Articles | Volume 7, issue 2
Solid Earth, 7, 415–423, 2016
Solid Earth, 7, 415–423, 2016

Research article 15 Mar 2016

Research article | 15 Mar 2016

Ion association in water solution of soil and vadose zone of chestnut saline solonetz as a driver of terrestrial carbon sink

Abdul-Malik A. Batukaev et al.

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Cited articles

Adams, F.: Ionic concentrations and activities in soil solutions, Soil Sci. Soc. Am. J., 35, 421–426,, 1971.
Ågren, A. M., Buffam, I., Cooper, D. M., Tiwari, T., Evans, C. D., and Laudon, H.: Can the heterogeneity in stream dissolved organic carbon be explained by contributing landscape elements?, Biogeosciences, 11, 1199–1213,, 2014.
Amakor, X. N., Jacobson, A. R., and Cardon, G. E.: Improving estimates of soil salinity from saturation paste extracts in calcareous soils, Soil Sci. Soc. Am. J., 3, 792–799,, 2013.
Anisimov, V. S., Anisimova, L. N., Frigidova, L. M., Dikarev, D. V., Frigidov, R. A., Kochetkov, I. V., and Sanzharova, N. I.: Evaluation of Migration Ability of Zn in the Soil-Plant System, Biogeosystem Technique, 4, 153–163,, 2015.
Bahn, M., Reichstein, M., Guan, K., Moreno, J. M., and Williams, C.: Climate extremes and biogeochemical cycles in the terrestrial biosphere: impacts and feedbacks across scales, Biogeosciences, 12, 4827–4830,, 2015.
Short summary
Calcium carbonate equilibrium in a solution of soil and vadose zone is a factor of geochemical cycle of the terrestrial system. The analytical concentration of ions was determined. The algorithm of computer program was developed to calculate the real equilibrium forms of ions. The concentration and mobility of ions in solution of soil and vadose zone is much higher compared to solubility product, and it promotes flux of carbon from soil.