Effect of freeze–thaw cycling on the soil‐freezing characteristic curve of five Canadian soils
Abstract The frozen soil processes and their interaction with the environment in the vadose zone of cold regions is vital in both agricultural and engineering practice applications. In a frozen soil, unfrozen water and pore ice coexist. The relationship between the unfrozen water content and subzero...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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Wiley
2020-01-01
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| Series: | Vadose Zone Journal |
| Online Access: | https://doi.org/10.1002/vzj2.20039 |
| _version_ | 1818606208669450240 |
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| author | Junping Ren Sai K. Vanapalli |
| author_facet | Junping Ren Sai K. Vanapalli |
| author_sort | Junping Ren |
| collection | DOAJ |
| description | Abstract The frozen soil processes and their interaction with the environment in the vadose zone of cold regions is vital in both agricultural and engineering practice applications. In a frozen soil, unfrozen water and pore ice coexist. The relationship between the unfrozen water content and subzero temperature is widely known as the soil‐freezing characteristic curve (SFCC). The SFCC is a valuable tool for predicting the hydromechanical properties and for modeling the coupled thermal–hydraulic–mechanical–chemical process in frozen soils. In spite of its importance, the effect of freeze–thaw (F–T) cycling on SFCC has not been well investigated or understood. In this technical note, the effect of F–T cycles on the SFCC of five soils from cold regions of Canada were investigated. The SFCC (including both freezing and thawing branches) of the five soils for different F–T cycles were measured using frequency domain reflectometry (FDR) technique. The experimental results suggest that the effect of F–T cycles on the SFCC of the five soils is not significant. Such a behavior may be attributed to the destruction of soil structure during the saturation process. However, all the five soils’ SFCC exhibited hysteresis behavior for all the F–T cycles. The results of the study are valuable and contribute towards better understanding of the fundamental behavior of SFCC of various cold region soils. |
| first_indexed | 2024-12-16T14:07:12Z |
| format | Article |
| id | doaj.art-93a5a04421ba4b20ac3d7c598cfdfd4e |
| institution | Directory Open Access Journal |
| issn | 1539-1663 |
| language | English |
| last_indexed | 2024-12-16T14:07:12Z |
| publishDate | 2020-01-01 |
| publisher | Wiley |
| record_format | Article |
| series | Vadose Zone Journal |
| spelling | doaj.art-93a5a04421ba4b20ac3d7c598cfdfd4e2022-12-21T22:28:54ZengWileyVadose Zone Journal1539-16632020-01-01191n/an/a10.1002/vzj2.20039Effect of freeze–thaw cycling on the soil‐freezing characteristic curve of five Canadian soilsJunping Ren0Sai K. Vanapalli1Division of Field Engineering for the Environment Hokkaido Univ. Kita 13, Nishi 8, Kita‐Ku Sapporo 060‐8628 JapanDep. of Civil Engineering Univ. of Ottawa 161 Louis‐Pasteur St Ottawa ON K1N6N5 CanadaAbstract The frozen soil processes and their interaction with the environment in the vadose zone of cold regions is vital in both agricultural and engineering practice applications. In a frozen soil, unfrozen water and pore ice coexist. The relationship between the unfrozen water content and subzero temperature is widely known as the soil‐freezing characteristic curve (SFCC). The SFCC is a valuable tool for predicting the hydromechanical properties and for modeling the coupled thermal–hydraulic–mechanical–chemical process in frozen soils. In spite of its importance, the effect of freeze–thaw (F–T) cycling on SFCC has not been well investigated or understood. In this technical note, the effect of F–T cycles on the SFCC of five soils from cold regions of Canada were investigated. The SFCC (including both freezing and thawing branches) of the five soils for different F–T cycles were measured using frequency domain reflectometry (FDR) technique. The experimental results suggest that the effect of F–T cycles on the SFCC of the five soils is not significant. Such a behavior may be attributed to the destruction of soil structure during the saturation process. However, all the five soils’ SFCC exhibited hysteresis behavior for all the F–T cycles. The results of the study are valuable and contribute towards better understanding of the fundamental behavior of SFCC of various cold region soils.https://doi.org/10.1002/vzj2.20039 |
| spellingShingle | Junping Ren Sai K. Vanapalli Effect of freeze–thaw cycling on the soil‐freezing characteristic curve of five Canadian soils Vadose Zone Journal |
| title | Effect of freeze–thaw cycling on the soil‐freezing characteristic curve of five Canadian soils |
| title_full | Effect of freeze–thaw cycling on the soil‐freezing characteristic curve of five Canadian soils |
| title_fullStr | Effect of freeze–thaw cycling on the soil‐freezing characteristic curve of five Canadian soils |
| title_full_unstemmed | Effect of freeze–thaw cycling on the soil‐freezing characteristic curve of five Canadian soils |
| title_short | Effect of freeze–thaw cycling on the soil‐freezing characteristic curve of five Canadian soils |
| title_sort | effect of freeze thaw cycling on the soil freezing characteristic curve of five canadian soils |
| url | https://doi.org/10.1002/vzj2.20039 |
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