Soil in Inderta
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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]
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]
- Amba Aradam Formation
- Agula Shale[8]
- Mekelle Dolerite[9]
- Antalo Limestone
- Quaternary alluvium and freshwater tufa[10]
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
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
- Inclusions
- Rock outcrops and very shallow soils (Lithic Leptosol) (1)
- Shallow very stony loamy soil on limestone (Skeletic Calcaric Cambisol) (5)
- Deep dark cracking clays with very good natural fertility, waterlogged during the wet season (Chromic Vertisol, Pellic Vertisol) (12)
- Brown to dark sands and silt loams on alluvium (Vertic Fluvisol, Eutric Fluvisol, Haplic Fluvisol) (30)
Gently undulating Agula shale plateau with dolerite
- Dominant soil type: stony, dark cracking clays with good natural fertility (Vertic Cambisol) (10)
- Associated soil types
- Inclusions
Mekelle Graben
- Associated soil types
- Inclusions
Strongly incised Giba gorge
- Dominant soil type: complex of rock outcrops, very stony and very shallow soils ((Lithic) Leptosol) (1)
- Associated soil types
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
Alluvial plains induced by tufa dams
- 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
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]
References
- ↑ Nyssen, Jan; Tielens, Sander; Gebreyohannes, Tesfamichael; Araya, Tigist; Teka, Kassa; Van De Wauw, Johan; Degeyndt, Karen; Descheemaeker, Katrien; Amare, Kassa; Haile, Mitiku; Zenebe, Amanuel; Munro, Neil; Walraevens, Kristine; Gebrehiwot, Kindeya; Poesen, Jean; Frankl, Amaury; Tsegay, Alemtsehay; Deckers, Jozef (2019). "Understanding spatial patterns of soils for sustainable agriculture in northern Ethiopia's tropical mountains". PLOS ONE. 14 (10) e0224041. Bibcode:2019PLoSO..1424041N. doi:10.1371/journal.pone.0224041. PMC 6804989. PMID 31639144.
- ↑ 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.
- ↑ IAO (2008). Land evaluation in Enderta District - Tigray Region, Ethiopia. Firenze, Italy: Ministry of Foreign Affairs, Istituto Agronomico per l'Oltremare.
- ↑ 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.
- ↑ 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. hdl:1854/LU-4252226. S2CID 140560276.
- ↑ 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. S2CID 199105560.
- ↑ 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.
- ↑ 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.
- ↑ Tefera, M.; Chernet, T.; Haro, W. Geological Map of Ethiopia (1:2,000,000). Addis Ababa, Ethiopia: Ethiopian Institute of Geological Survey.
- ↑ Moeyersons, J. and colleagues (2006). "Age and backfill/overfill stratigraphy of two tufa dams, Tigray Highlands, Ethiopia: Evidence for Late Pleistocene and Holocene wet conditions". Palaeogeography, Palaeoclimatology, Palaeoecology. 230 (1–2): 162–178. Bibcode:2006PPP...230..165M. doi:10.1016/j.palaeo.2005.07.013.
- 1 2 Nyssen, Jan; Poesen, Jean; Moeyersons, Jan; Deckers, Jozef; Haile, Mitiku; Lang, Andreas (2004). "Human impact on the environment in the Ethiopian and Eritrean highlands - a state of the art". Earth-Science Reviews. 64 (3–4): 273–320. Bibcode:2004ESRv...64..273N. doi:10.1016/S0012-8252(03)00078-3.
- ↑ 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)" (PDF). Géomorphologie: Relief, Processus, Environnement. 24 (3): 277–300. doi:10.4000/geomorphologie.12258. S2CID 134513245.
- ↑ 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.
- ↑ "Principes de la cartographie des pédopaysages dans les Alpes". Écologie. 29 (1–2): 49. 1998. ProQuest 223074690.
- ↑ Tielens, Sander (2012). Towards a soil map of the Geba catchment using benchmark soils. MSc thesis. Leuven, Belgium: K.U.Leuven.
- ↑ 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. S2CID 145550500.
- ↑ 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. S2CID 129501591.
- ↑ 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. S2CID 30898575.
- ↑ Virgo, K.J.; Munro, R.N. (1978). "Soil and erosion features of the Central Plateau region of Tigrai, Ethiopia". Geoderma. 20 (2): 131–157. Bibcode:1978Geode..20..131V. doi:10.1016/0016-7061(78)90040-X. S2CID 140536258.
- ↑ Fitsum Hagos, and colleagues (1999). Land degradation in the Highlands of Tigray and strategies for sustainable land management (No. 25) (PDF). ILRI.
- ↑ 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. S2CID 199104514.
- ↑ 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.
- ↑ 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. S2CID 98547102.
- ↑ 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.
- ↑ 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.