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Physical-mechanical and technological properties of eroded soils
The research aims to study and analyze the physical-mechanical and technological properties of eroded soils in Uzbekistan. The data on the susceptibility of water erosion to sloping lands is presented. The average monthly indicators of precipitation over the last ten years in Uzbekistan are analyzed...
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Published in: | E3S Web of Conferences 2021-01, Vol.264, p.4065 |
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description | The research aims to study and analyze the physical-mechanical and technological properties of eroded soils in Uzbekistan. The data on the susceptibility of water erosion to sloping lands is presented. The average monthly indicators of precipitation over the last ten years in Uzbekistan are analyzed. The results of determining the moisture, density, and hardness of the soil of slopes are presented. It has been established that with the traditional technology of tillage on moisture, density, and other technical properties of soil of slopes, water erosion and slope of fields have a significant effect. The physical-mechanical and technological properties of soil of the arable and subsurface layers of the soil of the top, the middle and lower part of the slope in spring and after grain harvesting differs significantly: in the spring period, the moisture of soil layers 0-10; 10-20; 30-40; 40-50 and 50-60 cm of the lower part of the slope is more moisture content of these layers of the top respectively, 1.16; 1.24; 1.1; 1.4; 1.54 and 2.15 times. Approximately such a picture of moisture is preserved after grain harvesting as well. |
doi_str_mv | 10.1051/e3sconf/202126404065 |
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The data on the susceptibility of water erosion to sloping lands is presented. The average monthly indicators of precipitation over the last ten years in Uzbekistan are analyzed. The results of determining the moisture, density, and hardness of the soil of slopes are presented. It has been established that with the traditional technology of tillage on moisture, density, and other technical properties of soil of slopes, water erosion and slope of fields have a significant effect. The physical-mechanical and technological properties of soil of the arable and subsurface layers of the soil of the top, the middle and lower part of the slope in spring and after grain harvesting differs significantly: in the spring period, the moisture of soil layers 0-10; 10-20; 30-40; 40-50 and 50-60 cm of the lower part of the slope is more moisture content of these layers of the top respectively, 1.16; 1.24; 1.1; 1.4; 1.54 and 2.15 times. Approximately such a picture of moisture is preserved after grain harvesting as well.</description><identifier>ISSN: 2267-1242</identifier><identifier>ISSN: 2555-0403</identifier><identifier>EISSN: 2267-1242</identifier><identifier>DOI: 10.1051/e3sconf/202126404065</identifier><language>eng</language><publisher>Les Ulis: EDP Sciences</publisher><subject>Arable land ; Density ; Harvesting ; Moisture content ; Slopes ; Soil erosion ; Soil layers ; Soil mechanics ; Soil moisture ; Soil properties ; Soil water ; Tillage ; Water content ; Water erosion</subject><ispartof>E3S Web of Conferences, 2021-01, Vol.264, p.4065</ispartof><rights>2021. This work is licensed under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3065-d62cbb7322e77996d3ff1095c2ecfc046d62912d1fe16d1f2fc12c9b4049d2ee3</citedby><cites>FETCH-LOGICAL-c3065-d62cbb7322e77996d3ff1095c2ecfc046d62912d1fe16d1f2fc12c9b4049d2ee3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.proquest.com/docview/2577566638?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>309,310,314,780,784,789,790,23930,23931,25140,25753,27924,27925,37012,44590</link.rule.ids></links><search><contributor>Bazarov, D.</contributor><creatorcontrib>Mamatov, Farmon</creatorcontrib><creatorcontrib>Umurzakov, Uktam</creatorcontrib><creatorcontrib>Mirzaev, Bakhadir</creatorcontrib><creatorcontrib>Rashidov, Nurbek</creatorcontrib><creatorcontrib>Eshchanova, Guzal</creatorcontrib><creatorcontrib>Avazov, Ikrom</creatorcontrib><title>Physical-mechanical and technological properties of eroded soils</title><title>E3S Web of Conferences</title><description>The research aims to study and analyze the physical-mechanical and technological properties of eroded soils in Uzbekistan. The data on the susceptibility of water erosion to sloping lands is presented. The average monthly indicators of precipitation over the last ten years in Uzbekistan are analyzed. The results of determining the moisture, density, and hardness of the soil of slopes are presented. It has been established that with the traditional technology of tillage on moisture, density, and other technical properties of soil of slopes, water erosion and slope of fields have a significant effect. The physical-mechanical and technological properties of soil of the arable and subsurface layers of the soil of the top, the middle and lower part of the slope in spring and after grain harvesting differs significantly: in the spring period, the moisture of soil layers 0-10; 10-20; 30-40; 40-50 and 50-60 cm of the lower part of the slope is more moisture content of these layers of the top respectively, 1.16; 1.24; 1.1; 1.4; 1.54 and 2.15 times. Approximately such a picture of moisture is preserved after grain harvesting as well.</description><subject>Arable land</subject><subject>Density</subject><subject>Harvesting</subject><subject>Moisture content</subject><subject>Slopes</subject><subject>Soil erosion</subject><subject>Soil layers</subject><subject>Soil mechanics</subject><subject>Soil moisture</subject><subject>Soil properties</subject><subject>Soil water</subject><subject>Tillage</subject><subject>Water content</subject><subject>Water erosion</subject><issn>2267-1242</issn><issn>2555-0403</issn><issn>2267-1242</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNpNUMtuwjAQtKpWKqL8QQ-Rek6x14_Et1aoDySk9tCeLcdZQ1CIqQ0H_r6moIrLPkaj2dkh5J7RR0YlmyJPLgx-ChQYKEEFVfKKjABUVTIQcH0x35JJSmtKKQNZZ-qIPH2uDqlzti836FZ2OI6FHdpil9ch9GH5h2xj2GLcdZiK4AuMocW2SKHr0x258bZPODn3Mfl-ffmavZeLj7f57HlROp4Nla0C1zQVB8Cq0lq13HtGtXSAzjsqVCZoBi3zyFSu4B0Dp5tsUreAyMdkftJtg12bbew2Nh5MsJ35A0JcGpsNuh4NMpQgFJMNrUTDqbZcaEXr2rqaeWaz1sNJK7_1s8e0M-uwj0O2b0BWlVRK8TqzxInlYkgpov-_yqg5Rm_O0ZvL6Pkv2cN25Q</recordid><startdate>20210101</startdate><enddate>20210101</enddate><creator>Mamatov, Farmon</creator><creator>Umurzakov, Uktam</creator><creator>Mirzaev, Bakhadir</creator><creator>Rashidov, Nurbek</creator><creator>Eshchanova, Guzal</creator><creator>Avazov, Ikrom</creator><general>EDP Sciences</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L6V</scope><scope>L7M</scope><scope>M7S</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>SOI</scope><scope>DOA</scope></search><sort><creationdate>20210101</creationdate><title>Physical-mechanical and technological properties of eroded soils</title><author>Mamatov, Farmon ; 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The data on the susceptibility of water erosion to sloping lands is presented. The average monthly indicators of precipitation over the last ten years in Uzbekistan are analyzed. The results of determining the moisture, density, and hardness of the soil of slopes are presented. It has been established that with the traditional technology of tillage on moisture, density, and other technical properties of soil of slopes, water erosion and slope of fields have a significant effect. The physical-mechanical and technological properties of soil of the arable and subsurface layers of the soil of the top, the middle and lower part of the slope in spring and after grain harvesting differs significantly: in the spring period, the moisture of soil layers 0-10; 10-20; 30-40; 40-50 and 50-60 cm of the lower part of the slope is more moisture content of these layers of the top respectively, 1.16; 1.24; 1.1; 1.4; 1.54 and 2.15 times. 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subjects | Arable land Density Harvesting Moisture content Slopes Soil erosion Soil layers Soil mechanics Soil moisture Soil properties Soil water Tillage Water content Water erosion |
title | Physical-mechanical and technological properties of eroded soils |
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