Indexed By
SJR Rank

SCImago Journal & Country Rank

Article Tools
Email this article (Login required)
Email the author (Login required)
About The Authors

Haymanot Tesfaye
Wolaita Sodo University

Bikila Warkineh
Addis Ababa University


Information for Author
Visitor Statistic

The impact of anthropogenic activities on the physicochemical characteristics of Cheleleka peat, Ethiopia

Haymanot Tesfaye, Bikila Warkineh
  J. Degrade. Min. Land Manage. , pp. 2751-2758  
Viewed : 81 times


Cheleleka peatland is located at the eastern side of Lake Hawassa and its biological communities face a variety of anthropogenic factors such as agricultural expansion, water diversion, settlement and subsequent peatland drainage and peat extraction. The decomposing products were influenced by various anthropogenic activities. This study aims to identify the impact of human activities on peat characteristics. The result indicates that the peat soil is acidic having a pH value ranging from 4.1-to-4.7 and containing humic acid due to excessive accumulation of organic matter and nutrients. The maturity level of the peat was almost similar in all study sites, except for the Daka site, and are classified under mostly decomposed. At Wesha, Werka, Wendo, Shalo, Cheffe, and Wendo, sites the maturity of the peat was classified under sapric soil. Exceptionally, at Daka Site, the peat maturity level was hemic. The percentage of sand, clay, and silt of the peatland range 40-50% clay, 30-40% silt and 10-20% sandy. The mean organic carbon content of Cheleleka peatland ranged from 4.48 to 38.65% and positively correlated with the thickness of the peat and negatively correlated with the ash content of the peat. The main effects of unsustainable landuse practice on peatland are peat reduction/complete loss, reduce water and nutrient retention capacity due to drainage and compaction of peat due to overgrazing. Changes in drainage, vegetation cover, and extraction of peat had resulted in differing outcomes from decomposition processes, and the properties of peats on the disturbed sites had changed.


acidic soil; Cheleleka peat; correlation analysis; human disturbance ; sapric soil

Full Text:



Andriesse, J.P. 1974. Tropical lowland peats in South East Asia. Commun. Nr.63, Royal Trop. Inst.Amsterdam, The Netherlands.

Boetler, D.H. 1969. Physical properties of peats as related to degree of decomposition. Soil Science Society of America Proceedings 33: 606-609.

Chakim, M.G., Mindari, M., Siswanto, and Sasongko, P.E. 2020. Humic acid characterization in soil from various land uses in Tutur District, Pasuruan Regency of East Java. Journal of Degraded and Mining Lands Management 7(4):2279-2286, doi: 10.15243/jdmlm. 2020.074.2279.

Clymo, R.S. 1984. The limits to peat bog growth. Philosophical Transactions of the Royal Society B: Biological Science 303(1117): 605–654.

Clymo, R.S., Turunen, J. and Tolonen, K.1998. Carbon accumulation in peatland. Oikos 81: 368–388.

Connors, B. and DiFranco, J. 2013. Protocols for Completing the Biological Monitoring Wetland Human Disturbance Assessment. Bureau of Land and Water Quality Division of Environmental Assessment Biomonitoring Program.

Dixon, R.K., Brown, S., Houghton, R.A., Solomon, A.M., Trexler, M.C. and Wisniewski, J. 1994. Carbon pools and flux of global forest ecosystems. Science 263:185–191.

Douglas, W.P. 2010. A critical review of the conventional SOC to SOM conversion factor. Geoderma 156: 75–83.

Driessen, P. and Sudjadi, M. 1984. Soils and soil specific problem of tidal Swamps. Workshop on ResearchPriorities in Tidal Swamp Rice. IRRI, Los Banos, Laguna, Philippines. Pp 143-160.

Bikila, W.D. Grootjans, A.P., Roelofs, J.G.M., Senbeta, A.F. and Fritz, C. 2015. Fen mires with cushion plants in Bale Mountains, Ethiopia. Mires and Peat 15: 1–10.

Hamilton, A.C. 1982. Environmental History of East Africa. A Study of the Quaternary. Academic Press, London, 328 pp.

Hikmatullah and Sukarman. 2014. Physical and chemical properties of cultivated peat soils in four trial sites of ICCTF in Kalimantan and Sumatra, Indonesia. Journal of Tropical Soils 19(3): 131-141.

Huang, P.T., Patel, M., Santagata, M.C. and Bobet, A. 2009. Classification of Organic Soils. Final Report, FHWA/IN/JTRP -2008/2, Project No. C-36-36TT, Joint Transportation Research Program, Indiana Department of Transportation and Purdue University, 63–81.

Indonesian Soil Survey Staff. 2010. Keys to Soil Taxonomy. 11st ed. NRCS-USDA, Washington DC. 333p.

Korhola, A., Ruppel,M., Seppa H., Valiranta M., Virtanen T. and Weckstrom J. 2010. The importance of northern peatland expansion to the late-Holocene rise of atmospheric methane, Quaternary Science Review doi:10.1016/j.quascirev.2009.12.010

McKenzie, N., Jacquier, D., Isbell, R. and Brown, K. 2004. Australian soils and landscapes: an illustrated compendium. CSIRO publishing.

Mitsch, W. and Gosselink, J.G. 2007. Wetlands, fourth edition. John Wiley & Sons, Inc., New York, USA.

Belete, M.D. 2018. Ecohydrology to harmonize industrialization and ecological safety in urban environment: Case of Hawassa Lake, industries 5 and Cheleleka wetland. Ecohydrology & Hydrobiology18: 192-200.

Osmaston, H.A., Mitchell, W.A. and Osmaston, J.A.N. 2005. Quaternary glaciations of the Bale Mountains, Ethiopia. Journal of Quaternary Science 20: 593–606.

Parish, F., Sirin, A., Charman, D., Joosten, H., Minayeva, T. and Stringer, L. 2008. Assessment on Peatlands, Biodiversity and Climate Change. Wageningen: Wetland International, 206.

Ramsar. 2016. The Nordic countries highlight the restoration of peatlands at COP21. Retrieved from Ramsar:

Rieley, J.O. and Page, S.E. 2005. Wise use of tropical peatlands: focus on Southeast Asia, Wageningen, The Netherlands: Alterra Wageningen University.

Shofiyati, R., Las, I. and Agus, F. 2010. Indonesian soil database and predicted stock of soil carbon. In: Chen, Z.S. and Agus, F. (eds). Proceedings of International Workshop on Evaluation And Sustainable Management of Soil Carbon Sequestration in Asian Countries. 28–29 September 2010. Bogor, Indonesia. Bogor, Indonesia: Indonesian Soil Research Institute; Taipei: Food and Fertilizer Technology Center for the Asian and Pacific Region; Tsukuba, Japan: National Institute for Agro-Environmental Sciences. p. 73–83.

Sprengel, C. 1826. About plant humus, humus acid and humus acid salts. Archive for the Entire Natural Science 8: 145 - 220.

Suhardjo, H. and Widjaja I.P.G. 1976. Chemical characteristics of the upper 30 cm of peat soils from Riau. In: Peat and Podzolic Soils and Their Potential for Agriculture in Indonesia. Proclamation. ATA 106 Midterm Seminar on Soil Research Institution Bulletin 3: 74-92.

Umer, M. and Bonnefille, R. 1998. A late Glacial/late Holocene pollen record from a highland peat at Tamsaa, Bale Mountains, south Ethiopia. Global and Planetary Change 16: 121–129.

Umer, M., Lamb, H.F., Bonnefille, R., Lézine, A.-M., Tiercelin, J.-J., Gibert, E., Cazet, J.-P. and Watrin, J. 2007. Late Pleistocene and Holocene vegetation history of the Bale Mountains, Ethiopia. Quaternary Science Reviews 26: 2229–2246.

Wolka, K., Tadesse, H., Garedew, E. and Yimer, F. 2015. Soil erosion risk assessment in the Chaleleka wetland watershed, Central Rift Valley of Ethiopia. Environmental System Research 4, Article number: 5: 1–12, doi: 10.1186/ s40068-015-0030-5.


Copyright (c) 2021 Journal of Degraded and Mining Lands Management

Creative Commons License
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.

Indexed By