GOVERNMENT OF ETHIOPIA WATER RESOURCES DEVELOPMENT AUTHORITY MASTER DRAINAGE PLAN FOR MELKA SADI AND AMIBARA AREAS o‘ z >1I 1 FINAL REPORT July 1985 Revised March 1986 VOLUME 2 MAIN REPORT Water Resources Development Authority P 0 Box 5673 Addis Ababa Ethiopia Sir William Halcrow & Partners Consulting Engineers Burderop Park Swindon Wiltshire SN4 ODD United KingdomMAIN REPORT 1. 2. THE STUDY AREA 2.1 Location 2.2 Topography 2.3 Climate and Hydrology 2.4 Geology and Hydrogeology 2.5 Soils and Soil Drainability 2.5.1 Characteristics and Distribution of Main Soil Types 2.5.2 Soil Drainability 2.6 Groundwater 2.7 Surface Waterlogging 2.8 Irrigation Systems 2.9 Drainage and Flood Protection 2.10 Current Land Use and Agricultural Production 2.10.1 Cotton 2.10.2 Bananas 2.10.3 Otner Crops 3. FUTURE WITHOUTDRAINAGE 3.1 Rise of Groundwater Tables 3.2 Surface Waterlogging 3.3 Secondary Salinisation * 4 5 $ 5 8 9 10 11 13 14 14 15 ie 18 203.4 Crop YicLd Decline 3.4.1 Method of Yield Evaluation 3.4.2 Cotton 3.4.3 Bananas 3.4.4 Other Crops 3.5 Land Use THE DRAINAGE MASTERPLAN 4.1 Introduction Page 21 21 23 25 26 27 30 30 4.2 The Development Options 31 4.3 The Drainage Masterplan 33 4.4 The Development Programme 38 4.5 Engineering Development Cost3 39 4.6 Guidelines for the Evaluation of Future Stages of Development -10 THE RECOMMENDED STAGE £ DEVELOPMENT 42 5.1 General Description 42 5.2 Detailed Features 43 5.3 Implementation Programme 45 5.4 Project Investment Costs and Phased Expenditure 47 5.5 Operation and Maintenance Costs 48 6. ORGANI5ATI0N AND MANAGEMENT, AND OPPORTUNITIES FOR AGRICULTURAL *9 IMPROVEMENTS 6.1 Implementation. Organisation 6.2 Operation and Maintenance 6.2.1 Irrigation Water Management 6.2.2 Operation and Maintenance of Drainage System 6.3 Opportunities for Agricultural Improvements *9 5C 50 50 51 6.3.1 Imoroved Water Management 52 6.3.2 Land Preparation 54 6.3.3 Crop Husbandry 55 (ii)7. INCREMENTAL PRODUCTION, MARKETING AND FINANCIAL RESULTS 7.1 Incremental Production 7.2 Marketing 7.2.1 Cotton Lint and Cotton Seed Meal 7.2.2 Fruit and Vegetables 7.2.3 Maize 7.2.4 Forestry Products 7.2.5 Milk and Meat 7.3 Financial Results Page No 5? 57 59 59 60 60 60 61 51 7.3.1 Melka Sadi Stage 1 Area 61 7.3.2 Amibara Stage 1 Area 62 7.3.3 Combined Stage 1 Area 63 8. BENEFITS AND JUSTIFICATION 8.1 Ceneral o 8.2 . Economic Evaluation . 8.2.1 Combined Stage 1 Areas 8.2.2 Melka Sadi and Amibara Stage 1 Areas 8.3 Discussion of Results REFERENCES APPENDICES TABLES FIGURES 64 64 34 65 65 67 68 (ill)APPENDICES APPENDIX A Index of Report Recommendations TABLES Table 1 Table 2 Table 3 Table 4 Table 5 Table b Table 7 Table 3 Table 9 Table 10 Table 11 Table 12 Table 13 Properties of Drainability Classes Land Use in the Study Area - 1984 Estimated Average Yield Expectations for the 1984 Cropping Season Cotton "ield Adjusted for Effect of 'Jacerlogging Summary of Cotton Yield Data from Random Sample Survey Fall in Cotton Production over next 20 years with no Remedial Action Projected Average Yields of Ocher Crops in the Settlement Scheme without Drainage Projected Land Use Without Drainage Project Investment Cost Estimates at 1984/85 Prices Decaileu Breakdown of Totai Project Investment Cost Estimates at 1984/85 Prices Project Investment Cost Estimate* at Current Prices Incremental Operations, Maintenance and Renewal Cost E* r -rma Summary of Project Investment CostsTABLES contd... Table 14 Table 15 Table 15A Table 16 Table 17 Table 18 Table 18a Table 18b Table 18C Table 19 Table 19a Table 19B Table 19C Revised Irrigation Schedules for Cotton Projected Incremental Production - Original Project Proposals Projected Incremental Production - Alternative Project Proposals in ASP Farmgate Prices used in Financial and Economic Evaluation Melka Sadi Stage I Area: Financial Analysis Amibara Stage I Area: Financial Analysis Amlbara Stage I Area: Financial Analysis (With Simplified Livestock Enterprise) Amibara Stage I Area: Financial Analysis (All Cotton in AS?) Amibara Stage I Area: Financial Analysis (50* Cotton, 25Z Maize, 25Z Pasture in ASP) Combined Stage I Areas: Financial Analysis Combined Stage I Areas: Financial Analysis (With Simplified Livestock Enterprise) Combined Stage I Areas: Financial Analysis (All Cotton in ASP) Combined Stage I Areas: Financial Analysis (50Z Cotton, 25Z Maize, 25Z Pasture in ASP)TABLES cor.td Table 20 Table 20a Table 20B Table 20C Table 21 Table 22 Table 22A Table 223 Table 22C Combined Stage I Areas: Economic Analysis Combined Stage I Areas: Economic Analysis (With Simplified Livestock Enterprise) Combined Stage I Areas: Economic Analysis (All Cotton in ASP) Combined Stage I Areas: Economic Analysis (50Z Cotton, 25Z Maize, 25X Pasture in ASP) Melka Sadi Stage I Area: Economic Analysis Amibara Stage I Area: Economic Analysis Amibara Stage L Area: Economic Analysis (With Simplified Livestock Enterprise) Amibara Stage I Area: Economic Analysis (ALL Cotton in ASP) Amibara Stage I Area: Economic Analysis (50Z Cotton, 25Z Maize, 25Z Pasture in ASP) (vi)FIGURES Figure I Figure 2 Figure 3 Figure 4 Figure 5 Figure 6 Figure 7 Figure 6 Study Area Location Master Drainage Plan Layout Master Drainage Plan - Indicative Development Programme Field Lateral Spacings for Stage I Areas Proposed Implementation Schedule for Stage I Melka Sadi Stage I Area - Surface and Subsurface Drainage Layout Amibara Stage I Area - Surface and Subsurface Drainage Layout Proposed Organisation for Site Supervision (vii)I. INTRODUCTION The Master Drainage Plan was commissioned by WRDA in May 1984 to provide an integrated plan for the eventual development of surface and subsurface drainage facilities for the Melka Sadi and Adibara areas of the Middle Awash Valley. Including the proposed Amibara Extension, the total gross irrigable area comprised some 17,000 ha. Tne initial identification phase of the study was completed in August 1984. For the purposes of further detailed field studies an immediate priority area of 3,800 ha gross was identified within which the groundwater tables were currently at or less than 3 tn depth and a further 4,100 ha with groundwater tables within 6 m. The detailed soils and drainability evaluation survey was concentrated mainly within the area identified as immediate priority. The initial studies also concluded that disposal of the surface and subsurface flows should be by gravity drainage, through the Angelele lands downstream of the study area and thence back into the Awash River. An alternative option of a combined gravity/ pumped scheme for drainage was evaluated but not favoured on cost grounds. At the conclusion of the field study phase (November 1984) a first Stage development area for subsurface drainage was defined comprising a total of 5200 ha gross within the Melka Sadi (including the Melka Sadi Banana Unit) and Amibara areas for which the immediate preparation of detailed design and tender documents were required. In the subsequent designs of this area the boundaries were extended to cover a gross area of 6200 ha. As the area requiring subsurface drainage extended northwards a further outfall into the Awash would be required, located in Angelele lands, some 12 km north of the study area. This second outfall could serve the future surface and subsurface drainage needs of the lower study area. The detailed tindings of the study are contained in the accompanying Annexes, and are summarised and discussed in this Main Report. The recommended development of the Stage I surface and subsurface drainage installation, with associated improvements to maximise returns, is used as the basis for economic and financial appraisals.1.1 General FeaCures The study area is shown on Figure I; it occupies a gross irrigable area estimated co be in the order of some 17,000 ha in the Melka Sadi and Amibara Plains. Irrigated development of the Amibara area commenced in the mid sixties with the establishment of the Melka Warer Research Station (300 ha). Further developments ensued in the lace sixties, initially under private concessionaires and subsequently, in 1975, under State Farms (1300 ha). The Awash Valley Authority (AVA) Settlement Farm was established in 1966 and had extended to approximately 1200 na by the mid seventies. The development of irrigated agriculture in Melka Sadi started in 1972 with the Melka Sadi Agricultural Estate Share Company (MAESCO) concessionary holding, where 1300 ha were irrigated, 900 ha of which were bananas. All irrigated areas used individual pumped warer supplies from the Awash River. Construction of the Amibara Irrigation project commenced in 1973, comprising che development of 7200 ha of new lands in tne Melka Sadi and Amibara areas and conversion co gravity supply of the Melka Sadi Banana Unit (formerly MAESCO), the Melka Warer Research Station and Che Awash Settlement Farm, giving a total area of 10,300 ha under gravity irrigation. Pumped irrigation continues in the remaining Amibara/Angelele State Farms, the total area under irrigation being about 12,000 ha. This will be increased to approximately 14,200 ha net area when the additional lands in the Amibara Extension Area are developed. Detailed designs for the implementation of this extension are currently being prepared and it is understood that imp Lenient at ion may be expected within the next five years. 1,2 lienci:ication oz Drainage Requirements The comprehensive survey of the Awash River Basin carried out by FaO between 1961 and 1965 (Ref 2) identified the Middle Awash Valley as a priority area for irrigated development. The feasibility study of the Melka Sadi - Amibara Irrigation Project complered m 1969 (Ref 3) concluded chat Che underlying aquifer possessed extremely Low permeaoilities and that the water cables in thearea could rise within 5-6 years after the onset of irrigation, with serious effects on yields. A system of deep open drains were incorporated into the feasibility designs. In 1973 the World Bank Appraisal Report of the Amibara Irrigation Project endorsed the need for subsurface drainage in the proposed project. HydropedologicaL studies were carried out in 1975 to determine the effect of intensive irrigation on water table levels and salinity, and the leaching practices required to maintain a favourable salt balance (Ref 4). This study reiterated the need for subsurface drainage. In 1975/76, hign water tables were reported in Melka Sadi, in areas where the irrigation of bananas had commenced four years earlier. Intermittent records obtained from observation wells installed during the earlier studies showed that groundwater had risen rapidly during this period. The more extensive coverage provided by the fifty observation wells installed by Amibara Irrigation Project in 1980 confirmed chat groundwater cables were rising throughout the project area. By 1981, 2700 ha of the project area had groundwater tables within 3 metres of the surface. A drainage and salinity study of Che Melka Sadi Banana Unit was carried out in 1981 to address the oroblems of yield loss and abandonment apparently caused by high groundwater tables. This study also provided outline coverage of the remainder of the Melka Sadi and Amibara areas. The report (Ret 5) provided outline subsurface drainage designs for the Melka Sadi Banana Unit and proposed a Pilot Drainage Project to verify drainage design and performance criteria, prior to the Large scale construction of drainage works. The Pilot Drainage Project was installed in 1983 and a draft final report on the drainage trials was presented in November 1984. This report provides quantitative results of .caching trials and on performance of subsurface drains under specific sice conditions. 3J * * V H n » i a a a a a i i i2. THE STUDY AREA 2.1 Location The Amibara and Melka Sadi areas are situated within the Ethiopian Rift in the Middle Awash Valley of East Central Ethiopia, at an altitude of approximately 740 m above sea level. The study area lies adjacent to the Awash-Mille Highway, with which it is connected by an all-weather road, and is 260 km by road from Addis Ababa. A meander of the Awash River effectively divides the study area into the Melka Sadi Plains (4900 ha gross) and the Amibara Plains (12,100 ha gross). The location of the study area is shown in Figure 1. 2.2 Topography The topography of the study area reflects the recent geomorphological history of the Middle Awash Valley, through which an extensive alluvial plain has been constructed by deposits from the Awash River. The present course of the river, which meanders extensively, is characterised by pronounced levee formations along the western boundary of the study area. In both the Melka Sadi and Amibara Plains, the overall slope is away from the river, generally along forme: flood paths of the river. Ground elevations range from approximately 745 m in the south to 725 m m the extreme north, descending gradually over a length of approximately 36 km. Gradients are generally very slight, predominantly lying in the range 0.05 co 1Z. To the east of the study area, the ground slopes gently away from the adjacent Aledeghi escarpment towards che north and north west, and a series of ill-defined drainage paths meander northwards through the study area towards th* Angelele plains. The suppressed relief of the study area is interrupted occasionally by volcanic cones, such as Dmile and Amibara Hill, which rise abruptly from the alluvial sequences of che flood plain. These provide evidenc of recent volcanic activity in che area. 42.3 Clunate and Hydrology The study area has a semi-arid climate with a bi-modal rainfall pattern giving a mean annual rainfall of 560 mm though rainfall varies considerably from year to year. Over 40Z of the annual rainfall usually occurs in July/August, with a further 30Z occurring during the period February/April. The 1 in 5 year maximum 24 hour rainfall is estimated to be 57 mm. * Mean monthly temperatures range from 22.5’C in December to 38.5*C in June and relative humidity values range from 5fiX in August to 36T in June. Wind runs are longest in June and July, exceeding 200 km/day. Annual sunshine hours are in excess of 3000. Annual potential evapotranspiration is estimated at 2400 rat. The Awash River has a pronounced seasonal regime, and flooding is a frequent event in the Middle Awash Valley during August and September. To the east of the study area lies an extensive but ill-defined catchment which extends towards the Aledeghi Plains. This catchment drains westwards towards the Awash River, and is characterised by short duration flood peaks resulting from storm rainfall □ver the Alede ghi Pl ains. Dykes have therefore been constructed to protect the irrigated area from inundation by floods originating from the Awash River in the west and also from the Eastern Catchment. Flood flow estimation for rhe Awash River and the Eastern Catchmenc flood dykes yielded the following resuLts: Return Period (years) Flood Peak (m^/sec) 10 20 25 50 Awash River 757 1012 - 1465 Eastern Catchment 94 • 128 - For the Awash River these flood estimates are based on the flows at Awash Station, transposed to the Melka Sadi diversion weir sice witr»o»*r, enhancement or reduction. Downstream of this point the natural attenuation resulting from flood routing in the river course and adjacent floodways has been determined from a hydraulic model analysis. Flows from the Eastern Catchmenc are Likely to be derived from part rather man the whoLe catchment at any one time due co the 6extensive nature of the catchment and to the short duration convective characteristics of storm rainfall in the area. The flood flow estimates for the catchment can be taken to apply *t all points along the dyke downstream of the first major tributary in the Melka Sadi area. Details of the climate and hydrology of the study area are given in Annex C. 2.4 Geology and Hydrogeology The study area is bounded on its north western side by the volcanic peaks of Dofan and Ehailu and on the south eastern side by a northerly trending fault scarp which delineates the edge of the Aledeghi Plain. The flood plain comprises a complex sequence of silts, sandy silts and clays which have been laid in places to depths exceeding 100 m. Towards the edges cf the plain the infill grades into gravels and hillwash. Beyond the fault scarp lie the lava and gravel sequences of the Aledeghi. A number of basaltic and cinder cone intrusions through the alluvial layer indicate recent volcanic activity. Groundwater exists xn all underlying formations although the consistently fine grained sedimentary materials exhibit low permeabilities and water can only be extracted where boreholes penetrate the gravels, or fractured or jointed volcanics. The feasibility study of the Melka Sadi-Amibara area (Italconsult 1969). concluded that the flood plain aquifer, with horizontal permeabilities of 6 10~ m/d»y, v«s essentially without flow. (Ref 3). 2.5 SoiLs and Soil Drainability Characteristics and Distribution of Main Soil Types The study area consists almost entirely of alluvial sediments which exhibit marked variation with depth as well as with location. The soils normally have a high silt content, the general range of textures being from clay, through silty clay loam to silt loam, while sandy loam, loamy sands and fine sand also occur. 6Soil textures reflect the geomorphology with Che coarse soils occurring in the Levees and the finer textured soils in the back-swamps. From an examination of previous studies of 350 soil profiles during the study and a detailed review the following main soil types were identified and mapped. V : Deep clay soils, ie soils with at least 200 cm of clay or silty clay at the surtace. The clays are often cracked when dry, they are classified as Vertisols. (3150 ha) : (incl Soils with appreciable amounts of clay in Che surface layers. Although fine textured material is dominant in this group, silt loam or silty clay loam also is present in a significant part of the profile. (5770 ha) M : Soils with mixed or medium textures. These are stratified materials in which the surface layers consist mainly of silty clay loam and silt learn. Silty clay or clay generally is found at a depth of 200 - 350 cm. (66^0 ha) C : Relatively coarse textured soils. These soils are dominated by silt loam and sandy loam. Some layers of sand or loamy sand are common. Clay or silty clay is often found between 250 and uOO cm, but in several profiles no clay occurred within 5 m of the surface. (2650 ha) Relatively minor soil units are the rock outcrops (R), areas with weathered tuff material (T) and the recent alluvium along the Awash River. (Total 1.700 ha). The total mapped area of the soil survey extends outside the gross irrigable area boundaries and amounts to an estimated gross of 19,910 ha. During feasibility soil studies of the Melka Sadi - Amibara area conducted in 1969-197! by Italconsult, localised areas of saline and alkali soils were identified but were largely excluded from the subsequent irrigation developments. The terrace soils .mediately soutn east of the currently 7developed area are in this category, and clearly exhibit features of salinity and/or alkalinity. It appears that the mapping of saline soils during these early studies was based on morphological features rather than on the results of chemical analysis, and the extent of salinity was underestimated. Since irrigation commenced, the level of salinity and the effects on cropping have increased considerably in certain areas, despite the irrigation water being of relatively good quality. This is largely Che result of secondary salinisation. In the southern part of the Melka Sadi immediate priority area, soil salinity is now widespread, but is almost absent in the north. The general levels of salinity in the Amibara area are considerably lower than those in the Melka Sadi area. In both, the detailed distribution of soil salinity is highly complex, with very saline soils occurring close to non-saline soils. A detailed description of the Soils and Drainability Classes is given in Annex Al, Volume 3. The Soils and Drainability Class Maps are given in Annex A2, Volume 4 and the Description of Auger Bores is given in Annex A3, Volume 5. 2.5.2 Soil Drainabilicy Drainability classes have been established on the basis of: the depth to relatively impermeable layers, the texture and hydraulic conductivity of the soil above the relatively impermeable layer (the ’’control section'1 2). Design hydraulic conductivity values were selected after thorough review of the results of field tests both for the present study and previous studies. Considerable attention was also paid to results derived from the 35 ha Pilot Drainage Scheme trials, which are reported separately D. Review methods included correlating soil textures with K values (for both pour-in and pump-out methods), and calculation of weighted K values. The results from both analyses were compared with values reported by FAO The design K values were selected 1) Amibara Irrigation Project II. Melka Sadi Pilot Drainage Scheme. Draft Final Report. Halcrow, 1984. 2) FAO Soils Bulletin No 42. Soil Survey Investigations for Irrigation. 8based on detailed knowledge of the specific site conditions, and having taken all available information into account. The resultant drainability classes are shown on Table I. 2.6 Groundwater Groundwater measurements have been carried out in the Melka Sadi - Anibara area on an intermittent basis since 1970, and the available drilling records show that all formations in the Awash River flood plain are water bearing. More recently, routine monitoring including measurements of the electrical conductivity of groundwater, has been carried out on the network of observation wells constructed in 1979/80 for the Amibara Irrigation Project. Analysis of the available ooservation well data has shown that since irrigation commenced, an overall rise in groundwater levels has taken place and is being sustained, the rate of rise being in the order of 1 metre per year in the irrigated areas. This effect is particularly evident in records of early Italconsult observation wells situated in the Melka Sadi area, which show that groundwater levels began to rise very soon after the installation of early pumped irrigation schemes. Such rises in the groundwater table accoro with the predictions of earlier studies which concluded chat the outflow potential from the underlying aquifers was very Limited. Earlier mapping of groundwater contours (Italconsu1c, Ref 3 and 6) showed a dominant south to north trough in the groundwater table with Lateral recharge from the Aledeghi Plains and from tne Awash river. Current observations indicate chat the trough feature in the Melka Sadi area has been largely infilled by the rising groundwater. In .Amibara rhe trough is retained aLong rhe eastern edge of the plain where groundwater depths are still in excess of 10 m below ground, with steep hydraulic gradients from the higher water cables in the western sections of Ar^bara which are within 3 m of the surface. Earlier studies also reported the existence of a perched water cable in the Melka Sadi area separated from the deeper groundwater by an extensive impermeable layer or varying thickness. Detailed fieldwork concucted during rhe 9current study has shown that a continuous relatively impermeable Layer seems unlikely to exist, and that the perched water tables are discontinuous rather than extensive features. These more recent findings are consistent with the existence of localised conditions of partial confinement in the fine grained alluvial sequence underlying Melka Sadi, in which the groundwaters are in direct hydraulic contact. In order to determine the required extent of the detailed soil and drainability evaluation survey co be carried out within this study a 3 metre depth to groundwater contour was selected as forming the boundary to areas requiring such immediate survey work. These were designated as immediate priority areas and covered some 2247 ha in Melka Sadi and 1597 ha in Amibara, totalling 3844 ha gross. Similarly the 6 m depth co groundwater contour, initially defined as priority within the next five years, enclosed areas of 4093 ha in Melka Sadi and 3897 ha in Amibara totalling 7990 ha, including these areas enclosed within the 3 m depth contour. Subsequent refinement to the projections of groundwater rise (Section 3.1) together with further information provided by the field survey indicated that currently the groundwater is estimated co nave reached a level of within 1 metre of ground surface in some 2000 ha in Melka Sadi and 500 ha in Amibara. Furthermore it is estimated chat by 1988/89, which would be the earliest expected date of completing an initial stage of subsurface drainage installation, the areas within which the groundwater could be within 1 metre of surface would extend co some 2800 ha in Melka Sadi and 2400 ha in Amibara, totalling 5,200 ha gross (Section 4.4). 2. 7 Surface Waterlogging In addition to the effect of high groundwater tables, temporary saturation of the rootzone results from surface waterlogging caused by: low porosity of the soil (an inherent condition) the persistence of saturated conditions close to the soil surface following irrigation, due to compact layers - maldistribution of water 10Approximately 20Z of the area considered to be in need of remedial drainage is occupied by silty clay and otherwise compact and Sine-textured soils. The porosity of these soils is so low chat following irrigation saturated conditions remain sufficiently Long to affect crop growth adversely. Stratified soils occupy a substantial part of the remainder, and che majority of these also have similar compact layers. There is Che likelihood that in some fields, machinery is compacting soil which is too moist, during cultivation and planting operac ions . Maldistribution of water results largely from variations in microtopography, with serious waterlogging occurring in the hollows. Moisture stress, and in some cases salinity, may occur on the nigh specs and on very steep slopes. Poor ploughing and land-planing may be contributing to possible subsidence of areas 'filled' during grading of slopes. 2.8 Irrigation Systems Seme 12,000 ha net are currently under irrigation in che study area of which 7300 ha lie in Che Melka Sadi and Melka Water State Farms of the Amibara Irrigation Project and 3000 na in the Melka Sadi Banana Unit, the Melka Warer Research Station and the Amibara Settlement Farm all of which are served by gravity through the Al? main canal. The remaining 1700 ha comprise the Amibara State Farms Units 1, 2 and 3, Algeta and Axabash and the Angelele Units 1 (Subelele), 2 and 3 all of which are irrigated by pumping directly from che Awash. Furrow irrigation is used on the new State Farms within AIP. Furrow lengths are typically 200-250 m with furrow slopes of 3.05Z co 0.3Z. Extensive land levelling was carried out during che project implementation with up co 500 m3 per hectare being moved in places. Resulting settlement in fill areas combined with agricultural operations has led co irregularities along furrows which adversely affects the uniformity of irrigation applications. The subsequent limited land planing operations hav*- not achieved the required uniformity of grade and further land planing operations will be required. 11Water is supplied to the furrows by syphons. Recommended application times, methods and irrigation intervals are described in the Water Management Manual (Ref 7). Annual water budgets and irrigation schedules are prepared jointly by the Project Control Centre and the State Farm Units. Flow measurement, using constant head orifice structures, if effected at primary canal offtakes. However, few facilities exist for the accurate measurement and distribution of water in the tertiary and field canal systems and some non-uniform.ty in distribution is inherent as a result of this. Actual irrigation schedules, application times and amounts have varied appreciably from those recommended. Field irrigators do not adhere to the recommended furrow streams nor to their stipulated durations although, as noted above, such deviations are also highly related to irregularities in microtopography. In the Amibara Settlement Farm and the Amibara/Angelele State Farms a combined furrow/basin method of irrigation is practised, the basin effectively shortening the furrow runs to between 50 and 100 m. Land levelling has not been carried out on these areas and field slopes are irregular with resultant non uniformity in water application. Basin irrigation is practised on bananas in the Melka Sadi Banana Unit under a designated field irrigation application regime of 100 mm every 15 days. The actual regime shows large variation in interval and application amounts are not recorded. During 1981 and 1982 no irrigations were carried out during March and April with Ebe main canal being closed for maintenance. Neither were any requisitions made fcr water during the month of August for both years. Apparent Large deficits in actual irrigations compared co net computed irrigation water requirements resulted in these years with a smaller deficit being estimated for 1983 wnen irrigation was continuous (Annex C). In practice the banana roots would have recovered the bulk of this deficit from high water tables and conversely waterlogging would have been exacerbated under an application regime appropriate to the estimated crop water requirements. The above described shortfalls in irrigation methods, non-uniformity of land slopes and low infiltration races impose constraints on the production levels which can be obtained even after subsurface drainage installation. The 12importance of achieving improvements in all tnese aspects in order to realise the potential value of subsurface drainage cannot be over-emphasised. 2.9 Drainage and Flood Protection The surface drainage system for the Amibara Irrigation Project was constructed to convey field runoff from excess irrigation or rainfall, together with irrigation rejection flows, back into the Awash River through a gravity flap outfall structure at the downstream end of the primary drain. Under high river levels the outfall remains closed and the excess flows pass over a rejection spillway into the uncultivated lands of Che Amibara Extension area. This drainage system has, in general, performed satisfactorily since its construct ion. A less formal system of surface drainage exists within the Melka Sadi 3anana Unit, constructed primarily to accept irrigation canal rejection flows. This system leads into the head of the AIP primary drain. No surface drainage facilities exist within the Melka Harer Research Station, the Amibara Settlement Farm and Che older Amibara and Angeleie State Farms and all excess flows, including canal rejections, are retained within their individual boundaries. The Awash (Western) flood dyke runs along Che entire western perimeter of the study area. The degree of protection afforded by this dyke against river floods is variable and it requires realignment and raising in places, particularly in the vicinity of the old State Farms in Amibara. The Eastern Catchment dyke and drain run along the eastern perimeter of the Amibara Irrigation Project and divert runoff from the ALedegni catchment northwards taco the Amibara Extension Area. Since its completion in I960 this dyke has teen subject to two severe flood events, one of which induced a series of breaches in the Amibara area. These were repaired and the dyke heightened Locally such Chat it is considered to be adequate against Che proposed design flood. Some minor spoil heaps, constituting obstructions, exist in the floodway and should be removed. Also some limited reaches of the drain itself should be 13realigned where currently too close to the dyke. These minor works could form part of the ongoing operation and maintenance activities. 2.10 Current Land Use and Agricultural Production Information on land use was obtained through interviews with official representatives of the various organisations involved; the current land use in the study area is summarised in Table 2. Estimated yield expectations for the 1984 cropping season are given in Table 3. 2.1C.1 Cotton Cotton is the predominant crop, with the area planted in the 1984 season exceeding 9800 ha. The net area of cotton land which had been abandoned by that season is estimated to be 125 ha, all located near to Melka Sadi village. The cotton yields, estimated in Table 3, are of planted area only but have been reduced from the estimated total yield Dy 10X co allow for loss of crop during harvesting and of standing crop due to livestock damage late in the season. There have been marked improvements in cotton husbandry in the 1984 season. Almost the whole crop was pre-irrigated, as a result of which germination and plant populations were satisfactory, and with the exception of areas seriously affected by waterlogging, the weed control was adequate. The planting period was slightly shorter and more of the crop was planted in the optimal period between mid-May and mid-Juue. There is some evidence that pink bollworm was not completely controlled in the early season in some areas and in lace season aphids and mites had reached levels which probably would make their control economic. The 1984 mite infestation was unpredicced at Amibara, and in those areas where boll splitting was delayed, will have caused measurable yield loss. The highest yields are expected at Melka Sadi and the lowest on the State Farms on che compact fine-textured soils at Angelele. The crop at the Settlement Scheme was noticeably poor due co excessive waterlogging and weed competition. 14Total production of seed cotton in the 1984/85 season is likely to be about 32,800 t, plus the small amount produced by LAR. 2.10.2 Bananas Much of the area within the Banana Unit which was originaLly designated for and planted with banana has been abandoned. A contributory factor to this has been the level of the watertable but reportedly the problems were aggravated in the dry season of 1983/84 by livestock damage. It is estimated that only 238 ha of bananas are currently productive and a further 100 ha approximately are expected to have been replanted by the end of the year. Being a forest speci.es originating from a humid tropical area, climatic conditions at Amibara are not ideal for the production of bananas. The species is sensitive to moisture stress, salinity and sodicity, is susceptibLe to wind damage and unsuited to compact fine textured soils. Despite these inherent disadvantages the returns from the potential yield level chat can be achieved, projected at 16 connes/ha. is such as co warrant Che continuation of this crop. However the present yield level is well below potential because of the poor water management, drainage and salinity factors. The average banana yield is difficult co estimate and the figures given in Table 3 take account of the area of replanted bananas which have yet to come into production. It is fait chat rhe maximum yield, two or three years after planting, is 15 t/ha bue the yield declines rapidly subsequently. A number of elements of husbandry contribute to the apparent lack of vigour. Ac present there appears to be no organised enact management; non-vigorous mates are tailing to regenerate and subsequent weed infestation hastens the decline of the plantation. Only the most vigorous and newly planted fields appear co benefit from fertiliser application; productivity in Che poorer fields is unlikely to justify the use of fertilisers. Infestation by banana weevil and nematodes was reported co be a major problem and the rapid decline in vigour is consistent with a serious level of mfes tat ion.Fields require to be replanted a: present in a four or five year cycle. This contrasts with the normal eight to ten years and is indicative of the general lack of vigour. In addition it was apparent chat the soil texture in some parts of the plantation is the Least desirable for this crop, compact silty clay soils normally being avoided for irrigated banana cultivation. Total banana production for 1984/85 is estimated at about 1800 t, but will depend on whether or not the recently planted areas fruit in this period. 2.10.3 Ocher Crops There are small areas of pasture on land formerly under bananas, and a larger area is being established at the Amibara Settlement Project (ASP). If the RRC objectives for the ASP are achieved then there will be soae 311 ha of planted and irrigated pasture by the end of 1984. The IAR has an experimental area of pasture totalling some 55 ha. The productivity of pasture is low for an irrigated crop; it is often of mixed, Largely self-sown species, the irrigation regime is incorrect and there is a lack of fertiliser application. In contrast the grass along the canals is generally vigorous, productive and of high feed value. Fodder is being baled for the first time, and the figures in Table 3 represent fodder conserved from all sources. The remaining crops within the Master Drainage Plan area in 1984 included some 28 ha of assorted experimental plantings at the IAR and an area of some 100 ha of maize at the Amibara Settlement Project. The maize was of very low plant population and was seriously moisture-stressed when inspected. The seed quality may have been indifferent but failure to maintain the required irrigation schedule would be a reason for the poor stand. The nasins were well-constructed and cne cropped been well interrow cultivated mechanically. The reason for the failure to weed the rows by hand ar.d to irrigate on schedule was reported co be insufficient labour. Such a crop would not justify the application of fertiliser. 16Sheep are fattened on the abandoned fields of the banana plantation. The sheep are purchased locally, kept for one to two months during which they are fattened to a minimum of 24 kg liveweight and re-sold, often for export to the Middle East. On the land area available this is equivalent to a throughout of up to 6 lots of 5 sheep per ha each year.3. FUTURE WITHOUT DRAINAGE 3.1 Rise of Groundwater Tables Examination of historic observation well records has shown that groundwater is rising within the project area at a rate of approximately 1 metre per year. This generalised raze of rise appears to be sustained until the groundwater reaches a depth of about 1.5 metres below soil surface, after which the rate ox rise decreases. Because of the limited records which are currently available for observation wells at which groundwater is within a depth of 1.5 metres, it is difficult to predict with accuracy Che rate of rise above this depth and the terminal average equilibrium position of the watertable. Analysis of the limited records available does however indicate that above a depth of 1.5 metres, the generalised rate of rise is in the order of 0.3 metres per year, and the terminal average equilibrium position may be in the range of 0.75 to 1.0 metres. The implication of these observations is that m time, watertables will rise over the whole of the project area to reach a final equilibrium position close to the soil surface, about which short-term fluctuations will occur. A knowledge of the timescale in which this can be expected is essential for implementation phasing, and Che methodology used for predicting changes in groundwater depth with time is discussed in detail in Annex B, Section 2.7. The result of these predictions shows that groundwater will have risen to within 1 metre over all of the Melka Sadi area and approximately half of the Amibara area within 14 years, if drainage is not provided. These longer term predictions must be viewed in the context of the relatively limited period of observations on which they are based. Further trends may emerge from a longer observation period. The proposed irrigated developments in Che Amibara Extension area could also affect the race of rise and bring forward the onset of high waturiables over the remaining part of Amibara. The above observations of groundwater rise have confirmed the predictions chat che natural drainage characteristics of the underlying aquifer are unable to cope with the recharge resulting from irrigation and this factor is accordingly 15identified as the prime cause of the high water tables. Studies of irrigation practices indicate that although there is much scope for improvements in the distribution and application of irrigation water, the contribution to groundwater, even from efficient surface irrigation techniques, will continue to be in excess of the naturaL drainage capacity of the aquifer. Estimates of the contribution to groundwater from irrigation indicate that the recharge level may be in the order of 200 mm/year (Annex C). In view of the low porosity of the soils such a level of recharge would be expected to induce a rate of rise of groundwater in excess of the observed 1 metre per year. It is thus possible that rates of rise have not yet stabilised in that lateral drainage into areas not yet irrigated may be effectively reducing the potential race. In this event the rate could be expected to increase as the irrigated area expands. An appreciable leveL of aquifer drainage out of the area could also explain the lower rate of rise; this latter alternative would appear from previous reports to oe unlikely. It is therefore concluded that the possibility of an increase in the rate of rise as the irrigated area expands must be anticipated. 3.2 Surface Waterlogging The existence of perched watertaoles has been noted during current detailed soil survey fieldwork. Although areas in which perched conditions have beer, observed appear co conform generally with areas affected by high watertables (the groundwater is believed to be in hydraulic contact regardless of geological formation), this is not necessarily the case. Furthermore, well records do not reflect perched conditions, and therefore no attempt has been made to predict the development of perched conditions on a time-related basis. Where they do occur, their implications in terms of salinisation are potentially serious, and will further shorten the time scale within which the need for drainage is envisaged. 193.3 Secondary Salinisation Routine monitoring of observation wells has included measurements of groundwater salinity, and although the records are insufficient for sophisticated predictive purposes, maps of indicative groundwater salinity contours have been prepared (Annex B, Section 2.4.2). These show that in certain areas the groundwater is of significant salinity. Ignoring the systematic effects of introducing additional salts into the groundwater through irrigation, ana assuming that the present levels of groundwater salinity will remain relatively unchanged as groundwater levels continue to rise, the implications are nevertheless serious. Once the critical depth for capillary rise has been reached, salts will accumulate in the soil profile during the fallow period through the process of secondary salinisation. The magnitude of secondary salinisation and race at which it takes place is dependent upon a number of factors, the more important of which are the depth of groundwater and its salinity, the evaporation rate at the soil surface, and the soil texture. A theoretical model has beer, developed to estimate the magnitude of salinisation which takes place during the fallow for use in evaluation of the recommended project, and is discussed in detail in Annex 3, Appendix C. This shows that at a terminal equilibrium watertable depth of 0.75 m and salinity 30 mScrn *, the EC of the plough layer (regarded as the top 20 cm of the soil - e profile) can be expected to increase by some 100 mScm“- during the fallow, for an alluvial soil. For a watercable of salinity 10 mScm”^ at the same depth, the corresponding increase in salinity would be approximately 30 mScm*^. The implication of this predicted increase is important in assessing the likely future situation without drainage, because a threshold is reached beyond which salinisation of the plough Layer is so severe chat germination cannot take place even following preplanting leaching applications. Continuation of the cyclic process of secondary salinisation during fallow periods followed by Leaching during the intervening cropping seasons once the terminal average equilibrium position of the wacertable has been reached will result initially in yield decline followed eventually by yield collapse and abandonment. At this point the secondary salinisation process is irreversible unless drainage is installed. The time scale and magnitude of yield decline is 201 discussed in detail with reference to vertisols and alluvial soils in Annex E. The results show that in the case of cotton, a watertable within 1 metre of soil surface and of salinity 5-10 mScm* is likely to result in yield collapse within 1 year; if the watertable is of low salinity (<2 mScm"^), yield collapse can be expected within 7 years. As watertables continue to rise, the areas considered to be at greatest risk of rapid yield decline are those in which the soils are predominantly fine-grained, which currently have moderate to high salinity levels in the subsoil, and which are underlain by watertables of high salinity. 3.4 Crop Yield Decline Waterlogging and salinity are causing a decline in yields of all crops grown in the project area, and without remedial action this will ultimately lead to total crop failure. 3.4.1 Me.hod of Yield Evaluation In order co provide a basis for the projection of yields both with and without remedial action a programme of field investigations was carried out on sample plots of bananas and cotton. The objective of these investigations was co quantify the effects on crop yields of salinity and waterlogging respectively in the root zone. The approach used is described m detail in Annex E, Section 2, and summarised below. A total of 54 yield sample pLocs were established within the cotton crop. Assessments were made of the morphological characteristics of the crop which are most affected by waterlogging and salinity. Both of these conditions tend co produce a plant shorter chan normal in stature. The waterlogged crop early in the season becomes characterised by yellow and red foliage, is weaker yet is strikingly precocious in flowering and boll splitting. The salinity affected crop is sturdy, lark green and somewhat delayed in flowering and boll splitting. All plots were therefore scored in terms of plant height, leaf redness (Class - no redness to Class 5 - 30X of leaves are reddened), lea: yellowing (Class 1 - dark green to Class 5 - pale green or yellow), leaf necrosis (Class 1 - nil to 21Class 5 - severe) and crop vigour (Class 1 - best to Class 5 - worst). The number of bolls was recorded and average boll weight measured at harvest. Accurate estimation of banana yield is more difficult, but plots within a radius of about 5 m from a selected sample point were assessed for average height of mature pseudostem and scored for vigour (on a scale of 1 to 10, with I best). The average number of hands per bunch was estimated from a sample of about 10 bunches. Visual scores were made of plant population (on a scale of 1 to 5, with 1 highest) and the yellowness of leaves (on a scale of 1 co 5, with 5 most ye 1 Low). Taking into account the above observations, an overall assessment of yield was made by scoring the site on a scale of I to 10, with 1 best. Based on present annual production data, a score of 1 may be taken to correspond to a yield of lBc/ha and a score of 10 to zero yield. Each unit change in score therefore corresponds co an increment in annual yield of 2t/ha. □n 32 cotton and 5 banana yield sample plots assessments were made of moisture conditions in the soils for ten days after irrigation. The moisture profile was described in terms of a Waterlogging Index which recognises the greater activity of roots m the surface horizons bv weighting the contribution to waterlogging of successive soil depths according co the following options: Horizon depth (cm) Weighting factors (Z) 0-25 25-50 50-75 75-100 100-125 125-150 150 Cotton 50 30 10 5 3 2 0 Banana 5 10 35 50 0 0 0 The Waterlogging Index (WI) is calculated on the assumption that rooting depth is not limited to less than 150 cm by any other feature than soil saturation. A very compact and generally saline nori2on was observed in the root zone of a feu cotton plots. In order to achieve a closer relationship between yield of cotton and the Waterlogging Index it was necessary Co treat the presence of any such rooting barrier as a notional watertable. The adjusted index is called the Rooting Index and is identical to the WI in the majority of plots. 22Similarly a Salinity Index was determined at each plot based on measurement of electrical conductivity. The index again took account of the diminishing effect of salinity on yield with depth by weighting successive horizons as above. The data from the yield sample plots was supplemented by a rapid survey of 145 random sample points. Each point was characterised in terras of its salinity index, waterlogging, chemical infertility and estimated yield. 3.4.2 Cocton Waterlogging and salinity are the primary factors responsible for declining cotton yields; perched water tables and groundwater tables both contribute to this. To date surface waterlogging and its associated salinisation have been the predominant problem but there is evidence that this is to some extent stabilising. The influence of high groundwater tables and their effect on soil salinity continues co increase'and will become the major cause of yield Loss and ultimate crop failure. An analysis of the effect on yield of waterlogging as measured by the WacerLogging Index has shown Chat in a sample of 39 plots actual mean estimated yield is 33 q/ha compared with a potential mean yield of -*6 q/ha (Table 4) had there been no waterlogging. On the basis of the random sample survey over 70S of the area was judged to be affected by waterlogging sufficiently to reduce its yield from an attainable potential of 55 q/ha co 38.8 q/'ha. Salinity was judged to affect only 12Z of the area but had a greater effect on yield with a mean yield in salt-affected plots of 34.6 q/ha. The respective effects of waterlogging, salinity and soil infertility, as assessed in the Random Sample Survey, are shown in Table 5. This indicates char of a total shortfall of potential production of over 13000 t of seed cotton, nearly 80Z is attributable to waterlogging effects. 23z. •* The influence of waterlogging and salinity is always irregularly distributed within a field so that there is not a unifora decline of crop vigour but rather the development of isolated patches of crop deterioration or germination failure. As these patches become more extensive, the point is reached at wu^ch it is no longer judged worthwhile to cultivate the field. This point has been aesignated the ’’Schedule Year”; the rate of build-up to this, and the further decline after thLS are shown below. Year Relative co Schedule Year(s) - 3 - 2 - 1 S ♦ 1 * 2 ♦ 3 ’ Z of Area Affected 5 15 30 70 85 95 100 | The occurrence of the Schedule Year is dependent on the depth of the groundwater table and its salinity. The estimated number of years before the Schedule Year crop failure occurs from the time at which groundwater of different levels of salinity reaches a specified mean annual depth is shown below. I Annual Average ) Depth of Watercable I (m) | Watertable Salinity (£Cwt in mScm~^) | 0-4 4-8 8-12 12-16 16-20 20-32 32-48 | <----------------------------- years to Schedule Year-------------------------------------------> I 2.0 1.5 1 16 1 15 12 11 9 8 5 4 2 1 2 I 2 0 1.0 1 14 1 10 7 3 0 0 0Sven prior to rhe effective crop failure in the Schedule Year, there is a substantial yield decline once the annual average depth of groundwater comes within 1 b, the extent of this depending on the salinity of the groundwater as detailed below. 1 1 1 Years Before Schedule Year 1 | 1 1 0-4 EC Groundwater (mScm-1) 1 I I 4-8 8-12 12 - 16 II or yield———————— 1 1 1 1 1 1 28 28 33 38 1 2 1 28 28 28 33 I 3 1 1 28 28 28 Based on current knowledge of the levels, movement and salinity of groundwater tables in the project area and the effect of these on crop yield, the fall in production of cotton over rhe next 20 years if no remedial action is taken, is shown in Table 6. 3.4.3 Bananas High uacertaoles have prevailed in the banana areas for a considerable time, such levels having been first reported in the aid-seventies. With the large ratio of abandoned to cultivated land it appears char an equilibrium has been reached whereby an apparently inadequate irrigation application is compensated to some extent by the crop abstracting from high watertables. At the same tine there is Little overall rise in the warertable as lateral movement rakes place from irrigated to non-irrigated Land and evaporation takes place over the total area of productive and abandoned land.Yield estimates indicate that without drainage, the production of bananas is likely to be maintained at about 10 t/ha. There is little possibility of improvement without drainage as any attempts to do so could upset the equilibrium postulated above Leading to further abandonment of land. Improved agronomic practices are unlikely to have any effect, unless these are done in conjunction with an improved irrigation and wacertable regime. 3.4.4 Other Crops Limited areas of maize and pasture are cultivated within the study area and there are small garden plots producing mixed vegetables. Plans have also been proposed by the RRC to develop fast growing timber species as a source of firewood and building materials. Similar considerations apply to declining yield for these crops as for those described above for cotton. However, the estimated number of years before the schedule year crop failure following the rise of groundwater table differs substantially from the estimates for cotton as is shown below. It will be noted that at even moderate salinity leveLs crop failure will occur in maize as soon as the water table is within 1.5 m. 1 1 Crop 1 Annual Average Depth of Wacertable Salinity (EC in mS cm*^) vc I 1 Wacertable 1 0-4 4-8 8-12 12-16 16-20 20-32 32-48 | 1 Cm) I <—- —veai rs to S ch< idule Year -------- > 1 1 ; Maize 1 1 2.0 1 1 3 An. 1 0 0 0 1 0 I 1 1 1.5 1 2 0 0 0 0 0 0 1 1 1 2 0 0 0 0 0 0 I 1 11 11 1.0 1 11 11 Pasture 2.0 1 3 3 2 2 1 1 0 [ 1.5 1 2 2 2 4i 1 0 0 1 1 1 1.0 1 2 1 1 0 0 0 0 0 I 1 26This same heightened effect of rising groundwater tabLe on yield is also noted in che predicted yields before the schedule year once the groundwater table comes within 1 m. 1 1 1 Years Before 1 0 - 4 EC Groundwater (mScm“l) Crop 4-8 8 - 12 1 12-16 : 1 I Schedule Year I <-- ------------------ Perc entage Loss of Yield— --------------- > | 1 Maize 1 1 20 100 100 100 1 1 2 1 15 100 100 LOO 1 1 3 1 10 100 100 100 1 1 4 1 5 100 LOO LOO 1 1 1i i1 I Pasture | I 1 20 25 30 35 1 1 2 15 20 25 30 1 1 3 1 io 15 20 25 1 1 4 1 5 10 15 20 1 5 1 o 5 10 15 The overall projections of yields for maize, pasture, garden crops and firewood in the resettlement area without the intervention of drainage are shown in Table 7 3.5 Land Use Without the introduction of drainage there will inevitably occur a change in land use leading to a large extent to the abandonment of cropping or reversion to rough grazmg. The declared policy of the Middle Awash Agricultural Development Enterprise is to develop and maintain a total cultivated area of some 450 ha >f banana. This represents about one third of the area within che banana unit and it would appear likely that such ar. area could be sustained provideG that the postulated equilibrium is not upset by any marked changes in the irrigation regime or by attempts to utilise abandoned lands. Even at its present low productivity 27levels, banana remains a profitable crop and there would seem little reason to. attempt a change to another crop under the present circumstances. As noted earlier it is unlikely under the present limited area cultivated, and with the apparant deficit in actual irrigated amounts, that the removal of bananas would significantly reduce the rate of rise of groundwater elsewhere. Similarly in Che future, with subsurface drainage installed, such that the drainable excess from bananas can be removed, there equally would appear to be no advantage in changing co another crop. Cotton is the predominant crop and probably is the most suited enterprise, as long as priority in the use of irrigable land resources remains with the production of exportable cash crops. It is the most climatically suited and highest vaLue in the list of the most salinity tolerant crops. It is an imperishable and high volume crop which is easily stored and transported. It is labour-intensive (unless mechanised) and provided that the labour shortages of recent years can be overcome permanently, the area has a clear comparative advantage in the production of cotton. Under such intensive production, however, it is inevitable that watertables and salinity will continue to rise and correspondingly the area under production will decline steadily. The ultimate abandonment of most, if not all, of the productive area must therefore be projected. The Relief and Rehabilitation Commission (RRC) have proposed, during the course of the preparation of the report, some changes to the land use and settler land allocation within rhe Amibara Settlement Project (ASP). In order to evaluate the benefits of the proposed drainage project the intended land use pattern was obtained from RRC and developed by the consultants. It is understood that these intentions do not at present constitute Government policy. The RRC propose to accelerate the settlement of families on the ASP. The infrastructure and cropping pattern is to be reorganised partly to accommodate the extra families, and partly to make the area self-sufficient in food and fuel. The proposed ratio of land use is as follows:- 2®Cotton as a cash crop Maize as a subsistence grain cron Garden for fresh vegetables Pasture to intensify milk and meat nroduction Forestry to supply fuel and building requirements The Settlement Scheme is one of the two areas of greatest need of subsurface drainage so that it will be very important to rationalise the planning of crop enterprises. It is assumed that already affected land would be used for planting tolerant tree species and that the land at least risk would be used for the arable crops. This would defer the onset of serious decline in productivity but the future for the scheme without subsurface drainage is Likely to be short lived. It is unlikely chat the costs of subsurface drainage could be supported by forestry, apart from the hazard of root penetration in field laterals which would also require the introduction of root inhibiting solutions, adding further costs. Based on the above initial land use patterns the projected overall change in land use over the next 20 years without the introduction of drainage is shown m Table 8. Following the client’s review of the draft final report, the consultants’ brief was expanded to include consideration and analysis of the affects of varying the Land use plan within the ASP area. The expansion to the brief comprised the following alternatives for Land use and production; (i) A reduction in the intensity of the dairy enterprise, Leading to lower □ilk yields, (ii) An alternative cropping pattern of 1002 cotton within the ASP lands, Z of area 14 14 5 53 14 (iii) An alternative cropping pattern the latter being utilised for a of 502 cotton, 25* maize and 252 pasture, simplified dairy enterprise. The projected overall change in land use, based on the adoption of alternatives (ii) and (iii) above, without the introduction of drainage, are also included in Table 8. 294. THE DRAINAGE MASTERPLAN 4.1 Introduction The earlier developments of irrigated entities within the study area followed a pattern of discrete implementation, each with its own pumped water supply from the Awash and each enclosed within flood dykes. No surface drainage works existed with the exception of those of the Melka Sadi Banana Unit. These drains were incorporated with those of the Amibara Irrigation Project during construction of the latter. As currently proposed, the forthcoming development in the Amibara Extension area would also have an independent system of surface drainage. The need therefore exists to rationalise these developments so that they are compatible and also interlinked, where the latter is appropriate. With the current encroachment of high water tables in part of the study area, which can ultimately be expected to extend throughout, the need for such rationalisation is emphasised. The removal of deep subsurface flows cannot be done independently within the individual entities without recourse to a number of pumped drainage areas. The Masterplan would provide the framework for the rational development of an integrated surface and subsurface drainage system, including flood protection works, throughout the study area. In its scope the Masterplan comprises the outline design of the major drainage network for the study area together with the detailed design of the surface and subsurface drainage works required to alleviate those areas currently being affected by high water tables or likely to become so affected in the near future. Included in the Masterplan, although not necessarily confined to chose areas requiring subsurface drainage works, would be associated recommendations for the improvement of yield levels through improved water management techniques and other husbandry practices. 304.2 The Development Options Much of the study area lies at or below the sustained high river levels in the adjacent reaches of the Awash such thac the direct and continuous disposal of drainage flows by gravity into the river is not possible. The options for drainage are therefore limited to direct pumping, during high river stages, or the discharge of flows by gravity into the Angelele Lands downstream of the study area. The option of pumping drainage flows was evaluated in the initial stages of this study and rejected on cost grounJs. Gravity drainage of the upper parts of Che study area can be achieved through the existing Primary Drain outfall constructed for the surface drainage of Al?. Drainage flows from the remaining lauds must be conveyed past the study area boundary and through the upper Angelele lands, being lead either back into the Awash at a point sufficiently far downstream to permit their discharge, or alternatively, being directed into Kortume swamp which forms the natural drainage sump for the entire flood plains area. These investigations have indicated chat the continuous utilisation of Kortuse for the disposal of the study area drainage flows was not appropriate in that: its capacity to absorb such flows was limited; the creation of a perennial body of water would provide breeding grounds for schistosomiasis and malaria; the use of the swamp and its environs for dry season grazing by the nomadic tribesmen would be lost. The disposal of flows into the Awash through a gravity flap structure, similar to the present outfall, would also pose probLems during high river stages in that closure of the flap would induce rejection of the drainage flows into Kortume, albeit for shorter durations. The recommended alternative is co provide an unrestricted oucLet for the drainage flows into the river, sufficiently far downstream in Angelele to minimise the backwater effects on the northernmost part of the study area caused by river flood levels. 3XThe flood flows from the eastern catchment are currently discharged onto Che uncultivated lands in the Amibara Extension area. The alternatives available under the Masterplan are to convey these intermittent flows back into the Awash by containing them within high level embankments leading from the eastern perimeter of the study area to the river, or to allow the flows to discharge into uncultivated lands in Angelele. As the existing arrangement has enhanced the dry land grazing without having any appreciable negative health impact it is recoimoended that the future extended dyke and drain should operate in a similar manner. Once the flood flows have passed the northern limit of the study area they would be directed into the natural drainage path leading through Angelele cowards Kortume. Consideration was also given to the use of Cada Bilen Swamp (See Figure 2) aa a flood attenuation pond for the eastern catchment drain. The storage capacity of the swamp, relative to the total contributing catchment area, is however insufficient to effect a significant level of attenuation and this option was not considered further. The existing hoc, medium saline, spring feeding the swamp has a total flow in the order of 500 lit/sec of which an estimated 50Z or thereabouts appears to infiltrate into the soil. It is not known whether or not this flow is affecting groundwater tables in the vicinity but there is no evidence of surface salinity or waterlogging downstream of the swamp. New observation wells proposed under the Masterplan will monitor groundwater levels adjacent to the swamp (Annex B, Figure 9). Unless such observations indicate that the swamp is significantly contributing to the groundwater levels in the future irrigation area, it is recommended that the swamp and its environs be left unchanged thereby retaining one of the few remaining and extensively utilised natural watering and grazing points in the area. For subsurface drainage the option of using well point drainage is ruled out by the predominantly Low horizontal permeabilities of the sedimentary materials in Che study area, combined with the presence of relatively impermeable layers at comparatively shallow depths. Similarly frequent shallow open drains, at depths 32of say 1 metre would not achieve a sufficient lowering of the watertable tor optimal crop yields, nor would such drains control the level of secondary salinisation. Cost comparison of buried pipe drams versus deep open drains strongly favour the former for all field laterals and for single collector drains. Where contributing areas are such as to exceed the flow capacity of a single collector pipe (approx 100 ha for 300 on dia pipe) a double pipe would also generally be more economical chan an open dram, requiring less maintenance, reducing land wastage and avoiding the health hazards associated with open drains. Consideration was given to the alternatives of using concrete, clay or PVC material in the manufacture of drainage pipes. The high sulphate ion concentration in samples of groundwater indicates chat concrete would not be suitable. There is no established Local experience in the production of clay pipes; the energy requirement in firing the clay is high and a high level of skill together with a well equipped factory would be required. PVC pipes are Light, convenient for handling or laying by trenching machine and can be readily imported or manufactured locally if appropriate plant is purchased. The use of ?VC pipes has been accordingly recommended. 4.3 The Drainage Masterplan The engineering features of Che drainage network recommended to achieve surface and subsurface drainage of the entire study area are as follows (l) The installation of buried field lateral drams, at an average depc.n of 1.3 m below ground, to achieve adequate control of the groundwater table during irrigation and to limit the rise of salts during fallow periods. Within the area surveyed for drainabilLty classification the recommended spacing of field laceraLs varies from 30 ra co 110 m. (ii) The conveyance of drainage water from laterals, through buried collector drains, into deep open drains. 33(m) The construction of in-field and tertiary surface drains to remove surface flows, derived from canal rejections, excess irrigations and rainfall. (iv) The deepening of existing secondary drains and the Amibara Irrigation Project primary drain as well as the construction of additional deep open drains to carry surface and subsurface flows. (v) The construction of a new main drain outfall co the .Awash in Angelele. (vi) The realignment and heightening of parts of the Awash flood dyke in lower Amibara and its extension into Angelele to the proposed drain outfall. (vii) The extension of the Eastern Catchment flood dyke and drain to the northern Limit of the study area. (viii) The installation of ten additional observation welLs in the Amibara Extension Area. The Master Drainage Plan layout is shown in Fig 2. The design of the above works takes into account the recommendations arising out of the environmental health component of the study. These include, inter alia, the elimination of all bodies of standing water, avoidance of inducing swamp conditions, where practicable the maintenance of higher design velocities in open drains and the alignment of open drains away from centres of population. In the Melka Sadi section of the Amibara Irrigation Project, including the 3anana Unit, the existing drainage network can be readily adapted to cater for the deeper subsurface drainage flows with partial realignment of one secondary dram only (SD1) co achieve sufficient gradient. In the Melka Warer State Farm the mair. drain (MDl) which runs along the eastern project boundary, will serve the surface drainage only of a limited area in its upper reach. All other surface and subsurface drainage is directed into secondary drains 4 and 6 (SD4, SDb) which are linked to form a continuous drain 34Leading into the existing main drain extension during the early stages of subsurface drainage installation in the southern part of the State Farm. Drainage from the Awash Settlement Farm (eastern extension) will also be conveyed into SD&. A new deep open secondary drain (SD7) will run from the Melka Warer Research Station, through the Amibara Settlement Farm, Algeta and Ambash Units before linking with the existing Secondary Dram 5 (SD5) which discharges into the main drain extension. This system will serve the subsurface drainage needs of the Research Station, the Settlement Farm and Algeta. As the need tor subsurface drainage extends northwards, towards the main drain extension, both secondary drains 5 and 6 will be diverted into a new deep mam drain (MD2) whicn will pass through the Amibara Extension Area and extend for a further 11 km along the Awash levee in Angelele before discnarging into the river. Main drain 2 wilL serve the entire northern part of the study area as well as conveying the rejection flows from MD1 during outfall closure period. Flow levels at the downstream end of MD2 wilL respond to those in the Awash. Under low Awash (Lows the drain will be unrestricted and natural scour of its bed will occur near its confluence. Conversely under high river flows the drain levels will be backed up. The outfall has been located sufficiently far downstream of the study area to prevent flooding from the river although limited impedance to subsurface drainage will occur under sustained high river levels. It is anticipated chat the effect on crop growth resulting from this impedance to flow would be virtually negligible. Nor would rhe temporary retention of drainage flows in the collector pipe be expected to induce unfavourable silcation problems and no special provision needs to be made for additional maintenance. Consideration of the aspect of silcation in Che drain indicates Chat limited deposition only can be expected frcm the dramwater silt itself or from silt supplied by reverse flow from Che river into the drain during high river stages. However localised deposition of silt ac high river leveLs due co eddy action a: 35Che outfall is expected co be both rapid and appreciable. During flood recession and thereafter ic is anticipated that the drain will scour down through this silt as occurs at a natural stream confluence. The subsurface collector drains are in general aligned parallel to maximum groundslope so that they can take full advantage of the natural gradient without requiring excessive deepening. With this configuration it is possible, within most of the AIP area, to maintain the collector drain alignments adjacent to the existing field or tertiary drains forming field boundaries. Field laterals would generally be at right angles to Che collectors which in the greater part of the AIP area allows the laterals to be parallel to the furrows and thus minimises disturbance to furrows. An exception to the above lies in the south western part of Melka Sadi where the direction of field irrigation is parallel to the groundslope and consequently parallel to the collector drains. In this instance the field laterals are at right angles to the furrow and, co avoid excessive lateral lengths, the collector is taken through the field rather chan along its boundary. A similar situation occurs in part of the Awash Settlement Project where collectors are aligned obliquely to the field boundary in order to maximise the slope component. Similarly the new surface drains in the Research Station, the Settlement Farm, Ambash, Algeta and Subelele nave been aligned, as far as practicable, to conform with the existing field, road and irrigation canal networks. In Angelele Units 2 and 3 however the retention of the existing field arrangement does not appear to be practicable from topographical considerations nor could this arrangement be easily incorporated into the proposed development of the surrounding lands. The outline conriguration of surface and subsurface drains indicated for this area is one essentially based on topographical considerations. At present there are no operational observation wells in the Amibara Extension area forming the northern part of the study area. A further ten wells are accordingly recommended at the Locations shown in Annex B (Figure 9) Seepage trials concluded in the Main Canal and indicated relatively low levels of seepage and in selected tertiary canals have it is considered that the estimated seepage from the present Main Canal would not cause significant 36overLoading of the drainage system. The proposed increase in capacity of the Main Canal to cater for the Angelele-BoLhamo expansion could however, if unlined, significantly increase the seepage, possibly to a level chat would surcharge the adjacent field drains. It is recommended that no specific action be taken unless such surcharging actually occurs. Should such occur then alleviation could be achieved by installing interceptor drains parallel to the canal at a depth similar co that of the field drains. Deeper interceptor drains, or drains placed immediately adjacent to the canal could effectively increase the level of seepage. Financial provision of Birr 1.9 million (1984/85 prices) has been included in the Masterplan estimates for such drainage. The Western (Awash) flood dyke extending from Algeta to the northern limit of the study area will be realigned and heightened along seLected reaches. The locations of sections requiring these remedial works have been determined from the routed profile of the I in 20 year return period flood (Annex C). Realignment would also be required where the present dyke lies within the 100 m reserve considered to be the minimum width appropriate for the floodway adjacent to the river bank. Downstream of Che study area the dy
200 cm of clay or silty clay at | the surface I Structure predominantly massive I APPROXIMATE HYDRAULIC CONDUCTIVITY (m/day) 2.0 SUB-CLASSES I I DEPTH TO RELATIVELY IMPERMEABLE LAYER (cm) a I bI cI dI < 200 200 - 300 300 - 400 > 400 I I I I I I 0.1 a I bI cI dI I Not sub-divided < 200 200 - 300 300 - 400 > 400 ITABLE 2 - LAM) ISE LN U£ STUDY AREA - 1984 (Areas in -*ectarea 1 | 111 III 1 1 FARM 1 COTTON 1 BANANA 1 PAS’LSE 1 OTHER I FALLOW 1 ABANOtoOtfaElD11 1 1 1 1 1 I 1 CHOP S1 1 1 1 1 1 1 2,770 1 1 1 1 1 1 1 1 I 1 1 1 1 1 i Malka Sedi State Farm 338^ I 36 1 - 1 -1 1 4,090 1 1 1 1 i 1 1 1 926 I -1 1 I ! 1 1 1 187 | 1 1 M Malka Merer I 301 -1 55 -1 300 | 1 1 1 1 1 1 1 28 1 1 1 J - 1 1 1 1 3,728 1 1 1 1 1 1 ' Malka war er State Farm -1 - i-1 -1 -1 1 1 1 1 1 1 1 1 1 3,728 I 1 1 1 Aaibara Settlement F tt(1 1 1 | Amibara Anqeleie State t r I 1 | Ami bars 1 1 1 1 Arqelele 1 1 1 1 132! 1 1 1 I1 1 - 1 200 1 1 1 1 ■ -1 1 1 1 100 I 1 1 1 1 1 1 I -1 Farm 1 I 1 1 i Unit 1 1 62B 1 1 1 1 - 1 1 918 | 1 1 1 1 1 1 Unit 2 1 340 I - 1 - Unit 3 1 M3 | Unit A 1 an | 1 1 1 1 Jmt 1 1 50 3 1 Jilt 2 1 359 f -1 • I-1 1 - 1 - 1 1 - 1 1,350 1 1 1 1 1 1 1 1 ■1 1 628 | 340 1 ; mi i -1 1 1 -1 - 1 - 1 1 1 1 1 1 - 1 ! 1 1 - 1 - 1 • 1 -1 -1 - 1 817 1 1 I1 1 5031 - 1 359 . 1 1 . Unit 5 1 262 | 1 1 -1 - 1 - 1 -1 - 1 262 1 L 1 1 1 1 1 1 1 1 1 1 1 1 1 totals by crop 1 9,932 1 Dfl I 311 1 128 I ’1 1,105 1 926 1 12,740 | 1 J L 1 1 J I 1/ The area of banana comprises 204 hectares of productive bananas and approx 134 ha -hich is expected to be replanted Oy the end of the year. Source: IAH; MAAE Proqromme Service; Awesn Settlement farm; AIP EngineersTABLE 3 - ESTIMATED AVERAGE YIELD EXPECTATIOUS FOR THE 1984 CROPPING SEASON \ LOCATION \ CROP \ 1 1 COTTON 1 BANANA PASTURE MAIZE FALLOW 1 1 1/ 11 Melka Sadi Stare Farm 1 37 Malka Warer State Farm 1 34 2/ 7.5 - - - 2/ 5.6 - 5.0 - 2/ - Amibara Settlement Fann 1 22 Ami bara/Ange 1ele State Farm 30 - 2.0 - 3/ 30 - - - 1/ q/ha of seed cotton assuming 2/ t/ha saleable bananas, conser 3/ fat sheep'ha/annum 10X harvest loss ved fodder, maize grainlABU: 4 - COTTOW FIELD AOJlfiTEQ for EFFECT of MAIERLOGCIM; 1 1 R.0T 1 NUMBER 1 FINAL Yl£lDV ADJU5TKNT2/ YIELD | PLOT ESTIMATE FOR HI 3 ADJlfiTED / | NUMBER 1 1 1 (q/h«) (q/M) («V*«) 1 FOR WI | | FINAL YIELD1'' ESTIMATE (q/ha) ADJU5T>€NT2/ FOR HI (Q/ta) 1 1 1 1 2 1 J 1 YIELD 1 3 AOJlfiTED ,! TOR HI | (o/he) | I 26.9 45.8 37.7 7.8 10.3 12.2 34.6 56.1 49.9 1 1 22 1 23 46.1 31.8 1 4 1 5 1 26 30.9 45.5 18.7 (17) (24) ____________ L 1 6.6 52.7 | 5.8 57.6 | 16 7 47 5 1 63 45 1 27 53.5 . 3.7 . 57.2 1 1 6 1 7 1 28 32.3 31.6 40.8 (17) ( 5) 25 2 57 5 | 49 46 . 1 JI 20.9 (12) . 33 | 1 9 1 9 19.9 30.4 15.1 9.7 1 32 9.1 1 2 10 3 34.9 40.1 1 33 7.1 . 1.3 .| 9.1 1 1 34 39.4 1 10 1 u 59.9 39.8 1.9 0.6 (5) 44 61.7 40.4 1 36 1 38 38.3 46.5 (12) 50 1 12 1 U 41.6 30.7 (7) 8.5 16.9 54 | 50.1 47.6 1 40 50.7 (7) 58 | 1 14 1 16 1 42 66.4 14.4 30.5 25.6 9.9 (7) 73 40.0 59.4 1 49 13.7 (14) 1 50 1 17 1 18 16.4 44.6 0.1 C 14.9 6.6 | 29 | 01 31.3 51.2 1 51 5.3 45.6 .| 50.9 | 1 52 18.4 1 19 1 20 16.6 36.7 3.5 3.5 39.6 58 0 | 52.1 40.2 1 53 33.7 23.9 i 21 1 _ 35.3 1 54 51.1 26 0 . 21.3 . 57.6 f 77 1 I . 56.6 1 1 1 1/ m«l yield estimate from Table 1, Arrwx £ r V feat by «h, h y .id i, ..peered to have been greater then enured nad there been -n CS waterlogging probl« at the site. bee Ann,, £ For calculation. Srackets indicate id;ocmenc by Cl 3/ 4dju>ted yield aeauHinq no
5.2 33. 7 26.5 25.2 25.1 25.0 25.2 25.0 24.5 24.2 24.6 25.9 22.9 23.3 21.4 17.7 16.1 0 0 11 1 Alb | 24.9 24.9 24.6 24. > 24.5 24.5 24.2 24.1 24.2 23.8 25.2 23.1 22.a 21.3 19.8 18.a 18.0 16.6 0 0 ! ASH I 24.6 24.6 24.6 24.6 24.6 24.6 24.6 24.6 24.6 21.2 20.5 2U.I 20.6 17.4 15.5 0 1) 0 0 0 1 24.6 24.6 24.6 24.6 24.6 24.6 24.6 24.6 24.6 24.6 21.5 18.6 24.6 19.7 15.5 0 0 0 0 0 1 1 MS - telku Sadi Mrf • Hulks Wafer ALC - Aiyulu Stole Fimn ASP - Aid bur u Settlement ProJoeI Note: Huatnl mi lublu 24, Anne* E, reiuliiij lu upucitic area within Lin abovo Holed enlitiuuTABLE 7 - PROJECTED AVERAGE YIELDS Of 0U€R CROPS IM THE SET TLE* NT SCh€< WITHOUT DRAINAGE II I 1 CROP I 1905 1996 1987 1998 1989 ’990 1991 1992 1993 1994 1995 1996 1997 111 2 3 4 5 6 7 8 9 10 11 12 13 I I M 1 3.68 3.72 3.48 2.96 1.74 C.41 0.4 0 0 0 0 1 G 1 17.6 16.9 15.0 13.7 10.5 6.5 6.0 0 0 0 0 II IrI. II 0 0 0 0 0.16 1.9 2.0 3.9 4.2 ! M I 3.92 3.76 3.56 3.18 2.26 0.62 0 0 I 0 0 0 0 0 | 0 0 | 14.4 D.O | 0 0 | I I I I I i F> I - 4.8 3.4 2.5 1.7 1.4 0.7 0.4 0.2 3 C 0 I M HaLze (t/ha) s G = Garden : mixed vegetables - average yield in t/ha) F « Forestry (irrigated • average yield firewood, poles, building, timber in a /na) ? a Irrigated Pastura (t/ha of cry letter) 5I ABU 8 - PROJCrtD LAND UM WITHOUT CWA1NA(X_ i—r ------------ 1 1 TARH IMPL N 1 1985 1989 5 1990 1992 1993 I,,* 1996 12 199 7 1986 2 J9B7 3 1986 4 J?95 1998 14 1999 15 20M 16 2001 17 2002 10 7003 19 2D'.U 20 2005 2DO6 I ini n YEAR | 1 6 8 7 13 11 13 21 22 2007 23 2008 24 2009 | 25 | na — 1—1- 1 »G | C 11 I 1 1129 1075 1003 93B 887 869 849 768 719 69} 574 11 11 11 11 1 MW | 11 11 1 1 Al C 1 11 B 1 | 448 44 B 448 448 448 448 448 44 e 448 449 448 496 450 236 158 109 67 20 0 C 0 0 0 0 01 J 448 448 448 448 448 440 44 B 44 B U8 448 448 ue 448 446 | 1 1 C 1 111 111 111 111 111 111 no 107 106 106 !03 94 89 85 68 58 49 20 0 0 0 0 0 0 1 1 C 1 411 411 411 391 MO 373 370 358 329 325 310 275 2 37 20B 158 97 43 19 0 0 0 0 0 0 1 1 j 1 0| 1 | 1 01 1 I | I lr 1 1 1 RRC | ASP | c 1 186 1B6 186 1B6 186 166 186 186 186 186 186 146 73 62 37 0 0 0 0 c 0 0 0 0 01 1 Proposals | | 1 11 M 1 186 186 166 186 186 170 20 0 0 0 0 0 0 0 □ 0 0 0 0 0 0 0 0 0 1 01 11 1 11 c 1 66 66 66 66 66 56 6 0 0 0 0 0 0 ft 0 0 0 0 0 0 0 0 0 0 11 1 01 1 11 F 1- 50 6C 90 120 ISO 186 1B6 186 186 186 186 186 186 186 186 186 186 186 186 186 186 186 186 186 1 1 1 1 P 1 KO 4110 494 542 429 28C 168 1D0 77 34 9 0 0 0 0 0 0 0 0 C 0 0 0 0 0 I 11 11 1 H 1 657 527 403 325 438 679 829 923 946 989 1014 1063 1136 1147 1172 1209 1209 1239 1209 209 1209 1209 1209 1209 1209 | I I IUDS 1 cotton I A! FERNATlvn 1 i i1 | ASP | !1! 1 C1 | | | 11 ir 1----------- 1 1281 1 1 1281 1281 1241 1235 1229 1221 1140 1119 1099 941 H64 810 635 480 385 296 34 9 G 0 0 0 0 1 50% cotton j ASP | | 25% n»ize 1 1 I C1 11 1 25% pas turd | M1 1 664 664 664 664 664 664 66 J 658 658 658 550 505 470 342 228 167 89 13 4 0 0 0 0 0 332 332 332 300 215 20 0 0 0 0 0 0 0 0 0 0 0 0 U 0 0 0 0 0 I AL lrRHATlVU | 111 ‘ 'I P 1 284 244 216 224 206 MO 302 251 2Z9 7 0 0 0 0 0 0 0 0 0 G 0 0 0 0 1 i 01 1 1 1I 01 1 01 1 1)1 J MS . Melka Sadi AIC r Alqetn State Farms MW = Melka Harer ASP = Arti bare Settlement Project FOFES: R Rough qrarang (total net area 1329 ho, minm productive land, pl lb 5% of total net area, tring verqea of canals and react, and easte areas out of command etc) C r Cotton H s Bananas M = Haire G s Garden (mixed vegetables) T s Forestry (irrigated) P z Irrigated pasture 1 £1 1il !l I I ITIBl£ 9 - PROJECT INV£STRET COST ESTIMATES AT 1984/85 PRICES Mr-1 i"Ml 1 •NUN i IWNN 47 •1RHR 1 rwani > miiia i*w Midi I <•*•! M'rl« m i — mw • wartm »F*»R 1 IMMR iMWaUF ! RffM ................. ! 1 t Mrr'RM IF • 1 1 •• IM MJ« M MM M RM 1M Hi’ r r » FM •» n IM ffi 1 w Ml || •N R.M rltl.M iMi M l. M •• MM • I V MW, ll n MM M 1 | JR MM •W ’».M ntR I.M •M 1" HN-M » 7 •N.H •a ItM.W ! I ll fl-51 i R• 151M 71, M I.M •M I.M •* rr 1 n JTT M m m«t r i m N.R i i 1f I.M n i.n •M I.M •M Hr * I n FIMJ W I.F 1N i I.M •M m.M I.M !,■» t.R nr • • fl 71.11 JI 71.11 • I.M n.n i I m IF M • M I.N I.M I.M in • i n irjwf’M W.M 1 I.M n f i.n nrr.M MR •NR M I.M IM I’CT.N t I* I TH IR tf MM II 1 II • R W1.M UI.M m* I.N IN • 71. JR • M •M.n W IM.JT 1 I.M 1 M nw m UU.M »H-M • N R.M HIM JI 1 <1 mi n u tn n 1 1 1 I.N him cu.m m.n 1 M R.M !<•» H f U iu.;i ir hi n i i.i JR F I.F JN.lt H-F i i i i i i i 5 l-H III ll R.N im m 771. M m .7 1 M • M ’tm.n • n • F ♦MR M W.N IJM.M • M I.M i»ni.» it whmm.nmiw.mi i.i jM.n UW aa ir.M win,** «,« Nl M l-F I.N Iff I.M I.M BU.M IIM.M *n»M i n rr* •• 1 T IIJI.NtJ.lt WR R.M I.M I.M R.M IHf.M WI.M nt».f i m irrr.F T FRR.N • t R on I.M R.N ».M nw.M m M I.M NfJ.M i II IW .9 M »M1F 1 I.M »-f? R.M I.M I.M IMtM JW.R I.M MN.R I .’J UI.N M fR.N • f.R W II I.M I.M I.M I.M nn m I.M nr..* i if RM-N W >JTT.» 1 I.F n.n R.M I.M I.M R.M IRM M RM IriI.m r 7 ’U, JT J* T* Ml l.F XU i.n INN R.M IM I.M I.M IM M • 3 f!J»M W HI N • I.M jin •.99 CTM IM jin.M W-N rm.M IHD.M 1 M tfn.R 11 HM.fl • 1 I f.R 41N I.M m.M M.M W.M IfW.F r M in.r •• IW.RI I I.I T7.F I.N I.M fur* «,N h.f I.M MI.F I.M I.N !.«.> * M ”11.M I.N tnt.M mi.M HU M IMtl M 1 It UTT R W wr N I t.| I.M TT7.II RIM IM.« NUM I l| IM - W Wl M 1 Ul r.n i.n •m •• m» - Hl* N.M m.» 71 R i I I I i ■,« t.F • n I.N •m.u wt.m •m m 4* F • I I I I *•1 rwl •Nral r1 I i R.n I.M i «.■ IN i i 1i •1 w R.N 1N.N I.N I.M • N IF NR N ’ N 1M-F F • N.|| 1 r.i LR i I.N T-U R.N I.M IN I.N •HIM 1.11 n IF 1 1.4 «.<• 1l IN. «R R.M »n.w I.N I.N “• — — ... I* • M in * • n m u F IM U • ll w. 1 .— — • in i — ii R.M •MM I.M a M R.M R.M •N M 1 W j’i.ii W IF II | I.I Ml 11 I.N I.W 11 li M.JM I.N M.M I.N I.M I.M • IR F-F N •> n * n m • 1.1 R.N i.n I.N 1.M RM R.N i n i w Ml * I.N 1 I.I ih.fr R.M m.F I.M I.N R.M IN IM F ! M CT. 14 w CT.ll I I.I ———— ... »• ------- 1 —— — | i.n •1 i.n i1 i.n i _ i1 IN rn.Aj I.M I.M R.M R.N Ni l) I w TM.ir w IF II 1 I.I r.n i f.RI • « It J R.N MJ.W R.N ■ M RM R.M «T.W ! M FIJI F 1 1 CT.n ? I.I 1 l.U : 4 ; I.n i.n I.N NNI F JKT.M GN.M mi - MF.M •Mrt.N 1 Ij •RRM.W IJ win
w» Ml NUM ■ MT'ka^lt • iVwltfH W'
’LM LH *1.7* Ml Uiwaay camrtw X N IMai IMIIII (Mil
cltfi - ImjI cooUactor lorrl^a conlractor Tllfll COSIS Al CURfiENI FRILLS - local contraclpr - foralfa coatraclor 10.01 21.01 3S.ll 44.11 41.11 17.21 0.81 iL n 28.31 39.91 SMI 51.01 ................................................... OlrrW .................................................................................... 0.00 I0M9.49 5047.00 •20I.04 0357.00 M9.O0 35015.41 0.00 7071.02 1801.40 35/9.21 4700.00 1451.70 13577.00 0.H 7'»I3.I3 1749.04 3477.51 1539.12 1347.50 13141.39 0.00 12408.51 ZAPS. Al 11717.70 13045.00 3470.70 48415.21 0.00 12472.4? 7551.04 II4B5. 54 12171.12 1421.53 40154.08 III Local toili • III for aniHial oHMhwv totlt 8 01 io 1105, 71 io 1704, 198/ 1 1700, Lil io 116? 4 41 Io 1190. DIVISION Of PRICE C0AIINGEK1E5 I local Contractor - Do Local Cocti 0.00 1774.18 1071.31 2170.55 2910.05 900.54 1370.43 H - 0o For <140 Colli 0.00 041.63 105 30 1100.74 1/97.11 523.34 5229.51 SO ’ lol al 0.00 70/9.02 1801.40 3571.20 4700.00 I43I.10 13599.00 100 (•rri^a Contractor * On local Coill O.BO 857.37 734.40 1452.27 1947.1? 407.74 5519.13 43 - Oh Forriyri Cull 0.00 1140.00 1014.34 7070.V 2597.00 754.81 7547.24 57 ■ lalak 0.00 7013.13 1749.01 3422.54 1537.17 1542.50 I3tll.11 100TABU 12 - 1 HC.IH HL kT AL OH i
I I ,1 IHAlLS t -Cl u£4*Im It*/..I 2 J 4 5 4 75 7 Id II I. r» • NT . 14 13-3 j*.I»-*mTI act 4 Jttp open kair>i i or . F«clor (Im: capihl ft (tpIvceMMl ■ ni tia 1.0 no 0 0 211 nr I.A 1.1 ■ C 121 Ml - |iMt aparating I I HI ZM .94 > IM V.M 314 ?n .■» 3C 2M 34 BA 34 aW Util, pltal (|>» rj(ors 4 a JI 111 144 H5 n IM 144 in 111 in in 111 111 ■JI • itfialb B 0 B .0 JO Q u u 40 4d 40 41 40 40 4B 1 17 I* Kill < 4‘aIIm burlilt trams /n»u/| rtturml i .B U n 91 >1 u n 71 93 •1 91 1J u 111 AdJit.iiul f-oubing 4t 21 20 20 ;o .1 :t «c .f .f ;o 1 .b 1.8. IvlAl J 0 cn 431 742 AC? AC? wt H.J t>4 AU MB MJ u/ CO? •»• tfliiili; ftlU Siai: 17.M B B d 262 4.4 J?J kfl M- nc IfiB 40? 112 JI. 35 .51 116 B.I7 *nw»ii h'i.H 0 .51 UJ J VO ♦N ns no 4.4 on 14D J4IJ .05 2E5 J5. r.B? .4>ain»4k imi 'uoh EirsbiuiriNi ti
Suboilmj lint Mlb 16.5OB i *•» 0 • B I B 157 B 1 0 B B 9 B 1 F a fl •V liy#r ■•lu.paenl l?2,4tf B S.4> luUl 1 d•1•001d1 • B 1 1 t ip B B 7 2. Ml-.ara — letctyi <140 144 h.p.,4 J-(H Util tent litre) f4,» B 1 B B fl • 75 c d • B KT? M M Jfl fl.17 I 1 1 1 1 B.fJ B 172 17 17 17 B.17 1 Ml U 56 U 0.17 1 95 1? 11 11 B 17 U»b tat 1 t*j hue mH 9 B 1 B fl 1 B 0 fl 5 1 1 0.17 Lri* it.dllng *Quip
» • B B fl d B • 0 d fl • 1 1 0 0 fl r. d fl 5 J B fl 1 fl fl 0 ;u 0 • 14 >IU Sadir 1 fl 17. 17 17 17 J.17 1 .Al 11 17 37 0.9/ 2 All 11 W 11 fl.77 66. I.* b3J AM NO • U 111 4H 112 112 172 d.eu - A%;tvr«; I • M3 09? tfl Jbl 1.4 A42 Hfll B'«4 •
2 4.4 323 MB 471 JA JU b|| 0 31 471 26B 40? 431 JJ8 4?4 451 140 All 1.1 121 Jft fl.ro p iTABLE 13 - SUWAR* Of PROJECT INVESThfWT COSTS I tew Local Contra ctor Foreign Contractor local Foreign Total FE local Foreign Total FT --------- Birr (Millio n)- - - - 5 — - - Birr (Million)- - --X Engineering -erics 8.42 6.36 14.7B 43 5.56 9.22 14.78 Farm Machinory/Equipment 0.04 0. 33 0.37 90 0.04 0. 33 0.37 S kb-totsl “TSZ 6.69 TOT n TT K“7 Physical Contingency 0.84 0.64 1.48 43 0.56 0.92 1.48 TOTAL (1984/85 Price*) 77H l£.l3 n TI? 10.47 16.6T Amjberi 5taqe I Area Engineering works 9.73 6.74 16.47 41 6.56 9.91 16.47 r im M«chineryAouipe»ent 0.03 0.24 0.27 90 0.03 0. Z4 0.27 SiA>-total o. 96 16. ^4 4l s. y* 16.13 16. 74 Physical Contingency 0.97 0.67 1.65 41 3.66 0.99 1.65 TOTAL (1984/B5 Prices) o -T7ST IB.39 IT T7T5 u. ii 18.39 C whole Project (1984/85 Prices) 20.03 14.9B 35.02 4J 13.41 21.61 35.02 62 0 Price Contingencies a. 37 5.23 13.61 38 5.60 7.54 D.14 57 E *«oLa Project (Cirrant Prices) 29.40 20.21 4B.63 41 19.01 29.15 48.16 60 SOIL: Variation 'ram Tao la 10 worn totals due SOURCE: Consultant's Estimates to rounding SI SB) 8fi IS ed 8BTABLE 14 - REVISED IRRIGATION SCHEDULES FOR COTION (Values in bud) I Preplan! Irrigation | Postplant Irrigation 1 Irrigation Number | 11 1 211 2 1 3 45 6 TOTAL i r 1 Interval (Days) | > 20 20 20 20 40 30 30 i yr 1 Fine-Textured Soils and Med i uin-Tex Lured Soils with Saline Groundwa ter 1 1 i r | Net Application | 220 220 105 91 91 182 130 130 | Gross Application | 286 286 11 150 130 130 260 185 185 1169 1612 i’ r “1 I Mrd i uin-Tex tured Soils (except wi Lh Saline Groundwater) and Coa rse-Textured Soils 11 I Net Appli cation | | Gross Application | - 220 28 b 105 150 91 I 10 91 DO 182 260 130 185 130 185 949 1 1326 11 1 Note: See Annex H loi calculation ol excess tor leachingTABLE 15: PROJECTED 1 NCREMfNT AL PRODUC T1 ON - OR TCI NAL PROXCT PROPO5A! 5 I Cotton I Bananas tonnes, tonnes 11300 .r.R'.B 16040 16B26 16826 I I---------------------------------------------- I ITEM II---------------------------------------------- I A.MelUa Sadi Priority Area I T5*e Annex A. Table rtfi) - I | S.Amibara Priority Area II (Intensive Dairy EnFr r prlse) I I I I 1 •Dair) CoBjoncnt (See Annex H, ’Tables M13 & H17) I Milk 1/ '030 ltrs 10 head 0 head 0 ID 14 6 45 471 1033 1337 1340 1333 1765 2106 2434 2S23 29 2 6 29 0 0 3052 3125 3363 J4J3 3413 3398 3494 3495 3496 I Cull bulls 0 0 0 0 0 3 2 3 2 3 2 3 2 3 2 J 2 3 2 3 2 3 2 3 I Cull Zebu cows 0 0 0 0 (143) 93 0 116 •97 193 271 319 0 0 0 0 0 0 0 0 0 □ □ 0 I Cull 1 Zebu I Zebu Friesian > Zebu co* a head D x Friesian cull calves head 0 0 0 0 0 0 (103) (82) (59) (U) 19 24 29 263 266 292 271 279 291 296 343 350 349 355 354 0 0 0 0 45 166 424 501 462 465 451 468 48 3 -90 502 515 527 539 536 533 534 535 534 calves head (80) tonnes 0 0 1B7 385 543 669 1076 1134 1205 12J4 1290 1401 1513 1630 1795 196C 2103 2203 2267 2267 2267 2267 2267 2267 2267 | tonnes 0 0 45 ior 128 184 200 210 219 240 v’(9 417 557 61! 675 742 744 744 744 744 744 744 744 744 744 | tonnes 0 0 94 200 513 054 1015 1116 1209 1302 1995 1400 14 RR 1400 1480 1400 i4es 14B8 1*88 1408 1408 1488 1488 1480 1480 | 0 0 0 0 336 553 219 0 D 0 0 D 0 0 0 0 □ 0 0 0 □ □ 0 0 I I 2.Crop Production Components I I I 1 I Cotton (State rarm) Cotton (Settlement Farm) Maize Garden (vegetables) tonnes 0 0 0 0 (3) 80 113 116 116 116 116 116 116 116 116 116 116 116 U6 116 116 116 116 116 116 | I F or age I 1 ores try tonnes 0 0 c 0 0 1554 3495 4773 5223 5610 5771 5914 6055 6196 6337 ^78 6619 6760 6901 7042 7050 7050 7050 7050 7050 | CU r. 0 o o o 0 (5) a 0 19 19 37 130 106 223 742 670 521 632 725 744 837 186 205 279 316 | I I I Rough grazing LSU* 0 0 0 0 (26) (110) (154) (172) (177) (116) (191) (200) (215) (217) (222) (230) (23D) (23C) (230) (230) (230) (230) (230) (230) (230 1 Figures have been rounded to nearest '000 Source: Consultants' Eat matesTABII 15A: PROJECTED I NCR F MENTAL PRODUCTION - ALTERNATIVE PROJECT PROPOSALS IN ASP 4 5 6 7 8 9 u 12 13 14 15 16 17 18 19 20 21 2? 23 24 25 I Aribara Priority A»r« I. _Simpl j t icd Dairy Cn^parirnt. (See Annex k, tables HUA'S H17A) Milk 1Z Cull bulls Cull Burun cows Cull Friesian » Boran cows Boran > Friesian cull calves Boran calves 2. AH Cot ton Srcnar io fAnnev H,~TaT?lc~H7nB) Colton (State Corr) Cotton (Settlenient Farr) 3. Cotlon/Maize/Pastutc Scenario (See Annea H, table H?0CV I Cotton (State Fam) I Cotton (Settlement Farm) I Maize I Tor age I I ’000 ltrs head head bead head tirad ti 0 fl D (39) 4 D □ 0 I) 0 6 □ 0 (] 0 fl I I I I I 2 23 123 27D 359 372 WJ *■60 653 715 737 665 881 9D6 93D loin 1037 102? 1020 1052 1053 *053 1 0 □ □ 3 2 J 2 3 2 3 ■» 3 7 3 2 i 7 3 7 3 2 31 1 (1) (21) (41) (30) 45 42 65 B4 4B 0 0 □ 0 0 u 0 0 0 0 0 0 I 0 0 0 0 (10) (32) (JO! (7) (5) 35 66 65 70 62 65 6R 71 85 09 88 «H He 1 (1) 0 6 45 105 12J 117 114 ll? lia 115 ne 119 174 129 133 1)6 US 114 134 134 1U I 0 0 62 111 52 fl I n D 0 fl 0 D 0 0 n 0 0 0 0 0 □ 1 tonnes tonnes G0 0 12 107 366 3B5 54 3 669 1076 1134 l?0'i 12 U 1298 UDI 1513 69 3 849 1664 1831 2015 219ft 2595 2769 3060 3352 3834 4196 4575 4340 5261 5302 5316 5316 5316 5316 5316 5316 | I I I I 16)0 1795 I960 2103 2203 2267 2267 2267 7267 2267 2267 22 6 7 | i tonnes tonnes tonnes tonnes 0 n o □ 0 o o n I I I I 2267 2267 72 fJ 2267 2267 7767 7267 | 159 359 45C 671 725 766 P52 956 1194 1377 1567 151) 1879 1630 2149 1795 2347 1960 2511 2103 2634 2203 26511 2656 2656 2656 2656 2656 2656 | 187 305 543 665* 1076 1134 1205 12M 1298 1401 C 0 27(1 258 1594 1S26 1992 2158 2324 2490 2656 2656 2656 2656 2t.56 7656 0 21 342 1479 209b 2467 765* 2722 2789 7855 2922 2988 W54 5121 2656 2656 2656 26*’6 2656 2656 2656 265b | 31B7 3254 3320 3320 3320 3320 3323 J32D | 1 Source: Consultants* EstimatesI I I I 1 I I I I 1 I I I I 1 I I I I I ITABLE 16 - FARMGATT PRICES USED IX FINANCIAL ANO ECONOMIC EVALCATION 1 ITLM 1 Outputs Seed cotton Grain sa ire 1 Sanina 1 Vegetables (weighted average) 1 Wood (poles/firewood) 1 1 1 Inputs UNIT 1 1 1 quintal FUfAJlClAL (Birr) 113.20 1 quintal MJ.00 quintal 1 quintal 1 cubic metres 1 1 1 40.00 23.00 20.00 fCCWSMIC (lirr) 121.30 34.00 M.00 17.25 15.00 1 i 1 1 Fertilisers 1 - urea (state faras) 1 quintal 33.00 91.60 - urea (settlement Mnss ) quintal 65.00 91.60 - tripLe superphosphate quintal 71.10 73.30 - muriate of potash I quintal 59,00 w.oo 1 1 1 1 Seed 1 1 1 i - cotton 1 kilograr=e 1.0 0.66 1 - xaize i kilagransne 0.45 0.30 i - vegetable * 1 hectare 100.00 66.00 - eucalyptus spp (average) grown*! 0,25 0.22 1 1 i 1 Pesticides i 1 1 1 - cypermechrin I. litre 79,00 73.64 1 “ carbafuran 1 kilograsse 9,50 9.12 - pencmvl I kilogramme 14.00 13.44 j 1 1 1 1 Labour (unskilled) I man-day 1.92 0.72 1 1 i 1 1 Fuel | * diesel 1 1 1 litre 1 - petrol 0.7665 0.7232 1 litre I 1.1311 1.0745 1 1 1 1a a a i a a a a a i ■ i i i i i i i II Mil < _5II AH 1IWIA Sl*G( I Alli A I IHAHCIAL AHAtVit5 U«f[8 hbif 1rM..I j i i > 1 i • 1 It ii ii ii 11 11 kt 1/ It 11 « 11 it 31 N hn II n K ItlllS "Ina »l Imi 1 H <9 pmO I.M 1 i ill m Hl I.U1 t.m MU J.111 i.m l.lll 13/1 Mil j 311 1311 i.m i.m MH ii nn Illi mu IM" in ji Illi 1411 n III ill 111 Hl m m Mi m m ci m in in I.in IU i.m i.m i.m I.IM i.m tmr’l kmlll htt l‘Mui Irilteil itltat luUll CISIS la"i|arll mil |*f lira aitHam |/«fti>f*«a| JhiJiarnlll l I l 1 mil IN III Nil/ tUl uni UH nt IM 143 i.m I.IU liM MJ* I.m i.m i.tii i.m i.m i.r.1 i.m i.m l.lll i.m 1.MI I.CI t.m I.UI 1.441 1311 fi 1 17 • Hl i i.m I.MI 1,01 1 1 1 • I i i111• I1111111 1 111 i i1i •11ti• i111•11t11111 rr »*| IMM >*■( 1 • 211 in Mt iij m m VI ill m m m m ni IW m nj ni in m m I3J m 141 IMS smIHiwilrsNlpMik 1 • t•1int1I i 7IJ 11 M 11 1/ it il it tl JI 11 1/ u II Imi 1 crop pl al t mis 171 11 m Cl :n 111 jii Ail til lit HI r-/ III 1311 i.m I,Hi 1,111 i.m 1311 1311 i.m 131k l.tkk i.m M1I l«hll IltAMim Ml MMIII HWH1 IMllMli UM; I. 7I» MT f Illi III" Illi 1111 IMLHIS ■ 110/111111 It Mtlillai Itl 1. Oalpal Yu t (JU 0 1 Ik" Ml mu IM7H Ml 171 1111 HI t.H -UN im t il im Hit Ml 7111 IM Mi JU n i .in m |aAM ■,F7 fjn i,in m • .111 I.IU i.m 1,111 I.IM 1.111 i.m i.m t.in i.m ijti I.MJ l.MI i.m I,Mt I.M4 3,Mt iimiijm iinm.miii.nuii.nji in /M 1 (tIt i.m i,m i.m i.m i.m 1.124 i.m J.UI 1.311 7.ill Mil 13*4 1311 i.m 1.441 i.m t- laiBilaiil mil Tut Hit rv 1 II" Ml Hilt 'UN Ml IJI I4M til Ml Htl IHI 171 nn HU 1 11 JIM im 1 ti tm C. I,iu mH tu ■ im my |. fl Um km ( Mil I Yu t Utt »Y 1 till IM mil 1 ■ant 111 IJI Nil Hl LH Mil Illi 4 11 nn lilt 3 41 nil nil J tl un 1. Mil mil Yu t mi irr 1 Illi IM mu *11114 Ml H.H If 111 i n nn 1111 Lil im Illi 1 31 till im Liz im i. Pail lu a fin n "1* jlllti 1 llri IM nut tint •11 ini nn in • si im ini t n nn 1111 s.ti 1.11 im 1 11 mt i ii" m mu mrt nt LU IHI 111 1.11 4FM mi 1 it im Ml HI I ME VAIIIIt futitl iMHtlt It |Mfe*MllBB Iiivfl 11 krlt, Jin l» Itl Ptririt Ar"RJ4Sla liitklMvl mil It lf|a.| fill I* 111 Iniaal - fticrtl III i|| Im
M«1 «wr|»|*«rf II MftJMf IK 111 ■! HU »i t|W> ti riiijiip IT* Til ■! TUI *t«IH «1 <*p* miuipMi »i iitiiMj kmw* ninnnr. ZZZil 1>I IMI •III II 1 lill Hit K I tin nut » t IH till 1VI in run win M4 nil 1 r.zi iri Iff 1 nn n z nzi Wl III iff t <•« in If 11 HIT K ( LUI mi « t mi Mil it t Till n t Til IW ii i IM ttll * mu III MH J tKi n i till MU TCI i»ll HIT K ! mi 1)41 It 1 Til flit- 11 c m HEh HZli ffl mi 1 fit! IE C mi ini it i mi /HI 11 1 IM itm irt- m van wen wt nil 1 Z!tt Hi til Mil Kt /Ki K 1 ini in. WK- 141 til !UI» TUI* HI nil i A JI Wil ‘JU Aja MH • *»A AM mu • "A IM HIM 1 H rf* Mi nil W*lJ Mil livairif jiij J • !*•» I’lM 1 <|MtJ wriwfaij | i|t«i itf'i j »}W} | 1114 H t TH W|i fern HI ni| 1 I AM mil * *A *1 IMI IKipilfi !»| LJM|| |9r n Sl;i hit- iin nin mi i nx Ik i -nil isinw wimnri 4111*11 Ifl'lZ HI'S t»l Mil Ml't HIE Ul'l flll'l tll'l IN't m'l U*l m'l m't m'i lll't m'l Ell't m’l m'l lll'l Ul'l rtr'i lif'l 511*1 nr'l I1C*I ki'i Zil’l Kt'l tn IW'I m'l Iff m'l in ZZl'l nr. KI IftT'lHUi'llim'lHlM] 414 «i‘l m't Kl'l iff'/ KI mi'iimn tn' 1 u m'l ni'i flt'l in i Ill'l nfi 111*1 EM'I m'l Hl’l UE*I •n't Ml'l Hi ICI Hl HI KI tit Mt 1TK fit KI VII u It i Hum in irjiwiMMi • HH"I ijm a.r i< m f, i iu| it tt fl it ii fl ft It It ii If ft ft Iff. i t • i u ■ 1 1 1 a 1 |■»lf>rfcl||< M-wtf KI KI Kt «r ECt KI KI let E5I ttr KI VIZ CBE IK hi •H HI ttl nl in HI rn 141 « 1 ■P| i*r rf>a |4 >« E*» ip«) 1 i'll1! |*|«M4IM| izz HI • i 1 i i 1 • 1 1 i 1 1 1 1 i 1 1 1 1 t • i 1 tzi • 1-4rtJi|fcfeia|i| lauKMI «FF | ui'11 I ■ i f i • 1 • 1 1 i 1 1 1 1 i 1 1 1 i Ml'l Kt'l HIT 1 Zlf • ivl Hillr•■isj 1R 11W) i«’n M'l Wl't •H’f «i't m'! IH't Wt lll'l kir‘1 fK’t iw'r ttl't TCl'E lift Ml'l nu'i im'i lit'l m'l Kl'l KA WT nr nzr IUII Tl’1’1 ii Mil'll KI'll hi I AM rnpn«| Ttl r IZM MMI mil ncn rim iKZI lift! liWI IMII ItHI Ifttl IMU mu IKO KfU IZiH mil mu iitti llltl mi 1(11 i rn't Ml'l Ul'l m'l Ml'l m'l UI’I 111*1 IH't lEl'l IK! tit't Zil't wr't Wl't ur'E Hl't zn’z m'l Wt*1 Ul tfi tit u U u it II •t 41 II 11 11 SI ll ri Zl il •1 4 I f 1 6 1 r III iin Kill •EH • >•11.1 «M| t, »M| i I tr ■ B tFii a •’Hl Mn | j>»i p mpA Ml i mu t J*’""! (»'■! j'Jji’PQ v>»r'*"i i '■■**) siSMm ivi wvNit i - vuiFiayiIMH( Hill AR]HARA 5lAG£ 1 ARIA ; FJRAICIAL ANAIT5IS All Cotton in A^ MMIII1 al IMf 1 Ulf Jill . ■•ail 1 ll Mill tea* I link Illi Mil Til if 1 fcMIB 1 IMU ............. LJi 1 • M 1 Ilk I 1 l 1 4 1 1 i ii It u 11 fail M II 11 M II ii H H « II H 11 n II I 111 I.IH I.H» ■ I R l.hk 1,111 1» UH 1 1,111 r,m i.ur 1R■ i.iij ■ i.m ■ .«« Rl ft f.m UM l,H| N.1H ■ l 1a MH 4 I, HI 1 Mil I Mil l Mil a I,U1 ii a.ui i nt hM4.il «rr VM«M 1 IU ik.m 4 II a ii tH l.lll i.tn r.m j.m 1,111 4,411 1,311 1 Ml 1, Ilk 1JH i.w r iff a.in a.Ht a, in •JU a, ilk 4,mi a. mi MH hm 1,I*T »,nr lbiJ Ikr+blMlI .Fill - MftNFilai |«k itiblMr'ilriilHIil l«.rrB""lil 1,0 1 iaill Hfl«H t»| l«a iil Man pFifMfiil i.l ii a Fl/ 1 MH a.m t.fci a 4 a 4 4 fl a 1/1 I a 4 a a ♦ 1 1 a a a 1 a ii,m a 4 HI ill nt
HI JT9 kw hi ill ■J l,IM 1,111 M rr I.H1 l.Hl 4.r» i.an J.U« I.MI iMUn i&Hnaifl mi amru f IMS ■■ MM mil IM* l*.kl| W » HI. ill.I W Mil mi p U T>irtin* a hipii ii l,na M« I.HI i,tii i.m I.KI ♦.Ml MW I.MJ 1.111 I.M I.H4 Mil I.T1I i,ni l.m I.IM t.Hl Mil i,r»i j,in J.Wl I.MJ 14,m i.m 1.lM l m l.ua i.ui I.IM l,MI I.IM n.ru r
i«>flll| HI al ^LHtl pits 4- auklan r^rpl—1 L i A|r( A : iLNUL.Ul AMUSlS 5DX Callon, 2!il Mmic. 25.1 Pasture in ASP — — ----------------—---------------- - _ ---------------- ------------------ '---------------- =—i ---------------------------------- ---------------- L'lltill *¥ kubflf lihlt H.J3 N 3, I i ! * 3 l 1 i 1 IB II ii il *.■4 M* II 11 II ii kt II Hurns bl Hit '1 i.f* M.4 ■ isrr'i htntlkl liua r»Lm.l iLlblduil ijlbkk 11 W n 71 73 hiitt 1 IU ♦ nil 0 iiDi im « it* 111 IJF) Illi 7,371 IIMi kill lllfi 4.1M liin 1,114 IlMI 4, PM hwi S./M Ilin iJJl b«oi 4,134 Ii in Liu IlWi 4JM IlMi BNI k.HII M7M *I|% I.MI lllh k.BI llltl III ’iSL 1H! bin Vm ... ft.HMI INI IN IMii hui ll lulili Illi lift! in Ul l,2H 7,11k 7,LU M12 3,101 l, kN ijh ijn 1,2.43 i.iii i.im 4,ill *,Flt I, Ml 4.141 4, Hl I, IM Mi? 3,111 14/-4F l»li ln*»vkw*l iwfcU il tAfllbtr |k-f < FBI u 4,111 i.HJ 1.461 1 4 1 * • i • ■ * i • 1 • 4 • 1 • • o ii,in !*•< in k-**» |i'ffea.|.MHl 1 m b 4 # D 0 1 • 0 • t I I ♦ i l 1 i • l Hi 111 1 ff bi bl <11 0,N 1 t 1M.H 1J i*fltrrrli*4 t U9 102 HI lart uttihri'v/imimi** i ml I 111 * 111 M ■n t 0 71 111 1 ■n.r‘ 1 ir*f jrid'N lath /H UQ 1 KJ lift 0 111 a MJ out Ml Illi MJ Hl l.ll? in JUj 31 7H3 11J »i rj m 112 DI K7 nz iw 131 a.Nft 74 F ji 17 W if 17 M » 1,717 l,«M Mil >.■* jj 7.MI 7,211 i.m 7,141 >,in IF 7.H7 w 7,0J J57 11 1,111 IF 7,117 7,111 MS 1,111 1 bl ill n i J31 171 J, fl* 1,011 J, III L7h 1.111 I.MI l.tn i,m ■ ,r»i l,1W l.ttl 1.411 7,111 !,» j.m 7,IN 1, J.BM 7,1M l.Hi 33,711 IMLMfttltl Hl 1 IIHUH minjjii IHHI i.JM* II, /HI 1 1,4k Ji i.m l»5H I.WI >.in 1,/rt 1,414 J,IN JJH i.»i 1.U I.M7 J,ill l.ltO 3,113 1,113 1.1“ 1,114 4,111 1,711 1 UM Ml Mtrl ll. Hili ii . in n i mu iii h moi I7t1 tf m«ilinh I* im 4 fta^l 1t iodwiik < Mll e. a.iu .»h I hrtiflllM (Ml* I. 1*1*1 I0 ll F. foil ft ■!***■ u*f 0*1'tt 1 IM NN 1 IMiT ftM ■Mil ’107* Oil fall UH 111 fl fl -mi IMI || 11 i;ti IIH 11 71 mo l?ui 15. il Mil flM'n 4 LU ■IT J 1hn'lM i rm Ml 11.Il ii a ir.i 1? Il Jtu IM.1 11.11 UM Utt 14 JZ U mi 1 11 LMI 1»rr* him 1 kiir'OM ‘inn 1# n UM ■ V 1 11N ' Ml ‘UilL l*r« Fill NO 1 Mii'Mi ■4114 HI774 ■fti If H IMF Mt H 31 71U b>l 14.41 *131 Ml II U IJI INI H II l?tt hi II H 7I1F mi II II l?fll 10Z |}4I 1411 IML ILII 17*1 -* HM I tlir-Mfi >1774 '«72l 1*1 I-Fl IS IT Ml 1.11 IM I Ml II.Il Illi 1141 H 11 I4M 1141 14 U 111 mi l.ll I4H IW 14 41 FI7 1711 1 LI Ml mi 1,31 1334 MlGflilft Oft it *1 Ifi i i*l lacrmr liMifhl ittrrAU IfHHit 4fCtt*lf Im pttaUt* **kn* u H I* ldi II M*vt1«fAl <«dii Id hlkf I IM li 114 I* fMldutlltl ciill l> Irlbj Fltt t* 1*1 Fwi M.l tarriM L* luUk <*iB l« Lf.^f I IM Io Hl I ■U in 131 II 111 Uti I* ffcfjiia-tfUf 4*»vlI*hI&| 141 ■! ^w.bnt plit I*- o.b.Btr fJraal ^kr«l.1 III FbIIumi«Q IRWflt uhrtrlf alhrtM’ll I’A UiMilIllp St** 1 : HtalMHAL Wmifi I Mb Sh^UHrd llrnlvk Ul'rpr III Fulilt*i4iq d|’.bur «,r*ent ^LlbiJUt Aith tiling cuaI r al L ur j .'ll mIiAitiHuh (H.huI, 1■aqtii|iqi4 jn; r «^ll« •!■?*•!•* li'*"'*'“I*'* Ihi-*K*1 HIli^ir l-r. uirhiwt- I Mfft'i I FlNhltl'lN MYS15 ■ >• (idlui. 241 fuui, .‘51 r«tw* m JI'i* I I 1 J 3 I I I I I I I I I I I I I I IIAH r ?ti LHnflU D Slittk IfJIlii! (CQM31K fiHIU T5I5 Um..I 7 I * 5 • I n 1 b> II k. I* II kJ 14 IP ti kf ?• iJHl'iS || M r II
n II Lt 1 L ♦»* if n lf.il IP 14 IPJI 1JJ1 IP. 10 IP JI IP.Ill IP HI >.IA iw.ia. la.rilkrnl lkt< tPtliLil 11. «Xi MJ I I'.i’V 1.H 4 *3 Ml n. 41 4.11 4. fl L*S *.W 1 JI 0.4/ o.n o,i; 1 1/4 t,u u.?l dju O.U't OJA B 71 4.'i M 11'. 1H> •.54 Ou •.bi ,H0 li.fcf D.*> MI 0.00 4.11 O.fr. 4.1? 4 V4 b.AI • »• i.kP Q.VO fr.v 0.UO 0 IP c.nv • IP •.On ■ IF ».u€ 1 J.P 71.Al 1 "j 1 in r * iir»L jI hr* [Lil& U.Bl i 1.54 2.17 IJl I.W 4 TO k?i 5.40 5.1'. 5« 4 .* 4.1? i.n US MS Mi hW Ml I PS P 15 P.is J.W l.c Ml in. bi llhlt «.U io.c-t Mi 10. Ul IM1 4 II 5.TH 5 41 l.l? Mi t R.' Ml J.ia p.ra P.DJ a «? o.is fl. 21 D.]? l,W H.17 I J? fl. If n. J? i.W i’j./ft iHTI^tllff RIJM ItM Al *111 M.All n it* 15. Hi ii hi* II./Uk 1.41 tit •J.‘ MA LK r it r l.’ UJJ fJ5 1.2? Ml 1.12 Ml US Mr MB UH 150 1.19 II.14 IM! ELIiMillL iMISilSj 11 Ml: II.vl; W* I 101s Im ■llll«r I5.M MAI 1515 111 9H5HMU Lu ■k/kMlhUi It: A. itl^uL 1. IkTrilProl inti £, d.hkH iinh • fl B0MI 1 Hill 1 IH| t 1 Mil 1 Dll » 1 ilu Hl rur»l|H (mtfMl« .................. — — Vii b i IfaH « 7 hi • (Ifcl ■» hi n TIN
rki 75. 121 Hip i F b lion* n-nhiLlDf mull IMfbmb Ihr Inchon ff
Hin liclor.IftUk „A CmMHMI 0 SIM I DU : EflAllML MNVSI5 I'll H Lunlod hltiprivl fe*r | 2 J i I 4 7 m T ID H 17 |A u IS It. II II It 2n 21 22 2J ?l 25 l*fl 1H1 urn* BUfFiis "»H * -dl Pi Itflh PfM '■•»bir t trior kb mu* Ilk Ul il b Mjn 4.12 lx MJ 5.1? 6 At B.W 9. h« MJ ID U Jl*l 12 U Lw ILU ILK IL ft Illi IM1 HAS IMI ILK IMI IJAJ 11. H list 41 Av
« O.(k* 4.04 v.W u.4t 4 00 4.40 U.DO 0.04 v.4u ILU4 71.15 l*r* rtfibhl L6.H.B k D- U
M HI W mH II h*A5» It HI IS,111 H.M (Mil Mi M7 4 At 5.29 S.tl 4. IM /on i.m 0 ?5 U.JA fl.U 1. ft Ml ILMI das in S« BA 4 HAS III.OB ri.n UvhJilL .Mkbhi Llhk 15.51; hf-U V |«: Birr uIUqa: 11.ft I'llinliSIS * W’ 111/11 k In >«*i«Iimi\ ml ft. Uuli.ul VwH IlhR WM 1 Hir« n H215I1 dm kl V 2 LIH 12.5 A.UJ ll'i'l U.S ii.ft Hui iii.; 2i.« Jjil 1'iM ’Mj 4, Inrr^lnifit (Olli UlM llkl MV I lire ■ U7J1I IJAJ HOL H A 14. ID W 14.2 IS.i J hrfl HA ILft HUI 14.1 L* 4< 1241 HA 11.22 L. u.ftkn <»Ui Vji h Hk1l M'U I Dih M. »t?H* d25] Hl 15.? H.U 141 ISA II ?v IM ISA ll.ft HOI 15.4 |L?I I'M ISA IMJ I h D*iX IlM (Pill ir*i » IIM (. talal (Mil d* t HfeH NPV L Ik* nl Itrtiqn cptilridflr tJHlTa 11.» l?1 Z Inr n. iUIH N2H Hill 111.1 711.4! vm II.H JF..M loQI ISA HAS llrt IL2 1I»A2 |?tt IM ?.?• I Birr fl. W'V ■ ID ti Hirr ■illmi >f2J]i d?JJ HD1 27.7 37.0*1 M4I I4A W.I0 |i«I ISA IJ.ft tlvl 17.B MJ 1241 (■. J « IJHi. Il-H MV 1 ID li (Birr iilllvnl I7.B1 C. 1 *'■ 'Htipl b( Hrnolili S.H ^IliHLUh ViiHIIS: UfLlS J-.r J* UlLJuC'lut ulku 10 - ir.rr>a = f J* invfElatul rMls Ip iFrr fj*" IM I f-J i- Or mg flH trinq fill <|kH fcft M-l: la loli 1*1; I b I a-ra I I fl Ij n<| b* 1*1*1 [
l pdifi nF Ji|| jo JviiiiMifl IfeufipM Jp AlHJ)v1 pr*|i| ntlJj*!) t |'> 4*i| 7l Mil mi UB|tA |lh|lttJ Hip‘.|nl| dl nt iff i 1DC W| 0] lj[j[] fiitijq. B| t|*Q> |ri*J| «| rffcH'Mi JIM *1 Mi l«H1 *1 '1M»J ■*} »l : Pi| •! Ml J >■••• °1 *1^*3 |f«l|14IIH II 4K4J14I . •I'd D1 IlHli cn ■< t| »*|H Mdii iiip-jjd JSjniiirt wliiulhS M'1| IMOI11 |V Hl|| II a! I Ml •rzi ni lid cri'Z rd W1 wtt 171 Hk'l U'lZ l II MCI till ru x^i IIXI iflIJ ^ii A’fl Illi tri/ V Bl :i-l i si •« 1 ‘11 l"ll il’C • II Idll irtf I7f lul l HT B'AI l*M uk im l«vl ia*k B’il WU H"W I II IDOI ini i'll :mi i|ip»iq j« «i jitdOp jrd | ‘J :<*h era 144 K'K
|IH 1 pjill| jap I’Jii » UtAIJKHA « SlsnsMr It K :«OL||iv ji|| =ID| 4 ftj| !lli| itffi? s$15IW JI Will)! H V* II K7i ITU K7I •m UXI trd 1171 HO II iG’ll ii ii irm •n'A UM 4 Ul W 1 If'fl Kt 417 ill'll Ill'll i/rci il/'il urn Hum i.fi i»rjiiimiriifi II II •rm K 01 KD1 Ki 1 K*M K’fl KM ii «i ori n 4 11*4 ri a d'i H'B 10 f orf AZ‘? lll'f IVi 11 4 IV 1 n i Hi 11J it i ID7 Wl ll’f io e Hi 111 iri fl 1 ThC HC zrc m G Im tro /Fl 11 • lift tlfl ill /I o 11 « in I'll' IS J v. ■ 111 BCD fl • iW’fl ZBD ii • wn in 4t • 17 •rt'O •0-6 Mi 4 Off wn OP 0 llO'f Oil* irt ** I»o' HD W'h 44 0 fro tri i‘/»7 if’ n’t BA U’iC Tl7£ lG7t wa H7E K'K U \7 IL7Z il’li ir i: HW H'4I K DI IC II fGrfl nil or ii nm 4G II ZS'4 nt frr Zii I£ Art K 4 tt’i <7'4 Dll Girt Ell fax it J LG*1 ♦4 G 11 fi Lt 1 uro ill ;ri •IS [fl'I II'II imi 407 H fl it'd 6i7 tri ill im rtf'll mm Ifi W J 11 0 AID tri in ira I0D Wf 1JH3 vjr| |f]MillilU| ! 1‘BD |»|-m**i«| |*npJtM| Cl HTI Till im irti 11 H rrn UTl If fl lill Dm nn cm TH'ud trcr lVII Ti'ni /l‘A HI ii
t|Mi ci I rm it Imiip) A JI K tr tt it wZ n 11 d fi II ll ;i II iM A D t 1 G 1 1 L • im i JSU ui 11V SISUUW JIMDWJl t CfJlf I mSO'IWII U". JMI•JOpq VOIIHiUVJ f** »|WJ |N
Add 11(1 ’Hill 017 C7I TtEI fill rll Iftll irw 14 X Q7l IC*|| |iu»i «i aMd
] uJip^i.1 fl iix 1(1 XI i/>: (71 1011 *X nil TOOI oepe All T« iri? ft’lll too Kth .» »’1 i *!■ nil ’ JTfl * »*•' |l! Ill’ll J Ulf Gil I0EI kll'bl nt 10 H WHE s n IWI H7? 111 1*4 iru 111 10U t wr» •UEH N Niff 1 AN BIU ■ W|| 1 poi pi4i|5d Ifl ■[ 1 T.E I’
ft| iiiAlir.itr. nr 5l
J| 51 Sfl I CT Ml « U irK 11X 01X 11 x 40 X (
ffjnlHUfll W IIM'H•wpr| UDIlH'hflp dq|i i-W M«> 14 *4 *'|| |* jinurtiW 1 itaffllfl wfcl*W>J If] KIDWI PI*** [ff «b11 *>L T |H »fl |£| ’« ml b| 1m|va irrtfilJi bui^p«| ||| E14I V] HIM HU' «| &]»> 1MM Ml *IN»M IBS Wl 111] 1*1*1 M sl«> uj m*iw> - Ilfj |P£ : IN *1 MH 11 “I ’I*8* !•" I ***•!■ Mi iilWUl -l«l O| 111 I *M1H
ilD I Mlf HUI t " *1 '( * *) iboi1.iiipmj a m-ii Z'*i 1W.I irri r« ZOII U II fit Iftil ii ii TN mt ii ti mi i*t EHf* UH* 'll ,J,i 1 AH HI! H’fl in Nil W/l GN l«l mu D If mi ■in I If 109 Oi'l rrr • "■ ll’U CN INI H’H T[J I" II U*j| t'N ?
■1 l$'1 1*1 Bl S U G All G •rs 11 s €i S SL'fl IE ‘fl ‘HJ'B Hl !L1 H'f sii Il 1 *ri C lie ni o uii‘n a# 7 fib l W 1 H 0 111 ft 1 Hl El'fl Elf Ik B k'L f Ik 4 N • « K » n* 11 'U i£ < 11‘U £i • 4E1 tl ■ til « Bl i. irtfl 00'Q M fl to-* non Du 1) «1 *i * i*Q# <*ri> M«
■ . ... .. ■ u . . x . a a. . a a a t a . . ............ . . a . a.. . . >. a a a . sisnj III "11 U’-P*J1 1 ]*“■ 1* J*I*A <11 j in iu ft BE If £i IE rf 41 ii £1 II SI ii 11 Zl ri id i a f iSt i e | - JPM M5I foffll IIHIHIH ViW I MVI5 I,ITS VPK IE 1 WMIAUH Z2 Awl BARA SIAGc t AREA;ECQHuMlC AMLVSISIMIHL 22A - STAGE I AR( A; ECOWME ABH ISIS (Milk S5«pl iFied LiweUtck InUrprUcI TtM 1 7 1 t 5 1 1 « 1 IB II 11 11 II IS II IF It IT 21 n 22 21 21 23 Imiajl Ut Mil Mt 1 III Mk ■« n
.11 1 11 7-71 L« 7 JI i n ... J.H Ml 1 .17 1 II 1.17 kN Ml <71 Lit < H 1 1.1 111 HU Ift.lOl ILBII 1.11 I.UF 11.111n.rti IL «l IL Hl II 111 ILI9I ■Mil IB 111i t Bl ILIN 11,111 LU l.ll 1.11 in 1.31 I.H 1 21 Ml 2 11 7.M 1 21 IM IU l.ll LIS 7 Bl I.H 1 II • M l.ll LU 1 II IH • H I.U LN l.ll I.H LU l.ll IM • 11 1.21 Lit Ml .M H . imii ii.Mi u.m n, J l:| ||.Ill 1 It. Iti It. n r II, J TI !• H1 H. 211 LI. I.U 11.Ill 1.31 1 ft Ml 1 11 l .ll lii 3.11 1.11 Ml l.tl 1.M > 11 Mi LU IM? Lil • M Ml I.H LU LU • Il LU I.H I.H I.H l.ll ill IM 11 l.ll LH LU I.U • II LU LU l.ll I.H l.ll 1.31 I.H 1 II i.ii rn III •31 1.13 I n 111 LW in Ml IM Ln 1. 73 i ii •JI •JI I JI 1 It 111 I 11 l.ll Ll| 111 l.ll l.ll 1 H III III III • n III Lil .«• .11 1 71 • ii 1.13 II! LH Lil 1.21 1.77 Ml 1.32 1 17 • li Ml 1 II • ii 131 737 III in HI III I.H I.H 1.11 111 1.11 111 Lit ill ■ 21 1iimibi«I*I fUhUm I.U Ml Lli I.U 1 31 Ml 1.31 M1 Mt Ml Ml Mi 3 71 Mill I.H III 1 11 Ml LM LB III i.tt 1.71 l.rr 111 1.51 1.71 M3 1.33 LII Ml I.H Ml Ml I.H Ml Ml Ml MI Lit 1131 IMUHIIM Ml MUI II IIJ5I ci.iiMi.in13.131 It MF IL 111 1 J? LU • 11 • Fl 1 II 1 W 141 I.U MF Mt 1 IU Ml M1 1.17 I.H Ml Ml I.U 1.31 11 Ml IIMBIC MMirVSi (lit l.Jlj irv 1 lib lilt I idliMl l,H Mursis V aMHltlH It tv nil Hl IM 1 BnlH 1. ItirtlMfl itill I. t.BU ml« D. ITHmlIim talk I. hid («Ji I. Vfrt «l I* Of* cmUmIwt IfiilH VT Yf [IU WY Im lit rr Ur n till ‘ UM n 1111 Ml 1 Birr th 1 Blit Bit t Ififf 111 I Ihf *!• 1 IHf ill UY 1 lit lllfr tllllMlll.BI <1717 Q 7I7 Flflll IJ1I7 d>H» *JJI2 dill* Uli] din uni •II LI Hl 1.1 LU 3.11 Hl M Mt 111 Ll 1.13 HZ 3.1 -Ml Mt 3.1 -1.25 DIZ 1.2 HZ l.l -Lil 2.11 Ml M 1-33 lit 21 -1.11 I. 1 jeN tl h IM-vipt nJ hriiFHi lUi 3.1 -I.U IHi 3 1 -I.H IHI LI Ml IHI LI 1 H INI 3.J LH ............ .............................................. Illi LI -7.31 nu i.l lh IHI LI M3 LLIZ M Ml Illi M -5.Bl 1 lit l.ll Hit II Ml 1211 1.1 111 1711 1.1 -Ml 1711 1,1 LH mt 11 -M3 NT t III IM it dillMMl33F feiiuiac vjuiiu k«f(*W l> IIm ulu l» IHn| IIM l» Illi 7D1 - inrun li lr>«tl«rtl ehIi Ii Vl*| IIH Ii Illi Wl taitifi hpUiKiiF mh ittoi*j rm it mi -hi (Him! li hid eqiIi l« toiM tIU It HU HI in till II J iftrripi tMlttLltr Mill k*rrfivt hit Inlip tl IU pi|rtl ri|lwrlM tni> mJ Um« IU nawakt lnl*.■||JH IMMhwi HMW4H 4i|| IJiJ, |*W !)W1 •«* <■/«!*■* **llfp4 tlf| |Q | H'i|fld«f41 > I fl ** | M* 11*1*1*' M||*«p4) r (U ||j w »ltl "I fftf **i *1 • ! tiw» 1*1*1 iwimi • in °I hut m *r**i wiiwtii m nuthi ! l*r • * ttj 1 ^MIM *1 t|WI t| itMJilil - /Fl 1MIIIW l'*|1 III I MI nil -------- —----------- -------- - — — mi IFI T IT llfl If 1 til Illi III 1 II 1MI nn m m cr ii rst i» (Mb flEI* Tl 1 i fi wi lit 171 nri IFI Fl1 ml IF! • 11 lit! If 1 tn 1411 Ifcl • n 11*1 |0 0n)ij II (II irn jfM 1 ■} mi 111 1H Hl hi 1H «■!! Ill 1 AM U|« mi I fl’ll FM 1*1 eifb ifltl I up "U i m u« m jh Ml Mill •JI HI HI IM < Hfa ifW up nil z A JI Mill III 111 in- IFI (11 tin IFI 171 tnr UI 1 11 14*1 ri ti F« »♦ It'll Ftt iiir« Hill’ ’I* 0*1 I AM nil . *»* rt| It W «*l■*! H «A 1 HUI |Fp| I »i«j ■n*r»»i i «wi VH C * -j 1|»1 |>14t1»l4li| | •1*1 M nr? M*j* •> «|M un||i*fHTfi is MHnap 15 in iw wmjiiirt nci 4 1/ ifi (t
MT If F Hi t(f EFf 111 UI Ct • rrt •* Ilf 11 n t ni h tri ti IHIRN m WIIKHJNI 51 R KI Hl HF Ml HI •i r •IF MT wi 5FT 111 Ifl 1*7 II Z Ifl U1 n1 1/ 1 Ml K7 irr tri IFt K1 iri tt t tpp| till r. r TCI K’l Ki m KF KT wi III HE ire Iff HI HI HI Jfl III HI UI Ml it i IT 1 if l tn ii • wi|pnpnt4 Mm |rpivfpii| It • H‘t HI II I HI Ht Ht HI HI Mt HI ifi Ml HI nt IF H It I IF! Ml Ml ii i Hl Hl Hl Hl IMdiiinbdJ ^upipi i it| rrt Ifl IF ■ K• IFI IT 1 IT ■ It 1 IT • lit iri ifi ?’♦ Wl It I Ml Ml ft 1 Mt w• «•! IFI IFI «1 It 1 HI - 1 ff| |HWtU>i|| nr K’4 Ml hi H'l HI iri •Ft •Fl •Fl •Ft Mt •i H IF II If 1 Wl It ■ tt 1 If • Mt It • Mt Mt Mt It t in HI Ml HI HI Mt •Fl H1 HI It • Mt •Fl Hl III «’• Al I III Ml Mi It 1 HI M’l (FI Cl 1 IFI HI Ht fill JlJMttwi HIT Ml •t 1 III H’l IZ1 111 til Ml (11 IE7 47! IFS if; TAI IFF ni ?FT HI TFE IFI IFI ffl It 1 Ml cfi Mt rrtr l*‘l HI Mt Mt H 1 Hl It 1 in lit HI Ml Ml HI H t Ml Ml tt 1 i« • it • it t •I t Mt Ml H t Nt •t I Fl «ri Ml Ml Hl «1 ■ri W1 fl 1 (17 «7 15 1 ♦H Hl Til •ft 1 lb ZFI Iff Fl f 4F1 IFI ft • IF# M I ”1 II” 1il|f ■■■ 51W J qrp| tJt|r* pMm| ■ |»|l,| 1« lipipq 1JVH *.*1111 p »Pft fitnuN Ml 1 **IM AM |M«I*1 « H rz rt If •f ii HI M fl Cl II fl fl II •1 A 1 t T 1 1 t I fr»| J! * »i w»)»3 H* sjsi ivh jtMMoai tTjiTj irr. vhhhim^^^hz^ i in*lI*>1H ??C - Ml non SIAM. I ARFA: ECtJNUKI L ANALYSIS S(lt M,UIC , 25X I'*-, tore ni *L rF I B v 1 £ 3I I ■ ■ a ■ ■ i a i i i i i i i i i i iFIGURE 1 Korftj™ Swamp L -* urwni / ' STUDY AREA □EBRE iE5H11 /ANGELELE .Mirsio AWASH STATIN / BOLHA pi'^. MF. □oton !&o Mfarer (A mi bora Irr. Project H V’:=MELKA SADI Dire Dowa ly A A £w05h Station Meta hora Aodis Ababa Atdis At-cca METAHARAI I I u D I I IL EHENfAflON Pt lllOOS IM5 - 1990 (STAGE T) 1990 - ms I99S - 2000 fikQ£K ® Mfl KA 5A0f (C) AMIDARA (b)MEI KA SADI (d)AMIBARA ®AM|||ARA EXTENSION (f) AMltlARA (G) AM I BARA EXTENSION NET AREAS - 2560 ho 3 I 4 MO ho - 2QBO ho J - 1330 ha - 5 LAC ho 3330 hQ - 930 ha -2 540 ho 3910 ha - I3JU ha TOTAL 14.200 hQ MASTER DRAINAGE PLAN FOR MELKA SADI AND AMI BARA AREAS MASTER DRAINAGE PLAN INDICATIVE DEVELOPMENT PROGRAMME q c * S4f WHIium Halcrowl Partneri July 1983FlGl Rl 4 r »>• LEGEND LOl*fOI Spoc«nq I "•■ ■"• i ■ 1 «>•" lT” J * RoborxMtttC Dr Oi nobiMy Clou no Cb EC HO L«***it o< voil Purvey S»Oge I Oreo bounOO’y MASTFR DRAINAGE P.AN FGR MElKA SADI AND AMlBARA AREAS FIELD LATERAL SPACINGS FOR STAGE I AREAS \kFIGURE SIR WILLIAM HALCROWS PARTNERS JULY I9e5 PROPOSED IMPLEMENTATION SCIIEDU|£ FOR STAGE I T ACTIVITY I CALENDER YEAR | I PROJECT YEAR | HELKA I SADI Arrange Funding I Tender & Award of Contract I Main A Secondary Drain Deepening incl Structures Subsurface Drainage> In-Field A CoJlectors Surface Drainage System including Structures Construct New Main Drain, Deepening at Existing Secondary Drains incl Structures Subsurface Drainage, In-Field A Collectors Surface Drainage System including S trudures I Area Under Annual Not Total - lui r~-----------------1----------------------- 1 11)60 I Subsurface 1 1 Drainage [ Cumulative Nut Total - ha 1 i 1060 1 1600 133Q 3660 __________ ________________ 750 4760.KFSSEM RIVER NEU UQRKS --------------------------------SUB - SURFACE COLLECTOR DRAINS DIRECTION OF SUB - SURFACE FIELD LATERALS ___________________ DEEP OPEN DRAINS NE* TERTlAOr DRAINS S’AGE I AREA BOUNDARY CULVERl 1 c 1I algfta farm AM'sAS- FIGURE 7 PROJSEHCTSETnEMENT p^*t, S Tl EM PROJECT EXTENSION r - ENT EiiFtinC ff.cn (Jro<- (BQ* ) Ou!‘c \\.^M \ 'Emrrgenry spiiiwc) \ flood dyke and dram ---------------------------- ACCESS ROADS DYKE SFTTiE’“ STS PUMP STATION SUB - SURFACE COLLECTOR CRAiN$ BECTON OFSUB-SU^ OEEP OPEN DRAINS NEW TERTiaRv DRAiss STAGE I AREA BOUNDARY © CULVFRT SCALE 1 4.3COO MASTER DRAINAGE PLAN FOR MELKA SADI AND AMlBARA AREAS AMlBARA STAGE I AREA SURFACE AND SUB-SURFACE DRAINAGE LAYOUT Sv Wilitfim Hotcro* 1 Pannpfj ju» <98* r■ I I I B I I nSIR WILLIAM HALCROW a PARTNERS JULY i98f MASTER DIM INAGE PLAN FOR ME IKA SADI AND AMIDARA AREAS Propoacd OrganlaatIon for Site Supervib Lon
🔊 Read Aloud
⏹ Stop
<
Summery
<
×
Summery