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潜水含水层给水度(μ)是表征含水层给水能力和贮水能力的基本参数。目前对潜水以垂直交替为主的平原地区,多依据水位动态资料,采用不同潜水蒸发经验公式推求μ值。但对潜水位埋藏较深,水平交替为主的已开采地区,如何计算μ值,尚缺乏成熟的方法。下面根据我们几年来对山西省几个洪积扇区地下水动态多年观测研究的结果,介绍一种适于山前地带
Submersible aquifer water supply (μ) is the basic parameter to characterize aquifer water supply capacity and water storage capacity. At present, the vertical distribution of the submersion in the plains is mainly based on the dynamic data of water level, and the empirical formula of different submersible evaporation is used to deduce the μ value. However, there is a lack of mature methods for how to calculate the μ value for the mined area where the diving position is buried deeply and the horizontal alternation is dominant. Hereunder, according to the results of many years of dynamic groundwater observations in several alluvial fan sectors in Shanxi Province over the past few years,