考虑下垫面空间分异的陆水流域产汇流特性分析

    Analysis on hydrological characteristics in Lushui watershed considering spatial heterogeneity of geographic features

    • 摘要: 深入理解流域产汇流特性,对于高精度洪水预报及流域水文数学物理模型的优化完善具有重要意义。以陆水流域为例,提取土壤、植被、地形坡度等地理要素以及降雨空间分布特点,选取2020~2024年汛期21场典型洪水过程,量化分析降雨以及下垫面特征空间分异对陆水流域产汇流过程的影响。结果表明:①陆水流域的降雨量与产流量之间的相关性较高,线性相关系数约为0.9,平均产流系数约为0.47;结合典型洪水过程分析结果发现,产流系数与土壤厚度具有较明显的负相关关系。②流域中毛家桥以上集水区域的土壤较薄、地形起伏变化明显,平均产流系数约为0.6,属于陆水流域中的易产流区。③陆水流域汇流时间约为12 h,崇阳站洪峰出现时间比陆水水库提前1~2 h,毛家桥和白霓桥以上流域汇流时间均为9 h左右。④由于陆水流域面积较小、降雨空间分异性较低、水系呈扇形发散等原因,降雨空间分布对于流域产汇流特性影响不明显,崇阳、毛家桥、白霓桥各站的洪峰在3 h内几乎同时到达陆水水库,是加剧陆水水库防洪压力的重要原因,其规律对深入认识流域水文特性、支撑洪水预报及调度具有重要参考作用。

       

      Abstract: An in-depth understanding of watershed runoff generation and flow confluence characteristics holds significant importance for enhancing high-precision flood forecasting and optimizing hydrological mathematical-physical models.Taking the Lushui watershed in eastern Hubei Province as a case study, we systematically extracted geographical elements including soil properties, vegetation coverage, topographic slopes, and rainfall spatial distribution characteristics.Twenty-one typical flood events from 2020 to 2024 were selected to quantitatively analyse impacts of rainfall and underlying surface characteristics′ spatial heterogeneity on runoff generation and flow confluence processes.The results demonstrated that: ① A strong correlation (linear correlation coefficient≈0.9) was observed between rainfall amount and runoff yield in the Lushui watershed, with an average runoff generation coefficient of approximately 0.47.Through analysis of typical flood events, the runoff generation coefficient was found to exhibit a distinct negative correlation with soil thickness.② In the upper watershed area above Maojiaqiao, where thinner soil layers and pronounced topographic relief were identified, the average runoff coefficient reached approximately 0.6, categorizing this sub-region as a high-runoff-yield zone within the basin.③ The basin confluence time of the Lushui watershed was determined to be approximately 12 hours.The flood peak at Chongyang Station was observed to precede that at the Lushui Reservoir by 1~2 hours, while both the Maojiaqiao and Bainiqiao sub-watersheds exhibited confluence times of approximately 9 hours.④ Due to the Lushui watershed′s limited areal extent, low rainfall spatial heterogeneity, and fan-shaped river network configuration, the spatial distribution of rainfall was shown to exert minimal influence on runoff generation characteristics.This hydrological pattern resulted in nearly simultaneous flood peak arrivals (within 3 hours) at the Lushui Reservoir from the Chongyang, Maojiaqiao, and Bainiqiao stations, which contributes significantly to the intensified flood control pressure on the Lushui Reservoir.The research results play an important reference role in understanding the hydrological characteristics of the basin and supporting flood forecasting and dispatching.

       

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