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砾石作用下松散红壤堆积体坡面产流产沙特征

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为了探究松散红壤工程堆积体在不同降雨条件下的径流产沙特性,基于野外调查统计结果构建堆积体试验槽模型,通过模拟降雨试验研究不同降雨强度下纯土和20%砾石含量堆积体的径流产沙的差异.结果表明:①砾石作用延缓堆积体坡面径流发生时间的平均滞后效益为299.56%;2种堆积体径流率随产流历时呈递增变化,随降雨强度增大,平均径流率递增34.48%~244.83%,土石混合堆积体平均径流率相较于纯土减少6.54%~45.83%,平均流速减少13.76%~30.54%.②降雨强度≤1.5 mm/min时堆积体侵蚀速率随产流历时总体缓慢递增或趋于稳定,土石混合堆积体平均侵蚀速率比纯土减少80.39%~84.95%;但在强降雨条件下(2.0 mm/min)纯土堆积体侵蚀速率呈快速增大后递减变化,土石混合堆积体侵蚀速率波动递增,且土石混合堆积体平均侵蚀速率比纯土增大20.04%.③降雨强度和砾石均会改变堆积体坡面径流产沙和流速,差异显著(P<0.05)且呈"水大沙多"的特点.研究结果可为堆积体水土流失防治措施布设提供指导,为建立工程堆积体土壤侵蚀预测模型提供基础数据.
Characteristics of Runoff and Sediment Yield on Loose Red Soil Accumulation Slope under Gravel Action
This study aims to explore the runoff and sediment yield characteristics on loose engineering accumula-tions under different rainfall conditions.Based on field investigations,we developed models of accumulation test tanks for simulated rainfall experiments to examine the runoff and sediment yield disparities between pure accumula-tion and accumulation with 20%gravel content under varied rainfall conditions.The findings revealed the following:1)Gravel effectively delayed runoff initiation on accumulation slopes,exhibiting an average delay benefit of 299.56%.Throughout the rainfall process,both pure and mixed soil and gravel accumulations demonstrated a simi-lar increasing trend in runoff rate with prolonged runoff generation duration.The average runoff rate escalated by 34.48%-244.83%with rising rainfall intensity.In comparison to pure accumulation,mixed soil and gravel accumu-lation displayed a decrease in average runoff rate by 6.54%-45.83%,along with a reduction in average flow veloci-ty by 13.76%-30.54%.2)The erosion rate of both pure and mixed soil and gravel accumulations generally exhibi-ted a gradual increase or tended to stabilize with runoff generation duration under rainfall intensities below 1.5 mm/min.The average erosion rate of mixed soil and gravel accumulation was 80.39%-84.95%lower than that of pure accumulation.However,under heavy rainfall conditions(2.0 mm/min),the erosion rate of pure soil accumulation experienced rapid escalation followed by a decline,while that of mixed soil and gravel accumulation increased in a fluctuating manner,with the average erosion rate 20.04%higher than the former.3)Both rainfall intensity and gravel content significantly influenced runoff,sediment yield,and flow velocity on accumulation slopes,indicating notable differences overall(P<0.05).The overall trend displayed an increase in both water and sediment.These results offer scientific guidance for implementing measures against soil erosion in production and construction pro-jects involving accumulations,and provide fundamental data for establishing soil erosion prediction models for accu-mulation engineering.

red soil accumulationsimulated rainfallrunoff and sediment yieldrunoff velocitymixed soil and gravel

芮茂刚、周彦辰、陶余铨、谢淑彦、薛杨

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云南省水利水电科学研究院,昆明 650228

长江科学院水资源综合利用研究所,武汉 430010

红壤堆积体 模拟降雨 产流产沙 流速 土石混合

云南省水利厅科技计划

YNSL2022-06

2024

长江科学院院报
长江科学院

长江科学院院报

CSTPCD北大核心
影响因子:0.618
ISSN:1001-5485
年,卷(期):2024.41(4)
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