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Characterization of problem soils in and around the south central Ethiopian Rift Valley

dc.contributor.authorAlemayehu, Kiflu
dc.contributor.authorSheleme, Beyene
dc.contributor.authorSchoenau, Jeffrey
dc.date.accessioned2023-09-25T20:22:02Z
dc.date.available2023-09-25T20:22:02Z
dc.date.issued2016
dc.descriptionAuthor(s) agree that this article remain permanently open access under the terms of the Creative Commons Attribution License 4.0 International Licenseen_US
dc.description.abstractSome soils in Ethiopia reduce plant productivity due to physical and/or chemical limitations. The morphological, physical and chemical properties of problem soils, including sodic, acidic, and saline soils, around southern Ethiopia were characterized and are described in this chapter. The intention is to characterize the soils and better understand the specific nature of the limitations. Sodic soils of Alage, acid soils of Hagereselam, and saline soils of Zeway areas were sampled to represent the problem soils. The soil properties determined included color, electrical conductivity (EC), structure, consistency, bulk density, texture, pH, organic carbon (OC), total nitrogen, available phosphorus (P) and K, exchangeable bases and available micro-nutrients. The soils had considerable heterogeneity in solum and regolith thickness, horizon depth, structural development in surface soils and subsurface horizons, pH, EC and available nutrients. The classification of these soils was made according to Soil Taxonomy and World Reference Base for Soil Resources systems. The sodic soils of Alage had high pH and sodium (Na) content, and low level of OC, available P, copper (Cu) and zinc (Zn). The epipedon was classified as an ochric and the profile also had variation in clay content down the profile to satisfy the requirements of having an argilic horizon and therefore these soils were classified as Typic Natragids. Soils of Hagereselam had very low available P. Available Cu and Zn contents were found to be at the marginal levels for production of most crops. The Hagereselam profile had an argilic horizon with umbric epipedon and was classified as Typic Paleustults. The saline soils in Zeway area had relatively high amounts of calcium and low OC. The profile was found to have ochric epipedon and these soils are classified as Typic Haplocambids. Application of fertilizer including P, Cu and Zn, and removal of sodium and salts from the soil profile may be means of improving the productivity of these soils. Application of organic amendments including manures and crop residues may also be beneficial in increasing the fertility as well as organic carbon content.en_US
dc.description.versionPeer Revieweden_US
dc.identifier.citationAlemayehu, K, Sheleme, B, Schoenau, J (2016). Characterization of problem soils in and around the south central Ethiopian Rift Valley. Journal of Soil Science and Environmental Management. Vol. 7(11), pp. 191-203. doi: 10.5897/JSSEM2016.0593en_US
dc.identifier.doi10.5897/JSSEM2016.0593
dc.identifier.urihttps://hdl.handle.net/10388/15055
dc.language.isoenen_US
dc.publisherAcademic Journalsen_US
dc.rightsAttribution 2.5 Canada*
dc.rights.urihttp://creativecommons.org/licenses/by/2.5/ca/*
dc.subjectacidicen_US
dc.subjectsaline and sodic soilsen_US
dc.subjectreclamationen_US
dc.subjectmorphologicalen_US
dc.subjectphysical and chemical soil propertiesen_US
dc.titleCharacterization of problem soils in and around the south central Ethiopian Rift Valleyen_US
dc.typeArticleen_US

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