| Peer-Reviewed

Effects of Liming on Physicochemical Properties and Nutrient Availability of Acidic Soils in Welmera Woreda, Central Highlands of Ethiopia

Received: 9 September 2017     Accepted: 8 October 2017     Published: 4 December 2017
Views:       Downloads:
Abstract

Soil acidity is one of chemical soil degradation problems which affect productivity of the soil in Ethiopian highlands. The purpose of this research was to identify the status of soil acidity and determine the amount of lime requirement for neutralization to increase plant nutrient availability in Welmera woreda, Oromia region. More specifically the study pointed out statistically, the nutrient availability before and after liming acidic soil using paired t-test. The results indicated that the soil of study area was strongly acidic (pH(H2O) < 5.3) and exchangeable acidity was from 2.86±0.01 - 3.55±0.07 cmol/Kg. The soil showed low concentration of plant nutrients (AP, TN, K, Ca, Mg) and high in micronutrients (Cu, Fe, Mn, and Zn) contents. After 90 days liming in greenhouse incubation of the soil samples, the results showed effective neutralization of the soil, which indicated it was properly limed and the effects of soil acidity on nutrient availability was clearly observed. The concentration of all anions (AP, TN, and OC), cations (Na+, K+, Ca+2 and Mg+2) and micronutrients were found to be significantly different except TN and OC, between the soil samples for before and after liming. After limed acidic soils, anion and cations are improved their availability for plant while micronutrients are decreased from toxicity to normal condition.

Published in Biochemistry and Molecular Biology (Volume 2, Issue 6)
DOI 10.11648/j.bmb.20170206.16
Page(s) 102-109
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), 2017. Published by Science Publishing Group

Keywords

Acidity, Incubation, Liming, Lime Materials, Soil pH

References
[1] Achalu C., (2012). Effects of Liming on Acidity-Related Chemical Properties of Soils of Different Land Use Systems in Western Oromia, Ethiopia. World Journal of agricultural society Vol. 8(6) pp. 560-567.
[2] Adane B. (2014). Effects of Liming Acidic Soils on Improving Soil Properties and Yield of Haricot Bean. Ethiopian Institute of Agricultural Research, Holetta ARC, Addis Ababa, Ethiopia. J Environ Anal Toxicology 4:248. doi: 10.4172/2161-0525.1000248
[3] Birhanu A. (2010). Soil Acidity Problems and Comparison of Lime Requirement, Determination Methods in Different Land Use in Fagetalekoma Woreda, Awi Zone, Amhara Region, Environmental Science Program, MSc. Thesis Submitted to School of Graduate Studies of AAU.
[4] Bouyoucos, G. (1962). Hydrometer method improvement for making particle size analysis of soils. Agronomy Journal Vol. 54 (1) pp. 54-57.
[5] Bray, R.. (1945). Determination of total organic and available phosphorous in soil (4th ed.). London: London Academic Press.
[6] Bremner, J. M. and C. S. Mulvaney, (1982). Nitrogen- Total. In: Page, A. L., R. H. Miller and D. R. Keeney (eds). Methods of Soil Analysis, Part 2. American Society Agronomy. Madison, Wiscosin, pp: 595-624.
[7] David, E. Kissel and Paul F. Vendrell,. ( 2012). Agricultural and Environmental Services Laboratories and Determining Lime Requirement Using the Equilibrium Lime Buffer Capacity (LBCEq).
[8] Desta, B. (2002). Effect of Liming and N and P Fertilization on Grain Yield of Barley in Ethiopian. Journal of Agricultural SciencesVol. 15) pp. 11-15.
[9] Haynes, J. R. (2001). Amelioration of aluminum toxicity and P deficiency in acid soils by additions of organic residues critical review of the phenomenon and the 22 mechanisms involved. Kluwer Academic Publishers Netherlands.
[10] Heluf G. and Kibebow, K. (2012). Effects of Liming on Acidity-Related Chemical Properties of Soils of Different Land Use Systems in Western Oromia, Ethiopia.
[11] Hue, N. V. ( 1998). Managing manganese toxicity in former sugarcane soils on Oahu. University of Hawaii at Manoa, College of Tropical Agriculture and Human Resources, publication SCM-1. p. 7.
[12] Huluka, G. (2005). A Modification of the Adams-Evans Soil Buffer Determination Solution. Communications in Soil Science and Plant Analysis (Vol. 36) pp. 949-951.
[13] Kamprath, E. J. (1984). Crop Response to Lime in the Tropics. In: Adams, F., Ed., Soil Acidity and Liming, 2nd Edition, Agronomy Monograph 12, Agronomy and Soil Science Society of America, Madison, 349-368.
[14] Ketterings, Q. M. ( 2005). Soil pH in field crops. Cornel University, College of Agriculture and Life Science, Department of crop and soil science, Cornel nutrient analysis laboratory Ithaca, NY 14853, Agronomy Fact Sheet S.
[15] Landon, J. ). (1991). Booker tropical soil manual: A Handbook for Soil Survey and Agricultural Land Evaluation in the Tropics and Subtropics. Longman Scientific and Technical, Essex, New York. (3rd Edition).
[16] Mesfin, A. (2009). Methods of Soil Analysis, Part 1: Physical and Mineralogical Methods, Cantarella, eds. Plant-Soil Interactions at Low pH. Campinas, Brazil: Brazilian So. (2nd editio, Ed.).
[17] MoFED, (2002). Ministry of Finance and Economic Development). Ethiopia: Sustainable Development and Poverty Reduction Program (SDPRP). Addis Ababa, Ethiopia.
[18] Rowell, D. L., 1994. Soil Science: Methods and Application, Addison Wesley Longman, Limited England.
[19] SAS Institute (2004). SAS User’s Guide, Statistics central & western Ethiopia, utilization of diversity in Version 9.1. (Ed.). SAS Inst., Cary, NC, USA.
[20] Simard, R. C. (1994). Effect oftillage, lime and phosphorus on soil pH and mehlich-3 Ababa, Ethiopia. extractable nutrients. Commun. Soil Sci. extractable nutrients. Commun. Soil Science and Pl. Anal., 25: 5.
[21] Solomon D. (2008). Presentation On the Relationships Existing in Minerals Soil Between pH On the One Hand and the Activity of Microorganisms and the Availability of Plant Nutrients On the Other. Bahir Dar University, Bahir Dar, Ethiopia.
[22] Sosulski, T. (2004). Estimation of liming and gypsum conservation division, USDA handbook No. 18. Usapplication on the content of exchangeable aluminum government printing office. Washington, D. C,: USA in sandy soil (in Polish).
[23] Taye, B. (2008). Estimation of Lime Requirment. Training Manual for Regional Soil Testing Laboratory Heads and Technicians. National Soil Testing Center, Ministry of Agriculture and Rural Development.
[24] Tekalign, B. (1992). Intensive training for soil laboratory technicians: Soil analysis on CEC, exchangeable base and calcium carbonate. National Soil Research Center. Addis Ababa, Ethiopia.
[25] Temesgen D. et al (2015). Effects of short-rotation Eucalyptus plantations on soil quality attributes in highly acidic soils of the central highlands of Ethiopia.
[26] Tilahun D,. (2004). Soil fertility status with emphasis on some micronutrients in vegetable growing areas of Kolfe, Addis Ababa, Ethiopia. M. Sc. Thesis Submitted to School of Graduate Studies, Haramaya University, Ethiopia.
[27] Van Lierop, W. (1991). Testing soils for pH and lime requirement. New York: Soil Science Society American Process.
[28] Walkley, A. F. (1934). An examination of the Degtjareff method for determining soil organic matter and a proposed modification of the chromic acid titration method. Soil Science Journal Vol. 6 pp 186-189.
[29] Wilding, L. (1985). Soil spatial variability: Its documentation, accommodation and implication to soil surveys, Soil Spatial Variability Proceedings of a Workshop of the ISSS and the SSA, Las Vegas PUDOC.
[30] Yihenew, G. (2002). Selected chemical and physical characteristics of soils Adet Research Center and its Testing Sites in North-Western Ethiopia. Ethiopian Journal of Natural Resources.
Cite This Article
  • APA Style

    Kebede Dinkecha, Dereje Tsegaye. (2017). Effects of Liming on Physicochemical Properties and Nutrient Availability of Acidic Soils in Welmera Woreda, Central Highlands of Ethiopia. Biochemistry and Molecular Biology, 2(6), 102-109. https://doi.org/10.11648/j.bmb.20170206.16

    Copy | Download

    ACS Style

    Kebede Dinkecha; Dereje Tsegaye. Effects of Liming on Physicochemical Properties and Nutrient Availability of Acidic Soils in Welmera Woreda, Central Highlands of Ethiopia. Biochem. Mol. Biol. 2017, 2(6), 102-109. doi: 10.11648/j.bmb.20170206.16

    Copy | Download

    AMA Style

    Kebede Dinkecha, Dereje Tsegaye. Effects of Liming on Physicochemical Properties and Nutrient Availability of Acidic Soils in Welmera Woreda, Central Highlands of Ethiopia. Biochem Mol Biol. 2017;2(6):102-109. doi: 10.11648/j.bmb.20170206.16

    Copy | Download

  • @article{10.11648/j.bmb.20170206.16,
      author = {Kebede Dinkecha and Dereje Tsegaye},
      title = {Effects of Liming on Physicochemical Properties and Nutrient Availability of Acidic Soils in Welmera Woreda, Central Highlands of Ethiopia},
      journal = {Biochemistry and Molecular Biology},
      volume = {2},
      number = {6},
      pages = {102-109},
      doi = {10.11648/j.bmb.20170206.16},
      url = {https://doi.org/10.11648/j.bmb.20170206.16},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.bmb.20170206.16},
      abstract = {Soil acidity is one of chemical soil degradation problems which affect productivity of the soil in Ethiopian highlands. The purpose of this research was to identify the status of soil acidity and determine the amount of lime requirement for neutralization to increase plant nutrient availability in Welmera woreda, Oromia region. More specifically the study pointed out statistically, the nutrient availability before and after liming acidic soil using paired t-test. The results indicated that the soil of study area was strongly acidic (pH(H2O) < 5.3) and exchangeable acidity was from 2.86±0.01 - 3.55±0.07 cmol/Kg. The soil showed low concentration of plant nutrients (AP, TN, K, Ca, Mg) and high in micronutrients (Cu, Fe, Mn, and Zn) contents. After 90 days liming in greenhouse incubation of the soil samples, the results showed effective neutralization of the soil, which indicated it was properly limed and the effects of soil acidity on nutrient availability was clearly observed. The concentration of all anions (AP, TN, and OC), cations (Na+, K+, Ca+2 and Mg+2) and micronutrients were found to be significantly different except TN and OC, between the soil samples for before and after liming. After limed acidic soils, anion and cations are improved their availability for plant while micronutrients are decreased from toxicity to normal condition.},
     year = {2017}
    }
    

    Copy | Download

  • TY  - JOUR
    T1  - Effects of Liming on Physicochemical Properties and Nutrient Availability of Acidic Soils in Welmera Woreda, Central Highlands of Ethiopia
    AU  - Kebede Dinkecha
    AU  - Dereje Tsegaye
    Y1  - 2017/12/04
    PY  - 2017
    N1  - https://doi.org/10.11648/j.bmb.20170206.16
    DO  - 10.11648/j.bmb.20170206.16
    T2  - Biochemistry and Molecular Biology
    JF  - Biochemistry and Molecular Biology
    JO  - Biochemistry and Molecular Biology
    SP  - 102
    EP  - 109
    PB  - Science Publishing Group
    SN  - 2575-5048
    UR  - https://doi.org/10.11648/j.bmb.20170206.16
    AB  - Soil acidity is one of chemical soil degradation problems which affect productivity of the soil in Ethiopian highlands. The purpose of this research was to identify the status of soil acidity and determine the amount of lime requirement for neutralization to increase plant nutrient availability in Welmera woreda, Oromia region. More specifically the study pointed out statistically, the nutrient availability before and after liming acidic soil using paired t-test. The results indicated that the soil of study area was strongly acidic (pH(H2O) < 5.3) and exchangeable acidity was from 2.86±0.01 - 3.55±0.07 cmol/Kg. The soil showed low concentration of plant nutrients (AP, TN, K, Ca, Mg) and high in micronutrients (Cu, Fe, Mn, and Zn) contents. After 90 days liming in greenhouse incubation of the soil samples, the results showed effective neutralization of the soil, which indicated it was properly limed and the effects of soil acidity on nutrient availability was clearly observed. The concentration of all anions (AP, TN, and OC), cations (Na+, K+, Ca+2 and Mg+2) and micronutrients were found to be significantly different except TN and OC, between the soil samples for before and after liming. After limed acidic soils, anion and cations are improved their availability for plant while micronutrients are decreased from toxicity to normal condition.
    VL  - 2
    IS  - 6
    ER  - 

    Copy | Download

Author Information
  • Department of Agricultural Chemistry, Melkassa Agriculture Research Centre, Adama, Ethiopia

  • Departments of Applied Chemistry, Adama Science and Technology University, Adama, Ethiopia

  • Sections