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

Batukaev, Abdul-Malik A.; Endovitsky, Anatoly P.; Andreev, Andrey G.; Kalinichenko, Valery P.; Minkina, Tatiana M.; Dikaev, Zaurbek S.; Mandzhieva, Saglara S.; Sushkova, Svetlana N.

doi:https://doi.org/10.5194/se-7-415-2016

Articles | Volume 7, issue 2

https://doi.org/10.5194/se-7-415-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/se-7-415-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 7, issue 2

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, Anatoly P. Endovitsky, Andrey G. Andreev, Valery P. Kalinichenko, Tatiana M. Minkina, Zaurbek S. Dikaev, Saglara S. Mandzhieva, and Svetlana N. Sushkova

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Final revised paper (published on 15 Mar 2016)
Preprint (discussion started on 18 Jan 2016)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'Reviewer's comments (Fedor Lisetsky)', Fedor Lisetsky, 28 Jan 2016
- AC1: 'Editor comment for Lisietsky', Tatiana Minkina, 17 Feb 2016
RC2: 'Review Prof. Valery Glazko', Valery Glazko, 29 Jan 2016
- AC2: 'Author comment for Glazko', Tatiana Minkina, 17 Feb 2016
RC3: 'Prof. Alla Okolelova Review', Alla Okolelova, 29 Jan 2016
- AC3: 'Author comment for Okolelova', Tatiana Minkina, 17 Feb 2016
SC1: 'Dr.Prof. M. Sokolov', michail sokolov, 03 Feb 2016
- AC4: 'Author comment for Sokolov', Tatiana Minkina, 17 Feb 2016

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.