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".
Abdullaev, B H.
"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
, Article 20.
Available at: https://uzjournals.edu.uz/ferpi/vol22/iss4/20