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冻融作用下高寒土细沟侵蚀过程与输沙能力经验模型

田方霄 周金龙 郝宇东 赵鸿博 万丹

水土保持学报2026,Vol.40Issue(1):89-98,109,11.
水土保持学报2026,Vol.40Issue(1):89-98,109,11.DOI:10.13870/j.cnki.stbcxb.2026.01.038

冻融作用下高寒土细沟侵蚀过程与输沙能力经验模型

Empirical Model of Rill Erosion Processes and Sediment Transport Capacity in Alpine Soil under Freeze-Thaw Action

田方霄 1周金龙 1郝宇东 1赵鸿博 1万丹1

作者信息

  • 1. 西藏农牧大学资源与环境学院,西藏 林芝 860000||西藏农牧大学高寒水土保持研究中心,西藏 林芝 860000
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摘要

Abstract

[Objective]This study aims to investigate the mechanisms by which freeze-thaw action affects rill erosion.[Methods]Laboratory flume scouring experiments were conducted to analyze rill sediment transport characteristics under different combinations of flow rate(q)and slope gradient(S),and sediment transport capacity factor models were constructed.[Results]1)Freeze-thaw action increased the sediment transport capacity of rills by up to 34.34%,with a pronounced dependence on slope gradient and flow rate.Additionally,it shortened the critical slope length from 6.8~8.1 m to 5.3~6.4 m.2)The sediment transport capacity maintained a linear relationship with flow rate(Tc=Aq)both before and after freeze-thaw processes,while its relationship with slope changed.Before freeze-thaw,it increased exponentially with slope(Tc=-ae(-S/b)+c),while after freeze-thaw,it followed a power-law growth(Tc=d Sf).The established models,Tc=-0.041 4+0.110 1S+192.5q before freeze-thaw and Tc=-0.039 8+0.107 7S+213.2q after freeze-thaw,exhibited high accuracy(R²=0.96).The changes in these coefficients indicated that the influence of flow rate on sediment transport capacity increased while that of slope decreased after freeze-thaw.[Conclusions]Overall,freeze-thaw action alters soil structure,enhances the sediment transport capacity of rills,and modifies the slope response relationship.Model comparisons indicate that freeze-thaw action,soil bulk density,soil type,and experimental settings all affect the prediction performance of the models.These findings provide important theoretical support for soil erosion prediction and control in alpine regions.

关键词

冻融作用/细沟侵蚀/输沙能力/预测模型

Key words

freeze-thaw action/rill erosion/sediment transport capacity/prediction model

分类

农业科技

引用本文复制引用

田方霄,周金龙,郝宇东,赵鸿博,万丹..冻融作用下高寒土细沟侵蚀过程与输沙能力经验模型[J].水土保持学报,2026,40(1):89-98,109,11.

基金项目

国家自然科学基金项目(32241036) (32241036)

西藏农牧大学林学博士点(一期)项目(533325001) (一期)

西藏农牧大学研究生创新计划项目(YJS-2024-37) (YJS-2024-37)

水土保持学报

1009-2242

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