The soils of the Kola Tembien woreda (district) in Tigray ( Ethiopia) reflect its longstanding agricultural history, highly seasonal rainfall regime, relatively high temperatures, overall dominance of sandstone and metamorphic lithology and steep slopes. [1]
Annual rainfall depth is very variable from year to year, but also from place to place. Whereas, there is around 500 mm annual rainfall near Tekezé River, this increases to 1600 mm in Abiy Addi, which benefits from the orographic rains induced by the Dogu’a Tembien massif. [2] Most rains fall during the main rainy season, which typically extends from June to September. Mean temperature in woreda town Abiy Addi is 22.4 °C, oscillating between average daily minimum of 12.8 °C and maximum of 31.5 °C. The contrasts between day and night air temperatures are much larger than seasonal contrasts. [3]
From the higher to the lower locations, the following geological formations are present: [4]
As part of the Ethiopian highlands the land has undergone a rapid tectonic uplift, leading the occurrence of mountain peaks, plateaus, valleys and gorges.
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.
Soil degradation in this district became important when humans started deforestation almost 5000 years ago. [5] [6] Depending on land use history, locations have been exposed in varying degrees to such land degradation.
Detailed information on soils is available for the southern part of the district which is part of the Giba River catchment. 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. [7] [8] [9] 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.
The reduced soil protection by vegetation cover, combined with steep slopes and erosive rainfall has led to excessive soil erosion. [5] [10] [11] 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. 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. [12] [13] Measures include the construction of infiltration trenches, stone bunds, [14] check dams, [15] small reservoirs such as Addi Asme'e as well as a major biological measure: exclosures in order to allow forest regeneration. [16]
The soils of the Kola Tembien woreda (district) in Tigray ( Ethiopia) reflect its longstanding agricultural history, highly seasonal rainfall regime, relatively high temperatures, overall dominance of sandstone and metamorphic lithology and steep slopes. [1]
Annual rainfall depth is very variable from year to year, but also from place to place. Whereas, there is around 500 mm annual rainfall near Tekezé River, this increases to 1600 mm in Abiy Addi, which benefits from the orographic rains induced by the Dogu’a Tembien massif. [2] Most rains fall during the main rainy season, which typically extends from June to September. Mean temperature in woreda town Abiy Addi is 22.4 °C, oscillating between average daily minimum of 12.8 °C and maximum of 31.5 °C. The contrasts between day and night air temperatures are much larger than seasonal contrasts. [3]
From the higher to the lower locations, the following geological formations are present: [4]
As part of the Ethiopian highlands the land has undergone a rapid tectonic uplift, leading the occurrence of mountain peaks, plateaus, valleys and gorges.
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.
Soil degradation in this district became important when humans started deforestation almost 5000 years ago. [5] [6] Depending on land use history, locations have been exposed in varying degrees to such land degradation.
Detailed information on soils is available for the southern part of the district which is part of the Giba River catchment. 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. [7] [8] [9] 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.
The reduced soil protection by vegetation cover, combined with steep slopes and erosive rainfall has led to excessive soil erosion. [5] [10] [11] 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. 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. [12] [13] Measures include the construction of infiltration trenches, stone bunds, [14] check dams, [15] small reservoirs such as Addi Asme'e as well as a major biological measure: exclosures in order to allow forest regeneration. [16]