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冻融条件下土壤侵蚀阻力影响因素

卢超 马周加态 李佳辉 张宽地

水土保持学报2023,Vol.37Issue(6):25-33,9.
水土保持学报2023,Vol.37Issue(6):25-33,9.DOI:10.13870/j.cnki.stbcxb.2023.06.004

冻融条件下土壤侵蚀阻力影响因素

The Factors Influencing Soil Erosion Resistance Under Freeze-thaw Conditions

卢超 1马周加态 1李佳辉 1张宽地2

作者信息

  • 1. 西北农林科技大学水利与建筑工程学院,陕西 杨陵 712100
  • 2. 西北农林科技大学水利与建筑工程学院,陕西 杨陵 712100||西北农林科技大学黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西 杨凌 712100
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摘要

Abstract

In order to reveal the change mechanism of soil erosion resistance in seasonal freeze-thaw region and determine the main controlling factors affecting soil erosion resistance,the Loess soil(SM silty loam),Aeolian sandy soil(WS sandy loam)and Black soil(KS clay loam)were studied by indoor freeze-thaw simulation,flume erosion test and soil shear test.The results showed that:(1)With the increase of freeze-thaw cycles,the value of rill erodibility gradually increased,while the critical shear stress decreased.After ten freeze-thaw cycles,the rill erodibility of SM silty loam,WS sandy loam and KS clay loam increased by 76%,63%and 11%,respectively,and the critical shear stress decreased by 37%,13%and 91%,respectively.(2)Rill erodibility decreased with the increase of soil shear strength,cohesion and internal friction angle,while the critical shear stress showed the opposite trend.Compared with the internal friction angle,cohesion was more suitable to characterize soil erosion resistance.The rill erodibility of SM silty loam,WS sandy loam and KS clay loam was predicted by cohesion,and the determination coefficients R2 were 0.42,0.78 and 0.50,respectively,with an average of 0.57.The prediction effect on the critical shear stress was poor,and R2 were 0.16,0.14 and 0.18,respectively,with an average of only 0.16.(3)According to the results of Pearson correlation analysis,the prediction models of rill erodibility(R2=0.85)and critical shear stress(R2 =0.79)were established based on initial soil moisture content,freeze-thaw cycles,mechanical properties and soil parameters,respectively.Studies have shown that the effects of freeze-thaw cycles on soil erosion are enormous in areas with seasonal freeze-thaw region.The findings can serve as a reference for optimizing soil and water conservation practices and controlling soil erosion across different regions.

关键词

冻融循环/土壤侵蚀/细沟可蚀性/临界剪切力/土壤性质

Key words

freeze-thaw cycles/soil erosion/rill erodibility/critical shear stress/soil properties

分类

农业科技

引用本文复制引用

卢超,马周加态,李佳辉,张宽地..冻融条件下土壤侵蚀阻力影响因素[J].水土保持学报,2023,37(6):25-33,9.

基金项目

国家自然科学基金项目(52179079,41877076) (52179079,41877076)

黄土高原土壤侵蚀与旱地农业国家重点实验室开放基金项目(F2010121002-202311,F2010121002-202319) (F2010121002-202311,F2010121002-202319)

中央高校基本科研业务费专项资金项目(2022 HHZX003) (2022 HHZX003)

水土保持学报

OA北大核心CSCDCSTPCD

1009-2242

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