Thermodynamic modeling of aqueous migration of chemical elements in irrigation water

Research of migration forms in irrigation water of flooded fields contributes to understanding geochemical barrier formation and functioning. It can improve pollution and nutrification control in the soil-water-plant system since geochemical barriers promote concentrating chemical elements at differ...

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Main Authors: Soldatova Evgeniya, Sidkina Evgeniya, Sun Zhanxue
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/82/e3sconf_daic2020_05022.pdf
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spelling doaj-bcb55ab94569437180e3ca818c4765b22021-04-02T16:40:26ZengEDP SciencesE3S Web of Conferences2267-12422020-01-012220502210.1051/e3sconf/202022205022e3sconf_daic2020_05022Thermodynamic modeling of aqueous migration of chemical elements in irrigation waterSoldatova Evgeniya0Sidkina Evgeniya1Sun Zhanxue2Vernadsky Institute of Geochemistry and Analytical Chemistry of Russian Academy of SciencesVernadsky Institute of Geochemistry and Analytical Chemistry of Russian Academy of SciencesEast China University of TechnologyResearch of migration forms in irrigation water of flooded fields contributes to understanding geochemical barrier formation and functioning. It can improve pollution and nutrification control in the soil-water-plant system since geochemical barriers promote concentrating chemical elements at different depths of a soil cross-section. The research aimed to simulate the aqueous migration of chemical elements and their precipitation in the flooded rice fields’ irrigation water to determine the potential of removing them from the solution at the sorption geochemical barrier. The samples of irrigation water were taken after harvesting in the Poyang Lake basin (China) and analyzed with a standard set of methods for natural water, including ICP-MS and ICP-AES. To assess the migration forms, the HCh software package was used. The thermodynamic values database was supplemented with free energies of formation of metal complexes with fulvic and humic acids for standard conditions. Modeling has shown that most of the considered chemical elements migrate in positively charging simple ions. The main agents of complexation with humic substances are Fe, Ca, and U. Kaolinite potentially precipitates from the irrigation water. Results show that sorption of positively charged simple ions and MoO42− on clay minerals should be under special attention.https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/82/e3sconf_daic2020_05022.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Soldatova Evgeniya
Sidkina Evgeniya
Sun Zhanxue
spellingShingle Soldatova Evgeniya
Sidkina Evgeniya
Sun Zhanxue
Thermodynamic modeling of aqueous migration of chemical elements in irrigation water
E3S Web of Conferences
author_facet Soldatova Evgeniya
Sidkina Evgeniya
Sun Zhanxue
author_sort Soldatova Evgeniya
title Thermodynamic modeling of aqueous migration of chemical elements in irrigation water
title_short Thermodynamic modeling of aqueous migration of chemical elements in irrigation water
title_full Thermodynamic modeling of aqueous migration of chemical elements in irrigation water
title_fullStr Thermodynamic modeling of aqueous migration of chemical elements in irrigation water
title_full_unstemmed Thermodynamic modeling of aqueous migration of chemical elements in irrigation water
title_sort thermodynamic modeling of aqueous migration of chemical elements in irrigation water
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description Research of migration forms in irrigation water of flooded fields contributes to understanding geochemical barrier formation and functioning. It can improve pollution and nutrification control in the soil-water-plant system since geochemical barriers promote concentrating chemical elements at different depths of a soil cross-section. The research aimed to simulate the aqueous migration of chemical elements and their precipitation in the flooded rice fields’ irrigation water to determine the potential of removing them from the solution at the sorption geochemical barrier. The samples of irrigation water were taken after harvesting in the Poyang Lake basin (China) and analyzed with a standard set of methods for natural water, including ICP-MS and ICP-AES. To assess the migration forms, the HCh software package was used. The thermodynamic values database was supplemented with free energies of formation of metal complexes with fulvic and humic acids for standard conditions. Modeling has shown that most of the considered chemical elements migrate in positively charging simple ions. The main agents of complexation with humic substances are Fe, Ca, and U. Kaolinite potentially precipitates from the irrigation water. Results show that sorption of positively charged simple ions and MoO42− on clay minerals should be under special attention.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/82/e3sconf_daic2020_05022.pdf
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AT sidkinaevgeniya thermodynamicmodelingofaqueousmigrationofchemicalelementsinirrigationwater
AT sunzhanxue thermodynamicmodelingofaqueousmigrationofchemicalelementsinirrigationwater
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