Soil and Water

Jeffrey Alahira

Nigeria is endowed with arable land and freshwater resources when viewed as a whole with approximately 61 million hectares of the land cultivable while the total renewable water resources are about 280 km3/year; which include river Niger, River Benue, lake Chad, Osun river, Hadejia River, Bonny river and a host of others. Soil conditions and […]

Nigeria is endowed with arable land and freshwater resources when viewed as a whole with approximately 61 million hectares of the land cultivable while the total renewable water resources are about 280 km3/year; which include river Niger, River Benue, lake Chad, Osun river, Hadejia River, Bonny river and a host of others. Soil conditions and water availability if effectively managed will help boost food production and address the food crisis in the nation.

Soil

Nigeria has a wide diversity of soil under different ecological conditions and with different levels of fertility. The different soils are a function of prevailing climatic conditions, vegetative cover, and topography of the area among others.

The major soil types in Nigeria, according to FAO soil taxonomy legends are fluvisols, regosols, gleysols, acrisols, ferrasols, alisols, lixisols, cambisols, luvisols, nitosols, arenosols, and vertisols. These soil types vary in their potential for agricultural use. None of these soils was rated as class 1 with high productivity by the FAO.

Nigerian soils can be classified into groups made up of four (climatic) zones that are soil associations. The groups are[2]:

1.       Northern zone of sandy soils

2.       Interior zone of laterite soils

3.       Southern belt of forest soils

4.      Alluvial soils Zones

Map showing soil zones and types in Nigeria

  Courtsey: Kushimo Oluwaseun

Northern zone of sandy soils: This area lies in the very northern parts of the country. This area lies in the extreme north with proximity to the fringes of the fast- encroaching Sahara desert. It is characterized by soils formed by the deposition of sand by the wind. These soils might have been formed from wind-sorted desert sands that accumulated over long periods of time when the Sahara desert encroached several kilometers south of its present limits. The soils of this zone are very good in the production of groundnut, sorghum, cowpea, and millet.

Interior zone of laterite soils: This zone is made up of a mixture of sand and clay. They are grey to black clay, poorly drained, and seasonally flooded forming the “fadama”. The soil in this zone is deeply corroded, generally sticky, and impervious to water and has low fertility. When the virgin forest on them is cleared it reduces fertility further, thus making them available soil of little agricultural value. However, not only laterite soils are found in this zone. The Biu Plateau has rich soil that is productive and offers prospects for the expansion of the areas of cotton production.

Southern belt of forest soils: Soils in this zone broadly represent those of the humid, tropical forest climate zones of the south where the wet season is long, the harmattan season short and forest cover is dense. Local soil types depend largely on parent rock; where the underlying rocks are granite or clay, the soils is a rich clayey loam. These soils are very good in growing crops like cocoa, oil palm, rubber and they are of considerable importance in Nigerian agriculture.

Zone of alluvial soils: These soils are found along the flooded plains of rivers, deltas, along the coastal flats. This zone extends from the coastal inland and runs along the valleys of the Niger and the Benue rivers, thus cutting across the vegetational zones. Soils in this zone are characteristic of fresh-water soil of grey to white sand, grey clay, and sandy clay with humic topsoil. Another group consists of brownish to black saline mangrove soils, with a mat of rootlets.

Soil management

The traditional land tenure system and soil management practices involving shifting cultivation, slash-and-burn processes, and traditional tillage method ensure the maintenance of soil physical properties and sustainable productivity. However, land-use pressure has reduced the duration of fallow to restore soil fertility below the recommended minimum threshold required for sustainability (FAO 1985)[3].

Soil management practices include;

  • Cover cropping: This involves the planting of crops that help manage soil fertility, water, weeds, pests, diseases. It helps to reduce erosion, suppress weed manifestation, etc. for example includes; Mucuna pruriens, centrosema pubescens, Pueraria phaseoloides.
  • Crop rotation: Alternating different crops with the different nutrient requirements on farmland in a predefined manner. It also helps in replenishing lost nutrients e.g Nitrogen fixation by legumes.
  • Nutrient management: The use of organic manure, plant residues helps to improve the fertility of the soil and the amount of organic matter content, which also improves the soil structure and function.
  • Tillage: The practice of reduced tillage or no-tillage operation limits the disturbance of the soil and retains plant residues. This is very helpful in soils that are easily prone to soil erosion.

Water

Image by Rifqi Ramadhan

Water is an important constituent of the ecosystem; it is the most abundant substance on earth. Water is an important requirement for sustainable agricultural production. Crops can be grown without fertilizers and even without soil, but they cannot survive without water. Without adequate moisture, plants cannot mobilize soil nutrients and lack of water at critical stages of development will result in stunted plant growth. The increasing population requires a proportionate increase in crop production, which has suffered little output due to dependence on rainfall. To meet future food needs, farmers will have to make better use of all available moisture by employing water harvesting, conservation, and efficient irrigation methods.

Rainfall: Nigerian agriculture is basically rainfed, making her dependent on rain as the source of water. This is however a limiting factor defining the low productivity level. Water is, therefore, a limiting factor to agricultural production in most parts of the country.

Rainfall patterns and distribution vary within the country with the average annual rainfall of between 1000 – 2000 mm in the humid areas and 500 – 600 mm in the semiarid areas[4]. The southern part of the country experienced a long raining season with a thick cloud which starts in March and last to the end of July, with a peak period in June. Also, a short dry season is known as “August break” which is generally observed in the last two weeks of August.  The dry season lasts between late October to early March; this period witnesses dusty north-east winds.

However, the Northern Nigeria which experience long dry season from October to mid-May, the wet season covers a relatively short period, from June to September. The rains are generally convectional, heavy, and short in duration, often characterized by frequent storms. This results in flash floods and in some places also in sheet or gully erosion.

Water management

Nigeria’s cultivation land has been estimated to about 71.2 million hectares but less than 50% is put to use due to water constraints. The seasonality of rainfall results in situations where water is available and often in excess at certain times followed subsequently by periods of intense drought.

Irrigation is the artificial application of water to the soil to assist growing crops in dry areas and during periods of inadequate rainfall. There are different types of irrigation techniques relating to how water is distributed from the source to the field or crops. This includes:

  • Surface irrigation system
  • Subsurface
  • Drip irrigation

Traditionally many farm families in Nigeria had cultivated small areas in Fadamas during the dry season, using water manually drawn from shallow wells or streams. Major Fadama areas are located along the flood plains of the Niger, Sokoto Rima, Benue, and Yobe rivers.  Irrigation practices in Nigeria central only on surface channeling of water from water bodies to the field, the use of precision or drip irrigation as practice in developed nations with high efficiency is yet to be recognized as a solution to water management.

Despite the abundance of different sources of water for irrigation Rivers, Lakes, dams, and reservoirs in Nigeria (e.g Oyan dam, Dadin Kowa dam, Tiga dam, Kiri dam and a host of others), Irrigation farming potentials have not been fully utilized which has kept Nigerian Agriculture mainly rainfed with a low output.

References


[1] FAO (1995). Irrigation in Africa in Figures. Rome

[3] FAO (1985). Changes in Shifting Cultivation in Africa: Seven Case Studies. FAO Forestry Paper 50 (1). Rome

[4] I. E. Ahaneku. Conservation of soil and water resources for combating food crisis in Nigeria. Pg. 1

[5] Aremu JA, Ogunwale SA (1994). Comparative Analysis of Small and Large-Scale Irrigation Schemes in Northern Nigeria in AO Sanda, SB Ayo (eds), Impact of Irrigation on Nigeria’s Environment, Fact Finders Int. pp. 165-185.

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Jeffrey Alahira