Research Article Open Access

THE ASSOCIATION OF IONS IN THE SOIL SOLUTION OF SALINE SOILS

A. P. Endovitsky1, T. M. Minkina2, V. P. Kalinichenko3, A. A. Batukaev4, Z. S. Dikaev4 and S. N. Sushkova2
  • 1 Don State Agrarian University, Oktyabrskiy District, 346493, Persianovsky Set, Russian Federatio, Russia
  • 2 Southern Federal University, Rostov-on-Don, 344006, Bolshaya Sadovaya St., 105, Russian Federation, Russia
  • 3 Don State Agrarian University, Oktyabrskiy District, 346493, Persianovsky Set, Russian Federation, Russia
  • 4 The Chechen State University, Chechen Republic, Grozny, 364907, Sheripov St., 32, Russian Federation, Russia

Abstract

The chemical equilibrium in the soil solution determines the dynamics of its material composition, migration and accumulation of salts. In the soil solution are formed electrically neutral ion pairs CaCO3°; CaSO4°, MgCO3°, MgSO4°, charged ion pairs CaHCO3+, MgHCO3+, NaCO3-, NaSO4-, CaOH+, MgOH+. The calculation method proposed for quantitative assessment of real ion forms in the soil solution of solonetz taking into account the ions association. Determination of real condition of the main ions in soil solution is based on ion association and its influence on physical and chemical properties of solution. Were calculated the free and associated ion form concentration according to analytical ion concentration. Were used an iteration to solve the equations of ion material balance, 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 following the law of operating masses. Upon completion of iterative procedure, was determined the quantity of ion free form and a coefficient of ion association γe as the ratio of ions free form to its analytical content γe = Cass/Can. For calculation procedure were used the own software products. The association of ions varies in individual soils and soil layers, Шncreasing the soil solution salinity amplifies the ions association. Depending on concentration and composition of soil solution the ionic pairs are: 15-45% Ca2+; 16-49% Mg2+; 0,6-8,4% Na+; 2,2-17,6% HCO3-, 16-51% SO42-, up to 88% CO32-. The proposed thermodynamic calculation method for quantitative assessment of real ion forms in the soil solution helps to explain the evolution of salted soils, maintain the soil, improve plant nutrition and irrigation.

American Journal of Agricultural and Biological Sciences
Volume 9 No. 2, 2014, 238-244

DOI: https://doi.org/10.3844/ajabssp.2014.238.244

Submitted On: 11 January 2014 Published On: 12 February 2014

How to Cite: Endovitsky, A. P., Minkina, T. M., Kalinichenko, V. P., Batukaev, A. A., Dikaev, Z. S. & Sushkova, S. N. (2014). THE ASSOCIATION OF IONS IN THE SOIL SOLUTION OF SALINE SOILS. American Journal of Agricultural and Biological Sciences, 9(2), 238-244. https://doi.org/10.3844/ajabssp.2014.238.244

  • 3,460 Views
  • 3,797 Downloads
  • 5 Citations

Download

Keywords

  • Soil Solution
  • Chemical Equilibrium
  • ION Association
  • Calculation Method