Home > STJ > Vol. 22 (2019) > Iss. 4
Scientific-technical journal
Abstract
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
106
Last Page
111
Recommended Citation
Abdullaev, B H.
(2019)
"THE DOUBLE LAYER THICKNESS OF WATER-BEARING ROCKS UNDER RAPID CHANGE IN PERMEABILITY AND PRESENCE OF VERTICAL WATEREXCHANGE BETWEEN LAYERS,"
Scientific-technical journal: Vol. 22
:
Iss.
4
, Article 20.
Available at:
https://uzjournals.edu.uz/ferpi/vol22/iss4/20