Author(s)

Theophile Mugerwa^1,2, Olugbenga A. Ehinola¹, Ibrahim A. Oladosu¹, Digne Rwabuhungu²

¹Institute of Life and Earth Sciences (Including Health & Agriculture), Pan African University-University of Ibadan, Ibadan, Nigeria.
²School of Mining and Geology, University of Rwanda, Kigali, Rwanda.

The peat deposits in Rwanda are distributed over an area of 50,000 ha and were formed about the end of last glaciations period. However Akanyaru peat is 20,000 years old and contains peat of glacial and postglacial period. The studies show that Rwanda has 155 million tons of dry peat which can generate electrical energy and this deposit is sufficient to meet country’s vast energy requirements for 30 years. Hence, it was felt necessary to map prospective locations of peat and their energy potential. The result of the study and assessment of peat to power in Rwanda show that the average in-situ ash content, in-situ moisture content and in-situ bulk density of the collected peat samples are 36 wt%, 70.8 wt% and 1112 kg/m³ respectively. Their average thickness ranges from 0.9 to 7.8 m. In Finland, peat was used as fuel in 1996 and produced 10% of total installed capacity. Rwanda has the same operational peat power plant in Gishoma: Rusizi District generating 15 MW connected to the national electrical grid. A peat-fuelled power plant is under construction and is expected to generate 80 MW. This plant, once completed, is expected to connect 50% more households into national grid. Thus, this effort along with other projects will increase electrical power from 208 MW to 563 MW in 2024. Peat deposit is expected to generate 500 Megawatt electrical powers for 30 years. Although an effort was done to use peat as fuel, the power plant is still vulnerable to the lack of good quality of dry peat to operate and thus efforts are on to develop suitable technology for exploitation.

Peat Deposits, Electrical Power, Energy, Rwanda

Mugerwa, T. , Ehinola, O. , Oladosu, I. and Rwabuhungu, D. (2020) Assessment of Peat Deposits in Rwanda. Journal of Geoscience and Environment Protection, 8, 1-11. doi: 10.4236/gep.2020.810001.