Melka Sadi-Amibara Proposed Irrigation Project Feasibility Study
Part II: Soil Science (Volume 2)
Commissioned by: Imperial Ethiopian Government, Awash Valley Authority
Conducted by: Italconsult, Rome
Date: July 1969
Study Area: Right bank of Awash River, covering 28,548 hectares
1. Introduction
The study was conducted between December 1968 and March 1969, involving:
- Preliminary photointerpretation using 1:10,000 aerial photographs
- Detailed soil classification at 1:5,000 scale
- Detailed land classification at 1:5,000 scale
Methodology: 1,682 soil profiles examined (400×400 m grid), 14 piezometers drilled, and 400 test holes sunk.
2. General Features of the Study Area
2.1 Geomorphology
Three main geomorphological units identified:
- Recent alluvial plain: Very recent deposits with variable textures
- Old fluviatile terraces: Two visible terraces with gravel and sand
- Volcanic formations: Lava flows and outcrops of various ages
2.2 Drainage
Characterized by temporary streams draining to the Awash River, with uncertain drainage patterns in some areas and a swamp in the northern part.
2.3 Vegetation
Three parallel strips from river to terraces:
- Tunnel forest along river banks
- Scrub vegetation on alluvial plain
- Sparse vegetation on upper terraces
2.4 Soil Formation Factors
Key factors influencing soil development:
- Parent material: Volcanic origin with variable textures
- Climate: 500-600 mm annual rainfall, mean temperature 25-26°C
- Relief: Significant impact on soil moisture and erosion
- Time: Different rates of weathering in various landscape positions
- Human influence: Overgrazing, vegetation clearing, and compaction
3. Soil Classification
Based on the U.S. Soil Survey System (7th Approximation), 12 soil mapping units identified:
Mapping Unit | Description | Area (ha) | Classification |
---|---|---|---|
1 | Soils on very recent alluvium | 2,076 | Ustifluvents (Entisols) |
3 | Vertisols on recent alluvium | 3,362 | Vertic Usthortents (Entisols) |
4 | Non-calcareous vertisols | 2,035 | Chromusterts/Pellusterts (Vertisols) |
5 | Hydromorphic vertisols | 3,710 | Udic Chromusterts (Vertisols) |
6 | Soils with frequent texture alternations | 8,251 | Ustifluvents (Entisols) |
9 | Soils on terrace alluvium | 5,803 | Calciorthids (Aridisols) |
10 | Saline and alkali soils | 1,899 | Saline/alkali phases |
11 | Calcareous soils on pebbly terraces | 451 | Calciorthids (Aridisols) |
12 | Lithosols on volcanic rocks | 193 | Lithosols |
4. Land Classification
Based on U.S. Bureau of Reclamation criteria, assessing suitability for sustained irrigation:
Land Class | Description | Area (ha) | Characteristics |
---|---|---|---|
1 | Prime arable land | 969 | Best soils, gentle slopes, good drainage |
2 | Good arable land | 13,124 | Moderate limitations, most of alluvial plain |
3 | Marginal arable land | 6,230 | Significant limitations, restricted crop options |
4 | Limited arable land | 457 | Severe limitations, special management needed |
6 | Non-arable land | 7,768 | Unsuitable for irrigation (terraces, rocky areas) |
5. Key Findings
- Most arable lands (Classes 1-3) are located on the alluvial plain (20,323 ha)
- Vertisols and Entisols dominate the alluvial plain
- Aridisols dominate the terraces
- Main limitations are salinity, soil reaction, and drainage
- About 27% of the area (7,768 ha) is classified as non-arable
6. Conclusions
The study provides detailed soil and land classification information essential for planning the irrigation project. The alluvial plain contains the most suitable lands for irrigation, while the terraces are largely unsuitable. Soil characteristics vary significantly across the landscape, requiring different management approaches for successful agricultural development.