Addi Amharay

Addi Amharay is a reservoir located in the Inderta woreda of the Tigray Region in Ethiopia. The earthen dam that holds the reservoir was built in 1997 by SAERT.[1]

Addi Amharay
Addi Amharay
Coordinates13.40500132°N 39.5733461°E / 13.40500132; 39.5733461
TypeReservoir
Basin countriesEthiopia
Surface area0.315 km2 (0.122 sq mi)
Water volume0.957×10^6 m3 (776 acre⋅ft)
Surface elevation2,320 m (7,610 ft)
SettlementsKwiha

Dam characteristics

  • Dam height: 14.7 metres
  • Dam crest length: 128 metres
  • Spillway width: 17 metres

Capacity

  • Original capacity: 957,000 m³
  • Dead storage: 175,000 m³
  • Reservoir area: 31.5 ha

In 2001, the life expectancy of the reservoir (the duration before it is filled with sediment) was estimated at 33 years.[1]

Irrigation

  • Designed irrigated area: 60 ha
  • Actual irrigated area in 2001: 5 ha

Environment

The catchment of the reservoir is 4.92 km² large, with a perimeter of 9.62 km and a length of 3560 metres. The reservoir suffers from rapid siltation.[2] [3] The lithology of the catchment is Antalo Limestone and Agula shale.[1] Part of the water that could be used for irrigation is lost through seepage; the positive side-effect is that this contributes to groundwater recharge.[4]

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References

  1. De Wit, Joke (2003). Stuwmeren in Tigray (Noord-Ethiopië): kenmerken, sedimentatie en sediment-bronnen. Unpub. M.Sc. thesis. Department of Geography, K.U.Leuven.
  2. Vanmaercke, M. and colleagues (2019). "Sediment Yield and Reservoir Siltation in Tigray". Geo-trekking in Ethiopia's Tropical Mountains. GeoGuide. Cham (CH): Springer Nature. pp. 345–357. doi:10.1007/978-3-030-04955-3_23. ISBN 978-3-030-04954-6.
  3. Nigussie Haregeweyn, and colleagues (2006). "Reservoirs in Tigray: characteristics and sediment deposition problems". Land Degradation and Development. 17: 211–230. doi:10.1002/ldr.698.
  4. Nigussie Haregeweyn, and colleagues (2008). "Sediment yield variability in Northern Ethiopia: A quantitative analysis of its controlling factors". Catena. 75: 65–76. doi:10.1016/j.catena.2008.04.011.
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