These are the design values. In practice, the runoff from the catchment is largely insufficient to fill the reservoir, which serves only as shallow drinking pond for livestock.[1]
Irrigation
Designed irrigated area: 50 ha
Actual irrigated area in 2002: 0 ha
Environment
The catchment of the reservoir is 13.5 km² large. The lithology of the catchment is Precambrianmetamorphic rock.[1] Land use is strongly dependent on lithology: soils on metamorphic black limestone are used for cropping, while those on the schist and slate formations are under savannahwoodland. Lands on the green-reddish-gray metamorphic banded marl formation are used for settlements. Most common soil types are:[2]
in the schist and slate formations: Leptosol both at the upper slope and at the foot slope positions; Regosol (Calcaric) over Hypercalcic Calcisol at the mid slope position and Fluvisol at the valley bottom
in the green-reddish-gray metamorphosed banded marl: LepticCalcisol at the upper slope, Haplic Calcisol at the foot slope, and Fluvisol at the valley bottom
^ abcDe Wit, Joke (2003). Stuwmeren in Tigray (Noord-Ethiopië): kenmerken, sedimentatie en sediment-bronnen. Unpub. M.Sc. thesis. Department of Geography, K.U.Leuven.
^Teka, Kassa; Nyssen, Jan; Teha, Nurhusen; Haile, Mitiku; Deckers, Jozef (1 August 2015). "Soil, land use and landform relationship in the Precambrian lowlands of northern Ethiopia". CATENA. 131: 84–91. Bibcode:2015Caten.131...84T. doi:10.1016/j.catena.2015.03.010.