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    王瑞滢, 覃光华, 肖鸿, 刘超. 西南山区典型中小河流场次洪水产沙估算[J]. 中国防汛抗旱, 2022, 32(8): 1-7. DOI: 10.16867/j.issn.1673-9264.2022272
    引用本文: 王瑞滢, 覃光华, 肖鸿, 刘超. 西南山区典型中小河流场次洪水产沙估算[J]. 中国防汛抗旱, 2022, 32(8): 1-7. DOI: 10.16867/j.issn.1673-9264.2022272
    WANG Ruiying, QIN Guanghua, XIAO Hong, LIU Chao. Sediment yield estimation of the floods of typical middle and small-sized rivers in Southwest mountainous area[J]. China Flood & Drought Management, 2022, 32(8): 1-7. DOI: 10.16867/j.issn.1673-9264.2022272
    Citation: WANG Ruiying, QIN Guanghua, XIAO Hong, LIU Chao. Sediment yield estimation of the floods of typical middle and small-sized rivers in Southwest mountainous area[J]. China Flood & Drought Management, 2022, 32(8): 1-7. DOI: 10.16867/j.issn.1673-9264.2022272

    西南山区典型中小河流场次洪水产沙估算

    Sediment yield estimation of the floods of typical middle and small-sized rivers in Southwest mountainous area

    • 摘要: 西南山区山洪灾害防治通常按照“暴雨-洪水-水位-淹没”的思路,主要关注“水”的影响,而忽视“泥沙”的作用。受洪水含沙量的影响,这些地区小水大灾时有发生。本研究以川西南典型山区河流寿溪河为例,基于HEC-HMS(The HydrologicEngineering Center's Hydrologic Modeling System)模型在进行场次洪水预报的基础上,利用SPSS(Statistical Product andService Solutions)软件分析降雨强度、下垫面情况、地形因子以及土壤粒径4种因素与流域产沙量的相关性。研究结果表明,对流域产沙影响最大的因素为土壤侵蚀因子,达到0.261;影响最小的为降雨强度,仅为0.073。为进一步估算场次洪水产沙量,简化了HECHMS模型中的MUSLE(Modified Universal Soil Loss Equation)公式,按主成分综合模型中各影响因素的综合权重进行分类,重新定义了流域场次洪水产沙的估算公式。研究结果对估算山区中小流域场次洪水产沙量有参考价值。

       

      Abstract: The prevention and control of flash flood disaster in mountainous areas of China Southwest Researchers usually follow the idea of "rainstorm-flood-water level-inundation", mainly focusing on the impact of "water", but ignoring the role of "sediment". Affected by the sediment concentration of floods, small floods with major disasters often occur in these areas. Taking Shouxi River, a typical mountain river in Southwest Sichuan Province, as an example, based on HEC-HMS (The Hydrologic Engineering Center's Hydrologic Modeling System) model, on the basis of flood prediction, SPSS (Statistical Product and Service Solutions) software is used to analyze the correlation between rainfall intensity, underlying surface conditions, topographic factors and soil particle size and sediment yield in the basin. The results show that the most influential factor on sediment yield is soil erosion factor, reaching 0.261, and the least influential factor is rainfall intensity, only 0.073. In order to further estimate the sediment yield of the flood, the MUSLE (Modified Universal Soil Loss Equation) formula in HEC-HMS model is simplified, and the sediment yield estimation formula of the flood in the watershed is redefined according to the comprehensive weight of each influencing factor in the principal component comprehensive model. The research results have reference value for estimating the sediment yield of the floods of middle and small-sized river basins in mountainous areas.

       

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