Akanyaru River

The Akanyaru River is the main tributary of the Nyabarongo River. It rises in the western highlands of Rwanda and Burundi, flows east and then north along the border between those countries before joining the Nyabarongo River. The lower stretches contain important but unprotected wetlands, which are under threat from human activity.

Akanyaru River
Akanyaru River in the Kagera catchment (center)
Location
Country	Burundi, Rwanda
Physical characteristics
Source
• elevation	2,450 m (8,040 ft)
Mouth
• coordinates	2.07504°S 30.018929°E / -2.07504; 30.018929
• elevation	1,400 m (4,600 ft)
Basin size	2,650 km^2 (1,020 sq mi)

Course

The Mugere River, a major headwater, rises at an elevation of 2,450 metres (8,040 ft) in Burundi. The river has sources at about 2,300 metres (7,500 ft) elevation in the south of Rwanda. Many of the valleys of the higher tributaries are choked by papyrus, which contains seasonal swamp forests.[1] The upstream portion of the river has a catchment area of about 2,650 square kilometres (1,020 sq mi).[2] The lower course of the river is a belt of permanent wetlands about 7 kilometres (4.3 mi) wide that ends where it reaches the Nyabarongo River. In this 80 kilometres (50 mi) stretch the river drops from an elevation of 1,465 metres (4,806 ft) to 1,400 metres (4,600 ft). The swamp belt is fed from the right by lakes Cyohoha North and Cyohoha South.[1] The Burundi side of the swamp belt has about 14,600 hectares (36,000 acres) of permanent swamp along a 63 kilometres (39 mi) stretch of the river, with the swamp reaching 6 to 10 kilometres (3.7 to 6.2 mi) up the valleys of tributaries.[3]

Climate

The upstream part of the river basin has average annual rainfall of about 1,200 millimetres (47 in).[2] Average annual rainfall in the wetlands is about 800 millimetres (31 in).[4] The climate of Rwanda is determined by the Intertropical Convergence Zone, which creates two rainy seasons. One lasts from mid-September to mid-December and the other from March to May. Climate change may be increasing the severity of both floods and droughts.[5] In the 1997-98 El Nino episode a large number of agricultural plantations in the shallows and swamps of the Nyabarongo and Akanyaru river basins were destroyed.[6]

Flora

Beside the open channels the main plants are Pistia stratiotes (water cabbage), Leersia hexandra (southern cutgrass) and Oryza barthii, a grass in the rice genus. Nearer to the shore is a combination of Typha australis, Miscanthidium violaceum, Cladium jamaicense with some papyrus. Cyperus denudatus, Cyperus latifolius and Echinochloa pyramidalis are also found in some parts. Other parts have pure stands of papyrus.[4] The swamp forest near the river is dominated by Bridelia micrantha, Ficus verruculosa, Myrica kandtiana and Phoenix reclinata. Further from the river common species include Acacia polyacantha and Albizia gummifera.[3]

Fauna

The marshland is an area of great biodiversity, particularly of birdlife.[7] There are records of at least 54 bird species with wetland habitats in the swamp region. These include migrant Malagasy pond heron, pallid harrier and great snipe. Lesser kestrel have been seen. The near-threatened papyrus gonolek is present as is the vulnerable papyrus yellow warbler. The sitatunga, an antelope, is found in the swamps.[4]

Human activities

The valley is not protected, and much of the land that is only flooded seasonally is cultivated at other times of the year. The local people also engage in fishing in the river and swamps.[3] The wetlands are increasingly being used for agriculture. In the dry season the local people cut and burn the marsh vegetation, steadily destroying the habitat.[4] In October 2005 Charles Karangwa, the Butare Director for Economic Affairs, said the people should increase their use of the Akanyaru wetland for crops, particularly maize.[8] In February 2011 the Minister of Lands and Environment told the people of the Gisagara District to make better use of the Akanyaru swamp, with more modern farming methods. According to Minister Kamanzi the Nile Basin Initiative Cooperative Framework did not debar use. He said, "There is no agreement that prevents our population from using the water...of course in a good way."[9]

In December 2012 the ministries of Infrastructure and Natural Resources were discussing how best to evaluate the quantity and quality of Akanyaru peat. Two companies, one from India and the other from Turkey, were to take over peat production.[10] A 100MW peat-fired power plant was to be built by the Turkish developer Hakan Mining and Generation Industry and Trade.[11]

References

Citations

1. Hughes, Hughes & Bernacsek 1992, p. 201.
2. Water and Wetlands Resources: REMA, p. 4.
3. Hughes, Hughes & Bernacsek 1992, p. 127.
4. Akanyaru wetlands: Birdlife Int.
5. Climate report Rwanda, p. 1.
6. Climate report Rwanda, p. 6.
7. Water and Wetlands Resources: REMA, p. 11.
8. Kanamugire 2005.
9. Bucyensenge 2011.
10. Assessing the volume...
11. Hakan Mining structures debt...

Sources

• "Assessing the volume and the quality of peat in Akanyaru north and south". Ministry of Infrastructure. 7 December 2012. Retrieved 2013-04-03.
• "Akanyaru wetlands". Important Bird Areas factsheet. BirdLife International. 2013. Retrieved 2013-04-03.
• Bucyensenge, Jean Pierre (28 February 2011). "Kamanzi Calls for Optimal Use of Akanyaru Swamp". New Times. Archived from the original on 18 April 2013. Retrieved 2013-04-03.CS1 maint: ref=harv (link)
• "Climate report Rwanda" (PDF). ICPAC. October 2009. Retrieved 2013-04-03.
• "Hakan Mining structures debt for Akanyaru peat power". Project Finance. 27 September 2012.
• Hughes, Ralph H.; Hughes, Jane S.; Bernacsek, G. M. (1992). Iucn Directory of African Wetlands. IUCN. ISBN 978-2-88032-949-5. Retrieved 2013-04-03.CS1 maint: ref=harv (link)
• Kanamugire, Judith (9 October 2005). "Butare Urged to Make Use of Akanyaru Wetland". The New Times. Retrieved 2013-04-03.CS1 maint: ref=harv (link)
• "Water and Wetlands Resources" (PDF). Rwanda State of Environment and Outlook Report. Rwanda Environment Management Authority. 2009. Retrieved 2013-04-03.