| Peer-Reviewed

Characterization and Classification of Soils Along the Toposequence of Medo Sub-watershed at Wondo Genet District, Ethiopia

Received: 5 April 2022    Accepted: 3 May 2022    Published: 12 May 2022
Views:       Downloads:
Abstract

Soil characterization and classification study under topographic position is essential to recognize the effects of slope on soil physicochemical, and morphological properties and to draw promising management practices. In view of this, the present study was implemented to characterize and classify the soils along the toposequence of Medo sub-watershed using the World Reference Base for Soil Resources. First, topographic positions were categorized as upper, middle, and lower slopes position. One representative pedon was opened per each slope position and the profiles were described in situ. Soil morphological properties were influenced by topographic position. Sandy clay loam was the dominant soil textural classes in the surface soils. In all pedons, soil bulk density ranged from 0.8 - 1.2 g cm-3. The soil pH. ranged from 5.43 – 5.81 in the surface to subsurface layers of the three pedons. Soil organic carbon contents were ranged from 1.46 - 2.23 in the upper, middle and lower slope positions, respectively. Total nitrogen contents of the soils were varied from 0.14 to 0.22 and rated as medium to high. The soils present base saturation was categorized as very high (> 80%) in all pedons, respectively. The upper, middle and lower pedons had Mollic epipedon in the surface horizon but they had different sub-surface horizons. The middle and lower pedons had Argic and Cambic sub-surface horizons, respectively. The upper, middle and lower slope pedons had Vitric, Leptic and Cambic principal qualifiers, respectively while Arenic, Arenic and Aric supplemental qualifiers for upper, middle and lower pedons, respectively. Therefore, the studied soils were classified as Vitric Andosols (Arenic), Leptic Retisols (Arenic) and Cambic Phaeozems (Aric) for upper, middle and lower slope positions, respectively. In conclusion, topography remarkably affects soil properties, therefore, site-specific soil management is vital to maintain and improve soil organic matter and essential plant nutrients.

Published in International Journal of Natural Resource Ecology and Management (Volume 7, Issue 2)
DOI 10.11648/j.ijnrem.20220702.12
Page(s) 73-85
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Pedon, Soils Horizons, Soil Properties, World Reference Base

References
[1] Abay A, Sheleme B, Walley F (2015). Characterization and classification of soils of selected areas in southern Ethiopia. J. Environ Earth Sci. 5 (11): 116-137.
[2] Abayneh E (2005). Characteristics, Genesis and Classification of Reddish Soils from Sidamo, Ethiopia. PhD Thesis University of Putra, Malaysia.
[3] Achalu, C., Heluf, G., Kibebew, K. and Abi, T. (2012). Status of selected physicochemical properties of soils under different land use systems of Western Oromia, Ethiopia. Journal of Biodiversity and Environmental Sciences 2 (3): 57-71.
[4] Adhanom, D., Toshome, T., 2016. Characterization and classification of soils of Aba-Midan sub watershed in Bambasi Wereda, West Ethiopia. International Journal of Scientific and Research Publications 6 (6): 390-399.
[5] Alem, H., Kibebew, K., Heluf, G., 2015. Characterization and classification of soils of Kabe Sub watershed in South Wollo Zone, Northeastern Ethiopia. African Journal of Soil Science 3 (7): 134-146.
[6] Alemayahu kiflu and Sheleme Beyene. 2013. Effect of different land use systems on selected soil properties in south Ethiopia. Journal of soil science and environmental management. 4 (5).: 100-107.
[7] Alemayehu K, Sheleme B, Schoenau J (2016). Characterization of problem soils in and around the south-central Ethiopian Rift Valley. J. Soil Sci. Environ. Manage. 7 (11): 191-203.
[8] Ali, A., Esayas, A., & Beyene, S, (2010), characterization soils of Delbo Wegene watershade woliyta zone, Southren Ethiopia for planting appropriate land management journal of soil science and environmental management, 1 (8), 184-199.
[9] Amsalu Aklilu, Stroosnijder L, de Graaff J, (2007). Long-term dynamics in land resource use and the driving forces in the Beressa watershed, highlands of Ethiopia. J. Envir. Manage. 83: 448-459.
[10] Asadi, M. E., Clement, R. S., Gupta, A. D., Loof, R., & Hanse, G. K., (2002). Impact f fertigation via sprinkiker Irrigation on nitrate leaching and corn yield in an acid Sulphur soil in Thiland, Agricultural water management, 52 (3), 197-213.
[11] Ashenafi, A, Abayneh E, Sheleme B (2010). Characterizing soils of Delbo Wegen watershed, Wolayita zone, southern Ethiopia, for planning appropriate land management. J. Soil Sci. Environ. Manage. 1 (8): 184-189.
[12] Bohn, H. L., McNeal, B. L. and O'Connor, G. A. (2001). Soil Chemistry. 3rd edition. John Willey and Sons, Inc., New York.
[13] Chadwick, O. A., Grahm, R. C., (2000). Pedogenic processes. In: Sumner, M. E. (Ed.), Handbook of Soil Science. CRC Press, Boca Raton, pp. 41–75.
[14] Chapman, HD (1965) Cation exchange capacity. In: CA Black, Ensminger LE, and FE. p 1569.
[15] Chekol, W., Mnalku, A., (2012). Selected Physical and Chemical Characteristics of Soils of the Middle Awash Irrigated Farm Lands, Ethiopia. Ethiopian Journal of Agricultural Sciences 22 (1): 127-142.
[16] Cools, N. and De Vos, B. (2010). Sampling and analysis of soil. Manual Part X, 208 pp. In: manual, on, methods and criteria for harmonized sampling, assessment, monitoring and analysis of the effects of air pollution on forests, UNECE, ICP Forests, Hamburg. ISBN: 978-3-926301-03-forests.org/Manual.
[17] Dent, D., Young, A., (1981). Soil survey and land evaluation. Allen and Unwin Ltd. London. FAO/UNDP, 1984. Provisional soils association map of Ethiopia (1:2,000,000).
[18] Dinku, D., Sheleme B, Nand Ram, Walley F, Gala TS (2014). Effects of Topography and land use on soil characteristics along the toposequence of Ele watershed in southern Ethiopia. Catena, 115: 47-54.
[19] Esayas, A. (2005). Characteristics, genesis and classification of reddish soil from Sidamo region of Ethiopia.
[20] EthioSIS (2016). Soil Fertility and Fertilizer recommendation Atlas of Tigray Region. Ministry of Agriculture (MOA) and Agricultural Transformation Agency (ATA), Ethiopia.
[21] FAO. Guidelines for soil profile description. Soil Resources, Management and Conservation Service, Land and Water Development Division FAO, (2006), Rome; 2006.
[22] FAO/world Reference Base for soil resource (2014). International soil classification system for naming soils and creating legends for soil maps. World soil resource reports No. 106. Food and Agricultural Organization the united nations (FAO), Rome Italy.
[23] Fikadu, E., Kibret, K., Bedadi, B., & Melese, A. (2018). Characterization and classification of soils of yikalo sub watershed in lay Gayint district, northwestern highlands of Ethiopia. Eurasian Journal of soil science, 7 (2), 151-166.
[24] Foth, H. D. and Ellis, B. G. (1997). Soil Fertility. 2nd Edition. Lewis Publication, Boca Raton, Florida.
[25] Hailu, A. H., Kibret, K., Gebrekidan, H., (2015). Characterization and classification of soils of Kabe Sub watershed in South Wollo Zone, Northeastern Ethiopia. African Journal of Soil Science 3 (7): 134-146.
[26] Havlin, J. L., and Nelson, W. L. (2014). Zinc, sulfur, calcium and Magnesium. Soil fertility and fertilizers. An Introduction to Nutrient Management, 219-243.
[27] Hazelton P, Murphy B (2007). Interpreting soil test results: What do all the numbers mean? 2nd Edition. CSIRO Publishing. P. 152.
[28] Idoga, S. and Azagaku, D. E. (2005). Characteristics and classification of soils of Janta area, plateau state Nigeria. Journal Soil Science, 15: 116 – 122.
[29] IUSS Working Group WRB. (2014). "World reference base for soil resources 2014: International soil classification system for naming soils and creating legends for soil maps." Food and Agriculture Organization (FAO), Rome, Italy.
[30] Jankson, M. L. (1958). Soil chemical analysis Hall. Inc., Englewood Cliffs, NJ, 498, 183-204.
[31] Jones, A., Breuning-Madsen, H., Brossard, M., Dampha, A., Deckers, J., Dewitte, O., Gallali, T., Hallett, S., Jones, R., Kilasara, M., Le Roux, P., Micheli, E., Montanarella, L., Spaargaren, O., Thiombiano, L., VanRanst, E., Yemefack, M., Longmore R., (eds.), (2013), Soil Atlas of Africa. European Commission, Publications Office of the European Union, Luxembourg. 176 pp.
[32] Jones, J. B., (2003). Agronomic Handbook: Management of Crops, Soils, and Their Fertility. CRC Press LLC, Boca Raton, Florida, USA. 482p.
[33] Khan, S. K, and Chatterjee, A. K. (2001). Effect of continuous rice cropping on change in Pedon’s characteristics in an Ustalf. J Indian Soc. Soil Science, 49: 368-370.
[34] Kravchenko, A. N. and Bullock, D. G. (2000). Correlation of corn and soybean grain yield with topography and soil properties. Argon. J. 92: 75-83.
[35] Landon, J. R. (1991). Booker tropical soil manual: a handbook for soil survey and agricultural land evaluation in the tropics and subtropics. Long man scientific and technical. Booker Tate Ltd. John Wiley and Sons, Inc., New York.
[36] Lindsay. L., & Norvell, W. A. (1978). Development of DTPA soil test for zinc, iron, manganese and copper. Soil Science Society of American Journal, 42, 421-428.
[37] Lufega, S. M., Msanya, B. M., (2017). Pedological characterization and soil classification of selected soil units of Morogoro District, Tanzania. International Journal of Plant and Soil Science 16 (1): 1-12.
[38] Madhan M (2008). Characterization and classification of soils and land suitability of a Micro-Watershed in Hanagal Taluk. An MSc thesis submitted to Department of Soil Science and Agricultural Chemistry College of Agriculture of University of Agricultural Sciences, Dharwad University. 117p.
[39] Mohammed Assen, P. A. L. Le Roux, C. H. Barker and Heluf G/Kidan, (2005). Soils of Jelo micro-catchment in the Chercher Highlands of eastern Ethiopia: I. Morphological and physicochemical properties. Ethiop. J. Nat. Res. 7 (1): 55-81.
[40] Mohammed, S., Kibret, K., & Mohammed, M. (2017). Characterization and classification of soils along Toposequence of Gobeya sub-watershed, south wello zone, Ethiopia, Asian Journal of soil science and plant Nutrition, 1-17.
[41] Moradi, S. (2013). Impacts of organic carbon on consistency limits in different soil textures. International J. Agriculture and Crop Science, 5 (12): 1381- 1388.
[42] Mulugeta D, Sheleme B (2010). Characterization and classification of soils along the toposequence of Kindo Koye watershed in southern Ethiopia. East Afr. J. Sci. 4 (2): 65-77.
[43] Munsell, S. C. C. (2000). Munsell soil color company. Gretagmacbeth.
[44] Nahusenay, A., Kibebew, K., Heluf, G., Abayneh, E., (2014). Characterization and classification of soils along the toposequence at the Wadla Delanta Massif, north central highlands of Ethiopia. Journal of Ecology and the Natural Environment 6 (9): 304-320.
[45] Nega, E. and Heluf, G. (2013). Influence of land use changes and soil depth on cation exchange capacity and contents of exchangeable bases in the soils of Senbat Watershed, western Ethiopia. Ethiopian Journal of Natural Resources, 11 (2): 195-206.
[46] Okalebo, JR, Gathua KW, Woomer PL. Laboratory Methods of Soil and Plant Analysis: A Working Manual. 2nd ed. TSBF-CIAT, SACRED Africa, KARI, SSEA, Nairobi, Kenya, (2002); 128 pp.
[47] Olsen, SR, Cole CV, Watanabe FS, Dean LA. Estimation of available phosphorus in soil by extraction with sodium bicarbonate. USDA, Circular. (1954); 939: 1-19.
[48] Onyekanne, C. F., Akamigbo, F. O., Nnaji, G. U., (2012). Characterization and classification of soils of Ideato North local government area. Nigerian Journal of Soil Science 22 (1): 11-17.
[49] Prasad, R, Power JF. (1997). Soil Fertility Management for Sustainable Agriculture. Lewis Publisher, Boca Raton.
[50] Rowell, DL. Soil science: Methods and applications. Addison Wesley Longman Singapore Pub. (Pvt) Ltd., UK. (1994); 350.
[51] Rust, R. H. (1983). Alfisols. In: Wilding, L. P., Smeck, N. E. and Hall, G. F. (eds.). Pedogenesis and Soil Taxonomy II. The soil orders. Elsevier Science Publishers, Amsterdam. pp. 253-281.
[52] Schoonover, J. E., Crim, J. F., 2015. An introduction to soil concepts and the role of soils in watershed management. Journal of Contemporary Water Research and Education 154 (1): 21-47.
[53] Sharma, RC, Singh R, Singh Y, Singh G (2006). Sodic soils of Shivari experimental farm site characteristics, reclaim ability and use potential for different land uses. CSSRI Publ. No. 1/2006, Karnal. P 36.
[54] Sharu, MB., Yakubu M., Noma SS, Tsafe AI (2013). Characterization and classification of soils on an agricultural landscape in Dingyadi District, Sokoto State, Nigeria. Niger. J. Basic Appl. Sci. 21 (2): 137-147.
[55] Sheleme, B. (2010). “Characterization of soils along a top sequence in Gununo area, southern Ethiopia”. Journal of Science and Development, 1 (1): 31-41.
[56] Shi X. Z., Yu D. S., Warner E. D., Sun W. X., Petersen G. W., Gong Z. T., Lin H., (2005).
[57] Shimeles Damene (2012). Effectiveness of soil and water conservation measures for land restoration in the Wello area, northern Ethiopian highlands. Ecology and Development.
[58] Tekalign, T (1991). Soil, plant, water, fertilizer, animal manure and compost analysis. Working Document No. 13. International Livestock Research Center for Africa, Addis Ababa.
[59] Teshome, Y, Heluf G, Kibebew K, Sheleme B (2013). Impacts of Land Use on Selected Physicochemical Properties of Soils of Abobo Area, Western Ethiopia. Agriculture, Forestry and Fisheries 2 (5): 177-183.
[60] Teshome, Y, Sheleme B, Kibebew K (2016). Characterization and classification of soils of Abobo.
[61] Tobiasova, E., V. simansky, Debeaks, B. and Banach-Szott, M., (2013). Soil structure and soil organic matter of selected soil types in different economics, Agriculture (Polnohospodarstvo), 59; 1-8.
[62] Wakene N, Heluf G (2003). Forms of phosphorus and status of available micronutrients under different land-use systems of Alfisols in Bako area of Ethiopia. J. Ethiopian Nat. Res. 5: 17-37.
[63] Wakene, N. (2001). Assessment of important physicochemical properties of Dystric Udalf (Dystric Nitosols) under different management systems in Bako area, western Ethiopia. M.Sc. Thesis, Alemaya University, Ethiopia.
[64] Walkley, A., and Black, C. A., 1934. An examination of the Digestion method for determining soil organic matter and proposed modification of the chromic acid titration method. Soil Science 37 (1): 29-38.
[65] Wakene, N. and Heluf, G. (2004). The impact of different land use systems on soil quality of western Ethiopia Alfisols. International Research on Food Security: Natural Resource Management and Rural Poverty Reduction through Research for Development and Transformation. Deutcher Tropentage-Berlin 5-7 October 2004. pp. 1-7.
[66] Wang, J., Fu B, Qiu Y, Chen L (2001). Soil nutrients in relation to land use and landscape position in semi-arid small catchment of the loess plateau in China. J. Arid Environ. 48: 537-550.
[67] Yitbarek, T., Beyene, S., & Kibret, K. (2016). Characterization and Classification of Soils of Abobo Area, Western Ethiopia. Applied and Environmental Soil Science.
Cite This Article
  • APA Style

    Abreham Yacob, Ashenafi Nigussie. (2022). Characterization and Classification of Soils Along the Toposequence of Medo Sub-watershed at Wondo Genet District, Ethiopia. International Journal of Natural Resource Ecology and Management, 7(2), 73-85. https://doi.org/10.11648/j.ijnrem.20220702.12

    Copy | Download

    ACS Style

    Abreham Yacob; Ashenafi Nigussie. Characterization and Classification of Soils Along the Toposequence of Medo Sub-watershed at Wondo Genet District, Ethiopia. Int. J. Nat. Resour. Ecol. Manag. 2022, 7(2), 73-85. doi: 10.11648/j.ijnrem.20220702.12

    Copy | Download

    AMA Style

    Abreham Yacob, Ashenafi Nigussie. Characterization and Classification of Soils Along the Toposequence of Medo Sub-watershed at Wondo Genet District, Ethiopia. Int J Nat Resour Ecol Manag. 2022;7(2):73-85. doi: 10.11648/j.ijnrem.20220702.12

    Copy | Download

  • @article{10.11648/j.ijnrem.20220702.12,
      author = {Abreham Yacob and Ashenafi Nigussie},
      title = {Characterization and Classification of Soils Along the Toposequence of Medo Sub-watershed at Wondo Genet District, Ethiopia},
      journal = {International Journal of Natural Resource Ecology and Management},
      volume = {7},
      number = {2},
      pages = {73-85},
      doi = {10.11648/j.ijnrem.20220702.12},
      url = {https://doi.org/10.11648/j.ijnrem.20220702.12},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijnrem.20220702.12},
      abstract = {Soil characterization and classification study under topographic position is essential to recognize the effects of slope on soil physicochemical, and morphological properties and to draw promising management practices. In view of this, the present study was implemented to characterize and classify the soils along the toposequence of Medo sub-watershed using the World Reference Base for Soil Resources. First, topographic positions were categorized as upper, middle, and lower slopes position. One representative pedon was opened per each slope position and the profiles were described in situ. Soil morphological properties were influenced by topographic position. Sandy clay loam was the dominant soil textural classes in the surface soils. In all pedons, soil bulk density ranged from 0.8 - 1.2 g cm-3. The soil pH. ranged from 5.43 – 5.81 in the surface to subsurface layers of the three pedons. Soil organic carbon contents were ranged from 1.46 - 2.23 in the upper, middle and lower slope positions, respectively. Total nitrogen contents of the soils were varied from 0.14 to 0.22 and rated as medium to high. The soils present base saturation was categorized as very high (> 80%) in all pedons, respectively. The upper, middle and lower pedons had Mollic epipedon in the surface horizon but they had different sub-surface horizons. The middle and lower pedons had Argic and Cambic sub-surface horizons, respectively. The upper, middle and lower slope pedons had Vitric, Leptic and Cambic principal qualifiers, respectively while Arenic, Arenic and Aric supplemental qualifiers for upper, middle and lower pedons, respectively. Therefore, the studied soils were classified as Vitric Andosols (Arenic), Leptic Retisols (Arenic) and Cambic Phaeozems (Aric) for upper, middle and lower slope positions, respectively. In conclusion, topography remarkably affects soil properties, therefore, site-specific soil management is vital to maintain and improve soil organic matter and essential plant nutrients.},
     year = {2022}
    }
    

    Copy | Download

  • TY  - JOUR
    T1  - Characterization and Classification of Soils Along the Toposequence of Medo Sub-watershed at Wondo Genet District, Ethiopia
    AU  - Abreham Yacob
    AU  - Ashenafi Nigussie
    Y1  - 2022/05/12
    PY  - 2022
    N1  - https://doi.org/10.11648/j.ijnrem.20220702.12
    DO  - 10.11648/j.ijnrem.20220702.12
    T2  - International Journal of Natural Resource Ecology and Management
    JF  - International Journal of Natural Resource Ecology and Management
    JO  - International Journal of Natural Resource Ecology and Management
    SP  - 73
    EP  - 85
    PB  - Science Publishing Group
    SN  - 2575-3061
    UR  - https://doi.org/10.11648/j.ijnrem.20220702.12
    AB  - Soil characterization and classification study under topographic position is essential to recognize the effects of slope on soil physicochemical, and morphological properties and to draw promising management practices. In view of this, the present study was implemented to characterize and classify the soils along the toposequence of Medo sub-watershed using the World Reference Base for Soil Resources. First, topographic positions were categorized as upper, middle, and lower slopes position. One representative pedon was opened per each slope position and the profiles were described in situ. Soil morphological properties were influenced by topographic position. Sandy clay loam was the dominant soil textural classes in the surface soils. In all pedons, soil bulk density ranged from 0.8 - 1.2 g cm-3. The soil pH. ranged from 5.43 – 5.81 in the surface to subsurface layers of the three pedons. Soil organic carbon contents were ranged from 1.46 - 2.23 in the upper, middle and lower slope positions, respectively. Total nitrogen contents of the soils were varied from 0.14 to 0.22 and rated as medium to high. The soils present base saturation was categorized as very high (> 80%) in all pedons, respectively. The upper, middle and lower pedons had Mollic epipedon in the surface horizon but they had different sub-surface horizons. The middle and lower pedons had Argic and Cambic sub-surface horizons, respectively. The upper, middle and lower slope pedons had Vitric, Leptic and Cambic principal qualifiers, respectively while Arenic, Arenic and Aric supplemental qualifiers for upper, middle and lower pedons, respectively. Therefore, the studied soils were classified as Vitric Andosols (Arenic), Leptic Retisols (Arenic) and Cambic Phaeozems (Aric) for upper, middle and lower slope positions, respectively. In conclusion, topography remarkably affects soil properties, therefore, site-specific soil management is vital to maintain and improve soil organic matter and essential plant nutrients.
    VL  - 7
    IS  - 2
    ER  - 

    Copy | Download

Author Information
  • Department of Natural Resource Management, Wondo Genet Agriculture Research Center, Shashemene, Ethiopia

  • Department of Natural Resource Management, Wondo Genet Agriculture Research Center, Shashemene, Ethiopia

  • Sections