Evaluation of upward flow of groundwater to freezing soils and rational per-freezing water table depth in agricultural areas
• A three-level iteration scheme to solve hydrothermal coupling model is developed. • The model can capture water table depth caused by freeze-thaw processes accurately. • The upward flow of groundwater to freezing soils is estimated. • The deepest impact depth of soil frozen process is 180 cm. • Th...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Cui, Lihong [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2020 |
|---|
| Schlagwörter: |
Pre-freezing water table depth |
|---|
| Übergeordnetes Werk: |
Enthalten in: Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China - Liu, Huiying ELSEVIER, 2021, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:585 ; year:2020 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.jhydrol.2020.124825 |
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| 520 | |a • A three-level iteration scheme to solve hydrothermal coupling model is developed. • The model can capture water table depth caused by freeze-thaw processes accurately. • The upward flow of groundwater to freezing soils is estimated. • The deepest impact depth of soil frozen process is 180 cm. • The per-freezing water table 100 cm can ensure required soil hydrothermal conditions. | ||
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Evaluation of upward flow of groundwater to freezing soils and rational per-freezing water table depth in agricultural areas |
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• A three-level iteration scheme to solve hydrothermal coupling model is developed. • The model can capture water table depth caused by freeze-thaw processes accurately. • The upward flow of groundwater to freezing soils is estimated. • The deepest impact depth of soil frozen process is 180 cm. • The per-freezing water table 100 cm can ensure required soil hydrothermal conditions. |
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• A three-level iteration scheme to solve hydrothermal coupling model is developed. • The model can capture water table depth caused by freeze-thaw processes accurately. • The upward flow of groundwater to freezing soils is estimated. • The deepest impact depth of soil frozen process is 180 cm. • The per-freezing water table 100 cm can ensure required soil hydrothermal conditions. |
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• A three-level iteration scheme to solve hydrothermal coupling model is developed. • The model can capture water table depth caused by freeze-thaw processes accurately. • The upward flow of groundwater to freezing soils is estimated. • The deepest impact depth of soil frozen process is 180 cm. • The per-freezing water table 100 cm can ensure required soil hydrothermal conditions. |
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