Temperature Factor of Soil Water-Holding Capacity
— The effect of temperature in the range from 4 to 50°C on the water retention curves in five soil samples of different textures was studied. The method of thermostatic centrifugation on the basis of a laboratory centrifuge Sigma 2-KHL (Germany) was used, which made it possible for the first time to...
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| Veröffentlicht in: | Eurasian soil science 2022-11, Vol.55 (11), p.1556-1567 |
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| container_title | Eurasian soil science |
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| creator | Smagin, A. V. Sadovnikova, N. B. |
| description | —
The effect of temperature in the range from 4 to 50°C on the water retention curves in five soil samples of different textures was studied. The method of thermostatic centrifugation on the basis of a laboratory centrifuge Sigma 2-KHL (Germany) was used, which made it possible for the first time to evaluate the influence of the temperature factor in a wide range of the thermodynamic potential of water from 0 to 3000 J/kg. Using statistical methods, two physically-based hypotheses of the relationship between temperature and thermodynamic potential—“capillary” (a decrease in water retention with increasing temperature) and “surface forces” (temperature invariance of water retention)—were evaluated. A representative analysis of 4–8 repetitions of each experiment did not reveal a statistically significant effect of the temperature factor on the water retention curves in all the studied samples. A fundamental explanation of the obtained results is proposed on the basis of Polanyi’s potential theory and the ion-electrostatic mechanism of disjoining water pressure according to Deryagin. |
| doi_str_mv | 10.1134/S1064229322110126 |
| format | Article |
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The effect of temperature in the range from 4 to 50°C on the water retention curves in five soil samples of different textures was studied. The method of thermostatic centrifugation on the basis of a laboratory centrifuge Sigma 2-KHL (Germany) was used, which made it possible for the first time to evaluate the influence of the temperature factor in a wide range of the thermodynamic potential of water from 0 to 3000 J/kg. Using statistical methods, two physically-based hypotheses of the relationship between temperature and thermodynamic potential—“capillary” (a decrease in water retention with increasing temperature) and “surface forces” (temperature invariance of water retention)—were evaluated. A representative analysis of 4–8 repetitions of each experiment did not reveal a statistically significant effect of the temperature factor on the water retention curves in all the studied samples. A fundamental explanation of the obtained results is proposed on the basis of Polanyi’s potential theory and the ion-electrostatic mechanism of disjoining water pressure according to Deryagin.</description><identifier>ISSN: 1064-2293</identifier><identifier>EISSN: 1556-195X</identifier><identifier>DOI: 10.1134/S1064229322110126</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Analysis ; Centrifugation ; Centrifuges ; Centrifuging ; Earth and Environmental Science ; Earth Sciences ; Electrostatic properties ; Geotechnical Engineering & Applied Earth Sciences ; Hydrostatic pressure ; Moisture content ; Potential theory ; Retention ; Samples ; Soil moisture ; Soil Physics ; Soil temperature ; Soil water ; Statistical analysis ; Statistical methods ; Temperature effects ; Thermodynamics ; Water ; Water pressure</subject><ispartof>Eurasian soil science, 2022-11, Vol.55 (11), p.1556-1567</ispartof><rights>Pleiades Publishing, Ltd. 2022. ISSN 1064-2293, Eurasian Soil Science, 2022, Vol. 55, No. 11, pp. 1556–1567. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Pochvovedenie, 2022, No. 11, pp. 1378–1390.</rights><rights>COPYRIGHT 2022 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c285t-7451a3bf8aed4714a08254ae076dd78ab04097cdd7d99d88aad7e79e4f7d78cd3</citedby><cites>FETCH-LOGICAL-c285t-7451a3bf8aed4714a08254ae076dd78ab04097cdd7d99d88aad7e79e4f7d78cd3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1064229322110126$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1064229322110126$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Smagin, A. V.</creatorcontrib><creatorcontrib>Sadovnikova, N. B.</creatorcontrib><title>Temperature Factor of Soil Water-Holding Capacity</title><title>Eurasian soil science</title><addtitle>Eurasian Soil Sc</addtitle><description>—
The effect of temperature in the range from 4 to 50°C on the water retention curves in five soil samples of different textures was studied. The method of thermostatic centrifugation on the basis of a laboratory centrifuge Sigma 2-KHL (Germany) was used, which made it possible for the first time to evaluate the influence of the temperature factor in a wide range of the thermodynamic potential of water from 0 to 3000 J/kg. Using statistical methods, two physically-based hypotheses of the relationship between temperature and thermodynamic potential—“capillary” (a decrease in water retention with increasing temperature) and “surface forces” (temperature invariance of water retention)—were evaluated. A representative analysis of 4–8 repetitions of each experiment did not reveal a statistically significant effect of the temperature factor on the water retention curves in all the studied samples. A fundamental explanation of the obtained results is proposed on the basis of Polanyi’s potential theory and the ion-electrostatic mechanism of disjoining water pressure according to Deryagin.</description><subject>Analysis</subject><subject>Centrifugation</subject><subject>Centrifuges</subject><subject>Centrifuging</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Electrostatic properties</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Hydrostatic pressure</subject><subject>Moisture content</subject><subject>Potential theory</subject><subject>Retention</subject><subject>Samples</subject><subject>Soil moisture</subject><subject>Soil Physics</subject><subject>Soil temperature</subject><subject>Soil water</subject><subject>Statistical analysis</subject><subject>Statistical methods</subject><subject>Temperature effects</subject><subject>Thermodynamics</subject><subject>Water</subject><subject>Water pressure</subject><issn>1064-2293</issn><issn>1556-195X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp1kM9LwzAUx4MoOKd_gLeC5868NG2S4xjOCYKHTfRW3pLX0dE1Ne0O--_NqOBBJIc83vf7eb8Yuwc-A8jk4xp4IYUwmRAAHERxwSaQ50UKJv-8jHGU07N-zW76fs95prXUEwYbOnQUcDgGSpZoBx8SXyVrXzfJBw4U0pVvXN3ukgV2aOvhdMuuKmx6uvv5p-x9-bRZrNLXt-eXxfw1tULnQ6pkDphtK43kpAKJXItcInFVOKc0brnkRtkYO2Oc1ohOkTIkKxVl67IpexjrdsF_Hakfyr0_hja2LIWSykAOWkfXbHTtsKGybis_BLTxOTrU1rdU1TE_V3FzHicyEYARsMH3faCq7EJ9wHAqgZfnU5Z_ThkZMTJ99LY7Cr-j_A99A7Pec50</recordid><startdate>20221101</startdate><enddate>20221101</enddate><creator>Smagin, A. 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B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c285t-7451a3bf8aed4714a08254ae076dd78ab04097cdd7d99d88aad7e79e4f7d78cd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Analysis</topic><topic>Centrifugation</topic><topic>Centrifuges</topic><topic>Centrifuging</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Electrostatic properties</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Hydrostatic pressure</topic><topic>Moisture content</topic><topic>Potential theory</topic><topic>Retention</topic><topic>Samples</topic><topic>Soil moisture</topic><topic>Soil Physics</topic><topic>Soil temperature</topic><topic>Soil water</topic><topic>Statistical analysis</topic><topic>Statistical methods</topic><topic>Temperature effects</topic><topic>Thermodynamics</topic><topic>Water</topic><topic>Water pressure</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Smagin, A. 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The effect of temperature in the range from 4 to 50°C on the water retention curves in five soil samples of different textures was studied. The method of thermostatic centrifugation on the basis of a laboratory centrifuge Sigma 2-KHL (Germany) was used, which made it possible for the first time to evaluate the influence of the temperature factor in a wide range of the thermodynamic potential of water from 0 to 3000 J/kg. Using statistical methods, two physically-based hypotheses of the relationship between temperature and thermodynamic potential—“capillary” (a decrease in water retention with increasing temperature) and “surface forces” (temperature invariance of water retention)—were evaluated. A representative analysis of 4–8 repetitions of each experiment did not reveal a statistically significant effect of the temperature factor on the water retention curves in all the studied samples. A fundamental explanation of the obtained results is proposed on the basis of Polanyi’s potential theory and the ion-electrostatic mechanism of disjoining water pressure according to Deryagin.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1064229322110126</doi><tpages>12</tpages></addata></record> |
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| subjects | Analysis Centrifugation Centrifuges Centrifuging Earth and Environmental Science Earth Sciences Electrostatic properties Geotechnical Engineering & Applied Earth Sciences Hydrostatic pressure Moisture content Potential theory Retention Samples Soil moisture Soil Physics Soil temperature Soil water Statistical analysis Statistical methods Temperature effects Thermodynamics Water Water pressure |
| title | Temperature Factor of Soil Water-Holding Capacity |
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