ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    基于地下水日动态的地下水蒸散发估算

    Estimation of Groundwater Evapotranspiration Based on Diurnal Groundwater-Level Fluctuations

    • 摘要: 地下水蒸散发作为地下水重要的排泄项,如何将估算误差控制在合理范围内是旱区地下水资源评价所面临的首要问题。因地下水动态数据易于获取,利用地下水日动态估算地下水蒸散发的方法(White方法)受到研究者们的广泛关注。受限于蒸散发驱动的潜水地下水位恢复滞后效应的机理复杂性,传统White方法及其改进型对水位日动态的恢复速率定量化不准确。本研究创新地将Boussinesq方程解析解与地下水动态谐波回归方法相结合,避免了直接计算地下水的恢复速率,实现了长时序、与地下水观测同频率的地下水蒸散发的快速计算。笔者将该方法应用于格尔木河流域2023年8~9月柽柳灌丛生长季节地下水蒸散发的估算。结果表明:①监测期内的地下水位表现出典型的依赖地下水型植被所产生的日动态特征,即夜间水位回升,白天水位下降。②该方法估算出的8月累计地下水蒸散量为55.96 mm,9月累计地下水蒸散量为88.14 mm,与格尔木河流域常见的ETg估算方法间具有良好的拟合度,平均偏差不足27%。③通过水位振幅计算的地下水折算系数与柽柳生长周期较为一致,能反映出植物蒸腾对地下水动态消耗的一般规律,但该无量纲系数的引入导致这种方法仍然存在改进空间。④这种从时间序列分析角度出发的估算方法,核心问题在于如何识别并提取水位日动态中仅与地下水蒸散有关的水位信息。结合先前于半旱区海流兔河流域沙柳地下水蒸散估算的研究成果,该方法可以同时适用于中国西北干旱区与半旱区植被生长季节的地下水蒸散发估算。

       

      Abstract: Groundwater evapotranspiration (ETg), as a critical discharge component of groundwater, has long been a key research focus in groundwater resource assessments. Due to the ease of obtaining groundwater dynamics data, the method of estimating ETg using diurnal groundwater fluctuations (White method) has attracted widespread attention from researchers. However, traditional White method and its variants face limitations in accurately quantifying groundwater recovery rates due to the mechanistic complexity of delayed water table recovery caused by phreatic water release driven by ETg. This study innovatively combines the analytical solution of the Boussinesq equation with dynamic harmonic regression analysis, avoiding direct calculation of groundwater recovery rates while enabling rapid, long-term ETg estimation at the same frequency as groundwater observations. Applying this method to estimate ETg during the Tamarix shrub growing season (August to September, 2023) in the Golmud River Catchment. The results show that: ① During the monitoring period, groundwater levels exhibited typical diurnal dynamics characteristic of groundwater-dependent vegetation, marked by nocturnal recovery and daytime decline. ② Cumulative ETg estimated by this method reached 55.96 mm in August and 88.14 mm in September, showing strong consistency with conventional ETg estimation approaches in the Golmud River Basin, with a mean deviation below 27%. ③ The groundwater specific coefficient (Kc,gw), calculated using water table amplitude, aligns with the growth cycles of Tamarix, reflecting general patterns of groundwater depletion by plant transpiration. However, the introduction of this dimensionless coefficient indicates potential for further refinement. ④ The core challenge of this time-series-based estimation method lies in identifying and extracting water table fluctuations solely attributable to ETg. Building on prior research estimating ETg for Salix shrubs in the semi-arid Hailiutu River Basin, this approach demonstrates applicability across both arid and semi-arid regions of northwestern China.

       

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