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引用次数: 0
摘要
衰退分析可用于流域之间的定性比较,也可用于涉及衰退曲线斜率和形状的定量分析。地下水位衰退水文图可用来估算表层含水层的水力扩散率。衰退指数可从溪流数据和包含含水层特性的公式中获得。对该方法的分析表明,非线性衰退可能是由下溪流成分、双重含水层效应以及含水层的渗漏造成的。重要的概念包括主导衰退指数和可能影响低流量的次级衰退特征。在顺水流条件下,跨水流成分往往对确定退水特征(包括水力扩散率和退水指数)很重要。这些发现与另一个衰退参数 a 有关,即从溪流到水文分界线的距离。
Recession analysis can be used for qualitative comparisons between basins and for quantitative analysis involving the slope and the shape of the recession curve. The groundwater-level recession hydrograph can be used to derive an estimate of the hydraulic diffusivity of a surficial aquifer. The recession index can be obtained from streamflow data and from a formulation that includes aquifer properties. The analysis of the method reveals nonlinear recession which can result from the down-valley flow component, a dual-aquifer effect, and leakage to or from the aquifer. Important concepts include the dominant recession index and secondary recession characteristics which can affect low flow. Under conditions of down-valley flow, the cross-valley flow component tends to be important for determining recession characteristics, including hydraulic diffusivity and the recession index. These findings are relevant to another recession parameter a which is the distance from the stream to the hydrologic divide and results are supported by test simulations of a technique for estimating recharge.
期刊介绍:
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