Field experimental study on the effect of thawed depth of frozen alpine meadow soil on rill erosion by snowmelt waterflow
Soil erosion by snow or ice melt waterflow is an important type of soil erosion in many high-altitude and high-latitude regions and is further aggravated by climate warming. The snowmelt waterflow erosion process is affected by soil freeze–thaws and is highly dynamically variable. In this study, a m...
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| Autors principals: | , , , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
KeAi Communications Co., Ltd.
2024-03-01
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| Col·lecció: | International Soil and Water Conservation Research |
| Matèries: | |
| Accés en línia: | http://www.sciencedirect.com/science/article/pii/S2095633922000910 |
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