Country Pasture/Forage Resource Profiles |
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Ethiopia
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The Federal Democratic Republic of Ethiopia (FDRE) is a landlocked country in the horn of Africa, bounded to the north by Eritrea, to the west by Sudan, to the south by Kenya and to the east by Somalia and Djibouti; it lies within the tropics between 3°24` and 14°53` North; and 32°42` and 48°12` East (see figure 1). It covers 1,120,000 square kilometres in nine regional states, one City Council and one City Administration. Smallholder peasants farm eight percent (about 10,000,000 ha) of the national land area and about 3,100,000 hectares are fallow. The total area of grazing and browse is estimated to be 61,000,000 –65,000,000 hectares, of which 12 percent is in mixed farming and the rest in pastoral areas (Alemayehu, 1998a; MoA, 2000). The population was estimated at about 63,000,000, making it the third most populous country in Africa, after Egypt and Nigeria, but according to the World Factbook the July 2006 estimate was 74,777,981 with a growth rate of 2.31%. The male-female ratio is almost one to one. 85.3 percent of the population lives in rural areas and the rest is urban (CSA, 1999).
Figure 1. Location map of Ethiopia. Ethiopia is culturally and biologically diverse, among the four most diverse countries in Africa for endemic vertebrates; fifteen percent of the estimated 7,000 vascular plants are thought to be endemic. Ethiopia has a diverse mix of ethnic and linguistic backgrounds; in fact among the top 25 countries in the world in endemic linguistic diversity. It is has more than 80 ethnic groups, each with its own language, and about 200 dialects, culture and traditions. The four main language groups are: Semitic, Cushitic, Omotic, and Nilo-Saharan. One of the most significant areas of Ethiopian culture is its literature which is represented predominantly by translations from ancient Greek and Hebrew religious texts into the ancient language Ge'ez, modern Amharic and Tigrigna. Ge'ez, one of the most ancient languages in the world, is still used by the Ethiopian Orthodox Church, which has its own unique customs and traditions and which have been influenced by Judaism. The agricultural sector plays a central role in the economic and social life of the nation and is a cornerstone of the economy. About 80-85 percent of the people are employed in agriculture, especially farming. The sector contributes about 40 percent of total GDP; livestock and their products account for about 20 percent of agricultural GDP. Smallholders, the backbone of the sector, cultivate 95 per cent of the cropped area and produce 90-95 percent of cereals, pulses and oilseeds. Subsistence agriculture is almost entirely rainfed and yields are generally low. Within agriculture, some 60 percent of the output is from crops, with livestock and forestry producing 30 percent and 7 percent, respectively. Crop production by area is predominantly cereals (84.55 percent) followed by pulses (11.13 percent) and others (4.32 percent). Five crops account for almost all cereal production: maize (15.75 percent), teff (Eragrostis tef) (25.78 percent), barley (12.29 percent), sorghum (12.39 percent) and wheat (10.76 percent) [CSA, 1995-1999]. However crops such as pulses e.g. Chick pea, Beans, Peas; oil crops e.g. sunflower, safflower, rape, neug (Guizotia abyssinica), groundnut; and root and plantation crops e.g. potato, sweet potato, yam, cassava, `enset` (Ensete ventricosum), and sugar-cane have great food and industrial value. Subsistence crop production is traditional and rainfed, with very limited areas of irrigation. Of around 166,000 hectares under irrigation some 64,000 hectares is small-scale; while the irrigation potential of the country is estimated at around 3,000,000 hectares, (EPA, 1997). Small-scale traditional irrigation has been practiced for decades in the highlands, where small streams are diverted seasonally for limited dry season cropping. Medium and large-scale schemes are of more recent origin, particularly in the Rift Valley. Ethiopia’s livestock population (2002) is the largest in Africa, with 30,000,000 cattle; 24,000,000 sheep; 18,000,000 goats; 7,000,000 equines; 1,000,000 camels and 53,000,000 poultry. About 70 percent of the cattle and sheep and 30 percent of the goats are in the highlands above 1,500 metres. All camels are in the lowlands (Alemayehu, 1998a). [FAO Statistical databases (Table 1) show somewhat different numbers for 2002 (and subsequent years): cattle 40.6M; sheep 14.3M; goats 9.6M; equines 5.7M; camels 0.48M; poultry 40.9M and these differences need to be checked].
Table 1. Ethiopia statistics for livestock numbers, meat and milk production and livestock exports and milk imports for the period 1995-2005
Source:FAOSTAT, 2006; n.r.=no record Production from cattle has been estimated to be 620,000 tons of meat; 244,000 tons of milk; 24,000,000 tons of manure; and 2,400,000 hides annually [FAO Statistical databases show somewhat different numbers for 2002 and these need checking]. Per capita consumption of milk is estimated at 19 litres per year, while meat consumption is about 13.9 kilos a year of which beef and veal contribute 64 percent; and sheep, goats, chicken and camels provide the remainder. Skin and hides are known contributors to local industries and 12-16 percent of the total export market (MoA, 1997; Alemayehu, 1998a). Official exports averaged 500,000 sheep and goats [FAO statistical databases show much lower totals and these need checking]; mainly to the Middle East especially Saudi Arabia. There are unrecorded cross-border exports to Djibouti, Somalia and Kenya. Domestic demand has outstripped supply, resulting in local prices for cattle which are higher than world prices, constituting a major bottleneck to exports. The current land tenure system, as per the national rural land proclamation No. 89/1994, assures some security through users’ rights. Land has been a common property of nations and nationalities and shall not be subjected to sale or to other means of transfer. The users’ right helped small farmers to own cultivated and grazing lands. Pastoralists have communal ownership rights to grazing lands. Periodic redistribution of land among farmers has been a strong disincentive to carry out improvement and/or erosion control measures. Land holdings are small and often fragmented into many parcels. Farms of less than a hectare comprise more than 26 percent of agricultural land; almost 60 percent is in holdings of less than two hectares and the rest in holdings between 2-2.5 hectares. Ethiopia’s population, currently about 63,000,000, is the second largest in Sub-Saharan Africa and is growing fast. High livestock numbers and human population exert pressure on land and force farmers to open new cropland at the expense of grazing and forest. Trade in farm products is almost entirely private with minimum involvement of the public sector. There are no legal restrictions and controls on markets, but local authorities have some regulations and charge fees. Ethiopia with its extremely variable agro-climatic conditions has several major ecological systems that support large and very diverse genetic resources. Despite this huge resource, Ethiopia’s latest estimate of real GDP per capita is Birr 1010.08 (US $ 118.00 at the exchange rate of June 2003). It is estimated that 60 percent of the population live below the line of absolute poverty. Average life expectancy is 49 years. The poor performance of agriculture is reflected in the national annual food deficit. The sector has been beset by natural disasters, in particular periodic severe droughts, so the substantial natural potential of the highlands, their fertile soil and good rainfall and irrigation have not been realized. Lack of modern inputs for the subsistence sector, especially fertilizer; inadequate availability of credit, poor credit recovery and widespread disorder and civil war are the main constraints. These situations have drawn resources from productive use in the agricultural sector. The major problems have their roots in poor sectorial policies including controls over input and output prices and insecurity of land tenure. In the lowlands the low rainfall produces inadequate, poor quality pastures; pastoralists mostly keep cattle for prestige so low livestock production is further aggravated by low off-take. Recently, government structural adjustments and trade liberalization policies are being considered; and these could include guidelines for changes in pricing and marketing of several farm products, including livestock. The intention to give incentives to farmers to target their crop/livestock production to market demands and to practice natural resource conservation could sustain the farming sector. |
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Major
Topographic Features The lowlands, the major grazing land of Ethiopia, form a wide apron surrounding the highland massif and part of the Great Rift Valley. This arid, hot zone, with up to 90 growing days per year, is suited mainly to extensive grazing. It includes the lowest elevation in the country at 126 metres below sea level. The lowlands make up nearly 61 - 65 percent of the land-mass, and are the major nomadic pastoralist and agro-pastoralist areas. The topographic diversity of the country has resulted in the formation of a multitude of agro-ecological zones and sub zones with varied farming systems (see section 3). Soils
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2. Main soils and agro-ecological zones There is limited information on the fertility status of the various soils. Research showed that Potassium; Nitrogen; Cation Exchange Capacity (CEC) and organic matter contents of most Ethiopian highland soils are generally high by international standards (EARO, 1998), whereas their phosphorous content is low to very low. Compared to the African standard most soils in the highlands of Ethiopia are fertile (FAO, 1984c). Contrary to most other African soils, the majority of Ethiopian highlands soils remain relatively fertile at depth. However, most highland soils are deficient in important nutrients and require fertilizer to sustain crop yields. Research has indicated that Ethiopian soils are generally low in available nitrogen and phosphorous and cannot produce high crop yields unless these are supplied.
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3. CLIMATE AND AGRO-ECOLOGICAL ZONES Climate
Temperature and rainfall are the most important climatic factors for agricultural production in Ethiopia. Altitude is a factor that determines the distribution of climatic factors and land suitability; this influences the crops to be grown, rate of crop growth, natural vegetation types and their species diversity. Taking the two extreme altitudes, temperatures range from the mean annual of 34.5° C in the Danakil Depression, while minimum temperatures fall below zero in the upper reaches of Mt Ras Degen (4,620 metres) with a mean of less than 0° C, where light snowfalls are recorded in most years. Between these extremes are vast areas of plateaux and marginal slopes where mean annual temperatures are between 10° and 20° C. According to FAO (1984 a) rainfall in Ethiopia is generally correlated with altitude. Middle and higher altitudes (above 1,500 metres) receive substantially greater falls than do the lowlands, except the lowlands in the west where rainfall is high. Generally average annual rainfall of areas above 1,500 metres exceeds 900 mm. In the lowlands (below 1,500 metres) rainfall is erratic and averages below 600 mm. There is strong inter-annual variability of rainfall all over the country. Despite variable rainfall which makes agricultural planning difficult, a substantial proportion of the country gets enough rain for rainfed crop production (FAO, 1984b). Distribution of rainfall is shown in Figure 3.
Figure 3. Long term average annual rainfall (mm.) In the north of the country the rainfall pattern is mainly bimodal, with the shorter of the seasons around March/April; the second rainy season often begins around June/July. In some areas the two seasons combine into a unimodal pattern; this is commoner in the west and some northern parts of the country where rainfall is generally higher. Between these extremes, in the central highlands, there is a tendency for the two seasons to merge. The lowlands of the east and southeast contrast with the rest of the country by having a bimodal rainfall distribution; and have marginal rainfall for crop production (MoA, 2000; FAO, 1984b). Temperature and rainfall, in combination with topography and soils determine moisture availability which determines vegetation and agricultural productivity. Based on moisture regimes FAO (FAO 1984a) classified 50 percent of the country as having sufficient moisture for annual crops and another 16 percent is thought to be reliable for perennial crops. Vegetation Figure
4. Vegetation map of Ethiopia According to Zirihun Woldu (1999), Ethiopia was once heavily treed with about 34 percent of its area and 57 percent of the land above 1,500 metres covered by dense forests and a further 20 percent by wooded savannah. Massive deforestation has reduced these figures to 3.6 percent of the total area and 9 percent of the land above 1,500 metres. Widespread deforestation started, particularly in the highlands, at the end of the nineteenth century with the expansion of agriculture. The current deforestation rate is estimated to be 200,000 ha/year with most of the surviving forest in remnant patches in inaccessible and remote areas. The main Ethiopian plateau is characterized by broad rolling uplands, immense cultivation with good soil. In June–September the landscape is green. In December it is yellow-tan with ripe grain and stubble. In March it is grey – black ploughed fields of traditional subsistence farms. The grazing lands of Ethiopia are in the arid, semi-arid and sub-humid zones which cover around 61 - 65 percent of the land mass and have a number of agro-ecological sub-zones with diverse types of crop and animal production. The arid zone altitude range is from 126 metres below sea level to 1,200 metres; mean annual rainfall is from 100 to 600 mm and the Potential Evapotranspiration (PET) is estimated at 1,700 – 3,000 mm. The mean temperature is above 27 0C. Since rainfall is erratic crops are irrigated. The arid zone plains are bushed grassland, except some patches of woodland. The Rift Valley and escarpments are covered by wooded grassland. Crop production is only along rivers (irrigated state farms). Cotton, maize and sorghum are the dominant annual crops, among the perennials are citrus, banana, and mango. Stock rearing (goat, sheep, camel and cattle) is the major land use. Dominant trees and shrubs include: Prosopis juliflora, Tamarix aphylla, Calotropis procera, Parkinsonia aculeata, Balanites aegypitiaca, Dodonaea angustifolia, Rumex nervosus, Acacia spp., Combretum molle, Azadirachta indica, Salix subserrata, Carissa edulis, Tamarindus indica, and Euclea schimepri. Among wildlife wild-ass, zebra, duiker, lion, leopard and ostrich are known to exist. Nomadic and semi-nomadic pastoralism is the common livestock production system in the arid zones. The semiarid zone (400 – 2,200 metres) has mean annual rainfall of 300 – 800 mm; PET ranges between 1,900 to 2,100 mm, and a growing period of 46 – 60 days. Hilly areas and stony terrain are under wooded grassland or bush grassland; flat land is under rainfed crops (often mechanized). Extensive grazing is the major land use and cattle, goats, sheep, and donkey are the major stock. Trees include: Boswellia papyrifera, Acacia seyal, Acacia senegal, Acacia nilotica, Ziziphus spp., Diospyros mespiliformis, and Balanites aegyptiaca. Common wildlife are: reticulated giraffe; Grant’s gazelle; oryx; Burchell’s zebra; waterbuck; elephant; lion; duiker; greater kudu, lesser kudu and buffalo. The Ethiopian rift system is in the arid-semi-arid zone; the main Rift Valley is a zone of intensive agricultural activity; increasing and progressive settlement has replaced grazing lands with small to medium farms, some of which are mechanized. Originally the vegetation in the rift floor and escarpments was wooded grassland with Balanites, Combretum and various species of Acacia. Broad-leaved woodland dominated by Combretum, Olea spp., Celtis, Dodonaea viscosa and Euclea, occupy the mid altitudes of the escarpments. Lake margins and swamps of the rift valley are covered by swampy genera of Typha, Phragmites, Cyperus, with Suaeda monoica on alkaline soils. Agro-ecological
zones
It is common to associate the traditional zones with elevation and temperature and try to recognize agroclimatic and vegetation zones. Authors have recognized different agroclimatic zones and associated them with the traditional system. Many researchers have classified the vegetation and ecological zones (Zerihun, 1999; MoA, 2000). General characteristic of the different zones are presented in Table 4. According
to MoA (2000) many of the classifications and characterizations are not
comprehensive and are discipline oriented. The current AEZ classification
(MoA, 2000) is based on the basic ecological elements of climate, physiography,
soils, vegetation, farming systems, etc. The intention of better characterization
is to suit the country’s diverse but unique natural and cultural
diversity. Current AEZs are based on temperature and moisture regimes.
Eighteen major AEZs are delineated and named by terms describing the broad
moisture and elevation conditions of areas (Box 1). A total of 49 agro-ecological
sub-zones are identified based on homogeneity in terms of climate, physiography,
soils, vegetation, land use, farming system and animal production (See
Figure 5). Box 1. The Current Major Agro-ecological Zones of Ethiopia No. Code Zone 1. A1 Hot to warm-arid lowland plains 2. A2 Tepid to cool arid mid highlands 3. SA 1 Hot to warm semi-arid lowlands 4. SA 2 Tepid to cool semi-arid mid highlands 5. SA 1 Hot to warm sub moist lowlands 6. SM 2 Tepid to cool sub moist mid highlands 7. SM 3 Cold to very cold sub-moist sub-afroalpine 8. M1 Hot to warm moist lowlands 9. M2 Tepid to cool moist mid highlands 10. M3 Cold to very cold sub-afroalpine to Afroalpine 11. SH 1 Hot to warm sub humid lowlands 12. SH 2 Tepid to cool sub humid mid highlands 13. H3 Cold to very cold sub-humid sub-afroalpine to Afroalpine 14. H1 Hot to warm humid lowlands 15. H2 Tepid to cool humid mid highlands 16. H3 Cold to very cold humid sub afroalpine to afroalpine 17. Ph 1 Hot to warm per-humid lowlands 18. Ph 2 Tepid to cool per-humid highlands Source: MoA, 2000
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5. Agro-ecological Zones of Ethiopia and Research Centres and Sub-centres Major
Agricultural Enterprises in the Different Agro-ecological Zones
The dominant agricultural enterprises in all agro-ecological zones are small-scale subsistence farms in the highlands and livestock rearing in the lowlands. Large enterprises (ex state farms) were government holdings which are being privatised. Current private investments are mainly in the agro-industrial sector especially on cash-crop and livestock production. Production systems in Ethiopia are as complex as the agro-ecological zones, and amplified further by the cultural diversity of people. General description of the major agricultural enterprises, crop-livestock and pastoral production enterprises are discussed below. Smallholder
Crop Production Small to Medium Scale Crop-Livestock Production. The most productive zones are between 3,200 and 1,500 metres highland, (‘dega’ ) and lowland (‘Woina dega’). In this agro-ecological zone a wide range of crops are grown and many species of livestock kept for different ends. Production systems are, in fact, of a mixed crop plus livestock type with draught power being important. Rainfall is generally not limiting except in the far north and growing seasons are often very long ,with two crops per year in some areas. Due to high population, farming is dominated by smallholdings. Medium–scale private crop production is beginning as a result of the recent state farms privatisation and the new investment policy. Medium or large scale dairying is found around big towns and cities. Small to Large-scale Livestock Production. In many agro-ecological zones at low altitudes 1,500-500 metres (kola-zone) growing seasons are short to very short, so only drought resistant crops can be grown, unless irrigation is possible. Livestock are important throughout this zone. The poor conditions for crops and the extensive system of livestock production imply low human population. There is large-scale ranching, particularly fattening for domestic and export markets; ELFORA Pvt. Ltd. Company (ex. Livestock/Meat Development Corporation) is one large-scale (commercial) livestock/Meat producing company operating here. The lowlands
are the home of a diverse array of pastoral people who depend on livestock,
which feed on native vegetation, and net productivity is very variable
over time and space. The lowlands are home to 29 ethnic groups, of which
more than 90 percent are pastoralists. Livestock provide subsistence and
employment for more than 10,000,000 people and are a source of meat, milk
and fibre for residents of some two dozen major towns and cities within
or adjacent to the lowlands. Subsistence nomadic and semi-nomadic pastoralists
are the major stockholders on the grazing land. Afar, Somali and Borana
are the major pastoral groups in the north eastern, eastern and southern
grazing lands. Production systems and stock management are described in
section 4 below. |
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Livestock feed resources in Ethiopia are mainly natural grazing and browse, crop residues, improved pasture, forage crops and agro-industrial by-products. As described in section 4, feeding systems include communal or private natural grazing and browsing, cut-and-carry feeding, hay and crop residues. At present, stock are fed almost entirely on natural pasture and crop residues. Grazing is on permanent grazing areas, fallow land and cropland after harvest. Forage availability and quality are not favourable year round and hence gains made in the wet season are totally or partially lost in the dry season. Table 5shows the feed resource balance of the country. Table 5. Estimated Feed Availability
to Livestock in Ethiopia At present, around dairy and fattening areas there is insignificant production of improved pasture and forages. The contribution of agro-industrial by-products is also minimal and restricted to some urban and peri-urban farms (dairying, poultry and fattening). In the past two decades, considerable efforts have been made to test the adaptability of pasture and forage crops to different agroecological zones; several useful forages have been selected for different zones. The medium and large-scale private enterprises could benefit from those findings. Natural
Pastures Grasslands are generally in regions of moderate precipitation, between 250 and 750 mm. Grasses in different parts of the country vary according to the altitude. Most grasses are used as forage and grasslands are usually for grazing, but also provide tall and strong grass for thatch. The grassland
region of Ethiopia accounts for some 30.5 percent of the area of the country
and is most extensive in the western, southern and south-eastern semi-arid
lowlands. On the more humid side, open grassland and grassland with some
trees are common; grasses may cover as much as 90 percent of the area.
In the drier parts patches of bush are common and the proportion of grass
is reduced to about 70 percent. Incense and honey harvesting are common.
Area and Productivity: Recent information on the area and productivity of natural pasture is scarce because of the expensive (in terms of time and money) nature of data collection. Previous estimates of areas and productivity are very variable. The total grazing and browsing land was estimated to be 61-65 million hectares (Alemayehu, 1998a), but it is changing due to increasing population and cropping. Productivity estimates also vary, probably due to variation in time and ecological change, rainfall, soil type and cropping intensity. The previous
estimate of natural pasture yield for the lowlands was one ton DM/ha while
for the highland and mid altitude on freely drained soils it was 3 tons
DM/ha, and, on seasonally water-logged fertile areas yields were about
4-6 tons DM/ha (Alemayehu, 1998a). MoA (1984) estimate was 1.5 and 0.56
tons DM/ha for the highland and lowland respectively. Another yield estimate
for different highland zones (MoA, 1989) was as follows: Species Composition. Natural grasslands constitute the main highland pastures. Besides grasses, they contain 28 Trifolium species out of which 8 are endemic (Kahurananga, 1986). The highlands have been divided into different altitude zones for the description of the grassland vegetation designated by the characteristics of the plants (Alemayehu,1985; Kahurananga, 1986). The proportion of legumes tends to increase with increasing altitude; particularly above 2,200 metres, there is a wide range of annual and perennial Trifolium spp., and annual Medicago spp. At lower altitudes native legumes are less abundant and commonly have a climbing or sprawling habit with a large variation in their range and density in wet bottomlands. This appears to be only partly due to edaphic differences. In the lowlands browse and shrubs are dominant plants. Areas
above 3,000 metres Areas
from 2,000 to 3,000 metres Areas
from 1,500 to 2,000 metres Areas
Between 1,500 to 500 metres Conditions
and Trends of Grazing-lands Water
Sources and Management Water for livestock and people is traditionally obtained from ephemeral ponds, perennial springs and rivers, seasonal streams and wells (Alemayehu, 1998b). Water supply in the Borana plateau is dominated by deep wells, which are less common in other areas. The different groups of Borana prefer to move animals to distant water sources in dry periods rather than invest a large effort in digging permanent wells. The Boran mostly use ponds in the rainy season and wells in dry periods. Ponds are easily accessed but are only available for short periods. Wells however, are unusually permanent water sources but require a large input of labour to lift it to the surface. Borana wells can broadly be grouped into shallow (‘adadi') and deep ('tula’). Wells are usually in groups of four to twenty. Adadi wells consist of a wide shaft dug into alluvium and can be up to 10 metres deep. The tula and crater (found in the bottom of volcanic craters) wells however, are usually much deeper and require massive excavation with shafts commonly sunk into rock. Adadi wells can be dug at any time and can be an opportune source of water. Tula and crater wells, in contrast, are old. It is often contended that another ethnic group dug them, possibly more than 500 years ago; if the Borana inherited the wells, they have had to adjust their original social system. At least until recently, new wells excavation has not been reported. The 'tula' wells comprise the most reliable source of water. They reportedly have similar discharge of water during dry and drought years and when watersheds receive lower than average rainfall. Tula wells are impressive feats of engineering. Animals and people enter the site by travelling down along a narrow ramp flanked by high earthen walls. Entry is regulated by a herder at the gate of a large storage basin, several metres above, which is a system of clay water troughs that water up to several dozen cattle or other stock at a time. A chain of 5 to 20 people stand on lashed wooden platforms, or rocky protrusions and pass water from the well with leather buckets (2-5 litre capacity). The whole water management task is physically intense and lifting begins early in the morning. The drinking area for animals is a large flat platform, some 5 to 10 metres below the ground and watering and exit of stock is orderly, supervised by a herder. Pasture
and Forage Crops |