Effect of total electrolyte concentration and sodium adsorption ratio on degree of dispersion of salt affected soils in Maharashtra, India

Bhargabi Chakraborty


The present investigation was carried out in the Purna valley of Vidarbha region of Maharashtra to study the effect of sodium adsorption ratio with total electrolyte concentration and on degree of dispersion of salt affected soils in Maharashtra. The sampling was done in the month of October, 2013. The soil samples were taken from two sites; at the depth of 0-20 cm (surface soil) and 20- 40 cm (sub-surface soil) respectively. For equilibration of soil samples the synthetic waters were prepared with 4 levels of total electrolyte concentrations (TEC) i.e. 10, 20,40,80 meL-1 with three levels of SAR viz., 5, 10 and 15 mmol1/2L-1/2. Electrolyte concentrations significantly affect the degree of dispersion. With increasing electrolyte concentration degree of dispersion decreases which usually increase the permeability of the soil. Dispersed clay particles clogged the micro pores which ultimately affect the hydraulic conductivity of the soil.

How to Cite
Bhargabi Chakraborty. (2015). Effect of total electrolyte concentration and sodium adsorption ratio on degree of dispersion of salt affected soils in Maharashtra, India. Journal of Innovative Agriculture, 2(1), 9-16. Retrieved from https://www.jinagri.com/index.php/jinagri/article/view/8


  1. Abhange, G.V. 1986. Drainage problems in Maharashtra past experiences and future challenges. Sinchan, 4: 50-80.
  2. Balpande, S.S. 1993. Factors and Processes of Soil degradation in Vertisols of Purna valley, Maharashtra, India. Land degradation and development, 7: 1-12.
  3. Gaikwad, S.T. and O. Challa. 1996. Soils of Maharashtra, their problems and potentials. Paper presented at state level Seminar Indian Soc. Soil Sci. Akola Chapter, Akola, Dec. 12-13, 1996.
  4. Giridhar, I.K. and J.S.P. Yadav. 1980. Effect of different Mg/Ca ratios and SAR values and electrolyte concentration in the leaching water on the dispersion and hydraulic conductivity of soil s. int. Symp. Salt affected Soils, Karnal 210-218.
  5. Hamid, K.S. and M.A. Mustafa. 1975. Dispersion as an index of relative hydraulic conductivity in salt affected soils of sudan. Geoderma, 14: 107.
  6. Jackson, M.L. 1973. Soil Chemical Analysis, Prentice Hall of India Pvt. Ltd., New Delhi.
  7. Jurinak, J.J., C. Amrhein and R.J. Wagenet. 1984. Sodic hazard: The effect of SAR and salinity in soils in overburden materials. Soil Sci., 137: 152-159.
  8. Lal, P., B.R. Chippa and A. Kumar. 1993. Salt affected soils and crop production. A modern synthesis. Management of salt affected soils by G.L. Maliwal. pp. 134-135.
  9. Padole, V.R., D.W. Deshmukh and R.K. Chakolkar. 1998. Water retention andhydraulic conductivity of salt affected Vertisols as influenced by physico-chemical properties. PKV Research J., 22 (2): 211-213.
  10. Page, A.L., R.H. Miller and D.R. Keeny. 1982. Methods of Soil Analysis, second edition, Part 2.Chemical and microbiological properties ASA, Madison, Wisconsin, USA.
  11. Panse, V.G. and P.V. Sukhatme. 1985. Statistical methods for Agricultural Workers, ICAR, New Delhi.
  12. Sharma, S.K. and I.C. Gupta, 1986. Saline environment and plant growth. Botanical Publisher, Bikaner. pp. 172.
  13. Sharma, R.C., A.K. Mandal, R.K. Saxena and K.S. Verma. 2004. Characteristics, formation and reclaimability of sodic soils under different geomorphic plains of Ganga basin. Extended summaries: International conference on sustainable management of sodic lands, 1: 168-170.
  14. U. S. Salinity laboratory staff 1954. Diagnosis and important of saline and alkaline soil. U. S. Dept. Agric. Handbook No. 60. Washington. D.C.
  15. Van, O.H. 1977. An introduction to clay colloid chemistry 2nd Ed.New York, John Willey and Sons.
  16. Walkely, A. and A.I. Black. 1934. An examination of degtijare FF method for determining soil organic matter and a propose modification of chromic acid titration method. Soil Science., 37: 29-38.