Profile of desert sandy soils formed in the Aral Sea dried-up seabed
In subsequent years, as a result of the strengthening of natural and anthropogenic factors, the inability of the Amu Darya and Sir Darya waters to flow into the Aral Sea, the mechanical composition of desert sandy soils, the type of salinization, the degree of salinization, the variety of humus cont...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
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EDP Sciences
2024-01-01
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| Series: | E3S Web of Conferences |
| Online Access: | https://www.e3s-conferences.org/articles/e3sconf/pdf/2024/16/e3sconf_agritech-ix2023_04010.pdf |
| _version_ | 1797315687605075968 |
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| author | Ismonov Аbduvaxob Dusaliev Аlijon Kalandarov Nazimkhon Mamajanova Uktamkhon Kattaeva Gulnoza |
| author_facet | Ismonov Аbduvaxob Dusaliev Аlijon Kalandarov Nazimkhon Mamajanova Uktamkhon Kattaeva Gulnoza |
| author_sort | Ismonov Аbduvaxob |
| collection | DOAJ |
| description | In subsequent years, as a result of the strengthening of natural and anthropogenic factors, the inability of the Amu Darya and Sir Darya waters to flow into the Aral Sea, the mechanical composition of desert sandy soils, the type of salinization, the degree of salinization, the variety of humus content in the soils common in the soil covers of the dried seabed were studied. During the study of the study area soils, the strong salinization of soils was noted by the chloride-sulfate salinization type and the salinization in the surface layer of the soil profile section No. 47, that is, in the layers 0- 9 cm and 9-50 cm deep, and weak salinization by the sulfate-chloride salinization type and the salinization in the lower layer of the soil profile. In the surface layer of the studied desert sandy soils, that is, by 0-9 cm and 9- 50 cm, the humus content ranged from 0.418% to 0.528%. On the dried bottom of the Aral Sea, because of strong evaporation of groundwater in the soil profile, an intensive process of accumulation of salt crystals took place, and desert sandy soils became highly saline. |
| first_indexed | 2024-03-08T03:07:24Z |
| format | Article |
| id | doaj.art-f4cd2970e11241c8ae9fb9bc18229ea8 |
| institution | Directory Open Access Journal |
| issn | 2267-1242 |
| language | English |
| last_indexed | 2024-03-08T03:07:24Z |
| publishDate | 2024-01-01 |
| publisher | EDP Sciences |
| record_format | Article |
| series | E3S Web of Conferences |
| spelling | doaj.art-f4cd2970e11241c8ae9fb9bc18229ea82024-02-13T08:28:05ZengEDP SciencesE3S Web of Conferences2267-12422024-01-014860401010.1051/e3sconf/202448604010e3sconf_agritech-ix2023_04010Profile of desert sandy soils formed in the Aral Sea dried-up seabedIsmonov Аbduvaxob0Dusaliev Аlijon1Kalandarov Nazimkhon2Mamajanova Uktamkhon3Kattaeva Gulnoza4Research Institute of Soil Science and AgrochemistryResearch Institute of Soil Science and AgrochemistryResearch Institute of Soil Science and AgrochemistryResearch Institute of Soil Science and AgrochemistryResearch Institute of Soil Science and AgrochemistryIn subsequent years, as a result of the strengthening of natural and anthropogenic factors, the inability of the Amu Darya and Sir Darya waters to flow into the Aral Sea, the mechanical composition of desert sandy soils, the type of salinization, the degree of salinization, the variety of humus content in the soils common in the soil covers of the dried seabed were studied. During the study of the study area soils, the strong salinization of soils was noted by the chloride-sulfate salinization type and the salinization in the surface layer of the soil profile section No. 47, that is, in the layers 0- 9 cm and 9-50 cm deep, and weak salinization by the sulfate-chloride salinization type and the salinization in the lower layer of the soil profile. In the surface layer of the studied desert sandy soils, that is, by 0-9 cm and 9- 50 cm, the humus content ranged from 0.418% to 0.528%. On the dried bottom of the Aral Sea, because of strong evaporation of groundwater in the soil profile, an intensive process of accumulation of salt crystals took place, and desert sandy soils became highly saline.https://www.e3s-conferences.org/articles/e3sconf/pdf/2024/16/e3sconf_agritech-ix2023_04010.pdf |
| spellingShingle | Ismonov Аbduvaxob Dusaliev Аlijon Kalandarov Nazimkhon Mamajanova Uktamkhon Kattaeva Gulnoza Profile of desert sandy soils formed in the Aral Sea dried-up seabed E3S Web of Conferences |
| title | Profile of desert sandy soils formed in the Aral Sea dried-up seabed |
| title_full | Profile of desert sandy soils formed in the Aral Sea dried-up seabed |
| title_fullStr | Profile of desert sandy soils formed in the Aral Sea dried-up seabed |
| title_full_unstemmed | Profile of desert sandy soils formed in the Aral Sea dried-up seabed |
| title_short | Profile of desert sandy soils formed in the Aral Sea dried-up seabed |
| title_sort | profile of desert sandy soils formed in the aral sea dried up seabed |
| url | https://www.e3s-conferences.org/articles/e3sconf/pdf/2024/16/e3sconf_agritech-ix2023_04010.pdf |
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