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Expanded Erosion Mechanism and Morphological Evolution Characteristics of Slope Rill Based on Two-phase Flow Modeling
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Wen-bin HUANG1, 2, Xiang-tian XU1, 2, *, Yong-tao WANG1, Yu-hang LIU1, Yong LIU3
Science Technology and Engineering | 2025, 25(8) : 3152 - 3160
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Science Technology and Engineering | 2025, 25(8): 3152-3160
Agricultural Science
Expanded Erosion Mechanism and Morphological Evolution Characteristics of Slope Rill Based on Two-phase Flow Modeling
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Wen-bin HUANG1, 2, Xiang-tian XU1, 2, *, Yong-tao WANG1, Yu-hang LIU1, Yong LIU3
Affiliations
  • 1 Institute of Transportation Inner Mongolia University Hohhot 010020 China
  • 2 School of Ecology and Environment Inner Mongolia University Hohhot 010020 China
  • 3 Water Conservancy Development Center Ordos 017200 China
Published: 2025-03-18 doi: 10.12404/j.issn.1671-1815.2403513
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In order to accurately calculate the hydrodynamic parameters of the slope rill at any point during the erosion process, and to avoid errors caused by using the average flow rate to calculate the hydrodynamic parameters in the traditional method. Based on the variability and complexity of the development process of slope rills, as well as the characteristics of water sand two-phase flow, the Euler-Euler two-phase flow model was used to calculate and analyze the morphological evolution characteristics and erosion mechanisms of slope rills at different stages of expansion erosion. The results show that the Euler-Euler two-phase flow model can accurately describe the morphology evolution process of slope rill in expanded erosion. Based on the morphology evolution characteristics of slope rill at different stages of expanded erosion, the expanded erosion of slope rill is divided into the period when the rill sidewall is slightly spreading and eroding (the early stage), the period when the expanded erosion become severe with a significant increase in the number and area of amalgamated arcs (the middle stage), and the period when the expanded erosion basically ceased and the rill morphology stabilized (the late stage). The influential factors of slope gradient, initial flow rate, and preset rill width on the Darcy-Weisbach resistance coefficient, Reynolds number, and real-time flow rate are significant. Optimal characterization parameters for different stages of slope rill development, such as erosion arc length and hydraulic radius, are proposed, aiding in determining the specific period of slope rill development and predicting the development trend of rill morphology through changes in these parameters. The research results provide a theoretical basis for soil erosion control measures and are of great significance for soil and water conservation.

slope rill  /  two-phase flow model  /  expanded erosion  /  morphological evolution  /  erosion mechanism
Wen-bin HUANG, Xiang-tian XU, Yong-tao WANG, Yu-hang LIU, Yong LIU. Expanded Erosion Mechanism and Morphological Evolution Characteristics of Slope Rill Based on Two-phase Flow Modeling[J]. Science Technology and Engineering, 2025 , 25 (8) : 3152 -3160 . DOI: 10.12404/j.issn.1671-1815.2403513
Year 2025 volume 25 Issue 8
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Article Info
doi: 10.12404/j.issn.1671-1815.2403513
  • Receive Date:2024-05-13
  • Online Date:2025-07-29
  • Published:2025-03-18
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  • Received:2024-05-13
  • Revised:2025-01-02
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    1 Institute of Transportation Inner Mongolia University Hohhot 010020 China
    2 School of Ecology and Environment Inner Mongolia University Hohhot 010020 China
    3 Water Conservancy Development Center Ordos 017200 China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
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Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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