Soil in Inderta

The soils of the Inderta woreda (district) in Tigray (Ethiopia) reflect its longstanding agricultural history, highly seasonal rainfall regime, relatively low temperatures, overall dominance of limestone and dolerite lithologies and steep slopes. Outstanding features in the soilscape are wide plains with Vertisols.[1][2][3][4]

Factors contributing to soil diversity

Climate

Annual rainfall depth is very variable with an average of around 600 mm.[5] Most rains fall during the main rainy season, which typically extends from June to September. Mean temperature in woreda town Kwiha is 20 °C, oscillating between average daily minimum of 11.3 °C and maximum of 28.4 °C. The contrasts between day and night air temperatures are much larger than seasonal contrasts.[6]

Geology

From the higher to the lower locations, the following geological formations are present:[7]

Topography

As part of the Ethiopian highlands the land has undergone a rapid tectonic uplift, leading the occurrence of mountain peaks, plateaus, valleys and gorges.

Land use

Generally speaking the level lands and intermediate slopes are occupied by cropland, while there is rangeland and shrubs on the steeper slopes. Remnant forests occur around Orthodox Christian churches and a few inaccessible places. A recent trend is the widespread planting of eucalyptus trees.

Environmental changes

Soil degradation in this district became important when humans started deforestation almost 5000 years ago.[11][12] Depending on land use history, locations have been exposed in varying degrees to such land degradation.

Geomorphic regions and soil units
Typical catena in the gently rolling Antalo limestone plateau

Given the complex geology and topography of the district, it has been organised into land systems - areas with specific and unique geomorphic and geological characteristics, characterised by a particular soil distribution along the soil catena.[13][14][15] Soil types are classified in line with World Reference Base for Soil Resources and reference made to main characteristics that can be observed in the field.

Gently rolling Antalo Limestone plateau, holding cliffs and valley bottoms
  • Associated soil types
    • shallow stony soils with a dark surface horizon overlying calcaric material (Calcaric Leptosol) (3)
    • moderately deep dark stony clays with good natural fertility (Vertic Cambisol) (10)
    • deep, dark cracking clays on calcaric material (Calcaric Vertisol, Calcic Vertisol) (11)
  • Inclusions


Gently undulating Agula shale plateau with dolerite
Typical catena on the undulating Agula shale plateau with dolerite
  • Dominant soil type: stony, dark cracking clays with good natural fertility (Vertic Cambisol) (10)
  • Associated soil types
    • rock outcrops, stony and shallow soils (Lithic Leptosol) (1)
    • red-brownish loamy soils with good natural fertility (Chromic Luvisol) (20)
  • Inclusions
    • deep, dark cracking clays on calcaric material with good fertility but poor drainage (Vertisol) (11,12)

Mekelle Graben
Typical catena along the Mekelle Fault escarpment
  • Associated soil types
    • moderately deep dark stony clays with good natural fertility (Vertic Cambisol) (10)
    • deep, dark cracking clays on calcaric material (Calcaric Vertisol, Calcic Vertisol) (11)
    • moderately deep, red-brownish, loamy soils with a good natural fertility (Chromic Luvisol) (20)
  • Inclusions
    • Rock outcrops and very shallow soils on limestone (Calcaric Leptosol) (2)
    • Shallow very stony loamy soil on limestone (Skeletic Calcaric Cambisol) (5)

Strongly incised Giba gorge
Typical catena in the severely incised Giba gorge
Giba river near Inda Mihtsun
  • Dominant soil type: complex of rock outcrops, very stony and very shallow soils ((Lithic) Leptosol) (1)
  • Associated soil types
    • shallow, stony, dark, loamy soils on calcaric material (Rendzic Leptosol) (3)
    • shallow, stony to sandy loam soils on calcaric material (Calcaric Regosol and Cambisol) (21)
    • brown loamy sands developed on alluvium along Giba River (Fluvisol)


Ancient river terraces
Typical catena on ancient river terraces
  • Associated soil types
    • shallow, stony, dark, loamy soils on calcaric material (Rendzic Leptosol) (3)
    • Deep, dark cracking clays with good fertility, but problems of waterlogging (Chromic and Pellic Vertisol) (12)
    • moderately deep, red-brownish, loamy soils with a good natural fertility (Chromic Luvisol) (20)
    • Brown to dark, silty clay loams to loamy sands developed on alluvium, with good natural fertility (Fluvisol) (30)
  • Inclusions
    • complex of rock outcrops, very stony and very shallow soils ((Lithic) Leptosol) (1)
    • shallow to very shallow, very stony, loamy soils (Skeletic/Leptic Cambisol and Regosol) (4)
    • shallow, dark, stony, loamy soils on calcaric material, rich on organic matter (Calcaric Mollic Cambisol) (23)

Alluvial plains induced by tufa dams
Typical catena on Tufa dam backfill
Tufa dam in Chelekwot
  • Dominant soil type: deep dark cracking clays with very good natural fertility, waterlogged during the wet season (Chromic Vertisol, Pellic Vertisol) (12)
  • Associated soil type: stony, dark cracking clays with good natural fertility (Vertic Cambisol) (10)
  • Inclusions
    • shallow, stony, dark, loamy soils on calcaric material (Rendzic Leptosol) (3)
    • shallow, very stony, silt loamy to loamy soils (Skeletic Cambisol, Leptic Cambisol, Skeletic Regosol) (4)


Soil erosion and conservation

The reduced soil protection by vegetation cover, combined with steep slopes and erosive rainfall has led to excessive soil erosion.[11][16][17] Nutrients and organic matter were lost and soil depth was reduced. Hence, soil erosion is an important problem, which results in low crop yields and biomass production.[18][19] As a response to the strong degradation and thanks to the hard labour of many people in the villages, soil conservation has been carried out on a large scale since the 1980s and especially 1980s; this has curbed rates of soil loss.[20][21] Measures include the construction of infiltration trenches, stone bunds,[22] check dams,[23] small reservoirs such as Addi Amharay, Arato and Hiza'iti Wedi Cheber as well as a major biological measure: exclosures in order to allow forest regeneration.[24] On the other hand, it remains difficult to convince farmers to carry out measures within the farmland (in situ soil management), such as bed and furrows or zero grazing, as there is a fear for loss of income from the land. Such techniques are however very effective.[25]

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gollark: Position a trampoline below the window.

References
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  2. Hunting Technical Services. Central Tigre Development Study – Tigre Province Ethiopia, Working Paper I: Soils and land classification. Hemel Hempstead (U.K.): Hunting Technical Services Ltd.
  3. IAO (2008). Land evaluation in Enderta District - Tigray Region, Ethiopia. Firenze, Italy: Ministry of Foreign Affairs, Istituto Agronomico per l'Oltremare.
  4. IAO (2014). Land evaluation in the May Gabat watershed Enderta-Hintalo Wejirat Districts (Northern Ethiopia). Firenze, Italy: Ministry of Foreign Affairs, Istituto Agronomico per l'Oltremare.
  5. Jacob, M. and colleagues (2013). "Assessing spatio-temporal rainfall variability in a tropical mountain area (Ethiopia) using NOAAs Rainfall Estimates". International Journal of Remote Sensing. 34 (23): 8305–8321. Bibcode:2013IJRS...34.8319J. doi:10.1080/01431161.2013.837230.
  6. Jacob, M. and colleagues (2019). Dogu'a Tembien's Tropical Mountain Climate. In: Geo-trekking in Ethiopia's Tropical Mountains — The Dogu'a Tembien District. SpringerNature. doi:10.1007/978-3-030-04955-3_3. ISBN 978-3-030-04954-6.
  7. Sembroni, A.; Molin, P.; Dramis, F. (2019). Regional geology of the Dogu'a Tembien massif. In: Geo-trekking in Ethiopia's Tropical Mountains — The Dogu'a Tembien District. SpringerNature. ISBN 978-3-030-04954-6.
  8. Bosellini, A.; Russo, A.; Fantozzi, P.; Assefa, G.; Tadesse, S. (1997). "The Mesozoic succession of the Mekelle Outlier (Tigrai Province, Ethiopia)". Mem. Sci. Geol. 49: 95–116.
  9. Tefera, M.; Chernet, T.; Haro, W. Geological Map of Ethiopia (1:2,000,000). Addis Ababa, Ethiopia: Ethiopian Institute of Geological Survey.
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  12. Blond, N. and colleagues (2018). "Terrasses alluviales et terrasses agricoles. Première approche des comblements sédimentaires et de leurs aménagements agricoles depuis 5000 av. n. è. à Wakarida (Éthiopie)". Géomorphologie: Relief, Processus, Environnement. 24 (3): 277–300. doi:10.4000/geomorphologie.12258.
  13. Bui, E.N. (2004). "Soil survey as a knowledge system". Geoderma. 120 (1–2): 17–26. Bibcode:2004Geode.120...17B. doi:10.1016/j.geoderma.2003.07.006.
  14. "Principes de la cartographie des pédopaysages dans les Alpes". Écologie. 29 (1–2): 49. 1998. ProQuest 223074690.
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  16. Demel Teketay (2001). "Deforestation, wood famine, and environmental degradation in Ethiopia's highland ecosystems: urgent need for action". Northeast African Studies. 8 (1): 53–76. doi:10.1353/nas.2005.0020. JSTOR 41931355.
  17. Nyssen, Jan; Frankl, Amaury; Zenebe, Amanuel; Deckers, Jozef; Poesen, Jean (2015). "Land management in the northern Ethiopian highlands: local and global perspectives; past, present and future". Land Degradation & Development. 26 (7): 759–794. doi:10.1002/ldr.2336.
  18. Tesfay Berihu, and colleagues (2017). "Soil carbon and nitrogen losses following deforestation in Ethiopia" (PDF). Agronomy for Sustainable Development. 37 (1). doi:10.1007/s13593-016-0408-4.
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  21. Munro, N. and colleagues (2019). "A History of Soil and Water Conservation in Tigray". Geo-trekking in Ethiopia's Tropical Mountains. GeoGuide. SpringerNature. pp. 477–493. doi:10.1007/978-3-030-04955-3_32. ISBN 978-3-030-04954-6.
  22. Nyssen, Jan; Poesen, Jean; Gebremichael, Desta; Vancampenhout, Karen; d'Aes, Margo; Yihdego, Gebremedhin; Govers, Gerard; Leirs, Herwig; Moeyersons, Jan; Naudts, Jozef; Haregeweyn, Nigussie; Haile, Mitiku; Deckers, Jozef (2007). "Interdisciplinary on-site evaluation of stone bunds to control soil erosion on cropland in Northern Ethiopia". Soil and Tillage Research. 94 (1): 151–163. doi:10.1016/j.still.2006.07.011. hdl:1854/LU-378900.
  23. Nyssen, J.; Veyret-Picot, M.; Poesen, J.; Moeyersons, J.; Haile, Mitiku; Deckers, J.; Govers, G. (2004). "The effectiveness of loose rock check dams for gully control in Tigray, Northern Ethiopia". Soil Use and Management. 20: 55–64. doi:10.1111/j.1475-2743.2004.tb00337.x.
  24. Descheemaeker, K. and colleagues (2006). "Sediment deposition and pedogenesis in exclosures in the Tigray Highlands, Ethiopia". Geoderma. 132 (3–4): 291–314. Bibcode:2006Geode.132..291D. doi:10.1016/j.geoderma.2005.04.027.
  25. Tewodros Gebreegziabher, and colleagues (2009). "Contour furrows for in situ soil and water conservation, Tigray, Northern Ethiopia". Soil and Tillage Research. 103 (2): 257–264. doi:10.1016/j.still.2008.05.021.
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