Research Article Open Access


A. A. Batukaev1, A. P. Endovitsky2, T. M. Minkina3, V. P. Kalinichenko2, Z. S. Dikaev1 and S. N. Sushkova3
  • 1 The Chechen State University, 364907, Grozny, Sheripov St., 32, Chechen Republic, Russia
  • 2 Institute of Fertility of Soils of South Russia, 346493, Persianovska, Rostov Region, Russia
  • 3 Southern Federal University, 344006, Bolshaya Sadovaya St., 105, Rostov-on-Don, Russia


Dynamics of material composition, migration and accumulation of salts is determined by chemical equilibrium in soil solution. Soil solution contains associated electrically neutral ion pairs CaCO30; CaSO40, MgCO30, MgSO40, charged ion pairs CaHCO3+, MgHCO3+, NaCO3-, NaSO4-, CaOH+, MgOH+. Calculation method is proposed for quantitative assessment of real ion forms in the soil solution of chestnut solonetz soil complex. Were proposed equations to calculate free and associated forms of ions. To solve the equations were used an iteration, a linear interpolation of equilibrium constants, a Method of Ionic Pairs including a law of initial concentration preservation, a law of the operating masses of equilibrium system, the concentration constants of ion pair dissociation on the law of operating masses. Was determined the quantity of ion free form and a coefficient of ion association as ratio of ions free form to analytical content γe = Cass/Can. The association of ions varies in individual soils and soil layer. Increasing soil solution salinity amplifies the ions association. In form of ionic pairs in soil solution are: 11.8-53.8% of Ca2+; 9.4-57.3% of Mg2+; 0.7-11.9% of Na+; 2.2-22.3% of HCO3-, 11.8-62.7% of SO42-. The ion CO32- is high associated, the share of ions in associated form is up to 92.7%. The degree of soil solution saturation was obtained for three level of approximation accounting on analytical concentration, calculated association coefficient, calculated coefficient of association. Relating to thermodynamic solubility product S0, the mathematical product of analytical ionic pairs indicated super saturation of soil solutions up to K1 = 100, taking into account calculated coefficient of association ion activity super saturation of soil solutions is absent, K3≈1. Only for solonetz chestnut meadow K3≈2-5. The soil solution saturation degree in soil profile and laterally in landscape varies. The quantitative assessment of real ion forms in the soil solution allows explain evolution of landscape of salted soils, structure of soil cover. Calculations fulfilled show that a possibility of soil degradation scenario taking into account the laws of association of ions in soil solution is much more probable and dangerous than it was assessed before. New understanding of water-salt transfer, geochemical barriers and ecological functions of soil will help to improve rainfed and irrigational agriculture.

American Journal of Agricultural and Biological Sciences
Volume 9 No. 3, 2014, 420-429


Submitted On: 29 May 2014 Published On: 24 June 2014

How to Cite: Batukaev, A. A., Endovitsky, A. P., Minkina, T. M., Kalinichenko, V. P., Dikaev, Z. S. & Sushkova, S. N. (2014). CHEMICAL EQUILIBRIUM OF SOIL SOLUTION IN STEPPE ZONE SOIL. American Journal of Agricultural and Biological Sciences, 9(3), 420-429.

  • 1 Citations



  • Soil Solution
  • Chemical Equilibrium
  • Ion Association
  • Calculation Method
  • Landscape
  • Structure of Soil Cover