Scientific-technical journal


The article considers two-layer structure of aquifer strata with horizontal bedding. On the upper, poorly permeable aquifer enclosed of water with a free surface. The bottom layer with greater permeability. Examines the movement of seepage waters. The double layer thickness of water-bearing rocks under rapid change in permeability and presence of vertical water exchange between layers".

First Page


Last Page




To view the content in your browser, please download Adobe Reader or, alternately,
you may Download the file to your hard drive.

NOTE: The latest versions of Adobe Reader do not support viewing PDF files within Firefox on Mac OS and if you are using a modern (Intel) Mac, there is no official plugin for viewing PDF files within the browser window.