American Journal of Agriculture and Forestry

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Pedology at Four Representative Sites of Southern Highland Zone of Tanzania

Received: 24 July 2018    Accepted: 09 August 2018    Published: 06 September 2018
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Abstract

To study the soils of Southern Highland Zone of Tanzania, four representative pedons of some landscapes were characterized. Their names and identifiers are Seatondale, Mbimba, Inyala, and Uyole, respectively TzSea 01, TzMb 02, TzIny 03, and TzUy04. The pedons were formed from the weathering of among other materials, colluvial igneous rocks, alluvium, eluvial soils, laterite, lacustrine sands and silts, andesite, pumice, aeolian deposits, and metamorphic rocks including coarse grained and strongly foliated biotite gneisses. Twenty soil samples were taken for laboratory characterization. In addition to classical horizon by horizon descriptions and laboratory analyses, 12 core samples were taken for soil-water retention characterization. The available water holding capacity was rated as very low to low. Pedon descriptions and particle size analysis showed clay eluviation-illuviation was the predominant pedogenic process in all pedons. Soil pH was rated slightly acidic to slightly alkaline. Available P ranged from 0.71 mg/kg at Mbimba to 10.67 mg/kg at Seatondale. Exchangeable bases were variable across and within the profiles; at Uyole and Inyala they were high, while at Seatondale and Mbimba they were low and medium. Values of exchangeable bases showed decreasing trends with profile depths in all sites. C/N ratios ranged between 6 and 18, total nitrogen was rated very low to low in both A and B horizons. CECsoil ranged between 17.2 and 36.4 cmol (+)/kg. Organic carbon ranged from very low to high. The soils apparently developed from extreme and moderate weathering of parent materials. According to the USDA Soil Taxonomy, the pedons classified as Fine, Illitic, Active, Isothermic Typic Hapludult; Fine, Illitic, Active, Isothermic Andic Paleudalf; Fine, Illitic, Active, Isothermic, Mollic Paleudalf; Pumiceous, Mixed, Superactive, Isothermic, Typic Hapludand for Seatondale, Mbimba, Inyala, and Uyole, respectively. The soil depths were deep and very deep. Moisture stress and low levels of some macro-elements highly limited the productivity of the soils.

DOI 10.11648/j.ajaf.20180605.11
Published in American Journal of Agriculture and Forestry (Volume 6, Issue 5, September 2018)
Page(s) 111-121
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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

Pedology, USDA Soil Taxonomy, Pedons, Southern Highlands, Tanzania

References
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Author Information
  • Tanzania Agricultural Research Institute: TARI – Uyole, Mbeya, Tanzania

  • Department of Soil and Geological Sciences, College of Agriculture, Morogoro, Tanzania

  • Agronomy Department, Iowa State University, Ames, USA

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    Johnson Godlove Mtama, Balthazar Michael Msanya, Charles Lee Burras. (2018). Pedology at Four Representative Sites of Southern Highland Zone of Tanzania. American Journal of Agriculture and Forestry, 6(5), 111-121. https://doi.org/10.11648/j.ajaf.20180605.11

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    Johnson Godlove Mtama; Balthazar Michael Msanya; Charles Lee Burras. Pedology at Four Representative Sites of Southern Highland Zone of Tanzania. Am. J. Agric. For. 2018, 6(5), 111-121. doi: 10.11648/j.ajaf.20180605.11

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    Johnson Godlove Mtama, Balthazar Michael Msanya, Charles Lee Burras. Pedology at Four Representative Sites of Southern Highland Zone of Tanzania. Am J Agric For. 2018;6(5):111-121. doi: 10.11648/j.ajaf.20180605.11

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  • @article{10.11648/j.ajaf.20180605.11,
      author = {Johnson Godlove Mtama and Balthazar Michael Msanya and Charles Lee Burras},
      title = {Pedology at Four Representative Sites of Southern Highland Zone of Tanzania},
      journal = {American Journal of Agriculture and Forestry},
      volume = {6},
      number = {5},
      pages = {111-121},
      doi = {10.11648/j.ajaf.20180605.11},
      url = {https://doi.org/10.11648/j.ajaf.20180605.11},
      eprint = {https://download.sciencepg.com/pdf/10.11648.j.ajaf.20180605.11},
      abstract = {To study the soils of Southern Highland Zone of Tanzania, four representative pedons of some landscapes were characterized. Their names and identifiers are Seatondale, Mbimba, Inyala, and Uyole, respectively TzSea 01, TzMb 02, TzIny 03, and TzUy04. The pedons were formed from the weathering of among other materials, colluvial igneous rocks, alluvium, eluvial soils, laterite, lacustrine sands and silts, andesite, pumice, aeolian deposits, and metamorphic rocks including coarse grained and strongly foliated biotite gneisses. Twenty soil samples were taken for laboratory characterization. In addition to classical horizon by horizon descriptions and laboratory analyses, 12 core samples were taken for soil-water retention characterization. The available water holding capacity was rated as very low to low. Pedon descriptions and particle size analysis showed clay eluviation-illuviation was the predominant pedogenic process in all pedons. Soil pH was rated slightly acidic to slightly alkaline. Available P ranged from 0.71 mg/kg at Mbimba to 10.67 mg/kg at Seatondale. Exchangeable bases were variable across and within the profiles; at Uyole and Inyala they were high, while at Seatondale and Mbimba they were low and medium. Values of exchangeable bases showed decreasing trends with profile depths in all sites. C/N ratios ranged between 6 and 18, total nitrogen was rated very low to low in both A and B horizons. CECsoil ranged between 17.2 and 36.4 cmol  (+)/kg. Organic carbon ranged from very low to high. The soils apparently developed from extreme and moderate weathering of parent materials. According to the USDA Soil Taxonomy, the pedons classified as Fine, Illitic, Active, Isothermic Typic Hapludult; Fine, Illitic, Active, Isothermic Andic Paleudalf; Fine, Illitic, Active, Isothermic, Mollic Paleudalf; Pumiceous, Mixed, Superactive, Isothermic, Typic Hapludand for Seatondale, Mbimba, Inyala, and Uyole, respectively. The soil depths were deep and very deep. Moisture stress and low levels of some macro-elements highly limited the productivity of the soils.},
     year = {2018}
    }
    

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  • TY  - JOUR
    T1  - Pedology at Four Representative Sites of Southern Highland Zone of Tanzania
    AU  - Johnson Godlove Mtama
    AU  - Balthazar Michael Msanya
    AU  - Charles Lee Burras
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    JF  - American Journal of Agriculture and Forestry
    JO  - American Journal of Agriculture and Forestry
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    PB  - Science Publishing Group
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    UR  - https://doi.org/10.11648/j.ajaf.20180605.11
    AB  - To study the soils of Southern Highland Zone of Tanzania, four representative pedons of some landscapes were characterized. Their names and identifiers are Seatondale, Mbimba, Inyala, and Uyole, respectively TzSea 01, TzMb 02, TzIny 03, and TzUy04. The pedons were formed from the weathering of among other materials, colluvial igneous rocks, alluvium, eluvial soils, laterite, lacustrine sands and silts, andesite, pumice, aeolian deposits, and metamorphic rocks including coarse grained and strongly foliated biotite gneisses. Twenty soil samples were taken for laboratory characterization. In addition to classical horizon by horizon descriptions and laboratory analyses, 12 core samples were taken for soil-water retention characterization. The available water holding capacity was rated as very low to low. Pedon descriptions and particle size analysis showed clay eluviation-illuviation was the predominant pedogenic process in all pedons. Soil pH was rated slightly acidic to slightly alkaline. Available P ranged from 0.71 mg/kg at Mbimba to 10.67 mg/kg at Seatondale. Exchangeable bases were variable across and within the profiles; at Uyole and Inyala they were high, while at Seatondale and Mbimba they were low and medium. Values of exchangeable bases showed decreasing trends with profile depths in all sites. C/N ratios ranged between 6 and 18, total nitrogen was rated very low to low in both A and B horizons. CECsoil ranged between 17.2 and 36.4 cmol  (+)/kg. Organic carbon ranged from very low to high. The soils apparently developed from extreme and moderate weathering of parent materials. According to the USDA Soil Taxonomy, the pedons classified as Fine, Illitic, Active, Isothermic Typic Hapludult; Fine, Illitic, Active, Isothermic Andic Paleudalf; Fine, Illitic, Active, Isothermic, Mollic Paleudalf; Pumiceous, Mixed, Superactive, Isothermic, Typic Hapludand for Seatondale, Mbimba, Inyala, and Uyole, respectively. The soil depths were deep and very deep. Moisture stress and low levels of some macro-elements highly limited the productivity of the soils.
    VL  - 6
    IS  - 5
    ER  - 

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