不同雨强和坡度下新安江流域典型土壤坡面的产流产沙特征
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中国地质调查局项目“江南丘陵区自然资源与地表基质观测监测评价”(DD20230515)


Runoff and sediment yield characteristics of typical soil slopes in Xin'an River basin under different rainfall intensities and slope gradients
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    [目的] 评估新安江流域坡面水土流失规律,为区域水土流失治理和区域生态可持续发展提供科学支撑。[方法] 采用人工模拟降雨试验,系统分析了该流域内黄壤和红壤在不同降雨强度和坡度组合下的产流产沙过程及两者间的差异性侵蚀特征,并构建水动力学参数与产沙强度的定量关系模型。[结果] ①黄壤和红壤坡面的径流速率和产沙速率均表现为降雨初期呈现陡坡式增加,之后逐渐趋于稳定的变化规律,且二者随着降雨强度和坡度的增大而增加。其中,红壤坡面产流产沙能力高于黄壤,尤其是在60 mm/h雨强下差异更加显著。②降雨强度与坡度协同加剧水沙侵蚀,其中降雨强度主导红壤坡面径流及泥沙输移过程;当坡度达15°且降雨强度升至60 mm/h时,坡度对黄壤坡面泥沙流失的贡献增加至59.06%。③2种土壤坡面产流与产沙呈高度相关性,黄壤坡面水沙关系普遍符合Y=a/[1+exp-bX-c],具有非线性函数特征,而红壤因结构性差导致快速饱和,产沙与产流在60 mm/h雨强下呈现同步指数增长特征,函数关系为Y=a+bX。④坡面水力学参数中,平均流速(V)可有效预测黄壤产沙趋势(R2=0.52),而弗劳德数(Fr)更适用于红壤产沙动态(R2=0.44)。[结论] 黄壤区需注重坡度管理,遏制土壤侵蚀加剧。

    Abstract:

    [Objective] The patterns of soil erosion on slopes in the Xin’an River basin were evaluated in order to provide scientific support for regional soil erosion control and sustainable ecological development. [Methods] Through artificial rainfall simulation experiments,the runoff and sediment yield processes,and their differential erosion characteristics were systematically analyzed under different combinations of rainfall intensity and slope gradient for yellow soil and red soil in the river basin,and a quantitative relationship model between hydrodynamic parameters and sediment yield intensity was established. [Results] ① The runoff rate and sediment yield rate on the slopes of both yellow soil and red soil exhibited a steep initial increase during rainfall onset,followed by gradual stabilization,with both increasing with higher rainfall intensity and slope gradient.Red soil slopes demonstrated higher runoff and sediment yield capacity than yellow soil slopes,particularly under a rainfall intensity of 60 mm/h.② Rainfall intensity and slope gradient synergistically exacerbated runoff and sediment erosion,with rainfall intensity dominating the runoff and sediment transport processes on red soil slopes.When the slope gradient reached 15°and rainfall intensity increased to 60 mm/h,the contribution of slope to sediment loss on yellow soil slopes increased to 59.06%.③ A high correlation was observed between runoff and sediment yield on both soil types.Yellow soil slopes generally exhibited a nonlinear relationship characterized by Y=a/[1+exp-bX-c].In contrast,due to rapid saturation caused by poor structure,red soil slopes showed synchronous linear growth between sediment yield and runoff yield under a rainfall intensity of 60 mm/h,described by the function Y=a+bX.④ Among the slope hydraulic parameters,average velocity (V) could effectively predict the sediment yield trend of yellow soil (R2=0.52),while the Froude number (Fr) was more suitable for predicting the sediment yield dynamics of red soil (R2=0.44). [Conclusion] This study clarifies the coupling mechanisms of rainfall intensity and slope gradient in soil slope erosion within the Xin’an River basin.It is recommended that rainfall intensity regulation should be strengthened in red soil areas,while slope management should be emphasized in yellow soil areas to curb the exacerbation of soil erosion.

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宋珍,孙泽龙,任继军,岳忠帅,袁威.不同雨强和坡度下新安江流域典型土壤坡面的产流产沙特征[J].水土保持通报,2026,46(2):65-75

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  • 收稿日期:2025-08-17
  • 最后修改日期:2025-11-05
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  • 在线发布日期: 2026-05-13
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