Extended HYDRUS-1D freezing module emphasizes thermal conductivity schemes for simulation of soil hydrothermal dynamics
Soil thermal conductivity (λ) is required to investigate coupled heat and water transport in disciplines such as agriculture, hydrology and engineering. Parameterization schemes or models of λ are also the critical input parameter for various numerical simulation programs like the widely used HYDRUS...
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| Format: | Article |
| Language: | English |
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Elsevier
2024-08-01
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| Series: | Geoderma |
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| Online Access: | http://www.sciencedirect.com/science/article/pii/S0016706124001757 |
| _version_ | 1827151754104406016 |
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| author | Xiaoyu Chen Yihong Zhao Jingqing Cheng You Hu Bingcheng Si Min Li Kadambot H.M. Siddique Nasrin Azad Hailong He |
| author_facet | Xiaoyu Chen Yihong Zhao Jingqing Cheng You Hu Bingcheng Si Min Li Kadambot H.M. Siddique Nasrin Azad Hailong He |
| author_sort | Xiaoyu Chen |
| collection | DOAJ |
| description | Soil thermal conductivity (λ) is required to investigate coupled heat and water transport in disciplines such as agriculture, hydrology and engineering. Parameterization schemes or models of λ are also the critical input parameter for various numerical simulation programs like the widely used HYDRUS, one of the most commonly used models for mimicking water, heat, and solute transport. However, λ has not received enough attention in HYDRUS, and it remains unclear how different λ schemes affect the simulated soil water and thermal regimes. Thus, we programmed 24 λ schemes (including two built-in schemes) used in mainstream land surface, hydrological, and soil–vegetation–atmosphere transfer models into HYDRUS-1D (freezing module) to assess the effects of different λ schemes on soil temperature and water content simulations under freezing–thawing. The results showed that the 24 λ schemes performed differently in the simulation of soil temperature within 1 m below ground, with eight λ schemes, i.e., de Vries 1963 scheme/DV1963 (R=0.99), Camillo and Schmugge 1981/CS1981 scheme (R=0.98), Desborough and Pitman 1998/DP1998 scheme (R=0.97), Cass et al. 1984/CS1984 scheme (R=0.96), Shmakin 1998/SA1998 scheme (R=0.95), Dharssi et al. 2009/DI2009 scheme (R=0.95), Becker et al. 1992/BB1992 scheme (R=0.95), Hubrechts 1998/HL1998 scheme (R=0.94), performing superiorly to the built-in λ schemes. This study highlights the importance of choosing appropriate λ schemes in soil water and heat simulations. |
| first_indexed | 2025-03-20T21:55:00Z |
| format | Article |
| id | doaj.art-085d41ac3ef04bd9bf8f6385573873af |
| institution | Directory Open Access Journal |
| issn | 1872-6259 |
| language | English |
| last_indexed | 2025-03-20T21:55:00Z |
| publishDate | 2024-08-01 |
| publisher | Elsevier |
| record_format | Article |
| series | Geoderma |
| spelling | doaj.art-085d41ac3ef04bd9bf8f6385573873af2024-08-10T05:24:47ZengElsevierGeoderma1872-62592024-08-01448116946Extended HYDRUS-1D freezing module emphasizes thermal conductivity schemes for simulation of soil hydrothermal dynamicsXiaoyu Chen0Yihong Zhao1Jingqing Cheng2You Hu3Bingcheng Si4Min Li5Kadambot H.M. Siddique6Nasrin Azad7Hailong He8College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China; Key Laboratory of Poyang Lake Water Resources and Environment of Jiangxi Province, Jiangxi Academy of Water Science and Engineering, Nanchang 330029, ChinaKey Laboratory of Poyang Lake Water Resources and Environment of Jiangxi Province, Jiangxi Academy of Water Science and Engineering, Nanchang 330029, China; College of Water Resources and Architectural Engineering, Northwest A&F University, Yangling, Shaanxi 712100, ChinaKey Laboratory of Poyang Lake Water Resources and Environment of Jiangxi Province, Jiangxi Academy of Water Science and Engineering, Nanchang 330029, ChinaKey Laboratory of Poyang Lake Water Resources and Environment of Jiangxi Province, Jiangxi Academy of Water Science and Engineering, Nanchang 330029, ChinaKey Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas, Ministry of Education, Northwest A&F University, Yangling, Shaanxi 712100, China; Department of Soil Science, University of Saskatchewan, Saskatoon, SK S7N5A8 CanadaCollege of Water Resources and Architectural Engineering, Northwest A&F University, Yangling, Shaanxi 712100, China; Key Laboratory of Agricultural Soil and Water Engineering in Arid and Semiarid Areas, Ministry of Education, Northwest A&F University, Yangling, Shaanxi 712100, China; Corresponding author at: College of Water Resources and Architectural Engineering, Northwest A&F University, Yangling, Shaanxi 712100, China.The UWA Institute of Agriculture and School of Agriculture and Environment, The University of Western Australia, Perth, WA 6001, AustraliaCollege of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, ChinaCollege of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China; Department of Soil Science, University of Manitoba, Winnipeg, MB R3T 2N2, Canada; Corresponding author at: College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China.Soil thermal conductivity (λ) is required to investigate coupled heat and water transport in disciplines such as agriculture, hydrology and engineering. Parameterization schemes or models of λ are also the critical input parameter for various numerical simulation programs like the widely used HYDRUS, one of the most commonly used models for mimicking water, heat, and solute transport. However, λ has not received enough attention in HYDRUS, and it remains unclear how different λ schemes affect the simulated soil water and thermal regimes. Thus, we programmed 24 λ schemes (including two built-in schemes) used in mainstream land surface, hydrological, and soil–vegetation–atmosphere transfer models into HYDRUS-1D (freezing module) to assess the effects of different λ schemes on soil temperature and water content simulations under freezing–thawing. The results showed that the 24 λ schemes performed differently in the simulation of soil temperature within 1 m below ground, with eight λ schemes, i.e., de Vries 1963 scheme/DV1963 (R=0.99), Camillo and Schmugge 1981/CS1981 scheme (R=0.98), Desborough and Pitman 1998/DP1998 scheme (R=0.97), Cass et al. 1984/CS1984 scheme (R=0.96), Shmakin 1998/SA1998 scheme (R=0.95), Dharssi et al. 2009/DI2009 scheme (R=0.95), Becker et al. 1992/BB1992 scheme (R=0.95), Hubrechts 1998/HL1998 scheme (R=0.94), performing superiorly to the built-in λ schemes. This study highlights the importance of choosing appropriate λ schemes in soil water and heat simulations.http://www.sciencedirect.com/science/article/pii/S0016706124001757Soil thermal conductivity schemeSoil water contentSoil thermal regimeHydrothermal couplingFrozen soils |
| spellingShingle | Xiaoyu Chen Yihong Zhao Jingqing Cheng You Hu Bingcheng Si Min Li Kadambot H.M. Siddique Nasrin Azad Hailong He Extended HYDRUS-1D freezing module emphasizes thermal conductivity schemes for simulation of soil hydrothermal dynamics Geoderma Soil thermal conductivity scheme Soil water content Soil thermal regime Hydrothermal coupling Frozen soils |
| title | Extended HYDRUS-1D freezing module emphasizes thermal conductivity schemes for simulation of soil hydrothermal dynamics |
| title_full | Extended HYDRUS-1D freezing module emphasizes thermal conductivity schemes for simulation of soil hydrothermal dynamics |
| title_fullStr | Extended HYDRUS-1D freezing module emphasizes thermal conductivity schemes for simulation of soil hydrothermal dynamics |
| title_full_unstemmed | Extended HYDRUS-1D freezing module emphasizes thermal conductivity schemes for simulation of soil hydrothermal dynamics |
| title_short | Extended HYDRUS-1D freezing module emphasizes thermal conductivity schemes for simulation of soil hydrothermal dynamics |
| title_sort | extended hydrus 1d freezing module emphasizes thermal conductivity schemes for simulation of soil hydrothermal dynamics |
| topic | Soil thermal conductivity scheme Soil water content Soil thermal regime Hydrothermal coupling Frozen soils |
| url | http://www.sciencedirect.com/science/article/pii/S0016706124001757 |
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