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马克西莫维奇根据地下水集水处的性质及其水力性质特征,将地下水集水处细分为三类:第一类为区域性分布,以层流运动为特征的区域集水处地下水,第二类为分散的,多半不是区域性分布的,以紊流运动为特征成脉状发育的集水处脉状水。第三类是处于区域和脉状之间的过渡类型的过渡水或中间水。无论在文献中或介绍方面,对脉状水的研究和讨论,是特别缺乏的,因而,对这方面的工作和发展,
According to the characteristics of the groundwater catchment and its hydraulic characteristics, Maximovic subdivides the groundwater catchment into three categories: the first category is the regional groundwater catchment with regional distribution and characterized by laminar flow, The second category is scattered, mostly not regional distribution, characterized by turbulent flow into vein-shaped water veins at the water. The third category is the transitional type of transitional or intermediate water between regions and veins. Whether in the literature or introduction, the study and discussion of the venous water is particularly scarce, therefore, to this aspect of the work and development,