over cultivation of cropland resulting in exhaustion of soil organic matter, destroys soil structure and makes soils very susceptible to erosion.

Utilisation of erosion susceptible areas without any soil conserving measures such as terracing, automatically results in soil erosion.

Continued destruction of forests in search of fi rewood, material for charcoal production and new cultivable land leads to soil erosion, floods and landslides, and reduces storage of rainwater in the soil and modifi es the availability of water in water bodies and groundwater.

How erosion affects agriculture:

Decrease in agricultural productivity:– Loss of the nutrient rich and biologically active upper soil layers results in loss or decrease of productivity of the soil.

In high rainfall areas part of the water which cannot be retained percolates to a deeper level or ground water and leach nutrients out of reach of the plant roots in the process.

Control of soil erosion

Irrespective of the extent of damage by soil erosion, land and soil can still be rehabilitated. If the topsoil is lost and erosion is severe, it will take much effort and considerable time to rehabilitate the land. Usually it takes the commitment of the entire community in order to improve the situation. However, even at the individual household level, there are many measures a farmer can establish to control soil erosion. These measures will at the same time control erosion and conserve soil moisture.


The easiest way to protect the soil from being eroded by water or wind is to keep it covered by a plant or mulch cover as much as possible. The soil can be covered with living plants (cover crops), especially within perennial crops, or dead mulching material. Erosion due to rains is more a problem in annual crops where the land is regularly tilled for planting and when soil preparation coincides with rainfall. To avoid erosion during this period, the soil is best covered with residues from the previous crop and other dry plant material, and soil cultivation is reduced by tilling strips only.

a) Erosion control with cover crops

Cover crops are usually low-growing perennial plant species, which are sown with the main intention to protect the soil, prevent weed growth and maintain soil fertility. They are also called ‘green’ or ‘living mulch’. Cover crops are used in a similar way as green manures with the main difference that green manures are grown to produce maximum biomass mainly and are usually slashed before flowering and incorporated into the soil. Cover crops may also require regular slashing, mowing or grazing to avoid competition with the main crop.
Some information sources do not distinguish between cover crops and green manures, as both can include the same species, and differences are little depending on their management. But it makes sense to approach them separately due to the different functions they can have in a cropping system.
The primary strength of cover crops is to rapidly cover the soil and to maintain it permanently covered. Cover crops benefit both short and long term productivity of a cropping system. They improve physical properties of the soil, reduce runoff and erosion, suppress weeds and, if the cover crop is a legume, transfer nitrogen to the main crop, when mulched. Soil organic matter levels are usually maintained under a cover crop from a combination of increased input of residues, reduced soil organic matter decomposition due to reduced exposure as a result of reduced or zero tillage, and decrease of soil temperature.
The benefits of cover crops can be limited by the competition of the cover crop for water and nutrients and the very slight increase of soil organic matter level. Slashing, mowing or selective cultivation temporarily reduce competition from the cover crop. While leguminous cover crops supply some nitrogen to the main crop, pure grass-based cover crops require nitrogen for proper growth.
The following characteristics make an ideal cover crop:

  • It is low-growing and not climbing;
  • It grows fast and covers the soil in a short time;
  • It is resistant against pests and diseases, and does not transmit any to the main crops;
  • It tolerates drought;
  • It fixes nitrogen from the air;
  • It develops a deep root system which is able to loosen the soil and contribute to regeneration of degraded soils;
  • It is easy to sow and to manage, and can be slashed, grazed or cut for fodder;
  • The seeds are cheap, easy to purchase or can be easily reproduced on the farm.

The residues of cover crops are usually not harvested, but are left to decompose in place. This explains, why they are also called living mulch. Some cover crops can be grazed, provide food or can be used to produce forage. Growing a cover crop limits possibilities of soil tillage. Therefore cover crops are usually grown in cropping systems, which include reduced tillage. Cover crops can be grouped into legumes, grasses, and other groups such as cucurbits, which also cover the soil well. For a permanent soil cover, a mixture of legumes and grasses is best, as their root systems usually complement each other well in their growing depths and together they provide a balanced source of feed for livestock.

How to integrate cover crops

Cover crops can be planted in different ways depending on the site conditions, the main crop and intended benefits:

  • Intercropping: The cover crop is planted at the same time as the main crop. In this case, the main crop should be one that grows high like maize to avoid being smothered by the cover crop. Creeping cover crops like mucuna should be avoided, because they will also smother the main crop. Intercropping is preferable in perennial crops.
  • Relay cropping: The cover crop is planted in an advanced growth stage of the main crop. For example, in a maize-bean intercrop the cover crop can be planted after beans are harvested. Here the farmer is able to harvest more crops and the risk of competition is greatly reduced. The cover crop is then left to continue growing, protecting the soil and smothering weeds.
  • Crop rotation and improved fallows: In this case, the cover crop is planted after the harvest of the main crop. If the soil has enough moisture, this can be done immediately after harvesting or it can be done as part of the main crop rotation cycle or incorporated during the fallow season.

To reduce the risk of damage by pests and diseases, different species of cover crops can be grown on different fields. If planted together with food crops, cover crops should also be rotated to avoid build-up of pests and diseases.
Recommended practices for sowing cover crops vary depending on the cropping ping system, seed size and climate. Small seeds are either broadcasted or sown in lines by hand or with a seed drill. Large seeds are best sown using a hand hoe or an animal drawn direct planter. In pure stands narrower spacing is recommended, while in intercropped cover crops and in dry climates, a wider spacing reduces competition with the main crop. In general, 2 to 4 seeds are planted per hole. Most cover crops will need at least one weeding during early stage of growth.

b) Erosion control with mulching

Mulching is the process of covering the topsoil with plant material such as leaves, grass, twigs, crop residues or straw. Sometimes artificial mulches, such as plastic cover, are used (for weed control mainly; they do not provide the same advantages as organic mulch). Mulching has many advantages, including protecting the topsoil from being washed away by strong rain and from drying out by the sun. Protection reduces evaporation of water and thus keeps the soil humid. As a result the plants need less irrigation or can use the available rain more efficiently. A humid soil also enhances the activity of soil organisms such as earthworms, and microorganisms as rhizobia and mycorrhiza.
Organic mulch material is an excellent food source for soil organisms and provides suitable conditions for their growth. As the mulch material decomposes, it also releases its nutrients, while part of the mulch material is transformed to stable humus, contributing positively to the soil’s organic matter content. A thick mulch layer further suppresses weed growth by inhibiting their germination. For all these reasons mulching plays a crucial role in preventing soil erosion.

Application of mulching materials

Sources of mulching material include weeds or cover crops, crop residues, grass, pruning material from trees, cuttings from hedges and wastes from agricultural processing or from forestry. Fast growing nitrogen-fixing shrubs that tolerate strong trimming provide good and considerable amounts of mulching material. The shrubs can be grown in hedgerows.
The kind of material used for mulching greatly influences its effect. In humid climates green material will decompose rapidly making nutrients available nutrients to the crops during the process. Soil protection is then limited to 1 to 3 months. In this case application can be repeated. Hardy materials such as straw or stalks in contrary will decompose more slowly and therefore cover the soil for a longer time. Where soil erosion is a problem, slowly decomposing mulch material (with low nitrogen content and a high carbon to nitrogen ratio) will provide long-term protection compared to quickly decomposing material.
When carbon rich materials are used for mulching, nitrogen from the soil may be used by microorganisms for decomposing the material (a process called immobilization). During this time, the microbes compete with the plants for nitrogen and the crop may suffer from malnutrition. To avoid nitrogen immobilisation, old or rough plant materials should be applied to the soil at least two months before planting or sowing the main crop. The decomposition of the mulch material can be accelerated by spreading organic manure such as animal dung on top of the mulch, thus increasing the nitrogen content.
In arid climates mulch material may be scarce and production or collection usually involves a considerable amount of labour and thus may compete with labour for the production of crops and of household activities. Especially in such climates, however, application of mulches is worthwhile.
In specific situations organisms such as slugs, snails, ants or termites can proliferate too much in the moist and protected conditions of the mulch layer and may cause damage to the crops. Damaging organisms such as stemborers may survive in the stalks of crops like cotton, corn or sugar cane. In such situations mulching materials must be carefully selected to avoid any disadvantages, or farmers renounce to protection of the soil with mulch and apply other methods for soil protection. As a general rule plant material infected with viral or fungal diseases should not be used if there is a risk that the disease might spread to the next crop. Proper crop rotation is very important to overcome these risks.
If possible, the mulch should be applied before or at the onset of the rainy season, as then the soil is most vulnerable. If mulch is applied prior to sowing or planting, the mulch layer should not be too thick in order to allow seedlings to penetrate it. If the layer of mulch is not too thick, seeds or seedlings can be directly sown or planted in between the mulching material. Mulch can also be applied in established crops, best directly after digging the soil. It can be applied between the rows, directly around single plants (especially for tree crops) or evenly spread on the fi eld. On vegetable plots it is best to apply mulch only after the young plants have become somewhat hardier, as they may be harmed by the products of decomposition from fresh mulch material.
In humid climates loose, bulky materials such as twigs are usually more appropriate for mulching, as they ensure adequate ventilation. Materials should not be too bulky though to prevent damage on crops or being blown away. If  mulch material is introduced into a fi eld, attention must be paid to not to introduce any unwanted seeds.
The ideal strategy for mulch application fi nally depends on local conditions and the crops that are grown. Whether mulch is best applied before or after planting, in strips along the rows or evenly over the entire surface, in a thick or a thin layer, must be found out through testing over several seasons.

c) Erosion control with reducing movement of water

Building contour bunds and digging ridges

An effective measure to limit above soil movement of water is digging ridges along the contour lines of a slope. Or natural drain ways are identifi ed and planted with grass to allow storm water to move smoothly over the fields without breaking into gullies. Waterways need dense vigorous vegetation and water should be directed with diversions. Ditches may be dug along the contour to trap the running water and encourage infi ltration into the soil. Contouring is often combined with strip cropping furrows between the contour ridges, in which strips of a crop such as maize alternate on the side of the hill with strips of denser vegetation like legumes. Much of the soil washed downhill from each strip of row crops is trapped by the strip of denser vegetation growing below it. Laying trash lines of stalks and other crop residues, instead of the dense vegetation, is also helpful.
The A-frame is a simple, cheap and easy-to-construct tool for marking contour lines along a slope, making it readily accessible to African farmers. The A-frame is made from three poles, some rope, a stone and a supply of stakes.

How to build and use an A-frame:

  1. Fix three poles of about 2.5 meters long each in a position forming an even ‘A’. If rope is not sufficient to tie the ends, use nails.
  2. Tie one end of a piece of cord to the top of the A and fix a stone tied to the other end so that the stone is at some distance from both the ground and the crossbar.
  3. Put the A-frame upright and mark the position of both legs. Then, mark the point where the string passes the crossbar of the A.
  4. Turn the A-frame so that the placement of the legs is reversed. Again mark the point where the string passes the crossbar. If the two marks are not at the same point, mark a third point with a knife exactly halfway between the first two.
  5. Drive the first stake at the edge at the top of the field. Place one leg of the A-frame above and touching the stake. Place the other leg in such a position that the string passes the level position point on the crossbar.
  6. Drive another stake into the ground just below the second leg. Move the A-frame and continue in the same way across the field.
  7. The next contour line is placed 3 to 6 meters below the first line. The steeper the slope, the closer the lines should be.

Placing grass strips
Fodder grasses such as vetiver grass (Vetiver zizanioides), napier grass (Pennisetum purpureum) and guinea grass (Panicum maximum), Bahia grass (Paspulum notatum) can be planted in strips at intervals across the slope to slow down runoff of water. In addition to reducing soil erosion, the grasses provide feed for the animals. The grass strips can be mixed or replaced with a hedge row of leguminous fodder trees such as Leucaena diversifola, Calliandra calothyrsus, Sesbania sesban, Gliricidia sepium.

Terracing

Mechanical measures for controlling erosion are usually more costly than those that depend primarily on vegetation. They require more labour, materials and skill to install. Terracing includes many different types of terraces, diversions and grade stabilization structures. Terraces break up a long slope into a series of short ones. Each terrace collects and controls the excess water from a definite area of the slope above it. Water collected in a terrace channel may be connected to protected outlets such as man-made ponds or natural water ways where it will cause no damage. If the soil in the field is permeable enough, terraces may be built level and water allowed to stand and soak into the ground. Even well-constructed terraces need continuous repair in order to be effective. Unless kept in good condition, terraces may cause more erosion than if they were not built.

  • Bench terraces. They are found on medium slopes and transform the steep slope into a series of level shelves or beds running across the slope on which crops are grown. The steps are separated by almost vertical risers (walls or bunds) of rock or earth protected by a heavy growth of vegetation. The risers need to be kept covered with grass and continuously repaired to maintain their stability. Although bench terraces take a lot of labor and time to construct, they can last a long time if well maintained
  • Stone lines. Use of stone lines is most applicable when stones are easily accessible in the area. Here stones are piled across the slope, breaking it into small sections where crops are grown. They slow down runoff and soil eventually builds up behind them, forming nearly leveled beds.
  • Fanya juu (Converse) terraces. Fanya juu (‘throw it upwards’ in Kiswahili) terraces are made by digging trenches along the contours and throwing the soil uphill to form embankments (bunds), which are stabilized with fodder grass such as Napier (Pennisentum purpureum) and multipurpose agroforestry trees. The space between the embankments is cultivated with crops and over time, the fanya juu develop into bench terraces. They are useful in semi-arid areas to harvest and conserve water.

Conserving vegetation

Plant roots hold soil particles together and protect the soil from being washed away by water or wind. Land that is covered with vegetation is less susceptible to erosion than unplanted land. This can be achieved by maintaining natural grass cover in perennial crops or by growing a cover crop. On the other hand, very steep slopes should be planted with trees instead of cultivating them for crops.
Growing trees in rows (alley cropping) and hedges in the fi elds or around the fields will reduce wind speed. They also create a micro-climate, which reduces evaporation and protects the soil and crops from the drying effects of wind. When trees are planted in rows in the fi eld, they often compete with the crops for water, and in drier areas, this will reduce the yields of the fi eld crops. In such areas, planting hedgerows is recommended or if planted with crops, they should be heavily pruned at the beginning of the growing season of the fi eld crop to reduce competition. During the dry season the trees will have grown again and be able to shade the soil.

Water harvesting

Water harvesting, water saving and soil moisture conservation strategies have highest priority in semi-arid and arid regions. As water is the limiting factor for crop yields, every drop of rain or irrigation water should be retained in the field. Sufficient soil water supply requires proper water harvesting of the available rainfall and reduction of runoff, and soil management strategies to increase wa-ter infi ltration, holding capacity and decrease evaporation through mulching and minimum tillage. Even where irrigation water is available, water application should be kept to an absolute minimum in order to avoid problems of salinity and over-exploitation of ground water.
Organic farmers seek to optimize the use of on-farm resources for water management improving their soils and designing farming systems in a way to capture water and store it for later use. The following measures have been used successfully in many areas:

Planting or water-retaining pits: Water retaining pits (also known as Zai in Burkina Faso and as tassa in Niger) are hand-dug circular holes along planting rows which collect and store water. The soil from the pits is used to make banks around the pits. The size of the pit depends on the amount of runoff. Manure or compost may be added in the pit before planting in the pits. After planting, the pits are not completely covered to allow more collection of water. The pits can be used season after season while improving soil fertility with application of manure or compost.

Water catchments: Water from roads and homestead compounds can be channeled into the farmland via field ditches or a water pond. From here the water can be slowly diverted into the field or used for irrigation.

Minimizing soil disturbance

Farmers till land for various reasons: to loosen the soil and prepare a seed bed to encourage seed germination, control weeds or incorporate manure and plant material into the soil. Turning the entire surface area of the field that is to be planted is common in many African countries. General ploughing, discing and harrowing are encouraged by the introduction of tractors. But also ridging using a hoe involves disturbance of the entire surface. These soil cultivation systems leave bare soil exposing it to erosion and water loss through evaporation, result in capping of the soil surface, accelerate decomposition of soil organic matter and contribute to destruction of soil structure. Repeated working depth and cultivation of soil in humid condition bears the risk of soil compaction and creation of a hardpan at the working depth. Mixing of soil layers can also severely harm certain soil organisms such as earthworms.
Most farmers, who plough their land, must wait for the rains to cultivate the soil. In this case planting cannot happen as long as the land is not prepared. In many regions each day of delay in seeding after the fi rst rains results in yield loss. Cultivation of the entire surface area of a fi eld is labour, energy and time intensive. Preparing a fi eld may take several days or weeks, requires strong draught power and much fuel if a tractor is used.
Traditional organic farming practices involve deep soil cultivation with inversion of the soil to allow incorporation of plant material and animal manure, and bury weeds. Increasing knowledge on the negative impacts of such a practice on soil organic matter, nutrient losses, soil biology, climate, use of energy and costs presently results in a basic change in the approach to soil cultivation with increasing adoption of practices, such as they are promoted by the approach of soil conservation farming.
Any soil cultivation activity has a more or less destructive impact on soil structure. But there are soil cultivation systems that minimize soil disturbance, maintain a protective cover on the soil surface and allow early land preparation before the rains. Such systems contribute to a good soil structure, reduce the risk of soil compaction, increase water infi ltration and reduce runoff, reduce evaporation and thus improve water storage. When the soil is protected and stays undisturbed, the topsoil layer becomes a favourable habitat for plant roots, worms, insects and microorganisms such as fungi and bacteria. This soil life recycles the organic matter from the soil cover and transforms it into humus and nutrients, and thus contributes to fertile soil and plant nutrition. This process may also be called ‘biological tillage’.
Reduced soil cultivation and maintenance of a soil cover, as they are recommended by the conservation farming approach, allow farmers to prepare their land after the harvest of the previous crop. Early land preparation allows planting at the onset of rains and early weeding. The soil conservation farming approach is very suitable to women, as labour for soil cultivation is reduced and can be done over a long period without loss of nutrients and precious time.
Soil cultivation should provide good growing conditions for seeds and seedlings, loosen the soil in a way to facilitate the penetration of the young plant roots, destroy or control weeds and soil pests, if necessary, and repair soil compaction caused by previous activities. Whether soil cultivation should serve incorporation of crop residues and manures into the soil or not, is a basic decision that needs to be taken in the local context. To minimize the negative impacts of soil cultivation while benefi ting from its advantages, farmers should aim on reducing the number of interventions to the minimum and choose methods that best conserve the natural qualities of the soil.
There is not just one right way to cultivate the soil. There is a range of options. Finding the most appropriate soil cultivation method depends on the crops that are grown, the cropping system, the soil type, climate, weed pressure and other factors. Thus, each farmer must assess the soil cultivation practice which is most suitable for his or her conditions minimizing the negative impacts of soil cultiva tion while benefi ting from its advantages. Organic farmers should aim to keep the number of interventions to a minimum and choose methods that conserve the natural qualities of the soil. Adoption of reduced soil tillage by farmers, who fully rely on natural practices and avoid herbicides and chemical fertilizers, may require specifi c adaptations to prevent weed problems and ensure appropriate plant nutrition.

Zero-tillage or no-till systems

No-till systems work without any soil tillage and seeds are planted or drilled directly into the vegetation cover without any seedbed preparation. Crop residues are left on the soil surface. The vegetation cover and weeds are destroyed by slashing them manually or mechanically or using herbicides to avoid competition between the crop and the soil covering vegetation. In conventional farming, synthetic fertilizers are either broadcasted or applied during seeding. For seeding, usually a narrow slot only wide and deep enough to obtain proper seed coverage is made, while crop residues basically remain undisturbed on the soil surface.
Zero-tillage systems help to build-up a natural soil structure with crumbly topsoil rich in organic matter and full of soil organisms. Nutrient losses are reduced to a minimum as there is no sudden decomposition of organic matter and nutrients are caught by a dense network of plant roots. Soil erosion will not be a problem as long as there is permanent plant cover or suffi cient input of organic material. Last but not least, farmers can save a lot of labour.
Zero-tillage requires soils with good drainage. Water-logged soils and soils with poor drainage are not suitable for zero-tillage, as the seeds and plant roots will rot in the soil. In compacted soils, sub-soiling deeper than the soil pan may be necessary to enhance drainage. Or deep rooting crops such as pigeon peas are grown in rotation to break pans before weaker rooting crops.
Successful zero-tillage depends on high biomass production to ensure a thick mulch cover. Proper crop rotation including leguminous green manure crops is essential to this system. Managing weed growth may be a challenge to organic farmers, who renounce the use of herbicides and rely on mechanical or natural methods for weed control only. Nevertheless, there is potential for introducing zero-tillage in organic farming.
In annual crops, for instance, zero-tillage can be applied easily when sowing a legume crop after a grain such as maize, wheat, sorghum or millet between the stalks.
Zero-tillage with living mulch is good mainly for perennial crops, for example coffee or banana, where competition by annual vegetation is limited and weeds can be controlled by regular slashing.

Reduced or minimum tillage systems

Reduced tillage is shallow soil tillage or loosening of the soil by a chisel without deep soil cultivation or making furrows or holes where seed is planted. Minimum tillage promotes build-up of organic matter in the soil, activity of soil organisms and contributes to more stable soil aggregates resulting in better water infiltration. Minimum tillage also implies reduced labour and about half as much energy and effort for land preparation. The greater the part of the soil surface that remains undisturbed and covered, the more positive the impact is. Ideally the seedbed is prepared only where the seeds are planted and the residues remain on the topsoil and are not buried.
Minimum tillage involves techniques such as scraping out shallow planting holes with a hoe, planting with a dibble stick or digging narrow furrows with a chisel-shaped ripper pulled by animals or a tractor. The distance between the furrows results from recommended spacing for the crop. Compared to a conventional plough a ripper is smaller, lighter and easier to operate, and also cheaper to buy and maintain. As a ripper requires about half of the draught force of that of a plough, farmers can use weaker and smaller animals also. For making planting holes with a hoe a long string with knots or bottle tops indicating the planting distance and pegs are helpful.
Reduced or minimum tillage is well suited to many tropical soils, in which intensive tillage leads to rapid breakdown of the soil structure and loss of water and organic matter. However, the adoption of reduced tillage also involves some challenges. The most important is weed control. Farmers who renounce the use of herbicides depend on mechanical weed control or on a thick mulch cover or on cover crops and proper crop rotation to prevent weed growth.
In systems, however, where the inter-row is never ploughed, weed pressure decreases over time, as weeds are not allowed to germinate.

Resources and further readings

  • Soil and Water Conservation in Organic Agriculture. Farmers’ Training Notes. Kenya Organic Agriculture Network KOAN. www.koan.co.ke
  • Conservation Farming & Conservation Agriculture. Handbook for Hoe Farmers in Agro-Ecological Regions l & lla - Flat Culture. 2009. Conservation Farming Unit. Zambia National Farmers Union. www.conservationagriculture.net
  • Conservation Farming & Conservation Agriculture. Handbook for Ox Farmers in Agro-Ecological Regions l & lla. 2007. Conservation Farming Unit. Zambia National Farmers Union. www.conservationagriculture.net
  • Conservation Tillage with Oxen. Conservation Farming Handbook. No. 2. 2002. Study Circle Material. Land Management and Conservation Farming programme. Republic of Zambia. Ministry of Agriculture & Cooperatives
  • Combatting soil erosion. Sustainable production practices COLEACP.PIP.  www.coleacp.org/pip
  • Erosion control in the tropics. Agrodok 11. 2005. Agromisa Foundation, NL. www.agromisa.org
  • Producing in Harmony with Nature through Conservation Tillage. 2002. African Conservation Tillage Network. www.act-africa.org
  • Integrated soil management and conservation practices. 2000. FAO. www.fao.org
  • Water harvesting and soil moisture retention. Agrodok 13. 2005. Agromisa Foundation, NL. www.agromisa.org
  • Conservation Agriculture. A manual for farmers and extension workers in Africa. 2005. International Institue of Rural Reconstruction IRRI; African Conservation Tillage Network ACT.
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