1887

Abstract

Summary

One of the main problems in working with these levels of groundwater is the incompleteness of the series. In this articl we consider the methods of filling the series of data of groundwater levels that have spaces. Correct filling of such series allows to characterize quantitatively the process of formation and change of hydrogeological conditions in time.

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/content/papers/10.3997/2214-4609.201801789
2018-05-14
2024-04-23
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