This study was done in Morogoro and Mbeya regions of Tanzania to classify and characterize their respective soils. Representative pedons (SUARAT-P1 and UYOLE-P1) were dug and described using FAO guidelines clarifying morphological features, physico-chemical properties and genesis. The representative pedons were geo-referenced using Global Positioning System (GPS) receiver. A total of nine (9) genetic soil horizons were identified from both sites and samples from each horizon collected for physical and chemical analyses. Soils from both sites were very deep and topsoil moist colors ranged from hue of 7.5YR to 10YR with chroma of less than 3 in SUARAT-P1 and UYOLE-P1 pedons. Soil structure ranged from strong fine crumbs in topsoils to medium coarse sub-angular blocks in subsoils of SUARAT-P1 while UYOLE-P1 had weak fine sub-angular blocks in topsoils and subsoils. The SUARAT-P1 had sandy clay (SC) texture in topsoil and clay texture in subsoil while UYOLE-P1 had sandy loam (SL) in topsoil and sand clay loam (SCL) in subsoil. Soil reaction were slightly acid to very strongly acid in SUARAT-P1 (pH 6.54 - 4.46) whereas UYOLE-P1 were slightly acid to neutral in subsoil horizons (pH 6.35 – 7.32). Organic carbon ranged from very low to low (0.12- 0.95%) in SUARAT-P1 and from very low to medium (0.47 – 1.5%) in UYOLE-P1. Nitrogen levels were very low to low (0.05 - 0.12%) in both sites whereas available P ranged from low (0.30 mg kg-1) to medium (8.55 mg kg-1) in both pedons. CEC of SUARAT-P1 was medium ranging from 12.4 to 23.2 cmol(c) kg-1, whereas UYOLE-P1 was medium to high (15 – 34 cmol(c) kg-1). In SUARAT-P1, topsoil BS was high (> 50%) and low (< 50%) in the subsoil while UYOLE-P1 registered high BS throughout its profile depth. As diagnostic horizons for soil classification, the SUARAT-P1 had an ochric epipedon overlying a kandic horizon and classified according to USDA Soil Taxonomy as Typic Kandiustults, while UYOLE-P1 had an ochric epipedon over a cambic horizon and was named as Andic Dystrudepts corresponding respectively to Haplic Lixisols and Eutric Andic Cambisols in the WRB for Soil Resources. The results have indicated that, studied soils are less fertile with possible reconstitution through land and crop managements which include but not limited to no-tilling or conservation tillage, manuring and proper fertilizer application; residue retention, possible fallowing, liming for potential buffering of soil pH especially at SUARAT-P1 and crop rotation and intercropping with leguminous crops.
| Published in | International Journal of Natural Resource Ecology and Management (Volume 6, Issue 2) |
| DOI | 10.11648/j.ijnrem.20210602.17 |
| Page(s) | 79-92 |
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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. |
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Copyright © The Author(s), 2024. Published by Science Publishing Group |
Pedological Characterization, Soil Morphological Characteristics, Physico-chemical Properties, Soil Classification, Tanzania
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APA Style
Said Hamadi Mohamed, Balthazar Michael Msanya, Hamisi Juma Tindwa, Ernest Semu. (2021). Pedological Characterization and Classification of Selected Soils of Morogoro and Mbeya Regions of Tanzania. International Journal of Natural Resource Ecology and Management, 6(2), 79-92. https://doi.org/10.11648/j.ijnrem.20210602.17
ACS Style
Said Hamadi Mohamed; Balthazar Michael Msanya; Hamisi Juma Tindwa; Ernest Semu. Pedological Characterization and Classification of Selected Soils of Morogoro and Mbeya Regions of Tanzania. Int. J. Nat. Resour. Ecol. Manag. 2021, 6(2), 79-92. doi: 10.11648/j.ijnrem.20210602.17
AMA Style
Said Hamadi Mohamed, Balthazar Michael Msanya, Hamisi Juma Tindwa, Ernest Semu. Pedological Characterization and Classification of Selected Soils of Morogoro and Mbeya Regions of Tanzania. Int J Nat Resour Ecol Manag. 2021;6(2):79-92. doi: 10.11648/j.ijnrem.20210602.17
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author = {Said Hamadi Mohamed and Balthazar Michael Msanya and Hamisi Juma Tindwa and Ernest Semu},
title = {Pedological Characterization and Classification of Selected Soils of Morogoro and Mbeya Regions of Tanzania},
journal = {International Journal of Natural Resource Ecology and Management},
volume = {6},
number = {2},
pages = {79-92},
doi = {10.11648/j.ijnrem.20210602.17},
url = {https://doi.org/10.11648/j.ijnrem.20210602.17},
eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijnrem.20210602.17},
abstract = {This study was done in Morogoro and Mbeya regions of Tanzania to classify and characterize their respective soils. Representative pedons (SUARAT-P1 and UYOLE-P1) were dug and described using FAO guidelines clarifying morphological features, physico-chemical properties and genesis. The representative pedons were geo-referenced using Global Positioning System (GPS) receiver. A total of nine (9) genetic soil horizons were identified from both sites and samples from each horizon collected for physical and chemical analyses. Soils from both sites were very deep and topsoil moist colors ranged from hue of 7.5YR to 10YR with chroma of less than 3 in SUARAT-P1 and UYOLE-P1 pedons. Soil structure ranged from strong fine crumbs in topsoils to medium coarse sub-angular blocks in subsoils of SUARAT-P1 while UYOLE-P1 had weak fine sub-angular blocks in topsoils and subsoils. The SUARAT-P1 had sandy clay (SC) texture in topsoil and clay texture in subsoil while UYOLE-P1 had sandy loam (SL) in topsoil and sand clay loam (SCL) in subsoil. Soil reaction were slightly acid to very strongly acid in SUARAT-P1 (pH 6.54 - 4.46) whereas UYOLE-P1 were slightly acid to neutral in subsoil horizons (pH 6.35 – 7.32). Organic carbon ranged from very low to low (0.12- 0.95%) in SUARAT-P1 and from very low to medium (0.47 – 1.5%) in UYOLE-P1. Nitrogen levels were very low to low (0.05 - 0.12%) in both sites whereas available P ranged from low (0.30 mg kg-1) to medium (8.55 mg kg-1) in both pedons. CEC of SUARAT-P1 was medium ranging from 12.4 to 23.2 cmol(c) kg-1, whereas UYOLE-P1 was medium to high (15 – 34 cmol(c) kg-1). In SUARAT-P1, topsoil BS was high (> 50%) and low (ochric epipedon overlying a kandic horizon and classified according to USDA Soil Taxonomy as Typic Kandiustults, while UYOLE-P1 had an ochric epipedon over a cambic horizon and was named as Andic Dystrudepts corresponding respectively to Haplic Lixisols and Eutric Andic Cambisols in the WRB for Soil Resources. The results have indicated that, studied soils are less fertile with possible reconstitution through land and crop managements which include but not limited to no-tilling or conservation tillage, manuring and proper fertilizer application; residue retention, possible fallowing, liming for potential buffering of soil pH especially at SUARAT-P1 and crop rotation and intercropping with leguminous crops.},
year = {2021}
}
TY - JOUR T1 - Pedological Characterization and Classification of Selected Soils of Morogoro and Mbeya Regions of Tanzania AU - Said Hamadi Mohamed AU - Balthazar Michael Msanya AU - Hamisi Juma Tindwa AU - Ernest Semu Y1 - 2021/06/16 PY - 2021 N1 - https://doi.org/10.11648/j.ijnrem.20210602.17 DO - 10.11648/j.ijnrem.20210602.17 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 - 79 EP - 92 PB - Science Publishing Group SN - 2575-3061 UR - https://doi.org/10.11648/j.ijnrem.20210602.17 AB - This study was done in Morogoro and Mbeya regions of Tanzania to classify and characterize their respective soils. Representative pedons (SUARAT-P1 and UYOLE-P1) were dug and described using FAO guidelines clarifying morphological features, physico-chemical properties and genesis. The representative pedons were geo-referenced using Global Positioning System (GPS) receiver. A total of nine (9) genetic soil horizons were identified from both sites and samples from each horizon collected for physical and chemical analyses. Soils from both sites were very deep and topsoil moist colors ranged from hue of 7.5YR to 10YR with chroma of less than 3 in SUARAT-P1 and UYOLE-P1 pedons. Soil structure ranged from strong fine crumbs in topsoils to medium coarse sub-angular blocks in subsoils of SUARAT-P1 while UYOLE-P1 had weak fine sub-angular blocks in topsoils and subsoils. The SUARAT-P1 had sandy clay (SC) texture in topsoil and clay texture in subsoil while UYOLE-P1 had sandy loam (SL) in topsoil and sand clay loam (SCL) in subsoil. Soil reaction were slightly acid to very strongly acid in SUARAT-P1 (pH 6.54 - 4.46) whereas UYOLE-P1 were slightly acid to neutral in subsoil horizons (pH 6.35 – 7.32). Organic carbon ranged from very low to low (0.12- 0.95%) in SUARAT-P1 and from very low to medium (0.47 – 1.5%) in UYOLE-P1. Nitrogen levels were very low to low (0.05 - 0.12%) in both sites whereas available P ranged from low (0.30 mg kg-1) to medium (8.55 mg kg-1) in both pedons. CEC of SUARAT-P1 was medium ranging from 12.4 to 23.2 cmol(c) kg-1, whereas UYOLE-P1 was medium to high (15 – 34 cmol(c) kg-1). In SUARAT-P1, topsoil BS was high (> 50%) and low (ochric epipedon overlying a kandic horizon and classified according to USDA Soil Taxonomy as Typic Kandiustults, while UYOLE-P1 had an ochric epipedon over a cambic horizon and was named as Andic Dystrudepts corresponding respectively to Haplic Lixisols and Eutric Andic Cambisols in the WRB for Soil Resources. The results have indicated that, studied soils are less fertile with possible reconstitution through land and crop managements which include but not limited to no-tilling or conservation tillage, manuring and proper fertilizer application; residue retention, possible fallowing, liming for potential buffering of soil pH especially at SUARAT-P1 and crop rotation and intercropping with leguminous crops. VL - 6 IS - 2 ER -
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