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    降雨特征和耕作措施对红壤缓坡地产流产沙及粒径分级的影响

    Influences of Rainfall Characteristics and Tillage Practices on Runoff, Sediment Yield, and Particle Size Distribution of Eroded Sediment on Gentle Red Soil Slopes

    • 摘要: 【目的】为明确降雨特征和耕作措施对红壤缓坡地水土流失及侵蚀泥沙粒径分选的作用,进而优选适用于高原红壤缓坡地的最佳耕作措施。【方法】本研究以云南省曲靖市马龙区缓坡地径流小区为研究对象,设置5种处理:顺坡耕作(CK)、横坡耕作(T1)、顺坡+横坡(T2)、顺坡+植物篱(T3)和顺坡+大豆间作(T4),4种降雨特征:Ⅰ类中历时中雨型降雨;Ⅱ类中长历时大暴雨型降雨;Ⅲ类长历时小雨型降雨;Ⅳ类短历时大雨型降雨,探究降雨特征与耕作措施对坡面侵蚀及泥沙粒径分级的影响。【结果】(1)降雨特征是控制产流产沙的首要因素(贡献率分别为71.75%和91.81%)。Ⅱ类降雨引发的径流深(1.38 mm)和泥沙量(2.39 g/m²)最大;Ⅳ类产沙量较低,但侵蚀泥沙粗砂(2-0.25 mm)占比最高(46.19%)。(2)与顺坡耕作(CK)相比,保护性耕作措施(T1-T4)平均减少径流深33.47%、泥沙量49.50%;其中T1处理减流效果最佳(43.98%),T3处理减沙效果最好(72.25%),且中值粒径最小(0.09 mm),粉粒(37.05%)和黏粒(8.82%)比例较高。(3)最大60分钟雨强(I60)是驱动侵蚀泥沙粒径分级的最关键因子,解释度高达48.70%。【结论】横坡耕作减流效果最佳,植物篱减沙效果最优,推荐二者作为红壤缓坡地水土保持措施,同时区域防治水土流失应重点关注中长历时大暴雨型降雨的侵蚀风险,并将I60作为预警的关键指标。研究结果可为西南山区坡耕地水土流失的精准阻控提供科学依据。

       

      Abstract: Objective To investigate the effects of different rainfall characteristics and tillage practices on soil erosion and the particle size sorting of eroded sediment on gentle red soil slopes, and to identify the most suitable tillage practice for plateau gentle red soil slopes. Method Runoff plot experiments were conducted on gentle slopes in Malong District, Qujing City, Yunnan Province. Five treatments were established: downslope tillage (CK), contour tillage (T1), downslope + contour tillage (T2), downslope + hedgerow (T3), and downslope + soybean intercropping (T4). Four rainfall characteristic types were identified: Type I—moderate-duration, moderate-intensity rainfall; Type Ⅱ—medium-to-long duration, heavy rainstorm; Type Ⅲ—long-duration, light rainfall; and Type Ⅳ—short-duration, heavy rainfall. Five tillage treatments were established: downslope tillage (CK), contour tillage (T1), downslope + contour tillage (T2), downslope + hedgerow (T3), and downslope + soybean intercropping (T4). Four rainfall types were classified: Type I – moderate duration, moderate intensity; Type Ⅱ – medium-to-long duration, heavy rainstorm; Type Ⅲ – long duration, light rainfall; and Type Ⅳ – short duration, heavy rainfall. The effects of rainfall characteristics and tillage practices on slope erosion and sediment particle size distribution were investigated. Results (1) Rainfall characteristics were the primary factor controlling runoff and sediment yield, with contribution rates of 71.75% and 91.81%, respectively. Type Ⅱ rainfall generated the largest runoff depth (1.38 mm) and sediment yield (2.39 g/m²); Type Ⅳ produced relatively low sediment yield but the highest proportion of coarse sand (2–0.25 mm, 46.19%) in the eroded sediment. (2) Compared with downslope tillage (CK), the conservation tillage practices (T1–T4) reduced runoff depth by an average of 33.47% and sediment yield by 49.50%. Among them, T1 achieved the best runoff reduction (43.98%), while T3 showed the greatest sediment reduction (72.25%) and the smallest median particle size (0.09 mm), along with higher proportions of silt (37.05%) and clay (8.82%). (3) The maximum 60-min rainfall intensity (I₆₀) was the most critical factor driving sediment particle size distribution, with an explanatory power of 48.70%. ConclusionContour tillage (T1) is most effective for reducing runoff, whereas hedgerow (T3) is optimal for reducing sediment yield; both are effective soil and water conservation measures for gentle red soil slopes. Regional erosion control efforts should focus on the erosion risk associated with medium-to-long duration heavy rainstorms and adopt I₆₀ as a key early warning indicator. These findings provide a scientific basis for precise erosion control on sloping farmland in the mountainous regions of Southwest China.

       

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