Mobilization of Soil Organic Matter by Ultrafresh Water: Modeling and Assessment of the Impact on the Mobility of Heavy Metals
The experiments on mobilization of soil organic matter during soil washing with ultrafresh water against the background of salinity pulsing were designed and performed. Unpolluted soil and the soil artificially polluted with copper(II) were used in experiments, namely, clay loamy typical chernozem (...
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| Veröffentlicht in: | Eurasian soil science 2021-06, Vol.54 (6), p.843-851 |
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| creator | Grechishcheva, N. Yu Yaroslavtsev, N. V. Kotelnikova, A. D. Ostakh, O. S. Kholodov, V. A. Zavorotny, V. L. Balaba, V. I. |
| description | The experiments on mobilization of soil organic matter during soil washing with ultrafresh water against the background of salinity pulsing were designed and performed. Unpolluted soil and the soil artificially polluted with copper(II) were used in experiments, namely, clay loamy typical chernozem (Haplic Chernozem) of the Alekhin Central Chernozemic Nature Reserve (Kursk oblast, Russia; 51°34.207 N, 36°05.444 E) and sandy loamy soddy-podzolic soil (Albic Glossic Retisol (Loamic, Cutanic, Ochric)) from the Domodedovo district of Moscow oblast, Russia (55°17.683 N, 37°50.045 E). Soil samples were taken from the upper humus-accumulative (A1) horizon (5–15 cm). A drastic change in the composition of washing solution from fresh water to 0.1 M NaCl solution and back led to destruction of soil aggregates under the impact of osmotic pressure. Soddy-podzolic soil proved to be more resistant to destruction as compared with typical chernozem. Copper(II) was leached off from artificially contaminated samples of soddy-podzolic soil with the flow of dissolved organic matter, whereas copper leaching from typical chernozem was associated with the destruction of aggregates and release of intraaggregate organic matter. It is argued that copper (II) migration models should take into account the amount of dissolved organic matter for soddy-podzolic soil and the content of aromatic fragments in the organic matter for typical chernozem. A conceptual model of the Cu(II) leaching from contaminated soddy-podzolic soil and typical chernozem in the course of soil washing with fresh water against the background of salinity pulsing and the destruction of soil structure is constructed. |
| doi_str_mv | 10.1134/S1064229321060053 |
| format | Article |
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Yu ; Yaroslavtsev, N. V. ; Kotelnikova, A. D. ; Ostakh, O. S. ; Kholodov, V. A. ; Zavorotny, V. L. ; Balaba, V. I.</creator><creatorcontrib>Grechishcheva, N. Yu ; Yaroslavtsev, N. V. ; Kotelnikova, A. D. ; Ostakh, O. S. ; Kholodov, V. A. ; Zavorotny, V. L. ; Balaba, V. I.</creatorcontrib><description>The experiments on mobilization of soil organic matter during soil washing with ultrafresh water against the background of salinity pulsing were designed and performed. Unpolluted soil and the soil artificially polluted with copper(II) were used in experiments, namely, clay loamy typical chernozem (Haplic Chernozem) of the Alekhin Central Chernozemic Nature Reserve (Kursk oblast, Russia; 51°34.207 N, 36°05.444 E) and sandy loamy soddy-podzolic soil (Albic Glossic Retisol (Loamic, Cutanic, Ochric)) from the Domodedovo district of Moscow oblast, Russia (55°17.683 N, 37°50.045 E). Soil samples were taken from the upper humus-accumulative (A1) horizon (5–15 cm). A drastic change in the composition of washing solution from fresh water to 0.1 M NaCl solution and back led to destruction of soil aggregates under the impact of osmotic pressure. Soddy-podzolic soil proved to be more resistant to destruction as compared with typical chernozem. Copper(II) was leached off from artificially contaminated samples of soddy-podzolic soil with the flow of dissolved organic matter, whereas copper leaching from typical chernozem was associated with the destruction of aggregates and release of intraaggregate organic matter. It is argued that copper (II) migration models should take into account the amount of dissolved organic matter for soddy-podzolic soil and the content of aromatic fragments in the organic matter for typical chernozem. A conceptual model of the Cu(II) leaching from contaminated soddy-podzolic soil and typical chernozem in the course of soil washing with fresh water against the background of salinity pulsing and the destruction of soil structure is constructed.</description><identifier>ISSN: 1064-2293</identifier><identifier>EISSN: 1556-195X</identifier><identifier>DOI: 10.1134/S1064229321060053</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Aggregates ; Analysis ; Aromatic compounds ; Copper ; Copper compounds ; Copper mattes ; Decomposing organic matter ; Destruction ; Dissolved organic matter ; Earth and Environmental Science ; Earth Sciences ; Fresh water ; Freshwater ; Geotechnical Engineering & Applied Earth Sciences ; Heavy metals ; Humus ; Inland water environment ; Leaching ; Metals ; Natural areas ; Nature reserves ; Organic soils ; Osmosis ; Osmotic pressure ; Podzolic soils ; Salinity ; Salinity effects ; Sandy soils ; Sodium chloride ; Soil ; Soil aggregates ; Soil Chemistry ; Soil contamination ; Soil organic matter ; Soil pollution ; Soil structure ; Soil water ; Soils ; Washing</subject><ispartof>Eurasian soil science, 2021-06, Vol.54 (6), p.843-851</ispartof><rights>The Author(s) 2021. ISSN 1064-2293, Eurasian Soil Science, 2021, Vol. 54, No. 6, pp. 843–851. © The Author(s), 2021. This article is an open access publication. Russian Text © The Author(s), 2021, published in Pochvovedenie, 2021, No. 6, pp. 675–685.</rights><rights>COPYRIGHT 2021 Springer</rights><rights>The Author(s) 2021. ISSN 1064-2293, Eurasian Soil Science, 2021, Vol. 54, No. 6, pp. 843–851. © The Author(s), 2021. This article is an open access publication. Russian Text © The Author(s), 2021, published in Pochvovedenie, 2021, No. 6, pp. 675–685. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). 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Unpolluted soil and the soil artificially polluted with copper(II) were used in experiments, namely, clay loamy typical chernozem (Haplic Chernozem) of the Alekhin Central Chernozemic Nature Reserve (Kursk oblast, Russia; 51°34.207 N, 36°05.444 E) and sandy loamy soddy-podzolic soil (Albic Glossic Retisol (Loamic, Cutanic, Ochric)) from the Domodedovo district of Moscow oblast, Russia (55°17.683 N, 37°50.045 E). Soil samples were taken from the upper humus-accumulative (A1) horizon (5–15 cm). A drastic change in the composition of washing solution from fresh water to 0.1 M NaCl solution and back led to destruction of soil aggregates under the impact of osmotic pressure. Soddy-podzolic soil proved to be more resistant to destruction as compared with typical chernozem. Copper(II) was leached off from artificially contaminated samples of soddy-podzolic soil with the flow of dissolved organic matter, whereas copper leaching from typical chernozem was associated with the destruction of aggregates and release of intraaggregate organic matter. It is argued that copper (II) migration models should take into account the amount of dissolved organic matter for soddy-podzolic soil and the content of aromatic fragments in the organic matter for typical chernozem. A conceptual model of the Cu(II) leaching from contaminated soddy-podzolic soil and typical chernozem in the course of soil washing with fresh water against the background of salinity pulsing and the destruction of soil structure is constructed.</description><subject>Aggregates</subject><subject>Analysis</subject><subject>Aromatic compounds</subject><subject>Copper</subject><subject>Copper compounds</subject><subject>Copper mattes</subject><subject>Decomposing organic matter</subject><subject>Destruction</subject><subject>Dissolved organic matter</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fresh water</subject><subject>Freshwater</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Heavy metals</subject><subject>Humus</subject><subject>Inland water environment</subject><subject>Leaching</subject><subject>Metals</subject><subject>Natural areas</subject><subject>Nature reserves</subject><subject>Organic soils</subject><subject>Osmosis</subject><subject>Osmotic pressure</subject><subject>Podzolic soils</subject><subject>Salinity</subject><subject>Salinity effects</subject><subject>Sandy soils</subject><subject>Sodium chloride</subject><subject>Soil</subject><subject>Soil aggregates</subject><subject>Soil Chemistry</subject><subject>Soil contamination</subject><subject>Soil organic matter</subject><subject>Soil pollution</subject><subject>Soil structure</subject><subject>Soil water</subject><subject>Soils</subject><subject>Washing</subject><issn>1064-2293</issn><issn>1556-195X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><recordid>eNp1UctKAzEUHUTB5we4C7geTSZJJ3FXio9CiwstuhvSyU0bmSY1SYW68NtNHcGFyF3cxznnPrhFcU7wJSGUXT0SPGBVJWmVA4w53SuOCOeDkkj-sp_jDJc7_LA4jvEVYyoEE0fF59TPbWc_VLLeIW_Qo7cdeggL5WyLpiolCGi-RbMuBWUCxCV6Vrl2jaZeQ2fdAimn0TBGiHEFLu16pCWg8Wqt2py576yfkrY79B7U-xZNIakunhYHJjs4-_Enxez25ml0X04e7saj4aRUtKap1LKlhlHgAywxa-uq5nqgmZZzLI1mDFoha4pFPotrQzOdGVlLrAUACK3pSXHR910H_7aBmJpXvwkuj2wqzpiQnHKSWZc9a6E6aKwzPh_dZtOwsq13YGyuD2siWCVqIbKA9II2-BgDmGYd7EqFbUNws_tL8-cvWVP1mpi5bgHhd5X_RV_8JI8U</recordid><startdate>20210601</startdate><enddate>20210601</enddate><creator>Grechishcheva, N. 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Yu</au><au>Yaroslavtsev, N. V.</au><au>Kotelnikova, A. D.</au><au>Ostakh, O. S.</au><au>Kholodov, V. A.</au><au>Zavorotny, V. L.</au><au>Balaba, V. I.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mobilization of Soil Organic Matter by Ultrafresh Water: Modeling and Assessment of the Impact on the Mobility of Heavy Metals</atitle><jtitle>Eurasian soil science</jtitle><stitle>Eurasian Soil Sc</stitle><date>2021-06-01</date><risdate>2021</risdate><volume>54</volume><issue>6</issue><spage>843</spage><epage>851</epage><pages>843-851</pages><issn>1064-2293</issn><eissn>1556-195X</eissn><abstract>The experiments on mobilization of soil organic matter during soil washing with ultrafresh water against the background of salinity pulsing were designed and performed. Unpolluted soil and the soil artificially polluted with copper(II) were used in experiments, namely, clay loamy typical chernozem (Haplic Chernozem) of the Alekhin Central Chernozemic Nature Reserve (Kursk oblast, Russia; 51°34.207 N, 36°05.444 E) and sandy loamy soddy-podzolic soil (Albic Glossic Retisol (Loamic, Cutanic, Ochric)) from the Domodedovo district of Moscow oblast, Russia (55°17.683 N, 37°50.045 E). Soil samples were taken from the upper humus-accumulative (A1) horizon (5–15 cm). A drastic change in the composition of washing solution from fresh water to 0.1 M NaCl solution and back led to destruction of soil aggregates under the impact of osmotic pressure. Soddy-podzolic soil proved to be more resistant to destruction as compared with typical chernozem. Copper(II) was leached off from artificially contaminated samples of soddy-podzolic soil with the flow of dissolved organic matter, whereas copper leaching from typical chernozem was associated with the destruction of aggregates and release of intraaggregate organic matter. It is argued that copper (II) migration models should take into account the amount of dissolved organic matter for soddy-podzolic soil and the content of aromatic fragments in the organic matter for typical chernozem. A conceptual model of the Cu(II) leaching from contaminated soddy-podzolic soil and typical chernozem in the course of soil washing with fresh water against the background of salinity pulsing and the destruction of soil structure is constructed.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1064229321060053</doi><tpages>9</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Aggregates Analysis Aromatic compounds Copper Copper compounds Copper mattes Decomposing organic matter Destruction Dissolved organic matter Earth and Environmental Science Earth Sciences Fresh water Freshwater Geotechnical Engineering & Applied Earth Sciences Heavy metals Humus Inland water environment Leaching Metals Natural areas Nature reserves Organic soils Osmosis Osmotic pressure Podzolic soils Salinity Salinity effects Sandy soils Sodium chloride Soil Soil aggregates Soil Chemistry Soil contamination Soil organic matter Soil pollution Soil structure Soil water Soils Washing |
| title | Mobilization of Soil Organic Matter by Ultrafresh Water: Modeling and Assessment of the Impact on the Mobility of Heavy Metals |
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