Pedological Characterization of Some Typical Alluvial Soils of Kilombero District, Tanzania
American Journal of Agriculture and Forestry
Volume 5, Issue 1, January 2017, Pages: 1-11
Received: Dec. 18, 2016; Accepted: Jan. 4, 2017; Published: Mar. 2, 2017
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Authors
Asheri Mwamba Kalala, Department of Soil and Geological Sciences, College of Agriculture, Sokoine University of Agriculture, Morogoro, Tanzania; Tumbi Agricultural Research Institute (ARI-Tumbi), Tabora, Tanzania
Balthazar Michael Msanya, Department of Soil and Geological Sciences, College of Agriculture, Sokoine University of Agriculture, Morogoro, Tanzania
Nyambilila Abdallah Amuri, Department of Soil and Geological Sciences, College of Agriculture, Sokoine University of Agriculture, Morogoro, Tanzania
Johnson Mashambo Semoka, Department of Soil and Geological Sciences, College of Agriculture, Sokoine University of Agriculture, Morogoro, Tanzania
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Abstract
This study was carried out in Kilombero District, Tanzania with the objective of characterizing the soils in terms of their morphology, genesis, physico-chemical properties and classification. Three pedons KISA-P1, MKU-P1 and MBA-P1 were identified within the Kilombero Valley, dug, described and sampled. Disturbed and undisturbed soil samples were taken from designated pedogenic horizons for physical and chemical analysis in the laboratory. Using both field and laboratory data soils were classified using both USDA Soil Taxonomy and World Reference Base for Soil Resources schemes of classification. Results show that the three pedons were developed under Isohyperthemic temperature and Aquic moisture regimes. All pedons were deep (100 - 120 cm). Whereas Pedons KISA-P1 and MBA-P1 had sandy clay loam topsoils overlying sandy clay subsoils, Pedon MKU-P1 had clayey texture throughout its profile depth. All pedons had low chromas of ≤ 3 and redoximorphic features in form of abundant mottles particularly in the subsoils. Topsoils of Pedons KISA-P1 and MBA-P1 had dominantly friable to very friable moist consistence while those of Pedon MKU-P1 had very firm moist consistence. Subsoil moist consistence varied from firm to extremely firm (Pedons KISA-P1 and MKU-P1) and from friable to very firm (Pedon MBA-P1). Structures were dominantly weak to moderate subangular blocky in all studied soils but some horizons were structureless single grained and massive. Soil reaction ranged from extremely acid (topsoil of MBA-P1) to mildly alkaline (subsoil of MKU-P1) with pH values of 4.44 and 6.73 respectively. Topsoil organic carbon and total nitrogen contents in the studied pedons were low (0.66 to 1.4%) and very low to low (0.08 to 0.19%) respectively. CECsoil values were rated as low to medium ranging from 8.4 to 23.8 cmol (+)/kg respectively in Pedon KISA-P1 and Pedon MKU-P1. Percent BS values varied between and within studied pedons and ranged from low < 50% to high > 50%. Studied soils manifested nutrient imbalances in respect of basic cations. On the overall, fertility of the studied soils was rated as low to medium. According to USDA Keys to Soil Taxonomy, Pedons KISA-P1 and MKU-P1 classified as Inceptisols, equivalent to Cambisols in WRB for Soil Resources whereas Pedon MBA-P1 classified as Entisols equivalent to Fluvisols. All three sites were recommended for paddy production.
Keywords
Physico-Chemical Properties, USDA Soil Taxonomy, WRB, Pedons, Kilombero District, Tanzania
To cite this article
Asheri Mwamba Kalala, Balthazar Michael Msanya, Nyambilila Abdallah Amuri, Johnson Mashambo Semoka, Pedological Characterization of Some Typical Alluvial Soils of Kilombero District, Tanzania, American Journal of Agriculture and Forestry. Vol. 5, No. 1, 2017, pp. 1-11. doi: 10.11648/j.ajaf.20170501.11
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Copyright © 2017 Authors retain the copyright of this article.
This article is an open access article distributed under the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/) which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
References
[1]
Brady, N. C. and Weil, R. R. (2008). The Nature and Properties of Soils, 12th edition. Prentice-Hall, Inc., Upper Saddle River, NJ, USA. 881 p.
[2]
Msanya, B. M., Munishi, J. A., Amuri, N., Semu, E., Mhoro, L and Malley, Z. (2016). Morphology, Genesis, Physico-chemical Properties, Classification and Potential of Soils, Derived from Volcanic Parent Materials in Selected Districts of Mbeya Region, Tanzania. International Journal of Plant Soil Science 10 (4): 1-19.
[3]
Jatzold, R. and Baum, E. (1968). The Kilombero Valley, Characteristic Features of Economic Geography of a Semihumid East African Floodplain and Its Margins. WeltforumVerlag, Munchen, Dillingen.
[4]
Kato, F. (2007). Development of major rice cultivation area in the Kilombero Valley, Tanzania. African Study Monograph 36: 3-18.
[5]
Sabugo, R. T. (2013). Adaptation strategies by smallholder rice farmers under the influence of climate change: A case of Kilombero basin, Tanzania. Dissertation for Master of Art in Rural Development Degree at SUA, Morogoro, Tanzania. 97 pp.
[6]
Gharibu F. N. (2014). Effectiveness of Minjingu Mazao as a Source of Phosphorus, Zinc and Copper in Rice Production in Kilombero District- Morogoro, Tanzania. Dissertation for MSc. Soil Science and Land Management of Sokoine University of Agriculture Morogoro, Tanzania. 87 pp.
[7]
Kilima, F. T. M. (2011). Scaling up Minjingu Phosphate Utilization for Balanced Fertilization of Crops in Tanzania. Participatory socio-economic and agronomic baseline survey Report. Sokoine University of Agriculture, Morogoro, 51 pp.
[8]
Massawe, B. H. J. and Amuri, N. (2012). Soil Fertility and Agronomic Practices Evaluation for Improved Rice Production in Lowland rice Producing areas Kilombero and Wami Valleys. A Report for ACDI/VOCA Project. Morogoro, Tanzania. 255pp.
[9]
Kalala, A. M., Amuri, N. A. and Semoka J. M. R. (2016). Sulphur and Zinc Fertilization Effects on Growth and Yield Response of Rice. International Journal of Plant Soil Science 11 (5): 1-12.
[10]
Msanya, B. M., Kaaya, A. K, Araki, S., Otsuka, H. and Nyadzi, G. I. (2003). Pedological characteristics, general fertility and classification of some benchmark soils of Morogoro District, Tanzania. Tanzania. African Journal of Science and Technology (AJST) Science and Engineering Series 4 (2): 101-112.
[11]
National Soil Service (1990). Laboratory procedures for routine analysis. 3rd edition. Agricultural Research Institute, Mlingano, Tanga, Tanzania. 212 pp.
[12]
Ministry of Agriculture Food Security and Cooperatives, Tanzania (MAFSC) (2008). Agricultural maps. Mlingano Agricultural Research Institute. www.kilimo.go.tz/agricultural maps/Tanzania Soil Maps/Soil maps. Site accessed April 2016.
[13]
De Pauw (1984). Soils, Physiographic and Agro-ecological Zones of Tanzania. Crop Monitoring and early warning systems project GCS/URT/047. NET. Ministry of Agricultural, Dar Es Salaam. Food and Agriculture organization of the United Nations.
[14]
FAO (2006). Guidelines for soil description. 4th edition. Food and Agriculture Organization of the United Nations. Rome, 66 pp.
[15]
Munsell Colour Company. (1940). Revised edition. Munsell soil colour charts. Macbeth Division of Kollmorgen Instruments Corporation, New York.
[16]
Blake, G. R. and Hartge, K. H. (1986). Bulk density. In: Methods of soil analysis, Part 1 Physical and mineralogical methods. (Edited by Klute A.). American Society of Agronomy. Madison, Wisconsin. Pp 364-374.
[17]
Day, P. R. (1965). Particle fractionation and particle size analysis. In: Black, C. A., Evans, D. D, White, J. L., Ensminger, L. E. and Clark F. E. (Eds.). Methods of soil analysis: Physical and mineralogical methods, American Society of Agronomy, Madison, Wisconsin. Pp 545-566.
[18]
Soil Survey Staff. (2014). Keys to Soil Taxonomy. 12th Edition. United States Department of Agriculture, Natural Resources Conservation Service.
[19]
Okalebo, J., R., Gathua, K. W. and Woomer, P. L. (2002). Laboratory Methods Of Soil and Plant Analysis: 2nd Edition. A working manual. 128pp.
[20]
Nelson, D. W. and Sommers, L. E. (1982). Total carbon, organic carbon and organic matter. In: Methods of soil analysis, Part 2; Chemical and mineralogical properties, 2nd edition. (Edited by Page, A. L., Miller, R. H. and Keeney, D. R.). American Society of Agronomy., Madison, Wisconsin. Pp 539-557.
[21]
Bremner, J. M. and Mulvaney, C. S. (1982). Total nitrogen. In: Methods of Soil Analysis. Part 2. Agronomy Monograph 9, American Society of Agronomy, Madison, Wisconsin, USA. pp 1149 -1170.
[22]
Thomas, G. W. (1996). Exchangeable cations. In: Methods of Soil Analysis. American Society ofAgronomy& Soil Science Society of America, Madison, Wisconsin.
[23]
Chapman, H. D. (1965). Cation exchange capacity. In: Methods of Soil Analysis. Edited by Black CA. American Institute of Agronomy 9: 891-901.
[24]
IUSS Working Group WRB (2014). World Reference Base for Soil Resources 2014 updates. International Soil Classification System for Naming Soils and Creating Legends for Soil Maps. World Soil Resource Report No. 106. FAO, Rome.
[25]
Akpan-Idiok, A. U. and Ogbaji, P. O. (2013). Characterization and Classification of Onwu River Floodplain Soils in Cross River State, Nigeria. International Journal of Agricultural Research 8: 107-122.
[26]
Obasi, S. N., Onweremadu, E. U., Egbuche, C. T. and Iwuanyanwu, U. P. (2015). Characterization and Classification of Selected Rice Soils of Tropical Rainforest Region, South-eastern Nigeria. Agriculture, Forestry and Fisheries 4 (3): 46-50.
[27]
Khan, Z. H., Hussain, M. S. and Ottner, F. (2012). Morphogenesis of Three Surface-Water Gley Soils from the Meghna Floodplain of Bangladesh. Dhaka University Journal of Biological Science 21 (2): 17-27.
[28]
Kebeney, S. J., Msanya, B. M., Ng’etich, W. K, Semoka, J. M. R. and Serrem. C. K. (2015). Pedological Characterization of Some Typical Soils of Busia County, Western Kenya: Soil Morphology, Physico-Chemical Properties, Classification and Fertility Trends. International Journal of Plant Soil Science 4 (1): 29-44.
[29]
Uwingabire, S., Msanya, B. M., Mtakwa, P. W., Uwitonze, P. and Sirikare, S. (2016). Pedological Characterization of Soils Developed on Gneissic- Granites in the Congo Nile Watershed Divide and Central Plateau Zones, Rwanda. International Journal of Current Research 8 (09): 39489-39501.
[30]
Uwitonze, P., Msanya B. M., Mtakwa, P. W., Uwingabire, S. and Sirikare, S. (2016). Pedological Characterization of Soils Developed from Volcanic Parent Materials of Northern Province of Rwanda. Agriculture, Forestry and Fisheries 5 (6): 225-236.
[31]
Landon, J. R. (1991). Booker Tropical Soil Manual: A handbook for soil survey and agricultural land evaluation in the tropics and subtropics. John Wiley and Sons: New York 450p.
[32]
USDA-NRCS (2016). Soil bulk density/moisture/aeration. Soil quality kit-Education for educators. Accessed October October, 2016.
[33]
Lal, R. and Shukla, M. K. (2005). Principles of soil physics. Marcel Dekker, Inc. New York. Basel. 699pp.
[34]
Massawe, B. H. J. (2015). Digital Soil Mapping and GIS-based Land Evaluation for Rice Suitability in Kilombero Valley, Tanzania. PhD thesis. Graduate School of Ohio State University.
[35]
EUROCONSULT. (1989). Agriculture Compendium for Rural Development in the Tropics and Sub-Tropics. 3rd Revised edition. Elsevier, Amsterdam. Oxford. New York. Tokyo. 740pp.
[36]
Msanya, B. M., Kimaro, D. N., Kimbi, G. G. and Munisi, A. L. M. (2001). Land resources inventory and suitability assessment for the production of the major crops in the eastern part of Morogoro Rural District, Tanzania. Department of Soil Science, 3: 1 - 69.
[37]
Magoggo, J. P., Msanya, B. M. and Kimaro, D. N. (1996). Environmental profile for agricultural production and development of conservation strategies in Mahenge Village, Mbinga District, Tanzania. Miombo Woodland Research Project, Natural Resources Study Team Technical Report 3. Department of Soil Science, Sokoine University of Agriculture, P. O. Box 3008, Morogoro, Tanzania & Ministry of Agriculture, National Soil Service, ARI Mlingano, Tanga, Tanzania. 38p.
[38]
Msanya, B. M., Kimaro, D. N. and Magoggo, J. P. (1995). Characteristics of two pedons and their implication for environmental management in parts of Mbinga District, Tanzania. Paper presented at the first annual Faculty of Agriculture Research Conference. August 28-30th. Sokoine University of Agriculture, Morogoro, Tanzania.
[39]
Meliyo, J. L. (1997). Pedological investigation and characterization in Litembo village, Mbinga District, Tanzania. MSc (Agric). Dissertation, Sokoine University of Agriculture, Morogoro, Tanzania. 113p.
[40]
Baba, M., Hennie, F. W., Soehady, E. and Sanudin, T. (2008). Geochemical characterization of volcanic soils from Tawau, abah. Geological Society of Malaysia Bulletin, 54: 33-36.
[41]
Nesbitt, H. W and Young, G. M. (1982). Early Proterozoic climates and plate motions inferred from major element chemistry of Lutites. Nature 299: 715-717.
[42]
FAO. (1961). The Rufiji Basin, Tanganyika. FAO Experts Technical. Assistance Programme. No. 1269, Vol. 7. Rome.
[43]
FAO. (2006). Country Pasture/Forage Resource Profiles. Philippines. http://www.fao.org/ag/aGp/agpc/doc/Counprof.Philippines.pdf. Accessed December 2016.
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